This document discusses acid soils, including their classification, formation processes, characteristics, impacts, and management. It defines acid soils as having a pH below 5.5 and lists various natural and human-induced causes of acidification like rainfall, parent material, and fertilizer use. Characteristics include low nutrient availability, aluminum toxicity, and reduced biological activity. Management involves applying lime to raise pH and supply calcium, with different lime sources and particle sizes impacting effectiveness. Crop residues and manures can also reduce acidity through mineralization reactions.
Characterisation and management of salt affected soils (1)aakvd
Salt affected soils are soils containing soluble salts that negatively impact plant growth. They are classified as saline soils containing neutral salts or alkali soils containing soluble sodium salts. Saline soils occur in arid regions due to insufficient rainfall for leaching salts out of the soil. Alkali soils form due to accumulation of soluble sodium salts that disperse soil particles. Management of salt affected soils involves physical measures like leaching and drainage, chemical amendments like gypsum, and soil management practices like basin irrigation and growing salt tolerant crops.
Unit 1 lecture-1 soil fertility and soil productivityLuxmiKantTripathi
The document discusses the concepts of soil fertility and productivity, outlining key factors that affect each such as parent material, climate, organic matter and crop management practices. It also reviews the history of understanding soil fertility from ancient Greek and Roman scholars to modern scientists who established theories of plant nutrition and developed agricultural experiments. The overall goal is for students to understand essential plant nutrients and their roles in agriculture and crop production.
This document provides an overview of integrated nutrient management (INM). It begins with introductions and headings submitted by M. Ashok Naik to Dr. P. Kavitha regarding a report on INM. It then defines INM as the optimization of all plant nutrient sources, including organic, inorganic, and biofertilizers, to maintain soil fertility and maximize crop yields. The document discusses the concepts, components, classification, and advantages of INM. It also summarizes different organic manure sources like farm yard manure, compost, vermicompost, and their composition and benefits. Finally, it provides details on brown manuring as a no-till practice for organic matter addition and weed control.
Weed indices are used to study the effect of weed density, growth, and suppression on crop plants. Common indices include weed infestation, weed index, weed control efficiency, and smothering efficiency. The document defines each of these indices and provides examples of how to calculate them. Higher values of weed control efficiency and smothering efficiency indicate better control of weeds. The weed index compares yields between treated and untreated plots, with lower values showing more effective herbicide treatment.
Fertilizer use efficiency depends on many factors related to the soil, climate, crop, and fertilizer characteristics. Only a fraction of the nutrients in fertilizer may be absorbed by crops, with the rest lost through leaching, volatilization, immobilization, or interactions between fertilizers. Maximum efficiency is obtained when the minimum amount of fertilizer needed is applied based on soil testing. Efficiency varies depending on soil properties like texture, pH, temperature, and moisture as well as the fertilizer type and application method used.
Saline, sodic, and saline-sodic soils occur when rainfall is insufficient to leach salts below the root zone, leaving soils high in salts like sodium, calcium, magnesium, chloride, and sulfate. Saline soils have high salt levels that increase osmotic pressure and reduce water availability to plants. Sodic soils have high sodium levels that disperse soil particles, reducing infiltration and root growth. Saline-sodic soils contain both high salts and sodium but remain flocculated if salt levels stay elevated; management focuses on exchanging sodium for calcium followed by leaching salts. Proper irrigation water quality and sufficient leaching are needed to manage all salt-affected soils for agriculture.
This document discusses various in-situ soil moisture conservation techniques. It introduces the topic and explains that these techniques are recommended in addition to large-scale watershed management structures to increase moisture availability for crops. The techniques aim to increase infiltration and temporarily store water at the soil surface. The document then describes several specific techniques in detail, including deep tillage, mulching, basin listing, broad-based beds and furrows, ridges and furrows, and compartmental bunding. It explains the principles and benefits of each technique for conserving soil moisture.
This document discusses acid soils, including their classification, formation processes, characteristics, impacts, and management. It defines acid soils as having a pH below 5.5 and lists various natural and human-induced causes of acidification like rainfall, parent material, and fertilizer use. Characteristics include low nutrient availability, aluminum toxicity, and reduced biological activity. Management involves applying lime to raise pH and supply calcium, with different lime sources and particle sizes impacting effectiveness. Crop residues and manures can also reduce acidity through mineralization reactions.
Characterisation and management of salt affected soils (1)aakvd
Salt affected soils are soils containing soluble salts that negatively impact plant growth. They are classified as saline soils containing neutral salts or alkali soils containing soluble sodium salts. Saline soils occur in arid regions due to insufficient rainfall for leaching salts out of the soil. Alkali soils form due to accumulation of soluble sodium salts that disperse soil particles. Management of salt affected soils involves physical measures like leaching and drainage, chemical amendments like gypsum, and soil management practices like basin irrigation and growing salt tolerant crops.
Unit 1 lecture-1 soil fertility and soil productivityLuxmiKantTripathi
The document discusses the concepts of soil fertility and productivity, outlining key factors that affect each such as parent material, climate, organic matter and crop management practices. It also reviews the history of understanding soil fertility from ancient Greek and Roman scholars to modern scientists who established theories of plant nutrition and developed agricultural experiments. The overall goal is for students to understand essential plant nutrients and their roles in agriculture and crop production.
This document provides an overview of integrated nutrient management (INM). It begins with introductions and headings submitted by M. Ashok Naik to Dr. P. Kavitha regarding a report on INM. It then defines INM as the optimization of all plant nutrient sources, including organic, inorganic, and biofertilizers, to maintain soil fertility and maximize crop yields. The document discusses the concepts, components, classification, and advantages of INM. It also summarizes different organic manure sources like farm yard manure, compost, vermicompost, and their composition and benefits. Finally, it provides details on brown manuring as a no-till practice for organic matter addition and weed control.
Weed indices are used to study the effect of weed density, growth, and suppression on crop plants. Common indices include weed infestation, weed index, weed control efficiency, and smothering efficiency. The document defines each of these indices and provides examples of how to calculate them. Higher values of weed control efficiency and smothering efficiency indicate better control of weeds. The weed index compares yields between treated and untreated plots, with lower values showing more effective herbicide treatment.
Fertilizer use efficiency depends on many factors related to the soil, climate, crop, and fertilizer characteristics. Only a fraction of the nutrients in fertilizer may be absorbed by crops, with the rest lost through leaching, volatilization, immobilization, or interactions between fertilizers. Maximum efficiency is obtained when the minimum amount of fertilizer needed is applied based on soil testing. Efficiency varies depending on soil properties like texture, pH, temperature, and moisture as well as the fertilizer type and application method used.
Saline, sodic, and saline-sodic soils occur when rainfall is insufficient to leach salts below the root zone, leaving soils high in salts like sodium, calcium, magnesium, chloride, and sulfate. Saline soils have high salt levels that increase osmotic pressure and reduce water availability to plants. Sodic soils have high sodium levels that disperse soil particles, reducing infiltration and root growth. Saline-sodic soils contain both high salts and sodium but remain flocculated if salt levels stay elevated; management focuses on exchanging sodium for calcium followed by leaching salts. Proper irrigation water quality and sufficient leaching are needed to manage all salt-affected soils for agriculture.
This document discusses various in-situ soil moisture conservation techniques. It introduces the topic and explains that these techniques are recommended in addition to large-scale watershed management structures to increase moisture availability for crops. The techniques aim to increase infiltration and temporarily store water at the soil surface. The document then describes several specific techniques in detail, including deep tillage, mulching, basin listing, broad-based beds and furrows, ridges and furrows, and compartmental bunding. It explains the principles and benefits of each technique for conserving soil moisture.
Site Specific nutrient Management for Precision Agriculture - Anjali Patel (I...Rahul Raj Tandon
Dr. V. N. Mishra is the course teacher and Anjali Patel is the speaker. The presentation discusses site specific nutrient management (SSNM), which aims to optimize nutrient supply according to differences in soil-plant systems for a particular crop in a given season. SSNM involves assessing indigenous nutrient supply from soil and crop residues, determining crop demand based on yield goals, and applying fertilizers based on those factors. Precision tools like GPS, GIS, remote sensing, and variable-rate technology help implement SSNM.
A brief study on Integrated Nutrient Management (INM). This presentation has created by me after studying many articles and research papers regarding INM. Suggestions are kindly invited.
This document discusses dryland agriculture, which refers to growing crops entirely through rainfall. It can be divided into dry farming (<750mm rainfall), dryland farming (750-1150mm rainfall), and rainfed farming (>1150mm rainfall). Dry farming occurs in arid regions and has frequent crop failures due to low and variable rainfall. Dryland farming occurs in semi-arid regions and has less frequent crop failures. Rainfed farming occurs in humid regions and has rare crop failures. The document also discusses various irrigation techniques like surface, localized, and subsurface irrigation that help supplement rainfall for crop growth.
This document discusses different types of salt-affected soils, including saline soils, sodic soils, and saline-sodic soils. It describes the properties of each soil type and methods for reclamation. Sodic soils have a high sodium content which reduces water intake, while saline soils contain water-soluble salts like chlorides and sulfates. Reclamation of saline soils involves leaching salts from the root zone through irrigation and drainage. Reclamation of sodic soils requires adding calcium amendments like gypsum to replace sodium on clay surfaces and improve soil structure and permeability. Proper drainage is also needed to manage salt levels in both soil types.
Weeds compete with crops for nutrients, moisture, space, sunlight and can release allelopathic compounds that inhibit crop growth. Weeds remove significant amounts of nutrients from the soil each season. They also transpire at higher rates than crops and can form dense canopies that shade out crops. The critical period of weed-crop competition varies by crop but is typically early in the growth cycle. Factors like weed density and species, soil fertility, moisture levels, pH, and climate can influence the intensity of competition between weeds and crops. Timely weed management is important for optimal crop yields.
This document discusses conservation agriculture in India. It notes that over 120 million hectares of land in India is degraded, including from water erosion, wind erosion, salinity, alkalinity and acidity. Conservation agriculture is presented as an alternative that can conserve natural resources by minimizing soil disturbance, maintaining soil cover, and diversifying crop species. The three principles of conservation agriculture are identified as minimum soil disturbance, permanent soil cover, and crop rotations. Benefits include improved soil structure, organic matter, and reduced erosion. Techniques discussed include zero-tillage, use of crop residues and cover crops, and machinery like the happy seeder.
Salt Affected Soils and Their ManagementDrAnandJadhav
1. The document discusses various types of problem soils including saline soils, saline-alkali soils, sodic soils, and their characteristics.
2. Saline soils contain excess neutral soluble salts like NaCl, CaCl2, MgCl2 which increase the osmotic pressure of the soil solution. Saline-alkali soils have both excess salts and alkalinity due to sodium.
3. Sodic soils have a high percentage of sodium ions that disperse clay particles and destroy the soil structure, reducing permeability and aeration. Reclamation methods include leaching salts, applying gypsum or other amendments, and growing salt-tolerant crops.
Soil crusting refers to the formation of a compact, dense layer on the surface of soil when it dries after rain or irrigation. This crust has very small pores and high density. It forms mainly in arid and semi-arid regions due to the breakdown of soil aggregates by raindrops. There are three main types of soil crusts: structural, erosion/depositional, and cryptogamic. Structural crusts form directly from the compaction of dispersed soil particles. Erosion/depositional crusts involve stripping away of upper layers. Cryptogamic crusts contain algae and fungi. Soil crusting reduces infiltration and aeration, negatively impacting plant growth. It can be prevented
This document discusses soil test crop response (STCR) studies. STCR studies determine the quantitative relationship between soil test values, crop yields, and fertilizer rates. The objectives are to study crop yield responses to soil nutrients, derive yield targeting equations, evaluate soil test methods, and determine how organic matter affects fertilizer needs. Targeted yield approaches estimate nutrient requirements for a given yield goal. STCR provides relationships between soil tests, crop yields, and allows precision in fertilizer doses based on soil conditions. Methods include gradient and test crop experiments. Yield targeting equations are meant for specific soil and climate conditions. STCR can help with precision agriculture by creating nutrient maps loaded into variable-rate fertilizer spreaders.
The document discusses the Diagnosis and Recommendation Integrated System (DRIS) method for interpreting plant tissue analysis. DRIS considers nutrient concentration ratios rather than individual elements. It measures the relative balance between nutrients using index values, with negative values indicating deficiencies. DRIS can reveal both the limiting nutrient and the order nutrients may become limiting. It identifies all nutritional factors limiting crop production to improve fertilizer recommendations and maximize yields.
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 summarizes the key points about crop residue management. It begins with definitions of crop residue and discusses the importance of crop residues as a source of organic matter and plant nutrients. It then discusses different types of crop residues including field residues and process residues. The potential uses of crop residues are outlined, including as animal feed, household purposes, composting, biofuels, and improving soil properties. Methods of recycling crop residues like surface mulching, in-situ incorporation, and composting are described. Tables show the effects of different crop residue management practices on soil physical, chemical and biological properties.
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.
Weeds can propagate and disperse through various means. They propagate sexually through seed production or asexually through vegetative structures like rhizomes, stolons, tubers, etc. Seeds and vegetative structures are then dispersed by different agents like wind, water, animals, man, and manure. This allows weeds to spread over long distances and colonize new habitats. Common dispersal mechanisms include seeds or fruits with feathers, pappus, wings, etc. that aid wind dispersal, barbs and hooks that catch on animal fur for transport, and mimicry of crop plants that results in accidental human dispersal during farming activities.
This document discusses various soil and moisture conservation techniques, which are divided into agronomic and engineering measures. Agronomic measures include conservation tillage, deep tillage, contour farming, strip cropping, mulching, and growing cover crops. These are used where land slopes are less than 2%. Engineering measures include bunding, terracing, trenching, and subsoiling, which are constructed barriers used on slopes greater than 2% to retain runoff. Broad bed furrows are also discussed as a technique using beds and furrows to store moisture and drain excess water.
Acid soil and acid sulphate soil, genesis and characteristicsMahiiKarthii
This document discusses acid soils and acid sulfate soils. It defines different levels of soil acidity and notes that about 8% of India's land area is affected by acid soils. The key causes of acid soil formation are excessive rainfall, acidic parent materials, fertilizer and organic matter decomposition, and human activities like drainage. Acid soils have light texture, low nutrient availability, and reduced biological activity. Liming can reduce acidity and aluminum toxicity. Acid sulfate soils form in coastal areas and produce sulfuric acid when drained, releasing toxic aluminum and iron. Maintaining flooding or controlling drainage helps manage acid sulfate soils.
Integrated nutrient management is an approach to optimize soil fertility and plant nutrition by using all possible sources of plant nutrients (organic and inorganic) in a balanced and efficient manner. The goals are to optimize plant production and profitability while conserving resources and improving soil quality. In conventional farming, emphasis was placed on chemical fertilizers and high yields, but this caused nutrient depletion and deterioration of soil health over time. Integrated nutrient management balances nutrient supply from organic sources like farmyard manure with inorganic fertilizers, and synchronizes nutrient availability with crop demand to maintain long-term productivity and soil function.
Calcareous soil , Origin, Properties and Distribution in India (IGKV RAIPUR ,...Rahul Raj Tandon
This document discusses calcareous soils, which contain high amounts of calcium carbonate. Calcareous soils form in both arid and humid regions through weathering of parent rocks containing calcium carbonate. They are characterized by a calcic horizon with over 15% calcium carbonate. Calcareous soils have properties like effervescing when acid is added, high pH between 7-8.5, and flocculated structure. Nutrient availability can be reduced for phosphorus, potassium and zinc due to high calcium carbonate levels. Calcareous soils are found distributed in parts of India like eastern Uttar Pradesh and north Bihar districts.
Lime requirement of acid soil, liming materials, reclamation and management o...MahiiKarthii
The document discusses lime requirement of acid soils and liming materials. It states that lime requirement is the amount of lime needed to raise the pH of an acidic soil to a desired level, as determined by the Shoemaker buffer method. Liming materials include oxides, hydroxides, carbonates, and silicates of calcium and magnesium. Examples given are limestone, dolomite, slags, and wood ash. The efficiency of liming materials depends on their purity, fineness, and neutralizing value. Liming raises the soil pH and reduces aluminum and manganese toxicity, while improving the availability of phosphorus, micronutrients, and nitrogen fixation.
This document discusses problems in forest soils and their management. It identifies physical problems such as slow permeability, excessive permeability, subsurface hardening, surface crusting, shallow soils, and waterlogging. It also identifies chemical problems including salt-affected soils, alkaline soils, saline soils, and acid soils. Management strategies are provided for each problem, such as drainage, adding organic matter or sand to change texture, liming, and selecting suitable tree species. The challenges of managing problematic forest soils are utilizing degraded lands for plantation, providing adequate nutrients, and balancing inputs with plant needs. Soil conservation is important as soil is fundamental to terrestrial ecology.
Agriculture is important for food security. Fertile soil is really needed in agriculture, however, all soil in the world is not fertile. In most areas in the world, when we grow crops we can also find some problem soil. There are many technologies on how to manage problem soil. In this ppt, you can clearly know what is problem soil and how to manage this soil.
Site Specific nutrient Management for Precision Agriculture - Anjali Patel (I...Rahul Raj Tandon
Dr. V. N. Mishra is the course teacher and Anjali Patel is the speaker. The presentation discusses site specific nutrient management (SSNM), which aims to optimize nutrient supply according to differences in soil-plant systems for a particular crop in a given season. SSNM involves assessing indigenous nutrient supply from soil and crop residues, determining crop demand based on yield goals, and applying fertilizers based on those factors. Precision tools like GPS, GIS, remote sensing, and variable-rate technology help implement SSNM.
A brief study on Integrated Nutrient Management (INM). This presentation has created by me after studying many articles and research papers regarding INM. Suggestions are kindly invited.
This document discusses dryland agriculture, which refers to growing crops entirely through rainfall. It can be divided into dry farming (<750mm rainfall), dryland farming (750-1150mm rainfall), and rainfed farming (>1150mm rainfall). Dry farming occurs in arid regions and has frequent crop failures due to low and variable rainfall. Dryland farming occurs in semi-arid regions and has less frequent crop failures. Rainfed farming occurs in humid regions and has rare crop failures. The document also discusses various irrigation techniques like surface, localized, and subsurface irrigation that help supplement rainfall for crop growth.
This document discusses different types of salt-affected soils, including saline soils, sodic soils, and saline-sodic soils. It describes the properties of each soil type and methods for reclamation. Sodic soils have a high sodium content which reduces water intake, while saline soils contain water-soluble salts like chlorides and sulfates. Reclamation of saline soils involves leaching salts from the root zone through irrigation and drainage. Reclamation of sodic soils requires adding calcium amendments like gypsum to replace sodium on clay surfaces and improve soil structure and permeability. Proper drainage is also needed to manage salt levels in both soil types.
Weeds compete with crops for nutrients, moisture, space, sunlight and can release allelopathic compounds that inhibit crop growth. Weeds remove significant amounts of nutrients from the soil each season. They also transpire at higher rates than crops and can form dense canopies that shade out crops. The critical period of weed-crop competition varies by crop but is typically early in the growth cycle. Factors like weed density and species, soil fertility, moisture levels, pH, and climate can influence the intensity of competition between weeds and crops. Timely weed management is important for optimal crop yields.
This document discusses conservation agriculture in India. It notes that over 120 million hectares of land in India is degraded, including from water erosion, wind erosion, salinity, alkalinity and acidity. Conservation agriculture is presented as an alternative that can conserve natural resources by minimizing soil disturbance, maintaining soil cover, and diversifying crop species. The three principles of conservation agriculture are identified as minimum soil disturbance, permanent soil cover, and crop rotations. Benefits include improved soil structure, organic matter, and reduced erosion. Techniques discussed include zero-tillage, use of crop residues and cover crops, and machinery like the happy seeder.
Salt Affected Soils and Their ManagementDrAnandJadhav
1. The document discusses various types of problem soils including saline soils, saline-alkali soils, sodic soils, and their characteristics.
2. Saline soils contain excess neutral soluble salts like NaCl, CaCl2, MgCl2 which increase the osmotic pressure of the soil solution. Saline-alkali soils have both excess salts and alkalinity due to sodium.
3. Sodic soils have a high percentage of sodium ions that disperse clay particles and destroy the soil structure, reducing permeability and aeration. Reclamation methods include leaching salts, applying gypsum or other amendments, and growing salt-tolerant crops.
Soil crusting refers to the formation of a compact, dense layer on the surface of soil when it dries after rain or irrigation. This crust has very small pores and high density. It forms mainly in arid and semi-arid regions due to the breakdown of soil aggregates by raindrops. There are three main types of soil crusts: structural, erosion/depositional, and cryptogamic. Structural crusts form directly from the compaction of dispersed soil particles. Erosion/depositional crusts involve stripping away of upper layers. Cryptogamic crusts contain algae and fungi. Soil crusting reduces infiltration and aeration, negatively impacting plant growth. It can be prevented
This document discusses soil test crop response (STCR) studies. STCR studies determine the quantitative relationship between soil test values, crop yields, and fertilizer rates. The objectives are to study crop yield responses to soil nutrients, derive yield targeting equations, evaluate soil test methods, and determine how organic matter affects fertilizer needs. Targeted yield approaches estimate nutrient requirements for a given yield goal. STCR provides relationships between soil tests, crop yields, and allows precision in fertilizer doses based on soil conditions. Methods include gradient and test crop experiments. Yield targeting equations are meant for specific soil and climate conditions. STCR can help with precision agriculture by creating nutrient maps loaded into variable-rate fertilizer spreaders.
The document discusses the Diagnosis and Recommendation Integrated System (DRIS) method for interpreting plant tissue analysis. DRIS considers nutrient concentration ratios rather than individual elements. It measures the relative balance between nutrients using index values, with negative values indicating deficiencies. DRIS can reveal both the limiting nutrient and the order nutrients may become limiting. It identifies all nutritional factors limiting crop production to improve fertilizer recommendations and maximize yields.
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 summarizes the key points about crop residue management. It begins with definitions of crop residue and discusses the importance of crop residues as a source of organic matter and plant nutrients. It then discusses different types of crop residues including field residues and process residues. The potential uses of crop residues are outlined, including as animal feed, household purposes, composting, biofuels, and improving soil properties. Methods of recycling crop residues like surface mulching, in-situ incorporation, and composting are described. Tables show the effects of different crop residue management practices on soil physical, chemical and biological properties.
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.
Weeds can propagate and disperse through various means. They propagate sexually through seed production or asexually through vegetative structures like rhizomes, stolons, tubers, etc. Seeds and vegetative structures are then dispersed by different agents like wind, water, animals, man, and manure. This allows weeds to spread over long distances and colonize new habitats. Common dispersal mechanisms include seeds or fruits with feathers, pappus, wings, etc. that aid wind dispersal, barbs and hooks that catch on animal fur for transport, and mimicry of crop plants that results in accidental human dispersal during farming activities.
This document discusses various soil and moisture conservation techniques, which are divided into agronomic and engineering measures. Agronomic measures include conservation tillage, deep tillage, contour farming, strip cropping, mulching, and growing cover crops. These are used where land slopes are less than 2%. Engineering measures include bunding, terracing, trenching, and subsoiling, which are constructed barriers used on slopes greater than 2% to retain runoff. Broad bed furrows are also discussed as a technique using beds and furrows to store moisture and drain excess water.
Acid soil and acid sulphate soil, genesis and characteristicsMahiiKarthii
This document discusses acid soils and acid sulfate soils. It defines different levels of soil acidity and notes that about 8% of India's land area is affected by acid soils. The key causes of acid soil formation are excessive rainfall, acidic parent materials, fertilizer and organic matter decomposition, and human activities like drainage. Acid soils have light texture, low nutrient availability, and reduced biological activity. Liming can reduce acidity and aluminum toxicity. Acid sulfate soils form in coastal areas and produce sulfuric acid when drained, releasing toxic aluminum and iron. Maintaining flooding or controlling drainage helps manage acid sulfate soils.
Integrated nutrient management is an approach to optimize soil fertility and plant nutrition by using all possible sources of plant nutrients (organic and inorganic) in a balanced and efficient manner. The goals are to optimize plant production and profitability while conserving resources and improving soil quality. In conventional farming, emphasis was placed on chemical fertilizers and high yields, but this caused nutrient depletion and deterioration of soil health over time. Integrated nutrient management balances nutrient supply from organic sources like farmyard manure with inorganic fertilizers, and synchronizes nutrient availability with crop demand to maintain long-term productivity and soil function.
Calcareous soil , Origin, Properties and Distribution in India (IGKV RAIPUR ,...Rahul Raj Tandon
This document discusses calcareous soils, which contain high amounts of calcium carbonate. Calcareous soils form in both arid and humid regions through weathering of parent rocks containing calcium carbonate. They are characterized by a calcic horizon with over 15% calcium carbonate. Calcareous soils have properties like effervescing when acid is added, high pH between 7-8.5, and flocculated structure. Nutrient availability can be reduced for phosphorus, potassium and zinc due to high calcium carbonate levels. Calcareous soils are found distributed in parts of India like eastern Uttar Pradesh and north Bihar districts.
Lime requirement of acid soil, liming materials, reclamation and management o...MahiiKarthii
The document discusses lime requirement of acid soils and liming materials. It states that lime requirement is the amount of lime needed to raise the pH of an acidic soil to a desired level, as determined by the Shoemaker buffer method. Liming materials include oxides, hydroxides, carbonates, and silicates of calcium and magnesium. Examples given are limestone, dolomite, slags, and wood ash. The efficiency of liming materials depends on their purity, fineness, and neutralizing value. Liming raises the soil pH and reduces aluminum and manganese toxicity, while improving the availability of phosphorus, micronutrients, and nitrogen fixation.
This document discusses problems in forest soils and their management. It identifies physical problems such as slow permeability, excessive permeability, subsurface hardening, surface crusting, shallow soils, and waterlogging. It also identifies chemical problems including salt-affected soils, alkaline soils, saline soils, and acid soils. Management strategies are provided for each problem, such as drainage, adding organic matter or sand to change texture, liming, and selecting suitable tree species. The challenges of managing problematic forest soils are utilizing degraded lands for plantation, providing adequate nutrients, and balancing inputs with plant needs. Soil conservation is important as soil is fundamental to terrestrial ecology.
Agriculture is important for food security. Fertile soil is really needed in agriculture, however, all soil in the world is not fertile. In most areas in the world, when we grow crops we can also find some problem soil. There are many technologies on how to manage problem soil. In this ppt, you can clearly know what is problem soil and how to manage this soil.
This document discusses different types of problem soils and their management. There are 4 main categories of problem soils - physical, chemical, biological, and nutritional. Some specific problem soil types discussed include slow permeable soils, soil surface crusting, subsoil hard pans, shallow soils, highly permeable soils, heavy clay soils, and fluffy paddy soils. Management strategies aim to improve soil structure and properties through measures like organic matter addition, drainage, tillage practices, and amendments.
The document discusses usar (sodic and saline) lands, which are soils affected by high levels of salts. Usar lands are found in India and other parts of the world with dry climates and poor drainage. They form due to processes like irrigation, which leaves salts behind, and capillary action, which brings salts to the surface. Usar lands are difficult to cultivate but can be reclaimed through drainage improvements, adding amendments like gypsum to replace sodium ions, and growing salt-tolerant crops. Proper management of irrigation and fertilization is also needed for productive use of these soils.
This document discusses improving fodder productivity on gochar (grazing) lands in arid regions of Rajasthan to support sustainable livestock production. It notes that gochar lands face degradation from overgrazing, lack of vegetation, and encroachment. It proposes forming village committees to inventory lands, develop restoration plans including fencing, field preparation, and sowing drought-resistant Cenchrus grass species. With proper sowing and rainwater harvesting techniques, grass coverage and 2-3 cuttings of 4-5 tons of dry fodder per hectare can be achieved annually to support the large and important livestock populations in the region.
This document summarizes different types of problematic soils, including their causes and solutions. There are two main types - chemical soils like acidic, saline, sodic, and alkaline soils which form due to chemical imbalances, and physical soils with issues like hard pans, waterlogging, and dispersion. Solutions include adding lime to acidic soil, leaching salts from saline soil, changing plant varieties for sodic soil, and installing drainage for waterlogged soils. The document provides details on the characteristics and remediation approaches for each problematic soil type.
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.
This document provides an overview of soil and water management topics including soil physical properties, erosion control, and residue management. It discusses key soil properties like texture, structure, bulk density and their effects. Texture is determined by sand, silt and clay content and affects properties like aeration and water retention. The Universal Soil Loss Equation is presented as a tool to calculate soil erosion based on rainfall, soil erodibility and management factors. Conservation practices to control erosion include crop rotation, residue management, contouring, grassed waterways and terraces. Proper soil and water management is important for soil health, water quality and agricultural productivity.
The document discusses developing soil health interpretations from soil survey data. It explains that soil interpretations make soil data more useful by predicting soil behavior for different land uses. Developing interpretations involves defining the activity, identifying relevant soil properties and site features, assigning rating classes, and backing them with research. The document provides examples of interpretations for soil organic carbon storage potential, earthworm habitat suitability, and high tunnel suitability. It emphasizes that new interpretations can extend the use of existing soil data and help assess dynamic soil properties related to soil health.
This document discusses soil water systems and properties. It defines key terms like field capacity, permanent wilting point, and available water. Soil water can exist as gravitational, capillary, or hygroscopic water. The water holding capacities of soils are expressed as constants like saturation capacity, field capacity, and permanent wilting point. These constants can be expressed as either percentages of water held or depth of water stored in the root zone. Plants extract most water from the upper layers of their root zone, with uptake decreasing with depth.
This document discusses soil conservation in Pakistan. It begins by defining soil and describing Pakistan's soil inventory. It then discusses land capability classes and current land use trends. Some major soil problems in Pakistan are identified as water erosion, wind erosion, salinity, waterlogging, and nutrient deficiencies. Strategies are suggested to address each problem, such as protecting vegetation, controlling grazing, improving drainage, using balanced fertilizers, and protecting agricultural land from urban expansion.
This document discusses soil erosion and methods to prevent it. It begins by defining soil and describing the different types of soil degradation, including physical, chemical, and biological degradation. It then focuses on soil erosion, describing it as the movement of soil particles from their original site via agents like water, wind, ice, and human activity. The main types of water erosion are then outlined, including splash erosion, sheet erosion, rill erosion, gully erosion, stream bank erosion, and shore erosion. Causes of erosion like deforestation and overgrazing are also listed. The document concludes by describing various biological and agronomic methods that can be used to prevent erosion, such as contour farming, strip cropping, intercro
Ground Improvement of Dune Sand Fields For The Purpose of Moisture RetentionIJERA Editor
Plant growth depends on the use of two important natural resources, soil and water. Soil provides the mechanical and nutrient support necessary for plant growth. Water is the major input for the growth and development of all types of plants. The availability of water, its movement and its retention are governed by the properties of soil. The properties like bulk density, mechanical composition, hydraulic conductivity etc depends on the nature and formation of soil and land use characteristics in addition to the weathering processes and the geological formations. Effective management of the resources for crop production requires the need to understand relationship between soil, water and plants. Study of soil and its water holding capacity is essential for the efficient utilization of irrigation water. Hence identification of geotechnical parameters which influences the water retention capacity and the method of adding admixtures to improve the retention capacity play an important role in Irrigation Engineering. This Paper aims to focuses on improving moisture retention of soil by addition of bentonite clay and experimental analysis for monitoring the variation of moisture retention.
IOSR Journal of Pharmacy (IOSRPHR), www.iosrphr.org, call for paper, research...iosrphr_editor
Sand mining can have negative environmental consequences if not properly regulated. The analyzed soil from mined areas in India and Malaysia showed elevated levels of heavy metals that exceeded permissible limits, indicating pollution from mining activities. Mining changes soil properties like infiltration rate and nutrient levels, and destroys habitat. Reclamation strategies like planting trees and adding amendments can help restore soil fertility but may not fully mitigate ecological damage from sand and soil mining.
The document describes various soil properties including physical, chemical, and biological characteristics. It defines key terms like texture, structure, topsoil, and discusses how soil type influences factors such as drainage, compaction, and crop selection. The document also examines soil mixtures, describing homogenous mixtures as containing one soil particle type, while heterogeneous mixtures contain different particle types.
The document describes various soil properties including physical, chemical, and biological characteristics. It defines key terms like texture, structure, topsoil, and discusses how soil type influences factors like drainage, compaction, and crop selection. The document also examines soil mixtures, describing homogenous mixtures as containing one soil particle type, while heterogeneous mixtures contain different particle types.
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Similar to Soil physical constraints – slow permeable, excessively permeable soils and fluffy paddy soils characteristics and management (20)
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photon flux threshold of approximately 2 × 10−8 photons cm−2
s
−1
. The X-ray sources exhibit a highly concentrated spatial distribution,
with 1075 sources located within the central 1 arcmin. We have successfully detected X-ray emissions from 126 out of the 166 known
massive stars of the cluster, and we have collected over 71 000 photons from the magnetar CXO J164710.20-455217.
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Assuming spherical symmetry and weak field, it is shown that if one solves the Poisson equation or the Einstein field
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The use of Nauplii and metanauplii artemia in aquaculture (brine shrimp).pptxMAGOTI ERNEST
Although Artemia has been known to man for centuries, its use as a food for the culture of larval organisms apparently began only in the 1930s, when several investigators found that it made an excellent food for newly hatched fish larvae (Litvinenko et al., 2023). As aquaculture developed in the 1960s and ‘70s, the use of Artemia also became more widespread, due both to its convenience and to its nutritional value for larval organisms (Arenas-Pardo et al., 2024). The fact that Artemia dormant cysts can be stored for long periods in cans, and then used as an off-the-shelf food requiring only 24 h of incubation makes them the most convenient, least labor-intensive, live food available for aquaculture (Sorgeloos & Roubach, 2021). The nutritional value of Artemia, especially for marine organisms, is not constant, but varies both geographically and temporally. During the last decade, however, both the causes of Artemia nutritional variability and methods to improve poorquality Artemia have been identified (Loufi et al., 2024).
Brine shrimp (Artemia spp.) are used in marine aquaculture worldwide. Annually, more than 2,000 metric tons of dry cysts are used for cultivation of fish, crustacean, and shellfish larva. Brine shrimp are important to aquaculture because newly hatched brine shrimp nauplii (larvae) provide a food source for many fish fry (Mozanzadeh et al., 2021). Culture and harvesting of brine shrimp eggs represents another aspect of the aquaculture industry. Nauplii and metanauplii of Artemia, commonly known as brine shrimp, play a crucial role in aquaculture due to their nutritional value and suitability as live feed for many aquatic species, particularly in larval stages (Sorgeloos & Roubach, 2021).
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Soil physical constraints – slow permeable, excessively permeable soils and fluffy paddy soils characteristics and management
1. Soil physical constraints – slow
permeable, excessively
permeable soils and fluffy
paddy soils - Characteristics
and management
K. Maheshwaran,Asst. Prof. (SS&AC)
Sethu Bhaskara Agricultural College &
Research Foundation
SAC 202 Problematic soil and their management (2+0)
2. An optimum physical environment of soils is
essential for better growth of plants,
consequently for better yields
Based on soils physical properties viz., infiltration,
bulk density, hydraulic conductivity, porosity (capillary
and non capillary, aggregates stability etc.)
Soil physical constraints
3. I. Slow permeable soils
II. Excessively permeable soils
III. Subsoil hardening
IV. Surface crusting
V. Fluffy paddy soils
VI. Shallow
Soil physical constraints
4. Infiltration rates less than 6 cm/day due to high
clay content of the soil
Due to low infiltration rates, the amount of
water entering the soil profile is reduced thus
increasing run-off
Encourages erosion of surface soil leading to
nutrient removal in the running water
Heavy clay content, the capillary porosity is
relatively high resulting in impeded drainage and
reduced soil conditions.
Slowly permeable soils
5. It also induces nutrient fixation in the clay
complex thereby making the nutrient
unavailable to crops
leading to deficiency of nutrients
Such soils are spread over Tamil Nadu in an area
of 7,54,631 has, which is 7.5% of total
geographical area.
Slowly permeable soils
7. Management
Provision of drainage facilities
Forming contour and compartmental bunding
to increase the infiltration rates of soils
Application of huge quantities of river sand or
red soils of coarser texture to reduce the
heaviness of the soil
Application of liberal doses of organic manures
Slowly permeable soils
8. Adopting ridges and furrows, raised beds, broad
bed and furrow systems
Application of soil conditioners like H-
concentrate, Vermiculite, Jalasakti etc to reduce
run-off and soil erosion
Slowly permeable soils
9. Excessively permeable soils are soils with high
amount of Sand (>70 %)
Soils are inert and unable to retain nutrient and
water
Due to low retaining capacity of the soils, the
fertilizer nutrients are also lost in the drainage
water
These soils are spread over 86 ha in Tamil Nadu
(23.97% of total geographic area)
Excessively Permeable Soils
11. Management
Compacting the field with 400kg stone roller
(tar drum filled with 400 kg of sand or stones
can also be used) 8-10 times at optimum
moisture conditions
Application of clay soil up to a level 100 t ha-1
based on the severity of the problem and
availability of clay materials
Excessively Permeable Soils
12. Application of organic materials like farm yard
manure, compost, press mud, sugar factory
slurry, composted coir pith, sewage sludge etc
Providing asphalt sheet, polythene sheets etc.
below the soil surface to reduce the infiltration
rate
Crop rotation with green manure crops like
Sunhemp,Sesbania, daincha, kolinchi etc.
Excessively Permeable Soils
13. The traditional method of preparing the soil for
transplanting rice consists of puddling
Which substantially breaks soil aggregates into a
uniform structure-less mass
Under continuous flooding for rice cultivation
in a cropping sequence of rice-rice-rice, the soil
mechanical strength is lost leading to the
fluffiness of the soils
About 25, 919 ha (0.26% TGA) in Tamil Nadu
have this problem
Fluffy paddy soils
15. Management
The irrigation should be stopped 10 days before
the harvest of rice crop
After the harvest of rice compact the field by
passing 400 kg stone roller or an tar drum filled
with 400 kg of sand for 8 times
The usual preparatory cultivation is carried out
after compaction
Fluffy paddy soils