This document provides information about different types of soils. It begins with introducing the topic of soil geography and defining what soil is. It then discusses several key components that make up soil, such as mineral particles, air, water, organic matter, and texture. The document also examines different types of soils like black soil, red soil, laterite soil, desert soil, mountain soil, and saline/alkaline soils. It provides details on the composition, characteristics, and geographical distribution of each soil type. Finally, the document concludes with introducing the branches of soil sciences including pedology, edaphology, and soil geography.
This document discusses soil erosion, its causes, impacts, and potential solutions. Some key points:
- Soil erosion is caused by factors like deforestation, wind, and water, which can wash away topsoil and nutrients. Deforestation is a major driver as it removes vegetation that anchors soil.
- Impacts of erosion include decreased soil quality and crop yields, increased production costs, water pollution, and flooding due to sedimentation. Eroded soil may deposit downstream and damage habitats.
- About 38% of the world's cropland is degraded and 15% of total land area has been degraded by human activities like poor farming practices, accelerating the loss of fertile topsoil.
This document discusses biological weathering, which is the breakdown of rocks and other materials caused by living organisms. It occurs through both mechanical and chemical means as organisms interact with rocks. The main causes of biological weathering are: 1) man and animals through activities like construction and burrowing; 2) higher plants and their roots, which can penetrate cracks and exert disruptive force; 3) microorganisms like bacteria, fungi, and mosses that extract nutrients and produce compounds aiding decomposition. An advantage is that biological weathering creates nutrient-rich soil allowing plant growth, though it can also cause rock instability.
This document provides an overview of soil, including its definition, formation, profile, components, types, properties, and human impacts. It defines soil as the organic and inorganic material on the surface of the earth that provides the medium for plant growth. The key factors that influence soil formation are climate, parent material, topography, biota, and time. The four main soil components are minerals, air, water, and organic material. Common soil types include sand, silt, clay and loam. Human activities like erosion, desertification, acidification, deforestation, and salinization can degrade soils.
Soil is the upper layer of earth that plants grow in and is made up of weathered rock, minerals, organic matter, water and air. It forms through geological and biological processes over long periods of time. Soil supports plant growth by providing nutrients, water and oxygen to roots and is vital for sustaining life on Earth.
Chemistry of Soil. Layer composition factors etcmiraronald16
Soil is a complex mixture of minerals, organic matter, air and water that forms from the weathering of rock and decay of organic material. Soil chemistry focuses on chemical reactions in soil and the fate of contaminants and nutrients, allowing scientists to monitor pollution effects. Soil formation is influenced by climate, organisms, topography, the underlying parent material, and time. These factors work together over long periods to break down parent material and produce distinct soil layers with varying compositions.
This document provides information about different types of soils. It begins with introducing the topic of soil geography and defining what soil is. It then discusses several key components that make up soil, such as mineral particles, air, water, organic matter, and texture. The document also examines different types of soils like black soil, red soil, laterite soil, desert soil, mountain soil, and saline/alkaline soils. It provides details on the composition, characteristics, and geographical distribution of each soil type. Finally, the document concludes with introducing the branches of soil sciences including pedology, edaphology, and soil geography.
This document discusses soil erosion, its causes, impacts, and potential solutions. Some key points:
- Soil erosion is caused by factors like deforestation, wind, and water, which can wash away topsoil and nutrients. Deforestation is a major driver as it removes vegetation that anchors soil.
- Impacts of erosion include decreased soil quality and crop yields, increased production costs, water pollution, and flooding due to sedimentation. Eroded soil may deposit downstream and damage habitats.
- About 38% of the world's cropland is degraded and 15% of total land area has been degraded by human activities like poor farming practices, accelerating the loss of fertile topsoil.
This document discusses biological weathering, which is the breakdown of rocks and other materials caused by living organisms. It occurs through both mechanical and chemical means as organisms interact with rocks. The main causes of biological weathering are: 1) man and animals through activities like construction and burrowing; 2) higher plants and their roots, which can penetrate cracks and exert disruptive force; 3) microorganisms like bacteria, fungi, and mosses that extract nutrients and produce compounds aiding decomposition. An advantage is that biological weathering creates nutrient-rich soil allowing plant growth, though it can also cause rock instability.
This document provides an overview of soil, including its definition, formation, profile, components, types, properties, and human impacts. It defines soil as the organic and inorganic material on the surface of the earth that provides the medium for plant growth. The key factors that influence soil formation are climate, parent material, topography, biota, and time. The four main soil components are minerals, air, water, and organic material. Common soil types include sand, silt, clay and loam. Human activities like erosion, desertification, acidification, deforestation, and salinization can degrade soils.
Soil is the upper layer of earth that plants grow in and is made up of weathered rock, minerals, organic matter, water and air. It forms through geological and biological processes over long periods of time. Soil supports plant growth by providing nutrients, water and oxygen to roots and is vital for sustaining life on Earth.
Chemistry of Soil. Layer composition factors etcmiraronald16
Soil is a complex mixture of minerals, organic matter, air and water that forms from the weathering of rock and decay of organic material. Soil chemistry focuses on chemical reactions in soil and the fate of contaminants and nutrients, allowing scientists to monitor pollution effects. Soil formation is influenced by climate, organisms, topography, the underlying parent material, and time. These factors work together over long periods to break down parent material and produce distinct soil layers with varying compositions.
The efficient fertilizer the efficient fertilizers guide Selected Paper By Al...Mr.Allah Dad Khan
The document summarizes key aspects of soil composition and properties. It describes the different soil horizons from the A horizon at the surface to the C horizon at the deepest level. It explains how soil texture is classified based on the percentage of sand, silt and clay. Important soil properties discussed include structure, color, organisms, cation exchange capacity, and nitrogen fixation by different crops.
Soil is formed by the weathering of rocks into particles and humus from decaying plants and animals. Different types of soil like clay, sand, and loam contain various sizes of rock particles and amounts of humus that determine their suitability for agriculture. Modern farming utilizes machinery, fertilizers, irrigation, and crop rotation to replenish nutrients in soil and maximize its productivity, supporting a high standard of living.
SOIL – relatively thin surface layer of the Earth’s crust consisting of mineral and organic matter tha is affected by agents such as weather, wind, water, and organisms.
Natural resource.
This document provides information about soil including its definition, composition, formation, and importance. It defines soil as a complex mixture of minerals, organic matter, water, and air that supports life on Earth. Soil is formed over long periods of time through the weathering of rock and interaction with climate and living organisms. It is composed of layers or horizons that develop distinct properties. Soil performs vital functions like sustaining plant and animal life, regulating water flow, filtering pollutants, storing nutrients, and providing structural support. Soil science studies soil as a living ecosystem and its role in agriculture, the environment, and supporting human civilization.
This document provides information about soil in three sentences or less:
The document discusses what soil is, how it is formed through weathering of parent materials and accumulation of organic matter, and defines important terms like soil profile, texture, structure, density and porosity. Key points include that soil has four important functions, is formed through weathering processes over time, and can be classified based on its texture, structure, and other characteristics.
Soil is composed of minerals, organic matter, water and air. It supports plant growth by providing structure, water, air, nutrients and regulating temperatures. The three main types of soil are sandy soil, loamy soil, and clay soil. Sandy soil drains well but lacks nutrients, clay soil retains nutrients and water well but drains poorly, and loamy soil has a good balance. Plants require 17 essential nutrients which are classified as macronutrients or micronutrients based on their abundance. Deficiency symptoms vary by nutrient but include stunted growth, leaf discoloration, and reduced yields. Inorganic fertilizers are added to soils to supply nutrients and are classified as straight or complex based on the number of nutrients
This document provides an introduction to soil biology for students. It defines key terms like soil and dirt, and explains the five factors that influence soil formation: climate, organisms, relief, parental material, and time. It describes the different layers that make up a soil profile. The document also discusses the microbes, fungi, and animals that live in soil and their roles in decomposition and nutrient cycling. Students will learn about these topics over three weeks, including a 1.5 hour test and 2 hour practical.
The document discusses the components and properties of soil. It describes the origins of soil parent material as being residual, transported, or cumulose. Soil develops layers over time from weathering of parent materials. Soil consists of solids, liquids, and gases, with mineral matter, organic matter, water, and air making up its volume. Key properties of soil discussed include color, texture, structure, consistence, and fertility/productivity. Texture refers to particle size and affects water holding and workability. Structure and consistence influence aeration and drainage.
Soil is formed through the weathering of rock and organic processes. It is composed of weathered rock particles, water, air, and organic matter. The type of soil that forms depends on the underlying rock type, climate, landforms, plant life, and soil organisms. Soil develops in horizontal layers called horizons, with the A horizon at the top containing more organic matter and the C horizon at the bottom containing larger rock particles. Climate, landforms, and the activities of organisms like plants, microbes, earthworms, and animals influence the characteristics of different soils.
The document summarizes key topics about weathering and soil formation:
- Weathering breaks down rocks into sediment through mechanical and chemical processes. Mechanical weathering doesn't change the rock's chemistry while chemical weathering does.
- Soil forms over thousands of years as rocks weather and organic matter decays. Soil profiles have distinct A, B, and C horizons with varying properties.
- Human activities like removing vegetation can disrupt the natural balance between soil production and erosion, degrading soil quality over time if erosion isn't controlled. Contour farming, terracing, and no-till methods help reduce erosion.
This document discusses soil formation and composition. It states that soil is formed from weathered rock and mineral particles through chemical and environmental processes like weathering and erosion. Key factors that influence soil formation are parent material, climate, topography, biological activity, and time. The document describes various soil layers and horizons that form as a result of these processes, and notes that soil composition and type can vary significantly depending on location.
Land covers 29% of the Earth's surface and supports human activities like agriculture. Large parts of land are uninhabitable due to factors like topography, climate, and forests/deserts. Land is classified based on physical factors like topography and climate as well as human factors like population and land use policies. In India, 30% of total land area is mountainous, 27% is plateaus, and 43% is plains. Soil conservation aims to prevent soil erosion and degradation through practices like crop rotation, cover crops, windbreaks, and runoff control.
Soil biological properties reflect how well soil supports life. Active carbon indicates readily available food for microbes. Soil enzymes catalyze biochemical reactions. Nitrogen fixation converts nitrogen gas to plant-usable forms via bacteria. Microorganisms play roles in soil formation, structure, fertility, and nutrient cycling. Respiration releases carbon dioxide from biological activity. Biofertilizers contain microbes that increase soil fertility. Soil organic matter improves nutrient storage and retention while allowing minerals to decompose. Earthworms and nematodes contribute to soil structure and nutrient availability.
Soil is essential for agriculture as it provides anchorage and nutrients for plant growth to produce food, clothing, and shelter. Soil is made up of different layers and contains decomposing organic matter called humus. Soil is formed through the weathering of rocks by wind, water, and climate and provides many uses beyond agriculture including building materials, pottery, cosmetics, and medicine. Proper management is needed to prevent soil contamination from industrial or agricultural pollution.
11 29 2017 the ground beneath my feet save soilaalleyne
Here are three ways to conserve soil:
1. Plant cover crops or leave plant residue on top of soil to prevent erosion from wind and water. Plant roots and above-ground matter hold soil in place.
2. Practice no-till or minimum tillage farming techniques to limit soil disturbance from tilling or plowing. This preserves soil structure and prevents erosion.
3. Leave buffer strips along waterways and avoid overgrazing or over-application of fertilizers/pesticides. This helps maintain soil nutrients and protects soil from running off into water sources.
This document discusses how volcanoes can affect the lifespan of Earth. Volcanic eruptions can reform surrounding landscapes by enriching soils with ash and mineral deposits over time. This improves the land for agriculture as soils become very nutrient-rich. While individual volcanoes only last a short period of geologic time, their cumulative effects over billions of years through soil enrichment and landscape changes have significantly impacted Earth's long-term development and sustainability of life.
Soil is a loose covering of broken rocky material and decaying organic matter that overlies Earth's bedrock surface. It is comprised of minerals, organic matter, air and water and is formed over long periods of time. Soil is a renewable resource that provides nutrients for plant growth, acts as a water filter and storage system, and helps decompose wastes. Soil degradation can occur through processes like erosion, desertification, and compaction, decreasing its ability to support life.
The Physical Properties of the Soil
Inckuding,
1. Soil Texture
2. Soil Structure
3. Soil Color
4. Soil Density
5. Soil Porosity
6. Soil Consistence
7. Soil Temperature
Soil is the thin layer of material on Earth's surface that supports plant growth and provides nutrients. It is formed over thousands of years from weathered rock and organic materials. There are many different soil types worldwide based on factors like climate, topography, and biology. Soil is a non-renewable resource that is important for food production, water regulation, and carbon storage, yet a third of soils are degraded. Maintaining soil health through sustainable management practices is crucial for food security and the environment.
The efficient fertilizer the efficient fertilizers guide Selected Paper By Al...Mr.Allah Dad Khan
The document summarizes key aspects of soil composition and properties. It describes the different soil horizons from the A horizon at the surface to the C horizon at the deepest level. It explains how soil texture is classified based on the percentage of sand, silt and clay. Important soil properties discussed include structure, color, organisms, cation exchange capacity, and nitrogen fixation by different crops.
Soil is formed by the weathering of rocks into particles and humus from decaying plants and animals. Different types of soil like clay, sand, and loam contain various sizes of rock particles and amounts of humus that determine their suitability for agriculture. Modern farming utilizes machinery, fertilizers, irrigation, and crop rotation to replenish nutrients in soil and maximize its productivity, supporting a high standard of living.
SOIL – relatively thin surface layer of the Earth’s crust consisting of mineral and organic matter tha is affected by agents such as weather, wind, water, and organisms.
Natural resource.
This document provides information about soil including its definition, composition, formation, and importance. It defines soil as a complex mixture of minerals, organic matter, water, and air that supports life on Earth. Soil is formed over long periods of time through the weathering of rock and interaction with climate and living organisms. It is composed of layers or horizons that develop distinct properties. Soil performs vital functions like sustaining plant and animal life, regulating water flow, filtering pollutants, storing nutrients, and providing structural support. Soil science studies soil as a living ecosystem and its role in agriculture, the environment, and supporting human civilization.
This document provides information about soil in three sentences or less:
The document discusses what soil is, how it is formed through weathering of parent materials and accumulation of organic matter, and defines important terms like soil profile, texture, structure, density and porosity. Key points include that soil has four important functions, is formed through weathering processes over time, and can be classified based on its texture, structure, and other characteristics.
Soil is composed of minerals, organic matter, water and air. It supports plant growth by providing structure, water, air, nutrients and regulating temperatures. The three main types of soil are sandy soil, loamy soil, and clay soil. Sandy soil drains well but lacks nutrients, clay soil retains nutrients and water well but drains poorly, and loamy soil has a good balance. Plants require 17 essential nutrients which are classified as macronutrients or micronutrients based on their abundance. Deficiency symptoms vary by nutrient but include stunted growth, leaf discoloration, and reduced yields. Inorganic fertilizers are added to soils to supply nutrients and are classified as straight or complex based on the number of nutrients
This document provides an introduction to soil biology for students. It defines key terms like soil and dirt, and explains the five factors that influence soil formation: climate, organisms, relief, parental material, and time. It describes the different layers that make up a soil profile. The document also discusses the microbes, fungi, and animals that live in soil and their roles in decomposition and nutrient cycling. Students will learn about these topics over three weeks, including a 1.5 hour test and 2 hour practical.
The document discusses the components and properties of soil. It describes the origins of soil parent material as being residual, transported, or cumulose. Soil develops layers over time from weathering of parent materials. Soil consists of solids, liquids, and gases, with mineral matter, organic matter, water, and air making up its volume. Key properties of soil discussed include color, texture, structure, consistence, and fertility/productivity. Texture refers to particle size and affects water holding and workability. Structure and consistence influence aeration and drainage.
Soil is formed through the weathering of rock and organic processes. It is composed of weathered rock particles, water, air, and organic matter. The type of soil that forms depends on the underlying rock type, climate, landforms, plant life, and soil organisms. Soil develops in horizontal layers called horizons, with the A horizon at the top containing more organic matter and the C horizon at the bottom containing larger rock particles. Climate, landforms, and the activities of organisms like plants, microbes, earthworms, and animals influence the characteristics of different soils.
The document summarizes key topics about weathering and soil formation:
- Weathering breaks down rocks into sediment through mechanical and chemical processes. Mechanical weathering doesn't change the rock's chemistry while chemical weathering does.
- Soil forms over thousands of years as rocks weather and organic matter decays. Soil profiles have distinct A, B, and C horizons with varying properties.
- Human activities like removing vegetation can disrupt the natural balance between soil production and erosion, degrading soil quality over time if erosion isn't controlled. Contour farming, terracing, and no-till methods help reduce erosion.
This document discusses soil formation and composition. It states that soil is formed from weathered rock and mineral particles through chemical and environmental processes like weathering and erosion. Key factors that influence soil formation are parent material, climate, topography, biological activity, and time. The document describes various soil layers and horizons that form as a result of these processes, and notes that soil composition and type can vary significantly depending on location.
Land covers 29% of the Earth's surface and supports human activities like agriculture. Large parts of land are uninhabitable due to factors like topography, climate, and forests/deserts. Land is classified based on physical factors like topography and climate as well as human factors like population and land use policies. In India, 30% of total land area is mountainous, 27% is plateaus, and 43% is plains. Soil conservation aims to prevent soil erosion and degradation through practices like crop rotation, cover crops, windbreaks, and runoff control.
Soil biological properties reflect how well soil supports life. Active carbon indicates readily available food for microbes. Soil enzymes catalyze biochemical reactions. Nitrogen fixation converts nitrogen gas to plant-usable forms via bacteria. Microorganisms play roles in soil formation, structure, fertility, and nutrient cycling. Respiration releases carbon dioxide from biological activity. Biofertilizers contain microbes that increase soil fertility. Soil organic matter improves nutrient storage and retention while allowing minerals to decompose. Earthworms and nematodes contribute to soil structure and nutrient availability.
Soil is essential for agriculture as it provides anchorage and nutrients for plant growth to produce food, clothing, and shelter. Soil is made up of different layers and contains decomposing organic matter called humus. Soil is formed through the weathering of rocks by wind, water, and climate and provides many uses beyond agriculture including building materials, pottery, cosmetics, and medicine. Proper management is needed to prevent soil contamination from industrial or agricultural pollution.
11 29 2017 the ground beneath my feet save soilaalleyne
Here are three ways to conserve soil:
1. Plant cover crops or leave plant residue on top of soil to prevent erosion from wind and water. Plant roots and above-ground matter hold soil in place.
2. Practice no-till or minimum tillage farming techniques to limit soil disturbance from tilling or plowing. This preserves soil structure and prevents erosion.
3. Leave buffer strips along waterways and avoid overgrazing or over-application of fertilizers/pesticides. This helps maintain soil nutrients and protects soil from running off into water sources.
This document discusses how volcanoes can affect the lifespan of Earth. Volcanic eruptions can reform surrounding landscapes by enriching soils with ash and mineral deposits over time. This improves the land for agriculture as soils become very nutrient-rich. While individual volcanoes only last a short period of geologic time, their cumulative effects over billions of years through soil enrichment and landscape changes have significantly impacted Earth's long-term development and sustainability of life.
Soil is a loose covering of broken rocky material and decaying organic matter that overlies Earth's bedrock surface. It is comprised of minerals, organic matter, air and water and is formed over long periods of time. Soil is a renewable resource that provides nutrients for plant growth, acts as a water filter and storage system, and helps decompose wastes. Soil degradation can occur through processes like erosion, desertification, and compaction, decreasing its ability to support life.
The Physical Properties of the Soil
Inckuding,
1. Soil Texture
2. Soil Structure
3. Soil Color
4. Soil Density
5. Soil Porosity
6. Soil Consistence
7. Soil Temperature
Soil is the thin layer of material on Earth's surface that supports plant growth and provides nutrients. It is formed over thousands of years from weathered rock and organic materials. There are many different soil types worldwide based on factors like climate, topography, and biology. Soil is a non-renewable resource that is important for food production, water regulation, and carbon storage, yet a third of soils are degraded. Maintaining soil health through sustainable management practices is crucial for food security and the environment.
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2. Define the conceptual terms soil,
land and minerals; and
Identify activities that causes
land pollution and their effect on
the environment.
3. Minerals are elements or
compounds which are solid,
inorganic, and naturally
occurring. They are often
combined with other substances.
Appropriate amounts of
nitrogen, phosphorus, and
potassium are components of
fertile soil.
4. Prof. Ernesto Serote described the
land as:
a natural resource
an economic good
a property
a territory
5. Soil is the material that makes
up the topmost part of the
crust.
The pedosphere is the thin
outermost layer of the Earth
made up of soil.
6. IMPORTANCE OF SOIL
Many ecosystems depend largely
on the soil.
It provides the nutrients which are
vital for plant growth.
It also allows water, air, and
energy to flow through it,
providing other resources which
are critical for the survival of
species.
7. HOW DO SOILS FORM?
WEATHERING
It is the breaking
down or dissolving
of rocks and
minerals on
Earth’s surface.
8. HOW DO SOILS FORM?
Soil is formed from
accumulated sediments,
weathered rocks, and
decaying organic matter.
9. Soil can be characterized by
its profile, texture, color,
consistency, and acidity.
11. Gritty – contains much sand
Smooth – contains more silt
Sticky – contains more clay
SOIL TEXTURE
12. Sand particles – measures up to 2
mm
Clay particles – particles are
smaller than 0.002 mm
Silt particles – particles measure
between 0.05 to 0.002 mm
13. Loam contains a good proportion
of these three soil types.
Particles that are bigger than 2
mm are no longer considered as
soil materials - classified as stone
or gravel.
14. The kind of elements or minerals
which are present in the soil gives
its characteristic color.
15. The ease or difficulty of breaking
the soil apart gives its consistency.
loose – cannot hold a single soil
structure
firm or extremely firm – if you
cannot break it apart by bare
hands.
16. It influences the kind of plants
which can grow in it.
The acidity of the soil is
affected by the water it
absorbs, natural and man-
made processes.
17. Land pollution is
the destruction and
contamination of
the land through
the direct and
indirect actions of
humans.
The pollution
results in changes to
the land, such as
22. Litter makes it difficult for
plants and other producers in
the food web to create
nutrients.
Animals can die if they
mistakenly eat plastic.
23. A massive landfill
at Payatas,
Quezon City was
the site of a land
pollution tragedy
in 2000.
Heavy rains
caused a trash
landslide, killing
218 people.
24. The chemical improperly disposed
of on the land could end up in the
ground water. The process is known
as leaching. It can occur on farms,
industrial sites, and landfills.
25. Effects of Land Pollution to Human
Some of the potential consequences
include birth defects, the development
of breathing disorders, skin diseases,
and cancer.
Land pollution has also been linked to
developmental deficits in children -
child’s cognitive development.