This document discusses soil quality and fertility as the most important factors in crop production. It explains that soil determines which crops yield best and the economic return a landowner can expect. The document covers soil profiles, texture, structure, composition, pH, essential nutrients, and how to determine soil reserves and nutrient needs to establish fertilization goals. Key factors like drainage, organic matter and limiting layers are addressed.
Soil is the home of million of organisms. In agriculture, from seed to grain, soil is a prima factor. It also acts a medium to store water for plants and form of water in soil called soil moisture. Some parameters to check the soil moisture called soil moisture constants. So, soil and water relationship is essential in agriculture.
Plant and growth development in agronomyUAS Dharwd
The document discusses various aspects of plant growth and development including cell growth, cell division, differentiation, and the role of plant growth regulators. It defines growth and growth rates, and describes the processes of differentiation and dedifferentiation in plant cells. The summary of key points are:
1. Plant growth and development involves processes like cell growth, division, differentiation and is regulated by plant growth regulators.
2. Growth can be arithmetic or geometric, and growth rates can be expressed mathematically.
3. Differentiation is the process by which less specialized cells become more specialized, while dedifferentiation allows cells to regain division capabilities.
4. Plant development results from the complex interactions between growth, differentiation, and
Splash erosion is caused by the impact of raindrops and is determined by climate, soil properties, topography, and plant cover. Sheet erosion involves the uniform removal of a thin layer of soil by splash erosion and the transportation of detached particles by surface runoff. Rill erosion occurs when sheet erosion advances to form shallow channels, and gully erosion is the most advanced stage where channels cannot be smoothed out by cultivation and are formed through water and channel erosion processes. Gullies are classified based on their shape, activity level, and dimensions, and progress through formation, development, healing, and stabilization stages over time.
This document discusses the quality of irrigation water and criteria for determining water quality. It outlines 5 classes of water salinity based on electrical conductivity and 4 classes of sodium level based on sodium adsorption ratio. It also discusses acceptable boron levels and provides management practices for using poor quality water, including applying gypsum, alternate irrigation strategies, fertilizer application techniques, irrigation methods, growing crop varieties, drainage, and other soil management practices. The document concludes with a discussion of soil fertility versus productivity and different methods for evaluating soil fertility.
QUALITY OF IRRIGATION WATER AND MANAGEMENT OF SALINE WATER FOR IRRIGATION
GOVARDHAN LODHA
Enroll. No. (160111017)
Department of Agronomy
M.Sc. (Ag) Agronomy 2nd semester
Tillage and tilth involve mechanical soil manipulation to create ideal conditions for plant growth. Tillage includes primary tillage like ploughing to open soil and secondary tillage like harrowing to break clods. The objectives are to prepare seedbeds, control weeds, aerate soil, and mix amendments. On-season tillage occurs before planting while off-season tillage conditions soil for future crops. Different tillage types include subsoiling to break hardpans and puddling for rice where soil is tilled under water. The depth and number of tillage operations varies by crop needs and soil conditions.
This document discusses various methods for organic weed management, including preventive, cultural, mechanical, biological, and chemical (organically approved) controls. Preventive measures aim to limit the introduction and spread of weed seeds. Cultural controls involve maintaining competitive crop conditions through methods like crop rotation, cover cropping, and mulching. Mechanical controls use hand/mechanical cultivation and mowing. Biological controls utilize allelopathy, beneficial organisms, and mycoherbicides. Organically approved chemicals like corn gluten meal and vinegar/essential oil mixtures are also options. The goal of an organic weed management system is to implement a whole farm approach that minimizes weed invasion and gives crops a competitive advantage over weeds.
A soil is composed primarily of minerals which are produced from parent material that is weathered or broken into small pieces. Like the classification systems for plants and animals, the soil classification system contains several levels of details, from the most general to the most specific types. The most general level of classification system is the soil order, of which there are 12 major types. This module explains these classes.
Soil is the home of million of organisms. In agriculture, from seed to grain, soil is a prima factor. It also acts a medium to store water for plants and form of water in soil called soil moisture. Some parameters to check the soil moisture called soil moisture constants. So, soil and water relationship is essential in agriculture.
Plant and growth development in agronomyUAS Dharwd
The document discusses various aspects of plant growth and development including cell growth, cell division, differentiation, and the role of plant growth regulators. It defines growth and growth rates, and describes the processes of differentiation and dedifferentiation in plant cells. The summary of key points are:
1. Plant growth and development involves processes like cell growth, division, differentiation and is regulated by plant growth regulators.
2. Growth can be arithmetic or geometric, and growth rates can be expressed mathematically.
3. Differentiation is the process by which less specialized cells become more specialized, while dedifferentiation allows cells to regain division capabilities.
4. Plant development results from the complex interactions between growth, differentiation, and
Splash erosion is caused by the impact of raindrops and is determined by climate, soil properties, topography, and plant cover. Sheet erosion involves the uniform removal of a thin layer of soil by splash erosion and the transportation of detached particles by surface runoff. Rill erosion occurs when sheet erosion advances to form shallow channels, and gully erosion is the most advanced stage where channels cannot be smoothed out by cultivation and are formed through water and channel erosion processes. Gullies are classified based on their shape, activity level, and dimensions, and progress through formation, development, healing, and stabilization stages over time.
This document discusses the quality of irrigation water and criteria for determining water quality. It outlines 5 classes of water salinity based on electrical conductivity and 4 classes of sodium level based on sodium adsorption ratio. It also discusses acceptable boron levels and provides management practices for using poor quality water, including applying gypsum, alternate irrigation strategies, fertilizer application techniques, irrigation methods, growing crop varieties, drainage, and other soil management practices. The document concludes with a discussion of soil fertility versus productivity and different methods for evaluating soil fertility.
QUALITY OF IRRIGATION WATER AND MANAGEMENT OF SALINE WATER FOR IRRIGATION
GOVARDHAN LODHA
Enroll. No. (160111017)
Department of Agronomy
M.Sc. (Ag) Agronomy 2nd semester
Tillage and tilth involve mechanical soil manipulation to create ideal conditions for plant growth. Tillage includes primary tillage like ploughing to open soil and secondary tillage like harrowing to break clods. The objectives are to prepare seedbeds, control weeds, aerate soil, and mix amendments. On-season tillage occurs before planting while off-season tillage conditions soil for future crops. Different tillage types include subsoiling to break hardpans and puddling for rice where soil is tilled under water. The depth and number of tillage operations varies by crop needs and soil conditions.
This document discusses various methods for organic weed management, including preventive, cultural, mechanical, biological, and chemical (organically approved) controls. Preventive measures aim to limit the introduction and spread of weed seeds. Cultural controls involve maintaining competitive crop conditions through methods like crop rotation, cover cropping, and mulching. Mechanical controls use hand/mechanical cultivation and mowing. Biological controls utilize allelopathy, beneficial organisms, and mycoherbicides. Organically approved chemicals like corn gluten meal and vinegar/essential oil mixtures are also options. The goal of an organic weed management system is to implement a whole farm approach that minimizes weed invasion and gives crops a competitive advantage over weeds.
A soil is composed primarily of minerals which are produced from parent material that is weathered or broken into small pieces. Like the classification systems for plants and animals, the soil classification system contains several levels of details, from the most general to the most specific types. The most general level of classification system is the soil order, of which there are 12 major types. This module explains these classes.
Potassium- Forms,Equilibrium in soils and its agricultural significance ,mech...Vaishali Sharma
The slide is conserned with the potassium fertilisers apllied in the soils. When the fertiliser applied in higher amount then it is avail in different form for plant uptake and there exist a equilibrium in soils and it has many agricultural significance and the slide also deal with brief on the mechanism of potassium fixation in the soil.
This document discusses various aspects of evaluating water quality for irrigation purposes. It provides guidelines on different criteria used to assess water quality, including salinity hazard, sodium hazard, bicarbonate hazard, and toxicities from boron and chlorine. Threshold values are given for different water quality classes based on these criteria. The document also discusses managing irrigation with marginal quality water through growing salt tolerant crops, applying organic matter, and following appropriate cropping sequences. Overall, the key criteria for evaluating irrigation water quality are salinity, sodium, and toxic concentrations of elements like boron and strategies for utilizing poorer quality water.
Methods to control soil erosion and water run offRajat Sharma
This document discusses soil erosion and methods for controlling it to maintain soil health. It defines soil erosion as the detachment, transport, and deposition of soil particles. Soil erosion reduces soil quality and agricultural productivity on-site, and causes siltation of waterways off-site. Factors that influence erosion include climate, soil type, topography, and human activities. The document then outlines various agronomic and engineering measures that can be taken to control erosion, such as using vegetation, contour farming, strip cropping, mulching, terracing, and building structures like check dams and ponds. The overall goal is to implement practices that protect the soil surface and slow runoff to prevent erosion.
This document provides information about soil amendments and fertilizers for saucer magnolia plants. It discusses adding compost to improve soil structure and provide nutrients. It also describes various nitrogen, phosphorus, and potassium amendment options and how they can affect soil pH levels. Organic amendments like compost, cottonseed meal, and manure are recommended to feed the plants and enrich the soil over time.
B Sc Agri II Sc,Sf & Nm, U 1 Soil And Plant NutrientRai University
The three main mechanisms by which nutrients move from soil to plant roots are root interception, mass flow, and diffusion. Root interception occurs when nutrients physically contact root surfaces. Mass flow transports nutrients to roots through water movement in soil via transpiration or percolation. Diffusion moves nutrients along concentration gradients from high to low concentrations. Factors like soil water content, temperature, root system size, and concentration gradients influence these mechanisms of nutrient transport from soil to roots.
This document summarizes key concepts related to weathering and soil formation processes. It describes how weathering breaks down rocks through physical and chemical processes, forming regolith. The main factors that influence soil formation are then outlined, including parent material, climate, topography, organisms/vegetation, and time. Specific weathering and soil forming processes are also defined, such as podzolization, laterization, and gleization. Key minerals and their weatherability are discussed. The role of various physical and chemical weathering agents such as water, wind, temperature changes are also summarized.
The document discusses soil water, including its classification, movement through soil, availability to plants, and factors that affect availability. It introduces key concepts like infiltration, percolation, pore space, and how soil acts as a sponge to take up and retain water, with pore space allowing for storage and movement of water. The document also covers indicators of plant water stress, development of water deficiency in plants, and concluding with factors that influence water availability.
This document discusses various types of environmental stresses that can affect plant growth including drought, high or low temperatures, excessive soil salinity, and inadequate minerals in the soil. It describes different mechanisms by which plants can adapt to or tolerate drought conditions, such as escaping drought by having a short lifecycle, avoiding stress through stomatal regulation and increased photosynthetic efficiency, and tolerating stress through enhanced water conservation and storage abilities. The document focuses on defining and classifying different types of drought, as well as adaptation strategies employed by crops to survive in drought environments.
Wind erosion occurs when wind detaches, transports, and deposits soil particles. It is a major cause of soil deterioration globally, including parts of India like Rajasthan. Factors like high winds, dry and loose soil, lack of vegetation make some regions more prone to wind erosion. Common management practices include maintaining crop residues on the soil surface, conservation tillage techniques, and mechanical barriers to disrupt wind flow over bare soils.
Soil productivity is defined as the capacity of soil to support plant growth and is affected by several key factors. These include the soil's parent material and physical conditions like texture, structure, bulk density, water, and atmosphere, which influence nutrient availability. Organic matter content is also important as it releases nutrients, improves the soil's water and nutrient holding capacity, and acts as a buffer. The soil's reaction, whether acid or alkaline, impacts which nutrients are involved and available to plants. Erosion and proper management practices further affect a soil's productivity.
Crop models can be used to estimate crop yield and its variability under different climate scenarios, account for nitrogen use efficiency, and help inform agricultural management decisions. The document discusses different types of crop models and provides examples of some models that have been successfully used in agrometeorology, including for rice, wheat, maize, sugarcane, and potato crops. It also outlines some limitations and advantages of using crop models.
The document discusses soil moisture characteristic curves, which describe the relationship between soil water content and water potential. It provides key details about soil moisture characteristic curves, including that they are affected by soil texture and structure, describe the amount of water retained at a given matric potential, and are important for modeling water flow in soils. The curves are nonlinear and cover a wide range of matric potentials, so they are often plotted on a logarithmic scale.
The document discusses soil water plant relationships and provides details on various topics related to soil properties, water movement and plant water needs. It discusses how soil properties like texture, structure and organic matter determine water holding capacity and infiltration rates. It describes the different types of water in soil like gravitational, capillary and hygroscopic water. Key soil water constants like field capacity, permanent wilting point and available water are explained. Factors affecting water movement like infiltration and factors influencing plant water uptake like rooting characteristics are also summarized.
Water erosion control measures aim to limit land damage from erosion. Mechanical measures include diversion drains, terracing, contour bunding, and waterways to redirect water flow. Agronomical measures include contour farming, strip cropping, conservation tillage, crop rotation and mixed cropping, and mulching to stabilize soil and reduce runoff. Properly implementing these control techniques can help reduce soil loss and land degradation caused by water erosion.
Soil fertility refers to a soil's ability to sustain plant growth through the supply of essential nutrients. There are 17 essential plant nutrients that come from the soil in various forms. Soil stores nutrients in minerals, organic matter, ions adsorbed to clay and humus particles, and dissolved ions in the soil solution. Plant roots absorb nutrients primarily as ionic forms through cation and anion exchange processes with the soil. A soil's cation exchange capacity determines its ability to store and supply nutrients to plants.
The document defines biological sickness of soils as an unfavorable condition for plant and microbe growth caused by biological problems that hinder decomposition and nutrient transformation. It discusses several types of biological sickness including low soil organic carbon, reduced soil respiration, lack of earthworms, and poor soil enzyme activity. The document then provides management practices for each type of sickness, such as no-till farming, manure application, and soil pH management, to improve soil biological conditions.
EFFECT OF MOISTURE STRESS ON PLANT GROWTH AND DEVELOPMENTSHRAVAN KUMAR REDDY
Moisture stress can negatively impact plant growth and development through various mechanisms. Crops have developed different adaptations to moisture stress including escaping drought through short lifecycles, avoiding stress through water conservation or improved uptake, and tolerating stress. Avoiding stress involves mechanisms like reducing leaf area, increasing waxiness, and regulating stomata to conserve water or developing deep, branched root systems and high root to shoot ratios to improve water uptake. Tolerating stress includes osmotic adjustment to maintain turgor under water deficits. Understanding crop adaptations is important for managing plants under moisture stress conditions.
1) Integrated nutrient management is the combined use of organic, inorganic and biological sources of nutrients to maintain soil fertility and ensure optimal plant growth.
2) It aims to optimize crop yields while preserving soil health and minimizing environmental impacts.
3) INM is important because it can improve soil properties and nutrient use efficiency compared to chemical fertilizers alone, while also providing locally sourced and cheaper alternatives to address rising input costs.
potassium fixation in different clay mineralsBharathM64
This document discusses potassium fixation in different clay minerals. It explains that potassium fixation was first reported in 1887 and involves potassium penetrating between clay layers and becoming tightly held. The degree of potassium fixation varies between clay types, with vermiculite showing the highest fixation due to its high charge density and large interlayer space, followed by illite, montmorillonite, and kaolinite. Factors like charge density, interlayer space size, solution concentration, and presence of other cations can influence how much potassium is fixed within clay minerals. The practical implication is that fixed potassium contributes to long-term potassium availability in soils.
This document discusses weather index crop insurance provided by Sanasa Insurance Company in Sri Lanka. [1] It provides payouts to farmers when weather indices like rainfall fall outside predetermined thresholds. [2] Sanasa first offered this insurance in 2010 and has since expanded coverage. [3] While it reduces issues like delays and human errors in claims, scaling it up faces challenges like the costs of implementation and lack of reliable weather data in all areas.
Presented by Eyob Meherette (NISCO) at the Workshop on Developing Index-Based Livestock Insurance to Reduce Vulnerability due to Drought-related Livestock Deaths, ILRI, Addis Ababa, Ethiopia, 12 July 2010.
Potassium- Forms,Equilibrium in soils and its agricultural significance ,mech...Vaishali Sharma
The slide is conserned with the potassium fertilisers apllied in the soils. When the fertiliser applied in higher amount then it is avail in different form for plant uptake and there exist a equilibrium in soils and it has many agricultural significance and the slide also deal with brief on the mechanism of potassium fixation in the soil.
This document discusses various aspects of evaluating water quality for irrigation purposes. It provides guidelines on different criteria used to assess water quality, including salinity hazard, sodium hazard, bicarbonate hazard, and toxicities from boron and chlorine. Threshold values are given for different water quality classes based on these criteria. The document also discusses managing irrigation with marginal quality water through growing salt tolerant crops, applying organic matter, and following appropriate cropping sequences. Overall, the key criteria for evaluating irrigation water quality are salinity, sodium, and toxic concentrations of elements like boron and strategies for utilizing poorer quality water.
Methods to control soil erosion and water run offRajat Sharma
This document discusses soil erosion and methods for controlling it to maintain soil health. It defines soil erosion as the detachment, transport, and deposition of soil particles. Soil erosion reduces soil quality and agricultural productivity on-site, and causes siltation of waterways off-site. Factors that influence erosion include climate, soil type, topography, and human activities. The document then outlines various agronomic and engineering measures that can be taken to control erosion, such as using vegetation, contour farming, strip cropping, mulching, terracing, and building structures like check dams and ponds. The overall goal is to implement practices that protect the soil surface and slow runoff to prevent erosion.
This document provides information about soil amendments and fertilizers for saucer magnolia plants. It discusses adding compost to improve soil structure and provide nutrients. It also describes various nitrogen, phosphorus, and potassium amendment options and how they can affect soil pH levels. Organic amendments like compost, cottonseed meal, and manure are recommended to feed the plants and enrich the soil over time.
B Sc Agri II Sc,Sf & Nm, U 1 Soil And Plant NutrientRai University
The three main mechanisms by which nutrients move from soil to plant roots are root interception, mass flow, and diffusion. Root interception occurs when nutrients physically contact root surfaces. Mass flow transports nutrients to roots through water movement in soil via transpiration or percolation. Diffusion moves nutrients along concentration gradients from high to low concentrations. Factors like soil water content, temperature, root system size, and concentration gradients influence these mechanisms of nutrient transport from soil to roots.
This document summarizes key concepts related to weathering and soil formation processes. It describes how weathering breaks down rocks through physical and chemical processes, forming regolith. The main factors that influence soil formation are then outlined, including parent material, climate, topography, organisms/vegetation, and time. Specific weathering and soil forming processes are also defined, such as podzolization, laterization, and gleization. Key minerals and their weatherability are discussed. The role of various physical and chemical weathering agents such as water, wind, temperature changes are also summarized.
The document discusses soil water, including its classification, movement through soil, availability to plants, and factors that affect availability. It introduces key concepts like infiltration, percolation, pore space, and how soil acts as a sponge to take up and retain water, with pore space allowing for storage and movement of water. The document also covers indicators of plant water stress, development of water deficiency in plants, and concluding with factors that influence water availability.
This document discusses various types of environmental stresses that can affect plant growth including drought, high or low temperatures, excessive soil salinity, and inadequate minerals in the soil. It describes different mechanisms by which plants can adapt to or tolerate drought conditions, such as escaping drought by having a short lifecycle, avoiding stress through stomatal regulation and increased photosynthetic efficiency, and tolerating stress through enhanced water conservation and storage abilities. The document focuses on defining and classifying different types of drought, as well as adaptation strategies employed by crops to survive in drought environments.
Wind erosion occurs when wind detaches, transports, and deposits soil particles. It is a major cause of soil deterioration globally, including parts of India like Rajasthan. Factors like high winds, dry and loose soil, lack of vegetation make some regions more prone to wind erosion. Common management practices include maintaining crop residues on the soil surface, conservation tillage techniques, and mechanical barriers to disrupt wind flow over bare soils.
Soil productivity is defined as the capacity of soil to support plant growth and is affected by several key factors. These include the soil's parent material and physical conditions like texture, structure, bulk density, water, and atmosphere, which influence nutrient availability. Organic matter content is also important as it releases nutrients, improves the soil's water and nutrient holding capacity, and acts as a buffer. The soil's reaction, whether acid or alkaline, impacts which nutrients are involved and available to plants. Erosion and proper management practices further affect a soil's productivity.
Crop models can be used to estimate crop yield and its variability under different climate scenarios, account for nitrogen use efficiency, and help inform agricultural management decisions. The document discusses different types of crop models and provides examples of some models that have been successfully used in agrometeorology, including for rice, wheat, maize, sugarcane, and potato crops. It also outlines some limitations and advantages of using crop models.
The document discusses soil moisture characteristic curves, which describe the relationship between soil water content and water potential. It provides key details about soil moisture characteristic curves, including that they are affected by soil texture and structure, describe the amount of water retained at a given matric potential, and are important for modeling water flow in soils. The curves are nonlinear and cover a wide range of matric potentials, so they are often plotted on a logarithmic scale.
The document discusses soil water plant relationships and provides details on various topics related to soil properties, water movement and plant water needs. It discusses how soil properties like texture, structure and organic matter determine water holding capacity and infiltration rates. It describes the different types of water in soil like gravitational, capillary and hygroscopic water. Key soil water constants like field capacity, permanent wilting point and available water are explained. Factors affecting water movement like infiltration and factors influencing plant water uptake like rooting characteristics are also summarized.
Water erosion control measures aim to limit land damage from erosion. Mechanical measures include diversion drains, terracing, contour bunding, and waterways to redirect water flow. Agronomical measures include contour farming, strip cropping, conservation tillage, crop rotation and mixed cropping, and mulching to stabilize soil and reduce runoff. Properly implementing these control techniques can help reduce soil loss and land degradation caused by water erosion.
Soil fertility refers to a soil's ability to sustain plant growth through the supply of essential nutrients. There are 17 essential plant nutrients that come from the soil in various forms. Soil stores nutrients in minerals, organic matter, ions adsorbed to clay and humus particles, and dissolved ions in the soil solution. Plant roots absorb nutrients primarily as ionic forms through cation and anion exchange processes with the soil. A soil's cation exchange capacity determines its ability to store and supply nutrients to plants.
The document defines biological sickness of soils as an unfavorable condition for plant and microbe growth caused by biological problems that hinder decomposition and nutrient transformation. It discusses several types of biological sickness including low soil organic carbon, reduced soil respiration, lack of earthworms, and poor soil enzyme activity. The document then provides management practices for each type of sickness, such as no-till farming, manure application, and soil pH management, to improve soil biological conditions.
EFFECT OF MOISTURE STRESS ON PLANT GROWTH AND DEVELOPMENTSHRAVAN KUMAR REDDY
Moisture stress can negatively impact plant growth and development through various mechanisms. Crops have developed different adaptations to moisture stress including escaping drought through short lifecycles, avoiding stress through water conservation or improved uptake, and tolerating stress. Avoiding stress involves mechanisms like reducing leaf area, increasing waxiness, and regulating stomata to conserve water or developing deep, branched root systems and high root to shoot ratios to improve water uptake. Tolerating stress includes osmotic adjustment to maintain turgor under water deficits. Understanding crop adaptations is important for managing plants under moisture stress conditions.
1) Integrated nutrient management is the combined use of organic, inorganic and biological sources of nutrients to maintain soil fertility and ensure optimal plant growth.
2) It aims to optimize crop yields while preserving soil health and minimizing environmental impacts.
3) INM is important because it can improve soil properties and nutrient use efficiency compared to chemical fertilizers alone, while also providing locally sourced and cheaper alternatives to address rising input costs.
potassium fixation in different clay mineralsBharathM64
This document discusses potassium fixation in different clay minerals. It explains that potassium fixation was first reported in 1887 and involves potassium penetrating between clay layers and becoming tightly held. The degree of potassium fixation varies between clay types, with vermiculite showing the highest fixation due to its high charge density and large interlayer space, followed by illite, montmorillonite, and kaolinite. Factors like charge density, interlayer space size, solution concentration, and presence of other cations can influence how much potassium is fixed within clay minerals. The practical implication is that fixed potassium contributes to long-term potassium availability in soils.
This document discusses weather index crop insurance provided by Sanasa Insurance Company in Sri Lanka. [1] It provides payouts to farmers when weather indices like rainfall fall outside predetermined thresholds. [2] Sanasa first offered this insurance in 2010 and has since expanded coverage. [3] While it reduces issues like delays and human errors in claims, scaling it up faces challenges like the costs of implementation and lack of reliable weather data in all areas.
Presented by Eyob Meherette (NISCO) at the Workshop on Developing Index-Based Livestock Insurance to Reduce Vulnerability due to Drought-related Livestock Deaths, ILRI, Addis Ababa, Ethiopia, 12 July 2010.
by Pramod Aggarwal, CGIAR Program on Climate Change, Agriculture, and Food Security. Presented at seminar on Insuring the future of farmers under climate change. London, UK. 28 January 2015. Learn more: http://ccafs.cgiar.org/weather-index-based-insurance
Weather insurance in India - A snaphot (2010)Outenga
This document discusses lessons learned from scaling crop weather index insurance programs in India. It addresses key challenges such as basis risk from imperfect relationships between indices and losses. It suggests using yield-tailored meteorological indices designed through regression of weather patterns on crop yields to better match farmer risks. The document also covers pricing approaches, factors that influence premium rates, and obstacles to insurance acceptability and sellability that must be addressed, such as complex models, trust issues, and service quality. Overall, the summary highlights lessons for improving the design and delivery of crop insurance programs through weather indices.
This article describes the various challenges and opportunities in implementing Agriculture insurance in India. It also details the historical insurance programs and crop insurance schemes implemented by the Government of India in the past few decades.
Presentation by P Joseph, Agriculture Insurance Company, on crop insurance in India at the CCAFS Workshop on Institutions and Policies to Scale out Climate Smart Agriculture held between 2-5 December 2013, in Colombo, Sri Lanka.
Crop insurance. presentation by gourav kumar vani pptxGourav kumar Vani
The document provides a web link and requests the reader to visit the link to access a presentation. It directs the reader to http://www.gouravkumarvani.co.in/ to get access to an online presentation available at that address. In 3 sentences or less.
This document provides an overview of crop insurance in India, including the evolution of different schemes. It discusses the risks faced by Indian farmers and different approaches to crop insurance. The major schemes discussed are the Pilot Crop Insurance Scheme from 1979-1984, the Comprehensive Crop Insurance Scheme from 1985-1999, the Experimental Crop Insurance Scheme in 1997-1998, and the National Agricultural Insurance Scheme implemented from 1999 to present. It provides details on the features and performance of each scheme. Key challenges identified include only covering loanee farmers, limited crop coverage, low sums insured, and high claim ratios under previous schemes.
Central excise duty is payable on goods before they are removed from the place of manufacture based on the assessable value determined by a central excise officer. The central excise act of 1944 and tariff act of 1985 along with rules issued by the central government and its notifications are the sources of central excise law. Goods covered under central excise include alcoholic liquors, opium, narcotic drugs, and other manufactured or produced goods except those exempted. There are two schedules under central excise - Schedule I covers duties determined on an ad valorem basis according to the tariff, while Schedule II covers specific uniform rates of 8% and 16%.
1. The document discusses weather-based crop insurance and describes various risks faced by farmers like droughts and floods. It also discusses different formal and informal risk management strategies.
2. Formal insurance programs are described, including a weather index insurance product offered by ICICI Lombard and BASIX to insure farmers against deficient rainfall. The program divides the monsoon season into growth phases and provides payouts if rainfall is below a trigger level.
3. Challenges in developing weather index insurance are also outlined, such as basis risk. But the product is seen as well-suited for catastrophe risks with simple design and low costs.
This document provides an overview of the soil system. It discusses how soil is formed through weathering of rocks, deposition of sediments, and decomposition of organic matter. Soil is a complex mixture that includes minerals, organic matter, water, air, and microorganisms. Mature soils have distinct horizontal layers called horizons. Soil properties like texture, structure, fertility, and acidity impact plant growth. The document also outlines nutrient and water cycles in soil as well as threats from erosion.
The document discusses soil management and conservation. It describes soil as a key resource for crop production that supports biological and chemical processes and regulates water flow. Soil quality is defined by attributes like texture, structure, carbon content and biological activity. The three main functions of soil are providing growth for plants, storing and regulating water flow, and buffering environmental changes. The document outlines different classifications of land capability and quality, including Land Capability Classes that range from I to VIII based on limitations for crop growth. It also discusses prime farmland designation, soil degradation processes, and conservation practices like rotational cropping and cover crops.
1) Agriculture provides 95% of human protein and calories from traditional crops and livestock grown on land.
2) Soil quality is important for agriculture but agriculture can degrade soil quality over time through erosion from plowing, deforestation, and overgrazing.
3) Erosion from agriculture removes an estimated 25.4 billion tons of soil globally each year, filling waterways and polluting them with sediment and fertilizers. Contour plowing, crop rotation, and no-till agriculture can help reduce erosion and make soils more sustainable.
This document discusses various topics related to soil and water management including land preparation, types of irrigation, mineral nutrition, and soil conservation. It describes the major purposes of land preparation such as leveling land and preparing seed beds. It discusses different types of irrigation like center-pivot, drip, and furrow irrigation. It also outlines the major mineral nutrients needed by plants like nitrogen, phosphorus, potassium, and their functions. Finally, it discusses soil conservation methods to prevent erosion like terracing, contour tillage, strip cropping, and grass waterways.
The document summarizes key information about soil resources. It defines soil and discusses soil-forming factors such as parent material, climate, topography and organisms. It also describes soil composition, nutrients, horizons, texture, characteristics, types of fertilizers and their pros and cons. Methods to prevent soil erosion, salinization, desertification and reclaim degraded land are also summarized.
Hawaii conservation Awareness 2006 Presentationoahuswcd
This document provides guidance for participants in the Hawaii Conservation Awareness Contest. It is divided into 5 parts that cover the physical features of soil, major factors affecting land use, land capability classification, recommended conservation practices, and judging land for a homesite. The first part describes key physical properties of soil including texture, permeability, depth, slope, and erosion. It provides definitions and classification examples for properly evaluating these characteristics. The second part identifies major factors like texture, permeability, depth, and slope that can impact land use if certain thresholds are met. The document aims to educate participants on properly assessing and classifying land conditions.
Soils and growing media provide nutrients, air, water and support for plant growth. Key properties include physical attributes like texture, chemical properties that influence nutrient supply, and biological factors from microorganisms. Texture, structure, permeability and pH all impact aeration, drainage and plant suitability. Safety precautions must be followed when working with soils. Improvements can address texture, structure, pH, salinity through amendments, drainage or plant selection.
Soil organic matter provides chemical, physical, and biological benefits to soil. Chemically, it acts as a reservoir of nutrients like nitrogen, phosphorus, and sulfur, contributes to the soil's cation exchange capacity, and forms chelates that make micronutrients available to plants. Physically, it improves the soil's structure, water holding capacity, and resistance to erosion, crusting, and compaction. Biologically, it supports vast numbers of soil microorganisms whose nutrient cycling and other functions are vital to soil fertility.
Eco 4 soil physical and chemical properties Rabia Aziz
soil
more chemistry contents are available
1. pdf file on Termmate: https://www.termmate.com/rabia.aziz
2. YouTube: https://www.youtube.com/channel/UCKxWnNdskGHnZFS0h1QRTEA
3. Facebook: https://web.facebook.com/Chemist.Rabia.Aziz/
4. Blogger: https://chemistry-academy.blogspot.com/
This document provides information about soil, including its composition, formation, types, and importance. Some key points:
- Soil is formed through weathering of rocks and decomposition of organic materials over time. It is composed of minerals, organic matter, water, and air.
- Soil type is determined by factors like parent material, climate, plants and animals, and time. The longer soil has been forming, the thicker it becomes.
- Important soil types include sandy soil, clay soil, silty soil, and loam soil. Loam soil contains a balanced mix of components and is very fertile.
- Soil provides an interface between the living and non-living parts of the Earth
Organic matter provides numerous chemical, physical, and biological benefits to soil. Chemically, it acts as a reservoir of nutrients, contributes to the soil's cation exchange capacity, and forms chelates that make nutrients more available to plants. Physically, organic matter improves soil structure, increases the soil's water holding capacity, and prevents erosion. Biologically, it supports soil microorganisms that drive nutrient cycling and helps maintain overall soil quality.
Organic matter provides numerous chemical, physical, and biological benefits to soil. Chemically, it acts as a reservoir of nutrients like nitrogen, phosphorus, and sulfur, contributes to the soil's cation exchange capacity, and forms chelates that make micronutrients more available to plants. Physically, organic matter improves soil structure, increases the soil's water holding capacity, reduces erosion, and lessens compaction. Biologically, it feeds soil microbes that drive nutrient cycling and supports a diverse array of soil organisms. Organic matter is essential for maintaining healthy, productive soil.
Surface and subsurface drainage systems are used to remove excess water from irrigated areas. Surface drainage involves open ditches and land grading to carry water away, while subsurface or tile drainage uses underground pipes to drain water from below the soil surface. Tile drains are made of porous material and laid in trenches backfilled with filter material to prevent soil intrusion. They are connected to larger surface drains or pumps. Different tile drainage layouts are used depending on topography, including natural, gridiron, herringbone, and interceptor systems. Soil salinity occurs when salt concentrations in the root zone inhibit plant growth. It can be caused by high water tables, arid climates with limited leaching, or poor quality
This document discusses the importance of soil organic matter. It states that soil organic matter affects chemical and physical soil properties and overall health. It is made up of living and dead biomass and humus. Soil organic matter content typically ranges from 1-6% and provides benefits like improved structure, water retention, and nutrient availability. Maintaining or increasing soil organic matter through practices like reduced tillage, cover crops, and reducing erosion can improve soil quality and sustainability.
The document provides an overview of soil components and properties. It discusses the four main components of soil - minerals, water, air, and organic matter. It describes the different soil horizons from O to R, and explains their characteristics. Key points include that it takes 550 years to make 1 inch of soil, texture affects water holding capacity and infiltration rates, and organic matter improves soil properties. Soil formation is influenced over time by parent material, climate, biology, topography, and human activities like tillage can impact soil organic matter levels.
The document discusses two case studies of soil degradation: the Dust Bowl of the 1930s in the US and the drying of the Aral Sea in Central Asia by the Soviet Union. Both events were caused by unsustainable farming and water use practices that removed protective vegetation from the soil, leading to widespread dust storms and desertification. The document also discusses the global issue of soil degradation, its causes like erosion, pollution, overgrazing and mismanaged farmland, and techniques to conserve soil like reducing erosion, managing nutrients, limiting compaction, and preventing overgrazing.
This document discusses soil properties and index properties of soil. It defines key terms related to soil texture, structure, drainage and composition. Soil texture refers to the relative percentages of sand, silt and clay in a soil. Structure describes how soil particles are grouped. Drainage is influenced by soil color, with greyer soils being poorer drained. The document also examines physical, chemical and biological properties of soil, including the microorganisms and processes involved.
Soil is a nonrenewable resource that provides many functions including being arable land for agriculture, regulating water and filtering pollutants, nutrient cycling, foundation and support, and containing mineral deposits. Human activities like soil erosion, compaction, intensive agriculture, urbanization, and desertification can degrade soil quality by reducing nutrients, organic matter, and biodiversity. Conservation methods include increasing soil organic matter, keeping the soil covered, reducing tillage, efficient pest and nutrient management, crop rotation, and preventing erosion and compaction.
Soil is the top layer of the Earth's crust and is formed through the natural process of weathering of rocks over hundreds of years. Soil is made up of various layers including the top soil, sub soil, and bedrock. It provides nutrients and support for plant growth. Soil erosion by wind and water is a major threat and can be reduced through practices like forestation, contour plowing, and crop rotation.
A Review on Recent Advances of Packaging in Food IndustryPriyankaKilaniya
Effective food packaging provides number of purposes. It functions as a container to hold and transport the food product, as well as a barrier to protect the food from outside contamination such as water, light, odours, bacteria, dust, and mechanical damage by maintaining the food quality. The package may also include barriers to keep the product's moisture content or gas composition consistent. Furthermore, convenience is vital role in packaging, and the desire for quick opening, dispensing, and resealing packages that maintain product quality until fully consumed is increasing. To facilitate trading, encourage sales, and inform on content and nutritional attributes, the packaging must be communicative. For storage of food there is huge scope for modified atmosphere packaging, intelligent packaging, active packaging, and controlled atmosphere packaging. Active packaging has a variety of uses, including carbon dioxide absorbers and emitters, oxygen scavengers, antimicrobials, and moisture control agents. Smart packaging is another term for intelligent packaging. Edible packaging, self-cooling and self-heating packaging, micro packaging, and water-soluble packaging are some of the advancements in package material.
Cacao, the main component used in the creation of chocolate and other cacao-b...AdelinePdelaCruz
Cacao, the main component used in the creation of chocolate and other cacao-based products is cacao beans, which are produced by the cacao tree in pods. The Maya and Aztecs, two of the earliest Mesoamerican civilizations, valued cacao as a sacred plant and used it in religious rituals, social gatherings, and medical treatments. It has a long and rich cultural history.
FOOD PSYCHOLOGY CHARLA EN INGLES SOBRE PSICOLOGIA NUTRICIONALNataliaLedezma6
Our decisions about what to put on our plate are far more intricate than simply following hunger cues. Food psychology delves into the fascinating world of why we choose the foods we do, revealing a complex interplay of emotions, stress, and even disorders.
The Menu affects everything in a restaurant; as our friend and FCSI consultant Bill Main says, “The Menu is your blueprint for profitability.”
Let’s start with the segment. What will be your marketing and brand positioning? It depends on what menu items you serve. What type of cooking methods and equipment will you use? GUEST EXPERIENCE = FACILITY (Space) DESIGN + MENU + SERVPOINTS™
W.H. Bender & Associates
408-784-7371
whb@whbender.com
www.whbender.com
San Jose, California
Panchkula offers a wide array of dining experiences. From traditional North Indian flavors to global cuisine, the city’s restaurants cater to every taste bud. Let’s dive into some of the best restaurants in Panchkula
Ang Chong Yi’s Culinary Revolution: Pioneering Plant-Based Meat Alternatives ...Ang Chong Yi Singapore
In the heart of Singapore’s bustling culinary scene, a visionary chef named Ang Chong Yi is quietly revolutionizing the way we think about food. His mission? To create delectable Ang Chong Yi Singapore — Plant-based meat: Next-gen food alternatives that not only tantalize our taste buds but also contribute to a more sustainable future.
Ang Chong Yi’s Culinary Revolution: Pioneering Plant-Based Meat Alternatives ...
Basics of crop production
1. Basics of Crop Production
Soil and Plant FertilitySoil and Plant Fertility
2. Soil Quality
• This is the most important factor inThis is the most important factor in
farm crop production.farm crop production.
• Soils will determine which plant speciesSoils will determine which plant species
yields the most, the time of harvest, andyields the most, the time of harvest, and
ultimately the investment a landownerultimately the investment a landowner
must make to yield an acceptablemust make to yield an acceptable
economic return from management.economic return from management.
3. Soil Profile
The soil profile
shows the layers,
known as horizons
that represent
the soil.
Horizons formed
over the centuries
due mostly form
weathering.
A lettering system
is used to name
the different
horizons.
4. Where can you find info
on a farm’s soil?
• In theIn the County SoilCounty Soil Survey MapSurvey Map..
• There are Tables on several landThere are Tables on several land
options such asoptions such as WoodlandWoodland
Management and ProductivityManagement and Productivity whichwhich
provides a lot of valuable informationprovides a lot of valuable information
on the potential for soil erosion,on the potential for soil erosion,
seedling mortality, species preference,seedling mortality, species preference,
and tree growth.and tree growth.
5. County Soils Map
There is even a table in the Soil SurveyThere is even a table in the Soil Survey
Map that evaluates sites for wildlifeMap that evaluates sites for wildlife
habitat.habitat.
6. Factors Controlling Plant
Growth
• LightLight
• Mechanical SupportMechanical Support
• HeatHeat
• AirAir
• WaterWater
• NutrientsNutrients
• All except for light, involves soilAll except for light, involves soil
8. Soil Terminology
• Soil textureSoil texture
- concerns the size of mineral- concerns the size of mineral
particles, specifically theparticles, specifically the
relative proportion of variousrelative proportion of various
size groups in a given soilsize groups in a given soil
• Soil structureSoil structure
- the arrangement of soil particles- the arrangement of soil particles
into groups of aggregatesinto groups of aggregates
9. Soil Texture
• Soil texture is separated into three soilSoil texture is separated into three soil
separates based on particle size.separates based on particle size.
1 SandSand
2 SiltSilt
3 ClayClay
10. Soil Texture
• Silt, claySilt, clay
- imparts a fine texture and slow- imparts a fine texture and slow
water and air movement, also highwater and air movement, also high
water holding capacitywater holding capacity
• Sandy to gravellySandy to gravelly
- are referred to as lighter soils with- are referred to as lighter soils with
lower water holding capacitylower water holding capacity
11. Soil Texture
• Sandy soils are normally very wellSandy soils are normally very well
drained and often lack nutrients due todrained and often lack nutrients due to
constant leaching loss.constant leaching loss.
• Mostly clay soils are at the opposite endMostly clay soils are at the opposite end
of the soil spectrum. They tend to allowof the soil spectrum. They tend to allow
water to move through more slowlywater to move through more slowly
and will stay wetter longer. They willand will stay wetter longer. They will
hold nutrients.hold nutrients.
12. Soil Terminology
• Pore spacePore space
- is that portion of the soil occupied- is that portion of the soil occupied
by air and waterby air and water
- sandy soils have low soil porosity,- sandy soils have low soil porosity,
while silt and clay soils have highwhile silt and clay soils have high
soil porositysoil porosity
• Soil compactionSoil compaction
- fine textured, wet soils are more- fine textured, wet soils are more
easily compactedeasily compacted
- compaction reduces pore spaces- compaction reduces pore spaces
13. Soil Terminology
• Soil depthSoil depth
- defined as that depth of soil material- defined as that depth of soil material
favorable for plant rootfavorable for plant root penetrationpenetration
- deep, well drained soils are the best- deep, well drained soils are the best
14. Soil TerminologySoil Terminology
• SlopeSlope
- land topography largely- land topography largely
determines the amount ofdetermines the amount of
drainage, runoff, and erosiondrainage, runoff, and erosion
- the steeper the land, the more- the steeper the land, the more
management is requiredmanagement is required
15. Soil Terminology
• Organic matterOrganic matter
- it consists of plant and animal- it consists of plant and animal
residues in various stages of decayresidues in various stages of decay
- adequate levels benefit soil by:- adequate levels benefit soil by:
1) improving physical condition1) improving physical condition
2) increasing water infiltration2) increasing water infiltration
3) improving soil tilth3) improving soil tilth
4) decreasing erosion losses4) decreasing erosion losses
5) supplying plant nutrients5) supplying plant nutrients
6) holding cation nutrients6) holding cation nutrients
16. Soil Terminology
• pHpH
- expression of both acidity and- expression of both acidity and
alkalinity on a scale whose valuesalkalinity on a scale whose values
run from 0 to 14 with 7run from 0 to 14 with 7
representingrepresenting neutrality, <7neutrality, <7
represents acidity,represents acidity, andand >7>7
represents alkalinityrepresents alkalinity
• pH has a significant impact on thepH has a significant impact on the
availability of soil nutrientsavailability of soil nutrients
• pH 6.5pH 6.5
17. pH ScalepH Scale
The figure shows
the break down
of where acidity
to alkalinity is on
the pH scale.
PH 7 is neutral.
18. pH Effect on NutrientpH Effect on Nutrient
AvailabilityAvailability
This graphic shows
how the major plant
nutrients change in
availability with the
increase and
decrease of pH.
The wider the black
band in this
graphic, the more
available the
nutrient.
This has a direct
impact on plant
health. For most
agricultural crop
recommendations,
the goal is to have
a 6.5 pH. At this pH
most of the
essential plant
nutrients are
available.
19. pH Preferences by PlantspH Preferences by Plants
This graphic
shows the range in
pH preferred by
plants. This
shows that it is
important for
producers to know
the fertility and pH
requirements of
the plants they
plan to grow.
As can be seen
from the black
bands, most plants
prefer a pH
between 5.5 and
7.0.
A pH below 5.5 is
considered to be
very acid and
above 7.0 is
alkaline.
.
20. Limiting Factors
• A layer which restricts the downwardA layer which restricts the downward
penetration of a plant’s root systempenetration of a plant’s root system
will reduce growth in direct relationwill reduce growth in direct relation
to the depth of the layer.to the depth of the layer.
• On rare occasions, a limiting layer mayOn rare occasions, a limiting layer may
increase site productivity, such as onincrease site productivity, such as on
sandy soils where the layer may retardsandy soils where the layer may retard
leaching of nutrients and increaseleaching of nutrients and increase
available moisture.available moisture.
Root
21. Subsoiling
There are farm implements
available that can breakup
soil hard pans and
improve the crop
production in otherwise
limited soils.
Subsoilers have long shanks that
physically dig down to break
open the hard soil to form
channels where plant roots can
penetrate.
22. 16 Essential Elements (part 1)
• PrimaryPrimary
Nitrogen (N)Nitrogen (N)
Phosphorus (P)Phosphorus (P)
Potassium (K)Potassium (K)
• SecondarySecondary
Sulfur (S)Sulfur (S)
Magnesium (Mg)Magnesium (Mg)
Calcium (Ca)Calcium (Ca)
The primary elements are plant nutrients that
are needed and most used by plants for
growth. The primary nutrients can be found
in commercial complete fertilizers as the
fertilizer number reflects these three
elements, i.e. 10-6-4.
Secondary elements are the next most
needed plant nutrients. Magnesium and
calcium are obtained from liming materials.
During the Industrial revolution, most of our
sulfur came from air pollution (sulfur
dioxide).
In recent years, producers have had to
routinely include supplemental sulfur to
their crop fertility programs as the air
around us becomes less contaminated with
sulfur.
24. 16 Essential Elements (part 3)
• The final three (3) essential elementsThe final three (3) essential elements
to plant growth come mostly from airto plant growth come mostly from air
and water.and water.
• They are:They are:
Carbon (C)Carbon (C)
Hydrogen (H)Hydrogen (H)
Oxygen (O)Oxygen (O)
25. The Primary Elements
• Nitrogen: It gives plants their green color,Nitrogen: It gives plants their green color,
promotes above ground growth, andpromotes above ground growth, and
regulates utilization of other elements.regulates utilization of other elements.
• Phosphorus: It has favorable affect onPhosphorus: It has favorable affect on
- cell division- cell division - stem strength- stem strength
- crop maturation - root development- crop maturation - root development
- flowering/fruiting - disease resistance- flowering/fruiting - disease resistance
26. • Potassium (K)Potassium (K)
-- It is essential for starch formationIt is essential for starch formation
and translocation of sugars. It isand translocation of sugars. It is
also essential to the development ofalso essential to the development of
chlorophyll. K helps plantschlorophyll. K helps plants
to over-winter.to over-winter.
The Primary Elements (con’t)
27. What is the nutrient contentWhat is the nutrient content
of commercial fertilizers?of commercial fertilizers?
• Expressed as a percent called theExpressed as a percent called the
“guaranteed analysis” or fertilizer“guaranteed analysis” or fertilizer
grade.grade.
• Nutrient content always appears inNutrient content always appears in
this order:this order:
% total nitrogen% total nitrogen
% available phosphate (P% available phosphate (P22OO55), or), or
phosphoric acidphosphoric acid
% soluble potash (K% soluble potash (K22O)O)
28. The Fertilizer Number
The fertilizer number refers to a ratio of N-P-KThe fertilizer number refers to a ratio of N-P-K
5-10-5 (1-2-1 ratio) has:5-10-5 (1-2-1 ratio) has:
5% N 10% P5% N 10% P220055 5% K5% K220 = 20%0 = 20%
The other 80% of the material is called theThe other 80% of the material is called the
carrier. This is typically some inert material.carrier. This is typically some inert material.
10 - 6 - 4 (2-1-1 ratio)10 - 6 - 4 (2-1-1 ratio)
10 -10 -10 (1-1-1 ratio)10 -10 -10 (1-1-1 ratio)
29. Ag-Gro-Pro
5-10-
15 50 lbs.
This bag contains:
5% nitrogen--10%
phosphate--15% potash
or
2.5 lbs. nitrogen
5 lbs.
phosphate
7.5 lbs. potash
What does a fertilizer guarantee mean?What does a fertilizer guarantee mean?
31. Determining Fertilizer Need
Production Goal: Total lb/A N - P - KProduction Goal: Total lb/A N - P - K
soil reservesoil reserve -- N –P - KN –P - K
crop residuecrop residue -- NN
manuremanure -- N - P - KN - P - K
____________________________
Commercial fertilizer + lb/A N - P - KCommercial fertilizer + lb/A N - P - K
32. Example: Calculating the Quantity of
Commercial Fertilizer Required to meet a
Nutrient Recommendation
Jasper Little Farm:Jasper Little Farm:
• needs 60 lbs./A of potash (Kneeds 60 lbs./A of potash (K22O) on hisO) on his
soybean cropsoybean crop
• broadcasts muriate of potash (0-0-60)broadcasts muriate of potash (0-0-60)
pre-plantpre-plant
• see Example 4-1, p.18 in training guidesee Example 4-1, p.18 in training guide
33. Calculating Quantity of
Commercial Fertilizer
1) RECORD recommended quantity of1) RECORD recommended quantity of
nutrient (see nutrient managementnutrient (see nutrient management
plan).plan).
2) RECORD the percentage of nutrient2) RECORD the percentage of nutrient
in the preferred product, muriate ofin the preferred product, muriate of
potash.potash.
3) CONVERT the percentage of3) CONVERT the percentage of
nutrient to a decimal fraction bynutrient to a decimal fraction by
multiplying the % by .01multiplying the % by .01
60 lbs./A
60%
60 x 0.01 = .60
34. Calculating the Quantity of
Commercial Fertilizer
CALCULATE the quantity of muriate of
potash required in lbs./A: divide the
recommended quantity of nutrient by
the nutrient content expressed as a
decimal fraction.
Little needs 100 lbs. of muriate ofLittle needs 100 lbs. of muriate of
potash to supply 60 lbs. of potash.potash to supply 60 lbs. of potash.
Done!Done!
60 lbs./A ÷ 0.60 = 100 lbs./A
35. Determining Production
Goal
• Cropping historyCropping history
• Soil Survey Map/Soil Capability ChartSoil Survey Map/Soil Capability Chart
• Investigate species/variety potentialInvestigate species/variety potential
- other growers- other growers
- field days- field days
- private and university trial results- private and university trial results
• FSA recordsFSA records
• ExperimentationExperimentation
36. MASCAP
MARYLAND’S
AGRONOMIC SOIL
CAPABILITY
ASSESSMENT
PROGRAM
Va. A. Bandel, and
E.A. Heger
Agronomy Department
Cooperative Extension
Service
University of Maryland
September 1994
Determining Yield GoalDetermining Yield Goal
• Take the average yield for typicalTake the average yield for typical
years that a crop is grown in a certainyears that a crop is grown in a certain
field.field.
• Estimate yields goal by averaging theEstimate yields goal by averaging the
yield from the best 3 of 5 growingyield from the best 3 of 5 growing
seasons.seasons.
• When actual yield data is notWhen actual yield data is not
available, estimated yields for the soilavailable, estimated yields for the soil
type in the field can be found intype in the field can be found in
“MASCAP”.“MASCAP”.
37. Soil Reserve
• Soil testSoil test
- university lab- university lab
- private labs- private labs
• Frequency of testingFrequency of testing
- depends on crop and management- depends on crop and management
• Typical test looks at P, K, Ca, Mg,Typical test looks at P, K, Ca, Mg,
O.M., and pH. Minors are as needed.O.M., and pH. Minors are as needed.
38. Fig. 1-1: Phosphate RecommendationFig. 1-1: Phosphate Recommendation (lbs/A)(lbs/A)
as a function of soil fertility level (FIV-P)
for corn grain (yield goal-150 bu/A)
110
85
70
65
45 45
35
30
20 20
0
0
20
40
60
80
100
120
10
30
50
70
90
110
FIV-P
Low Medium Optimum Excessive
# P205/A
39. Crop Residue
• Benefits left by a previous crop orBenefits left by a previous crop or
cover cropcover crop
• Previous crops leave little unless itPrevious crops leave little unless it
was a leguminous cropwas a leguminous crop
• Leguminous crops leave nitrogenLeguminous crops leave nitrogen
• The amount of N left depends on theThe amount of N left depends on the
species of legume and the standspecies of legume and the stand
density and maturity.density and maturity.
• Cover crops are not harvested and willCover crops are not harvested and will
recover nutrients otherwise lost.
41. How much of the nitrogen inHow much of the nitrogen in
manure is plant-available?manure is plant-available?
It depends on:It depends on:
** the nitrogen contentthe nitrogen content
** animal speciesanimal species
** incorporation practicesincorporation practices
42. 3
9
Ammonium
nitrogen
Organic
nitrogen
Figure 2- 3b. Distribution of organic nitrogenFigure 2- 3b. Distribution of organic nitrogen
& ammonium nitrogen in dairy manure& ammonium nitrogen in dairy manure
This dairy manure contains 12 pounds of total nitrogen per ton.
43. Available Organic NitrogenAvailable Organic Nitrogen
Only part of the nitrogen in manure
becomes plant-available -- through the
process of mineralization -- the year
it’s applied.
44. Nitrogen “Credits”Nitrogen “Credits”
• Organic nitrogen in organic sourcesOrganic nitrogen in organic sources
continues to break down or mineralizecontinues to break down or mineralize
for several years after application.for several years after application.
• The largest proportion of this organicThe largest proportion of this organic
nitrogen breaks down and becomesnitrogen breaks down and becomes
available in the year of application.available in the year of application.
• Organic sources include manure,Organic sources include manure,
biosolids (sludge), and composts.biosolids (sludge), and composts.
45. Nitrogen “Credits”Nitrogen “Credits”
• Progressively smaller amounts of theProgressively smaller amounts of the
organic nitrogen break down andorganic nitrogen break down and
become available in the subsequentbecome available in the subsequent
years.years.
• Credit needs to be given to thisCredit needs to be given to this
available nitrogen from previouslyavailable nitrogen from previously
applied manure to the current year’sapplied manure to the current year’s
nitrogen recommendation.nitrogen recommendation.
46. Ammonium
nitrogen
Available
ammonium
nitrogen
Available
organic
nitrogen
Organic
nitrogen
Figure 2- 4b: Distribution of Available NitrogenFigure 2- 4b: Distribution of Available Nitrogen
from Organic and Ammonium Nitrogenfrom Organic and Ammonium Nitrogen
Components in Dairy ManureComponents in Dairy Manure
This dairy manure contains 12 pounds of total nitrogen and
5.4 pounds of available nitrogen per ton
2.4 lb
0.6
lb
3 lb
6 lb
47. Don’t Overload!
A funny slide to breakup the class. This could be an Iraqi surface to air
missile.
48. Manure Mineralization FactorsManure Mineralization Factors
•Vary by animal species.
•See Table 2-1 in the
Nutrient Applicator Guide.
The mineralization rate of manure varies
between animal species. A table
explaining these differences can be found
in the Nutrient Applicator Guide on page
10.
49. • NHNH44 is a plant-available form of N.is a plant-available form of N.
• When manure is left on the soil surface afterWhen manure is left on the soil surface after
application, it can be lost through theapplication, it can be lost through the
process ofprocess of volatilizationvolatilization..
Nitrogen LossNitrogen Loss
Available Ammonium NitrogenAvailable Ammonium Nitrogen
51. Example: Calculating Quantity of DairyExample: Calculating Quantity of Dairy
Manure to Meet Crop NutrientManure to Meet Crop Nutrient
RecommendationRecommendation
Ralph Gonzales Farm
• PAN content of semi-solid dairyPAN content of semi-solid dairy
manure is 6 lbs./Tmanure is 6 lbs./T
• wants to supply the N for his corn cropwants to supply the N for his corn crop
• yield goal is 120 bu/Ayield goal is 120 bu/A
• incorporates the manure the same dayincorporates the manure the same day
as applicationas application
• see Example 4-2, p.19 in training guidesee Example 4-2, p.19 in training guide
52. Calculating Quantity of Dairy ManureCalculating Quantity of Dairy Manure
to Meet Recommendationto Meet Recommendation
Note: The nitrogen recommendationNote: The nitrogen recommendation
for corn grain is 1 lb./A of PAN perfor corn grain is 1 lb./A of PAN per
bushel of yield.bushel of yield.
1) RECORD nitrogen recommendation1) RECORD nitrogen recommendation
(lbs./A) from the nutrient management(lbs./A) from the nutrient management
plan.plan.
2) RECORD PAN of manure (lbs./T)2) RECORD PAN of manure (lbs./T)
120 lbs./A
6 lbs./T
53. Calculating Quantity of Dairy ManureCalculating Quantity of Dairy Manure
to Meet Recommendationto Meet Recommendation
CALCULATE the quantity of manure
required in T/A: divide the nitrogen
recommendation by the PAN of manure.
Twenty tons of a dairy manure withTwenty tons of a dairy manure with
this PAN are needed to provide 120this PAN are needed to provide 120
lbs./A of PAN.lbs./A of PAN.
Done!Done!
120 lbs./A ÷ 6 = 20 T/A
54. Use of Raw Manure
• Heavy applications can throw offHeavy applications can throw off
nutrient balancenutrient balance
• Excess available N can lead toExcess available N can lead to
excessive growth and nitrate buildupexcessive growth and nitrate buildup
in plantin plant
• Plants with high nitrates do not storePlants with high nitrates do not store
as well and attract insectsas well and attract insects
• Nitrogen and phosphorus areNitrogen and phosphorus are
pollutantspollutants
• Weed seeds pass through animals
55. Often Forgotten Sources of N
• Carryover from past manure/biosolidsCarryover from past manure/biosolids
• Cover crops ( fixed & recycled N)Cover crops ( fixed & recycled N)
• N released from soil organic matterN released from soil organic matter
(40-80 lb/A)(40-80 lb/A)
• Nitrates in rain & irrigation waterNitrates in rain & irrigation water
• Weeds, plowed down have slow-release N,Weeds, plowed down have slow-release N,
85 lb/T pigweed, 80 lb/T lambsquarter85 lb/T pigweed, 80 lb/T lambsquarter
• Crop residues, humus, bedding, andCrop residues, humus, bedding, and
compostscomposts
56. The Nitrogen Cycle
Atmospheric
nitrogen
Atmospheric
fixation
and deposition
Animal
manures
and biosolids
Industrial fixation
(commercial fertilizers)
Crop
harvest
Volatilization
Denitrification
Runoff and
erosion
Leaching
Organic
nitrogen
Ammonium
(NH4)
Nitrate
(NO3)
Plant
residues
Biological
fixation by
legume plants Plant
uptake
Im
m
obilization
Im
m
obilization
M
ineralization
M
ineralization
Input to soilComponent Loss from soil
-
+
57. The Phosphorus Cycle
Animal
manures
and biosolids Mineral
fertilizers
Crop
harvest
Runoff and
erosion
Leaching
(usually minor)
Organic phosphorus
•Microbial
•Plant residue
•Humus
Primary
minerals
(apatite)
Plant
residues
Plant
uptake
Soil solution
phosphorus
•HPO4
-2
•H2PO4
-1
Secondary
compounds
(CaP, FeP, MnP, AlP)
DissolutionDissolution
PrecipitationPrecipitation
Mineral
surfaces
(clays, Fe and
Al oxides,
carbonates)W
eathering
W
eathering
Adsorption
Adsorption
Mineralization
Mineralization
Immobilization
Immobilization
Desorption
Desorption
Input to soilComponent Loss from soil
Atmospheric
deposition
58. The Potassium Cycle
Animal
manures
and biosolids
Mineral
fertilizers
Crop
harvest
Runoff and
erosion
Leaching
Soil solution
potassium (K+
)
Plant
residues
Plant
uptake
Mineral
potassium
Fixed
potassium
Exchangeable
potassium
Input to soilComponent Loss from soil
59. The Sulfur Cycle
Animal
manures
and biosolids
Mineral
fertilizers
Crop
harvest
Runoff and
erosion
Leaching
Absorbed or
mineral sulfur
Plant
residues
Plant
uptake
Sulfate
Sulfur
(SO4)
Atmospheric
sulfur
Elemental
sulfur
Organic
sulfur Immobilization
Immobilization
Mineralization
Mineralization
Bacterial reduction
Bacterial reduction
Bacterial oxidation
Bacterial oxidation
O
xidation
O
xidation
SOSO22 gasgas
Reduced sulfur
Input to soilComponent Loss from soil
Volatilization
Atmospheric
deposition
-
60. Fertilizer Application Terms
• BroadcastBroadcast
- fertilizer is applied uniformly to- fertilizer is applied uniformly to
entire field before crop emergesentire field before crop emerges
• TopdressTopdress
- fertilizer is applied uniformly to- fertilizer is applied uniformly to
entire field after crop emergesentire field after crop emerges
• Plowed down or tilled inPlowed down or tilled in
- fertilizer is applied to field then is- fertilizer is applied to field then is
tilled in with a disk or a plowtilled in with a disk or a plow
61. Fertilizer Application Terms
• BandedBanded
- fertilizer is applied directly over- fertilizer is applied directly over
the top of the crop row, generallythe top of the crop row, generally
before the crop emerges, omittingbefore the crop emerges, omitting
the area between the rowsthe area between the rows
• Side-dressedSide-dressed
- fertilizer is applied directly to- fertilizer is applied directly to
growing crop, generally in a bandgrowing crop, generally in a band
at the base of the plantat the base of the plant
62. Calibrating NutrientCalibrating Nutrient
Application EquipmentApplication Equipment
• Calibration is a way to set yourCalibration is a way to set your
application equipment to applyapplication equipment to apply
material uniformly at the desired rate.material uniformly at the desired rate.
• It insures application of the requiredIt insures application of the required
amount of nutrients without over-amount of nutrients without over-
fertilizing.fertilizing.
• Two common methods are used:Two common methods are used:
- weight-area method- weight-area method
- load-area method- load-area method
63. Basics of Calibration
Width
Area = Length x Width
L
e
n
g
t
h
Width
L
e
n
g
t
h
Determining the square feet in an area is basic to
the calibration of farm equipment. The size of an
area can be determined by multiplying length X
width.
64. How to Calibrate NutrientHow to Calibrate Nutrient
Application EquipmentApplication Equipment
• Measure the actual rate of application.Measure the actual rate of application.
• Compare actual application rate to theCompare actual application rate to the
recommended application rate.recommended application rate.
• If the application rate is substantiallyIf the application rate is substantially
greater or less than the recommendedgreater or less than the recommended
rate, try:rate, try:
-- changing equipment settings, orchanging equipment settings, or
- changing ground speed of the- changing ground speed of the
tractortractor
65. Load-Area MethodLoad-Area Method
Know:Know:
• capacity of the spreadercapacity of the spreader
• size of the area where manure issize of the area where manure is
spreadspread
Apply nutrient supplying material,Apply nutrient supplying material,
then measure area of application.then measure area of application.
Project rate of application to a per-acreProject rate of application to a per-acre
basis.basis.
66. Weight-Area Method forWeight-Area Method for
ManureManure
1. Arrange at least 3 plastic sheets in the center1. Arrange at least 3 plastic sheets in the center
of the spreader’s path.of the spreader’s path.
2. Drive the spreader over the center of the2. Drive the spreader over the center of the
sheets at a known speed with specificsheets at a known speed with specific
equipment settings.equipment settings.
3. Collect & weigh the manure on each sheet.3. Collect & weigh the manure on each sheet.
4. Average the quantity applied to the sheets4. Average the quantity applied to the sheets
and project to T/A.and project to T/A.
67. Weight-Area Method
• Works well with calibrating fertilizerWorks well with calibrating fertilizer
spreaders and planters.spreaders and planters.
• Works well with calibrating both dry andWorks well with calibrating both dry and
liquid manure spreaders.liquid manure spreaders.
- pans can be used to catch liquid manure- pans can be used to catch liquid manure
- plastic sheets can be used to catch dry- plastic sheets can be used to catch dry
manuremanure
68. Basics of Calibration
Using Sheets and Pans
1 2 3
91 7
8
4 6
5
10
2
3
Spread manure
Spread manure
This diagram shows how pans and sheets can be arranged in a field to calibrate a spreader.
69. Refer to your “Nutrient
Applicator’s Training Guide “
for additional help
70. Let’s take a quick look at some
other materials we apply to
our soils.
71. LimestoneLimestone
• Supplies calcium and magnesiumSupplies calcium and magnesium
• Mined calcium carbonate is theMined calcium carbonate is the
principle liming material, typicallyprinciple liming material, typically
50% oxides50% oxides
• CaCOCaCO33 equivalent is the basis forequivalent is the basis for
liming material recommendation ratesliming material recommendation rates
• Comes in various forms and gradesComes in various forms and grades
72. Effective Neutralizing ValueEffective Neutralizing Value
E.N.V.E.N.V.
This is a comparative value that refersThis is a comparative value that refers
to the ability of a liming material toto the ability of a liming material to
modify soil pH within a year.modify soil pH within a year.
Reference Standard:Reference Standard:
Calcium carbonate (CaCOCalcium carbonate (CaCO33))
E.N.V.= 100E.N.V.= 100
Comparing Liming Materials
This means that liming
materials are compared
(greater than or less than) to
the neutralizing ability of
calcium carbonate. E.N.V.
can be found on the labels of
liming materials and fertilizer
as an indicator of the
products impact on soil pH.
73. LimestoneLimestone
• Mesh size determines how quickly itMesh size determines how quickly it
reacts in the soilreacts in the soil
• Good quality ag lime is typically 80%Good quality ag lime is typically 80%
90-100 mesh and 20% 40 mesh90-100 mesh and 20% 40 mesh
• Ground dolomite (dolomitic lime) isGround dolomite (dolomitic lime) is
over 10% magnesium; it is a goodover 10% magnesium; it is a good
source of Mg when neededsource of Mg when needed
74. Other Liming AgentsOther Liming Agents
• These are typically industrialThese are typically industrial
byproductsbyproducts
• These include stack dust, sludge lime,These include stack dust, sludge lime,
and river mudand river mud
• Domino Sugar lime is a new sourceDomino Sugar lime is a new source
• Solubility and % oxides vary, so get anSolubility and % oxides vary, so get an
analysisanalysis
• These contain mostly Ca and traces ofThese contain mostly Ca and traces of
other elements and materialsother elements and materials
75. Liming RecommendationsLiming Recommendations
• Know the analysis, especially % oxidesKnow the analysis, especially % oxides --
Application rate is based on lb/AApplication rate is based on lb/A
oxidesoxides
• % calcium and magnesium% calcium and magnesium - may not- may not
need additional Mgneed additional Mg
• Oxide form of calcium (CaO) is readilyOxide form of calcium (CaO) is readily
availableavailable
• Mesh size of carbonate form of CaMesh size of carbonate form of Ca
(CaCO(CaCO33 )) reflects its availabilityreflects its availability --
smaller particles work fastersmaller particles work faster
76. Liming NotesLiming Notes
• Limestone recommendations are based onLimestone recommendations are based on
raising the pH of the plow layer (top 7-9”)raising the pH of the plow layer (top 7-9”)
to 6.5; except for special crops; i.e. alfalfa.to 6.5; except for special crops; i.e. alfalfa.
• Limited to 1,500 lb/A oxides/year when notLimited to 1,500 lb/A oxides/year when not
incorporating; i.e. pasturesincorporating; i.e. pastures
• Avoid applying liming products andAvoid applying liming products and
fertilizer at, or around the same time.fertilizer at, or around the same time.
• Liming materials laying on the surface willLiming materials laying on the surface will
neutralize pesticides.neutralize pesticides.
77. CompostCompost
Decomposed Plant & animal MatterDecomposed Plant & animal Matter
• When correctly done:When correctly done:
- pH is near neutral- pH is near neutral
- C:N ratio is 15:1- C:N ratio is 15:1
- Majority of weed seeds & disease- Majority of weed seeds & disease
organisms are deadorganisms are dead
- Offers a well balanced slow release- Offers a well balanced slow release
supply of nutrientssupply of nutrients
- As much as 1/4 of compost weight is- As much as 1/4 of compost weight is
microbes (dead & alive)microbes (dead & alive)
78. Principles of CompostingPrinciples of Composting
• Best composts come from piles withBest composts come from piles with
the highest microbial activitythe highest microbial activity
• Temperature is easiest sign ofTemperature is easiest sign of
microbial activitymicrobial activity
• Good composts heat to approximatelyGood composts heat to approximately
140 - 160140 - 16000
F within the first 3 or 4 daysF within the first 3 or 4 days
79. Principles of CompostingPrinciples of Composting
• Small particle size makes a greaterSmall particle size makes a greater
surface area available to microbessurface area available to microbes
- particles that are too small- particles that are too small
however can pack a pilehowever can pack a pile
• Adequate volume, or size of pile keepsAdequate volume, or size of pile keeps
it from cooling too quicklyit from cooling too quickly
- piles 4 x 4 x 4 ft. do well- piles 4 x 4 x 4 ft. do well
80. Unfinished CompostsUnfinished Composts
• Can hurt cropsCan hurt crops
• Chemicals formed in process are toxicChemicals formed in process are toxic
to plantsto plants
• N can be tied upN can be tied up
• Good composts take 12 - 18 monthsGood composts take 12 - 18 months
• Moisture must be adequate (50 - 70%)Moisture must be adequate (50 - 70%)
similar to a squeezed spongesimilar to a squeezed sponge
• C:N ratio in initial pile should be 30:1C:N ratio in initial pile should be 30:1
82. Compost Problem SolvingCompost Problem Solving
• Bad OdorBad Odor
- not enough air- not enough air
- turn the pile more frequently- turn the pile more frequently
• Center of pile too dryCenter of pile too dry
- not enough water- not enough water
- moisten while turning- moisten while turning
83. Compost Problem SolvingCompost Problem Solving
• Pile is damp & warm in center, but nowherePile is damp & warm in center, but nowhere
elseelse
- pile is too small- pile is too small
- collect more material and mix the old- collect more material and mix the old
ingredients into a new pileingredients into a new pile
• Pile is damp and sweet smelling, but willPile is damp and sweet smelling, but will
not heat upnot heat up
- lack of nitrogen- lack of nitrogen
- mix in N-rich material like fresh- mix in N-rich material like fresh
grass, manure, or ureagrass, manure, or urea
84. Crop Rotation and Cover CropsCrop Rotation and Cover Crops
• Benefits crop fertilityBenefits crop fertility
- fixed and recaptured nutrients- fixed and recaptured nutrients
• Benefits soil structure (tilth)Benefits soil structure (tilth)
- cover crops add organic matter- cover crops add organic matter
- variability in root growth- variability in root growth
improves soil pores and waterimproves soil pores and water
penetrationpenetration
• Pest managementPest management
- breaks the parasite life cycle- breaks the parasite life cycle
• Harvest vs. cover crop is the decisionHarvest vs. cover crop is the decision
85. Some Parting AdviceSome Parting Advice
• Seek help when you are not sure about whatSeek help when you are not sure about what
you are doing. There are a lot of resourcesyou are doing. There are a lot of resources
out there for you.out there for you.
• Don’t be like the old farmer who told theDon’t be like the old farmer who told the
County Agent that he did not need anyCounty Agent that he did not need any
advice. He told the Agent that he hasadvice. He told the Agent that he has
already worn out two farms and that he hadalready worn out two farms and that he had
his own way of doing things.his own way of doing things.
If you are viewing this file with PowerPoint, simply use your F5 key to have it play full screen like a movie.
Soil quality is the most important factor in farm crop production. It largely determines what can be produced on the farm and directly affects the landowner’s economic investments on the farm. For this reason, soil quality gets a gold star for importance.
The soil profile shows the layers, known as horizons that represent the soil. Horizons have formed over the centuries due mostly from weathering. A lettering system is used to name the different horizons.
All of the information that you need to know about your farm’s soil can be found in the County Soil Survey Map. You can find a copy of the Soil Survey Map at your county Soil Conservation District. The Soil Survey Map has a wealth of information that includes tables that can help you to plan a forest planting.
The Soil Survey Map even has tables to help you to plan a wildlife habitat planting.
The 6 factors controlling plant growth are 1) light, 2) mechanical support, 3) heat, 4) air, 5) water, and 6) nutrients. Of these six, all but one, light, is supplied by the soil. Soil provides a place for roots to grow for support. Soil temperature largely regulates plant growth. As we will see shortly, one-half of the soil is made up of air and water. Soil contains minerals and organic matter that provide essential nutrients to plants.
This pie chart shows the four major components of a typical silt loam soil. The components are 45% mineral, 5% organic matter, 25% water, and 25% air. The thing to note here is that the soil is 50% air and water. This tells you that soil is not a solid thing. It is actually one-half pore space occupied by air and water. This is where the action takes place in the soil.
It is important to know and understand the terminology used in agriculture. There are some key words and terms associated with soils that agricultural producers should know.
Soil texture: concerns the size of mineral particles, specifically the relative proportion of various size groups in a given soil. (This will become clearer when we discuss the various soil texture types).
Soil structure: the arrangement of soil particles into groups of aggregates.
Soil texture is separated into three soil separates based on particle size.
1) sand
2) silt
3) clay
Silt, clay: imparts a fine texture and slow water and air movement, also high water holding capacity.
Sandy to gravelly: are referred to as lighter soils with lower water holding capacity.
Silt and clay soils are referred to as not only fine textured soils but also as heavy soils. Clay, which is the finest soil particle, will produce the heaviest soils. Because the soil particles in silt and clay soils are small, these particles will be more densely packed with many small pore spaces. This causes water and air to move more slowly through them than in the coarser sandy or gravelly soils where larger pores allow more rapid movement. Due to the abundance of the pore spaces in fine textured soils, they are able to hold more water within them than in lighter soils. This is one reason why the fine textured soils can resist drying out longer than lighter soils.
Because they are generally well drained, sandy soils often lack plant nutrients due to constant leaching.
Soils that contain mostly clay are just the opposite in that they tend to hold moisture and will retain plant nutrients. Leaching is less of a problem in heavier soils.
We saw in earlier slides that one-half of soil is made up of pore spaces, which contains air and water. Due to the greater abundance of these pore spaces, fine textured soils are able to hold more air and water than the lighter sandy soils with larger, but fewer pore spaces. Because of the small particles in fine textured, the soil is denser and therefore more sensitive to compaction when wet. Compacted soils have reduced pore space and are less productive. Soil activity for plant production takes place in pore spaces.
Soil depth: defined as that depth of soil material favorable for plant root penetration. Soils referred to as deep and well drained are considered to be the best. A shallow soil would be one that has only a few inches of topsoil before getting into a less productive substrate material.
Slope: land topography largely determines the amount of drainage, runoff, and erosion. The steeper the land, the more management is required.
Organic matter: it consists of plant and animal residues in various stages of decay. Adequate levels of organic matter benefits the soil in several ways:
1) improves the physical condition of the soil,
2) helps to increase water infiltration,
3) improves soil tilth (those properties of soil that are conducive to plant growth),
4) helps to decrease soil erosion,
5) supplies plant nutrients (as it breaks down, it releases nutrients back into the soil),
6) holds cation nutrients (positively charged ions which include most plant nutrients).
pH: expression of both acidity and alkalinity on a scale whose values run from 0 to 14 with:
7 representing neutrality,
less than 7 represents acidity and
greater than 7 represents alkalinity.
pH has a significant impact on the availability of plant soil nutrients.
Most agricultural crops prefer a pH 6.5 for best growth.
The figure shows the break down of where acidity to alkalinity is on the pH scale. PH 7 is neutral.
Graphic shows how the major plant nutrients change in availability with the increase and decrease of pH.
The wider the black band in this graphic, the more available the nutrient.
This has a direct impact on plant health. For most agricultural crop recommendations, the goal is to have a 6.5 pH. At this pH most of the essential plant nutrients are available.
Graphic shows the range in pH preferred by plants. This shows that it is important for producers to know the fertility and pH requirements of the plants they plan to grow.
As can be seen from the black bands, most plants prefer a pH between 5.5 and 7.0. A pH below 5.5 is considered to be very acid and above 7.0 is alkaline.
Sometimes a soil has a layer that can restrict the penetration of plant roots. This can limit the growth of a plant. This limiting layer can be man-made or naturally occurring. A man-made hard pan can develop at the bottom of a plow layer as a result of years of plowing. A look at the county Soil Survey Map can tell you if your soil has a naturally occurring limiting layer.
Under some conditions, a limiting layer can be of benefit. For example, in a sandy soil leached plant nutrients would accumulate at the limiting layer where plant roots would be able to utilize these otherwise lost nutrients.
There are farm implements available that can breakup soil hard pans and improve the crop production in otherwise limited soils.
Subsoilers have long shanks that physically dig down to break open the hard soil to form channels where plant roots can penetrate.
There are three primary elements. They are nitrogen, phosphorus, and potassium. Primary elements are those plant nutrients that are needed and most used by plants for growth. Secondary elements are the next most needed plant nutrients. These include sulfur, magnesium, and calcium. The primary nutrients can be found in commercial complete fertilizers as the fertilizer number reflects these three elements, i.e. 10-6-4. Magnesium and calcium are obtained from liming materials. During the Industrial revolution, most of our sulfur came from air pollution (sulfur dioxide). In recent years, producers have had to routinely include supplemental sulfur to their crop fertility programs as the air around us becomes less contaminated with sulfur.
Micronutrients are plant nutrients that are needed in only small amounts. These include iron, manganese, boron, chlorine, zinc, copper, and molybdenum. All 16 essential elements are important. A deficiency in any one of them will impact on plant growth.
The final three- (3) essential elements to plant growth come mostly from air and water. They are carbon, hydrogen, and oxygen. Carbon in the form of carbon dioxide (CO2) and oxygen are found in abundance in the air. Water (H2O) is a source of hydrogen and oxygen.
Nitrogen: It gives plants their green color, promotes above ground growth, and since it stimulates plant growth, it regulates the utilization of the other 15 essential elements.
Phosphorus: It has a favorable affect on: cell division, stem strength, crop maturation, root development, flowering/fruiting, and disease resistance.
Potassium: It is essential for starch formation and translocation of sugars. It is also essential to the development of chlorophyll. Potassium helps plants to over winter. For this reason, high ratios of potash (K2O) can be found in crop/plant winterizing fertilizers.
The nutrient content of commercially available fertilizer is expressed as a percent called the guaranteed analysis or fertilizer grade. This always appears as % total nitrogen, % available phosphate, or phosphoric acid, and % soluble potash.
The fertilizer number refers to a ratio of nitrogen to phosphorus to potassium. 5-10-5 fertilizer is an example of a 1-2-1 ratio fertilizer. The fertilizer number reflects the percentage of nutrients in the material. 5-10-5 fertilizer has a total of 20% nutrients, with the other 80% of the material being inert, or carrier material.
Using the analysis (grade) of the fertilizer and the total weight of the bag, the actual amount of plant nutrients in the bag can be easily calculated. For example, this 50 lb. bag of 5-10-15 contains 5% nitrogen, 10% phosphate, and 15% potash. By multiplying the nutrient percentages times the total weight in the bag, we find that the bag contains 2.5 lbs. Of nitrogen, 5 lbs. Of phosphate, and 7.5 lbs. of potash. This means that the bag contains 15 lbs. of plant nutrients and 35 lbs. of inert ingredients.
Slide reflects a list of the most commonly used fertilizers in the region and their analyses. Many of these materials are custom mixed together to meet the specific fertility needs of a crop based on soil test results.
Slide reflects the basic outline of a nutrient management plan for crop production on a specific field. The primary nutrient requirements to meet the production goal will provide the amount of N-P-K needed to meet that goal. A soil test will provide the amount of soil reserves of nutrients, which can be subtracted from the total needed.
Next, if any legumes such as clover were grown in the field the previous year, the residual nitrogen left in the field can be subtracted from the total needed.
Finally, if any manure or biosolids are applied to the field, the nutrient value of the N-P-K in manure can be subtracted from the total.
The net result of the amount of nutrients needed to meet the crop production goal can be supplied by commercial fertilizer. This process helps to avoid applying unnecessary nutrients, which impacts on the environment and also wastes the crop producer’s money.
This example can be found on page 18 in the Nutrient Applicator Training Guide.
This slide is a continuation of the previous example.
This slide concludes the example used in the two previous slides.
One of the most important factors in developing an accurate nutrient management plan is determining realistic production goals. Often producers strive for crop yield goals that they would like to obtain, but in reality can never achieve due to factors beyond their control. This wastes resources. Realistic crop yields can be determined by
1) looking at the crop production history of the field,
2) reviewing the Soil Survey Map and Soil Capability Chart (these will provide soil engineer’s assessments at the potential production ability of the soil in the field),
3) investigate how the crop species and varieties you want to grow have done for other growers in your area and in research and demonstration plots,
4) Farm Service Agency (FSA) keeps records on the yields of some crops that are reported to them by producers, and
5) your experimentation with a small, limited planting of a new crop before committing to a large planting will provide valuable experience on how to grow the crop and what kind of yield to expect.
Actual crop yields from the farm are best for setting yield estimates. Taking the average yield for typical crop production years grown in a certain field can provide a good estimate of yield. Taking an average of three of the top five growing seasons can make another yield estimate. When actual yield data is not available, the MASCAP chart is available at the county Soil Conservation District office. This can provide an estimate based on the farm’s soil types.
Keeping an eye on the nutrients in the soil reserve is essential to maintaining good soil fertility. Soil testing for these nutrients is simple and economical. They can be obtained through private industry and university labs.
Soil tests should be done annually for high production crops like alfalfa and annual crops. Permanent pastures, grass and mixed hay fields can be soil tested every three to five years once the fertility level for best plant growth has been met.
This graph shows how the recommended rate of a plant nutrient (Phosphate) will increase or decrease depending on the level of that nutrient found in the soil test. This is why soil testing for plant nutrients is important. This helps to avoid over applying nutrients, which can harm the environment and waste money. Also, soil testing helps to avoid crop losses from plant nutrient deficiencies.
Plant fertility benefits left in the soil by a previous crop is often overlooked and not taken advantage of by producers.
Leguminous crops provide the most benefit to following crops since they “fix” nitrogen and leave it in the soil for following crops to utilize. Leguminous crops can be used as crops grown for either cash, or animal feed, or as a cover crop.
Manure, biosolids (sludge), and composts contribute to the pool of plant nutrients in the soil. As an organic source, the nutrients are in various stages of decomposition. This will result in a long, slow release of these nutrients. These materials can be analyzed to obtain the amount of nutrients they contain. This plus accurate spreading over the field is essential to the best use of these important fertility resources.
The answer to this question depends on the nitrogen content of the manure, the animal species, and if the manure was incorporated into the soil or surface applied.
This pie chart shows that this example of one ton of dairy manure has a total of 12 lbs. of nitrogen. Of this 12 pounds, nine pounds of it is in the form of organic nitrogen and 3 pounds is in the form of ammonium nitrogen.
Only part of the nitrogen in manure becomes plant-available in the year of application. The rest of the nitrogen in the manure becomes slowly available through a process called mineralization over the next couple of years. Mineralization involves the breaking down of the organic matter in the manure by microorganisms to a point where the nitrogen is rendered into a form that plants can use.
Usually about one-half of the total nitrogen becomes plant-available in the first year. Through mineralization, the rest of the nitrogen becomes plant-available in progressively lower amounts over the next two to three years. Organic sources of nitrogen include manure, biosolids (sludge), and composts.
Since all of the nitrogen in manure does not become plant-available in the year that it is applied, credit needs to be given to the nitrogen that becomes available over the following two years. This helps to prevent the application of excessive amounts of nitrogen.
This pie chart shows that of the 12 pounds of total nitrogen in this ton of dairy manure, 5.4 pounds of it is plant-available. This includes 3 lbs. of organic nitrogen and 2.4 lbs. of ammonium nitrogen. The balance of the nitrogen in this manure will become available over time through mineralization.
A funny slide to breakup the class. This could be an Iraqi surface to air missile.
The mineralization rate of manure varies between animal species. A table explaining these differences can be found in the Nutrient Applicator Guide on page 10.
Ammonium is a plant-available form of nitrogen found in manure. When left on the soil surface, it can be lost through volatilization. When you can smell manure that has been applied to a field, it is losing nitrogen through volatilization. The odor of manure is largely nitrogen-based. Incorporating manure into the soil reduces the odor coming off of the field and traps the volatile nitrogen in the soil preventing its loss.
Ammonium is a plant-available form of nitrogen found in manure. When left on the soil surface, it can be lost through volatilization. When you can smell manure that has been applied to a field, it is losing nitrogen through volatilization. The odor of manure is largely nitrogen-based. Incorporating manure into the soil reduces the odor coming off of the field and traps the volatile nitrogen in the soil preventing its loss.
This example can be found on page 19 in the Nutrient Applicator Training Guide. This example helps to show how one can use the plant available nitrogen content of a manure to calculate the amount of manure to use to meet plant nutrient requirements.
This slide continues with the calculation of the previous slide.
This slide completes the calculation of the previous two slides.
Because of all of the soluble, readily available nutrients in fresh manure, its application to a field can throw off the nutrient balance of a field. The excess available nitrogen in it can lead to excessive plant growth and a nitrate build up in the plant. Excess nitrate build up in plants can lead to insect pest problems, poor storage quality, and toxicity as a forage plant. Excess soluble forms of nitrogen and phosphorus can move off of the field and pollute surface waters. Composting manure can help to reduce the impact of these nutrients on the field and also kill some of the weed seeds in the manure that would otherwise germinate in the field.
Nitrogen is a dynamic element in the environment around the farm. Plants can receive nitrogen from many other sources in addition to the fertilizer applications by the producer. Some of these often over-looked sources include: 1) carryover from previous manure/biosolids applications (As discussed earlier, the organic material will break down over a period of three years releasing nutrients.), 2) cover crops (As discussed earlier, legumes leave behind nitrogen in the soil. Also, deep-rooted cover crops can bring up nutrients from deep in the soil for use by following crops once the cover crop decomposes. These nutrients would otherwise be lost.), 3) Nitrogen is constantly being released from decomposing organic matter; as much as 40-80 lb./A is released annually.), 4) The nitrogen released from plowed down, decomposed weeds can be as much as 85 lb./A.), 5) Crop residues, humus, bedding, and composts all contain organic nitrogen that can benefit crops.
This diagram shows the nitrogen cycle and how dynamic it is in the environment. It is constantly changing forms. This makes it difficult to measure in the soil.
The phosphorus cycle is not as complicated as nitrogen, but it is not simple either. There are many factors at work in the soil that directly impact on its plant-availability.
The potassium cycle shows that, by nitrogen and phosphorus cycle standards, it has a little simpler life in the environment.
The sulfur cycle shows that this is another plant nutrient that has a complex life in the environment. For this reason, nitrogen and sulfur are two plant nutrients that are difficult to soil test for plant available nutrients. At one time, air pollution (sulfur dioxide) was a good source of plant available sulfur to farm crops.
Crop producers need to be familiar with the terminology associated with the application of fertilizer. These are:
Broadcast: fertilizer applied uniformly to entire field before the crop emerges.
Topdress: fertilizer is applied uniformly to entire field after the crop emerges.
Plowed down: fertilizer is applied to the field then is tilled in with a disk or plow.
Banded: fertilizer is applied directly over the top of the crop row, generally before the crop emerges, omitting the area between the rows.
Side-dresses: fertilizer is applied directly to a growing crop, generally in a band at the base of the plant.
Calibration is how we insure that sprayers and spreaders apply the proper amount of material in the field. Incorrect applications of manure or fertilizer can adversely affect the yield potential of a crop. Low applications will restrict crop yield and excessive applications will waste money and can harm the environment. The two commonly used methods of calibrating spreaders are the weight-area method and the load-area method.
Determining the square feet in an area is basic to the calibration of farm equipment. The size of an area can be determined by multiplying length X width.
Calibrating a spreader basically involves measuring the actual rate of application and then comparing it to the recommended application rate. If the actual rate is substantially more or less than the recommended rate, try changing equipment settings, or changing the ground speed of the tractor.
The load-area method of calibration is described on page 22 in the Nutrient Applicators Training Guide. Essentially in the method, the applicator needs to know the capacity of the spreader and the size of the area applied. By measuring the amount of material applied in this known area, the rate per acre of material can be calculated. The amount of total material applied is based on the weight or volume of material that was applied out of the spreader into the calibration area. An acre is equal to 43,560 square feet.
In the weight-area method, it differs from the load-area method in that the applicator has to collect material spread in the field. This can be done with pans, or plastic sheets. The applicator drives the tractor over the collection site then collects/weighs the samples. The average quantity of material collected is calculated out to a tons/acre rate. This is then compared to the recommended rate. The weight-area method is described on page 22 of the Nutrient Applicators Training Guide.
The weight-area method works well with calibrating both fertilizer spreaders and planters. This method can be used for both liquid and dry manure spreaders. Pans can be used to catch liquid manure and plastic sheets can be used to catch dry manure.
This diagram shows how pans and sheets can be arranged in a field to calibrate a spreader.
The Nutrient Applicators Training Guide has detailed examples of how to properly calibrate nutrient application equipment.
This is a lead-in slide to a discussion on liming materials and compost.
Limestone supplies calcium and magnesium. Mined calcium carbonate (CaCO3) is typically 50% oxides, which is that portion of the liming material that reacts in the soil to raise the pH. The other 50% of the material is inert. CaCO3 equivalent is the basis used for measuring the neutralizing capacity of all liming materials. Limestone comes in many different forms and grades.
Effective Neutralizing Value (E.N.V.) is a comparative value that refers to the ability of a liming material to modify soil pH within a year. The reference standard is calcium carbonate (CaCO3), where E.N.V. = 100. This means that liming materials are compared (greater than or less than) to the neutralizing ability of calcium carbonate. E.N.V. can be found on the labels of liming materials and fertilizer as an indicator of the products impact on soil pH.
The liming material label (or tag) will tell you the mesh size of the material. This will tell you how quickly the limestone will react in the soil. Good quality Ag lime will be 80% 90-100 mesh and 20% 40 mesh. The 90-100-mesh portion of the limestone will react almost immediately in the soil, while the 40-mesh portion will take 6 months to a year. This will provide a rapid and a slow release of the lime. Most Ag lime is only 1-2% magnesium oxide (MgO). This is usually fine for most soils. However there are soils that need more magnesium. In this situation, Dolomitic limestone can be applied. Ground Dolomite contains over 10% magnesium.
There are other liming agents available besides Ag lime. These materials are typically industrial byproducts. These include stack dust, sludge lime, river mud, and sugar lime. These materials usually have very soluble, rapid forms of calcium (CaO) and traces of other elements. Most of these materials work very quickly. Their percent of oxides can vary; so always ask to see an analysis of the material before calculating how much you need. These materials are much cheaper than Ag lime, but can be hard to apply.
It is essential that you know the analysis of the liming material, especially the percent oxides. The amount of material you apply will be based on your soil pH and the percent oxides of the liming material. It is not necessary to apply high magnesium lime to soils that do not need the extra magnesium. This wastes money and does not benefit the nutrient balance in the soil.
Liming material recommendations are typically based on raising the pH of the plow layer (top 9 inches of the soil) to 6.5; except for those crops requiring a higher or lower pH. In situations where the soil cannot be tilled, such as pastures and no-till crops, the liming material is surface applied annually at no more than 1,500 lb. per acre of oxides until the requirement is met. Caution should be taken when applying liming materials in or around those times that you are planning to apply nitrogen-based fertilizer, or pesticides. Limestone can react with ammonium forms of nitrogen and cause it to volatilize, and limestone will neutralize pesticides. Limestone will free up herbicides tied-up in the soil, which could injure newly germinating seedlings sensitive to that herbicide. Liming a few months in advance of seeding will help to avoid this problem.
When compost is made properly it is near pH 7 (neutral), has a carbon: nitrogen ratio of about 15:1, most of the weed seeds and disease organisms are dead, contains a well balanced supply of slow release plant nutrients, and has as much as one-quarter of its weight in micro-organisms (dead and alive).
The best composts come from piles with the highest microbial activity. Temperature is the easiest way to judge the level of microbial activity. Good composts heat to approximately 140-1600 F within the first 3 or 4 days.
The size of the particles in the compost pile is important to its success. Small particle size provides greater surface area availability to microbes, however if the particles are too small, they will pack too tightly and exclude the air necessary to good heating. Adequate volume is important as well. Piles need to be big enough to keep from cooling too rapidly. Piles 4x4x4 ft. do well.
Improperly made or unfinished composts can be harmful to plants. They can contain toxic chemicals formed in the process, or the valuable nutrient nitrogen can be tied-up. Good composts take 12-18 months to make and will have the moisture content similar to that of a squeezed sponge. The C:N ratio in the initial startup of the pile should be 30:1.
This slide shows the carbon: nitrogen ratios of some familiar materials around the farm. The higher the C:N ratio, the longer it takes to decompose, or compost.
Bad odor: not enough air, so turn the pile more frequently
Center of pile too dry: not enough water, so moisten while turning
Pile is damp &warm in center, but nowhere else: pile is too small, so collect more material and mix the old ingredients into a new pile.
Pile is damp and sweet smelling but will not heat up: lack of nitrogen, so mix in N-rich materials like fresh grass, manure, or urea.
Crop rotation provides nutrients to plants by recapturing nutrients that having moved down the soil below the root zone of most crop roots. Rotating to a deeper-rooted crop helps to capture these nutrients before they are lost. This helps the environment by preventing these nutrients from getting into groundwater. Rotating to leguminous crops helps plant fertility, since legumes fix nitrogen that benefits following crops. Using cover crops (crops not harvested) in a rotation provides benefits directly to the soil by improving soil tilth and water infiltration, and organic matter. Crop rotation is one of the best methods of pest management, as pest populations can often be kept low through alternating different species of plants. The decision to use a cover crop in the crop rotation system is difficult, since the cover crop is not harvested and there is no direct financial return.
Be sure to seek help when you are not sure about what you are doing. There are a lot of resources around to help you. Don’t be like the old farmer who told the County Agent that he didn’t need any advice. He told the Agent he has already worn out two farms and that he has his own way of doing things.