Soil and Agriculture
| Site: | Young Education |
| Cursus: | Environmental Chemistry |
| Boek: | Soil and Agriculture |
| Afgedrukt door: | 访客用户 |
| Datum: | maandag, 5 oktober 2026, 04:59 |
1. Soil Composition and Fertility
Learning outcomes
- I can identify the main components of soil.
- I can explain the factors that influence soil fertility.
- I can describe the role of organic matter in soil health.
- I can compare different soil types.
- I can evaluate how soil properties affect plant growth.
Soil Composition and Fertility
Soil is the loose material covering much of Earth's land surface in which plants can grow. It is much more than broken rock. Healthy soil is a complex mixture of mineral particles, organic matter, water, air, and living organisms.
Soil supports terrestrial ecosystems by:
- providing plants with water and mineral nutrients
- anchoring plant roots
- storing and filtering water
- providing habitats for organisms
- recycling nutrients
- storing carbon
The properties of soil strongly influence which plants can grow successfully in an area.
What Is Soil Made Of?
Most soils contain five major components:
- mineral particles
- organic matter
- water
- air
- living organisms
The proportions vary greatly between different soils.
A fertile agricultural soil, a sandy beach soil, and a forest soil may therefore have very different properties even though they contain the same basic components.
Mineral Particles
Most of the solid material in soil comes from the weathering of rocks.
Weathering gradually breaks rocks into smaller mineral particles.
These particles are commonly classified by size as:
sand → silt → clay
The proportions of sand, silt, and clay determine a soil's texture.
Sand
Sand contains relatively large mineral particles.
Sandy soils usually:
- have large spaces between particles
- allow water to drain quickly
- contain plenty of air
- warm relatively quickly
- hold fewer nutrients than many other soils
Because water drains rapidly, sandy soil may dry out quickly.
Plants growing in sandy soils may therefore require more frequent watering.
Clay
Clay contains extremely small mineral particles.
Clay soils usually:
- have very small spaces between particles
- hold water well
- retain many nutrients
- drain slowly
- can become waterlogged
- may contain less air when saturated
Clay soils can also become compacted.
When wet, clay can be sticky. When dry, some clay soils become hard and difficult for roots to penetrate.
Silt
Silt particles are intermediate in size between sand and clay.
Silty soils often:
- hold more water than sandy soils
- drain better than heavy clay soils
- feel smooth
- retain nutrients relatively well
However, soils containing large amounts of silt may be vulnerable to erosion.
Comparing Sand, Silt, and Clay
| Property | Sand | Silt | Clay |
|---|---|---|---|
| Particle size | Largest | Medium | Smallest |
| Drainage | Fast | Moderate | Slow |
| Water retention | Low | Moderate | High |
| Air spaces | Large | Moderate | Small |
| Nutrient retention | Often lower | Moderate | Often high |
| Compaction | Usually lower | Moderate | Can be high |
No soil type is automatically "best."
The suitability of a soil depends on:
- plant species
- climate
- rainfall
- drainage
- management
Loam
Loam is soil containing a useful mixture of:
- sand
- silt
- clay
Loamy soils are often well suited to agriculture because they can combine:
- good drainage
- good water retention
- nutrient retention
- sufficient air spaces
- workable soil structure
Loam is not an equal mixture of the three particle types. Different types of loam can contain different proportions.
Soil Texture
Soil texture describes the relative amounts of sand, silt, and clay.
Texture affects:
- drainage
- water retention
- aeration
- nutrient retention
- root growth
- ease of cultivation
Texture is mainly determined by the mineral particles present and is difficult to change substantially over a large area.
Farmers can, however, improve many soil properties by adding organic matter.
Soil Structure
Soil structure describes how individual soil particles are arranged into larger clusters called aggregates.
Good soil structure creates spaces of different sizes.
These spaces allow:
- water movement
- air movement
- root growth
- movement of soil organisms
A soil can therefore have suitable texture but poor structure if it has become heavily compacted.
Pore Spaces
The spaces between soil particles are called pores.
Some pores contain:
water
while others contain:
air
The balance is important.
Roots need water, but they also require oxygen for cellular respiration.
A healthy soil therefore needs both:
water + air
Water in Soil
Soil water supplies plants with:
- water needed for photosynthesis
- dissolved mineral ions
- materials required for cellular processes
Plants absorb much of their water through their roots.
However:
too little water → wilting and reduced growth
while:
too much water → reduced soil oxygen and possible root damage
Good soil should usually hold water while allowing excess water to drain.
Soil Air
Plant roots carry out cellular respiration.
They therefore require oxygen.
Soil organisms also require oxygen.
If all the pore spaces become filled with water, oxygen availability can decrease.
This explains why some plants grow poorly in permanently waterlogged soils.
Organic Matter
Organic matter consists of material derived from living or once-living organisms.
Examples include:
- dead leaves
- dead roots
- animal remains
- waste material
- decomposing organisms
Soil organisms gradually break this material down.
Organic matter is one of the most important contributors to healthy soil.
Humus
Humus is dark, relatively stable organic material formed after extensive decomposition.
Humus can improve:
- nutrient availability
- nutrient retention
- water retention
- soil structure
- aeration
It can help sandy soils retain more water and help clay-rich soils develop better structure.
This makes organic matter valuable across many different soil types.
Decomposers
Soil contains enormous communities of living organisms.
Important decomposers include:
- bacteria
- fungi
- earthworms
- insects
- other invertebrates
These organisms break down dead material.
During decomposition, nutrients contained in organisms can eventually become available for plants again.
A simplified nutrient cycle is:
plant → dead organic matter → decomposers → mineral nutrients in soil → plant
Earthworms and Soil
Earthworms can influence soil by:
- breaking down organic material
- mixing soil
- producing nutrient-rich casts
- creating channels
- improving aeration
- improving water movement
Earthworms are therefore often associated with biologically active soils.
However, soil ecosystems contain many organisms besides earthworms, and their importance varies among ecosystems.
What Is Soil Fertility?
Soil fertility describes the ability of soil to provide conditions and nutrients that support plant growth.
Fertility depends on several interacting factors.
These include:
- nutrient availability
- organic matter
- pH
- water availability
- drainage
- aeration
- soil structure
- biological activity
A soil can contain many nutrients but still support poor plant growth if other conditions are unsuitable.
Essential Plant Nutrients
Plants require several mineral nutrients.
Three important nutrients frequently discussed in agriculture are:
nitrogen (N)
phosphorus (P)
potassium (K)
Commercial fertilizers often display these as an N-P-K ratio.
Different nutrients perform different roles in plant growth.
Nitrogen
Nitrogen is needed to produce important biological molecules including:
- amino acids
- proteins
- nucleic acids
- chlorophyll
Nitrogen deficiency may lead to:
- poor growth
- pale or yellowing leaves
Nitrogen compounds in soil can come from:
- decomposition
- fertilizers
- animal waste
- nitrogen fixation
Phosphorus
Phosphorus is important in:
- ATP and energy transfer
- DNA and RNA
- cell membranes
- root development
- reproduction
A phosphorus deficiency can reduce plant development.
However, excessive phosphorus entering waterways can contribute to eutrophication.
Potassium
Potassium contributes to processes including:
- enzyme function
- water regulation
- stomatal function
- plant stress responses
Adequate potassium can help plants maintain healthy physiological processes.
Nutrients Are Not the Whole Story
Adding more fertilizer does not automatically make soil healthier.
Plants can only benefit from nutrients if other conditions are appropriate.
For example, poor growth could result from:
- unsuitable pH
- waterlogging
- drought
- soil compaction
- disease
- poor soil structure
rather than nutrient deficiency.
Good soil management therefore requires identifying the actual limiting factor.
Soil pH
Soil pH measures how acidic or alkaline the soil is.
The pH scale is commonly represented from:
0 to 14
with:
pH 7 = neutral
below 7 = acidic
above 7 = alkaline
Many plants grow well in slightly acidic to approximately neutral soil, but the preferred range depends on the species.
Why Soil pH Matters
pH influences the chemical forms and availability of nutrients.
At unsuitable pH values:
- some nutrients become less available
- some substances may become more soluble
- microbial activity can change
- plant growth can decline
Therefore, soil may contain a nutrient but plants may have difficulty absorbing it.
This is one reason soil testing can be useful before adding fertilizer.
Soil Testing
Farmers, gardeners, and scientists can test soil for characteristics such as:
- pH
- nutrient concentrations
- organic matter
- moisture
- texture
Testing provides evidence that can guide management decisions.
Instead of simply adding fertilizer, a farmer can determine which nutrients are actually deficient.
Water-Holding Capacity
Water-holding capacity describes how effectively soil retains water.
Sandy soils generally have:
lower water-holding capacity
Clay-rich and organic-rich soils generally have:
higher water-holding capacity
However, holding the maximum possible amount of water is not always desirable.
Plants need a balance between:
water retention + drainage + aeration
Drainage
Drainage describes how easily excess water moves through and away from soil.
Poor drainage can cause:
- waterlogging
- reduced oxygen
- root stress
- increased risk of some plant diseases
Extremely rapid drainage can also be problematic because soil may dry too quickly.
Soil Compaction
Soil compaction occurs when soil particles are pressed closely together.
It can result from:
- heavy machinery
- vehicles
- repeated foot traffic
- livestock
- working wet soils
Compaction reduces pore space.
This can cause:
less pore space → less air and water movement → more difficult root growth
Comparing Plant Growth in Different Soils
Imagine identical plants are grown under the same conditions.
Soil A
- mostly sand
- low organic matter
- drains rapidly
Likely result:
Water and nutrients may be lost quickly.
Soil B
- heavy clay
- strongly compacted
- poor drainage
Likely result:
Roots may receive insufficient oxygen.
Soil C
- loamy
- rich in organic matter
- good structure
Likely result:
The soil may provide a more favorable balance of water, nutrients, drainage, and aeration.
This demonstrates why plant growth depends on several soil properties interacting together.
Soil Profiles
Soil often develops in layers called horizons.
Together these layers form a soil profile.
A simplified profile may contain:
O horizon — surface organic material
A horizon — topsoil
B horizon — subsoil
C horizon — partly weathered parent material
Below these may be solid bedrock.
Topsoil
Topsoil is usually the upper mineral soil layer.
It often contains:
- mineral particles
- organic matter
- plant roots
- microorganisms
Topsoil is particularly important for plant growth.
Loss of topsoil through erosion can greatly reduce agricultural productivity.
Factors Affecting Soil Formation
Soils develop over long periods.
Important factors include:
- parent rock or material
- climate
- organisms
- topography
- time
For example, rainfall influences:
- weathering
- leaching
- plant growth
- decomposition
Different combinations of these factors produce different soils.
Climate and Soil Fertility
Climate influences soil through:
- rainfall
- temperature
- weathering
- decomposition
- vegetation
Warm, wet conditions can promote rapid decomposition but may also increase leaching.
Dry conditions may slow biological activity and limit plant growth.
Climate therefore affects both soil formation and nutrient cycling.
Leaching
Leaching occurs when water moving through soil carries dissolved substances downward.
Heavy rainfall can increase leaching.
Some nutrients may therefore move below the depth reached by plant roots.
Sandy soils can be particularly vulnerable because water moves through them relatively quickly.
Soil Erosion
Soil erosion is the movement and removal of soil by agents such as:
- water
- wind
Human activities can increase erosion by removing vegetation.
Bare soil is particularly vulnerable because plant roots and surface vegetation normally help hold soil in place.
Why Erosion Reduces Fertility
Erosion often removes nutrient-rich topsoil.
This can reduce:
- organic matter
- nutrients
- water-holding capacity
- soil depth
- biological activity
Severe erosion can make productive land increasingly difficult to farm.
Protecting soil is therefore an important part of sustainable agriculture.
Improving Soil Fertility
Farmers and gardeners can improve soil health using several approaches.
These include:
- adding compost
- adding appropriate fertilizers
- planting cover crops
- rotating crops
- reducing erosion
- reducing compaction
- maintaining vegetation
- managing irrigation
- monitoring soil pH
The best strategy depends on the soil problem.
Compost
Compost is partially decomposed organic material.
Adding compost can:
- add organic matter
- improve soil structure
- increase water retention
- supply nutrients
- support soil organisms
Compost therefore improves more than simply nutrient concentration.
Fertilizers
Fertilizers supply plant nutrients.
They may be:
- organic
- mineral or synthetic
Fertilizers can improve crop growth when nutrients are limiting.
However, excessive fertilizer use can cause:
- nutrient runoff
- groundwater contamination
- eutrophication
- unnecessary expense
The sustainable approach is:
right nutrient + right amount + right place + right time
Crop Rotation
Crop rotation involves growing different crops in a planned sequence.
This can help:
- manage nutrient demand
- reduce some pests and diseases
- improve soil structure
- reduce erosion
Some rotations include legumes, which form associations with nitrogen-fixing bacteria.
These bacteria can increase biologically available nitrogen within the system.
Cover Crops
Cover crops are grown partly to protect or improve soil rather than primarily for harvest.
They can:
- protect soil from erosion
- add organic material
- reduce nutrient loss
- improve structure
- suppress some weeds
Roots also help hold soil in place.
Evaluating Soil for Plant Growth
When evaluating soil, do not look at only one characteristic.
Consider:
Texture — How much sand, silt, and clay?
Structure — Are particles arranged into healthy aggregates?
Organic matter — Is there material supporting nutrient cycling and soil structure?
pH — Are nutrients available to the plants?
Water retention — Can the soil store sufficient water?
Drainage — Can excess water escape?
Aeration — Can roots obtain oxygen?
Nutrients — Are essential mineral nutrients available?
Biological activity — Is there a functioning soil community?
Together, these determine how effectively soil can support plants.
Example: Choosing Soil for Tomatoes
Suppose three soils are available.
| Property | Soil A | Soil B | Soil C |
|---|---|---|---|
| Texture | Sandy | Heavy clay | Loam |
| Organic matter | Low | Medium | High |
| Drainage | Very fast | Very slow | Moderate |
| Aeration | High | Low | Good |
| Nutrient retention | Low | High | Good |
Soil C would probably provide the most balanced conditions.
However, Soil A could potentially be improved by adding organic matter, while Soil B could benefit from management that improves structure and drainage.
Soil properties can often be managed, even when the basic texture cannot easily be changed.
Example: Investigating Soil Fertility
Students could investigate how soil type affects plant growth.
Use identical seedlings and grow them in:
- sandy soil
- clay-rich soil
- loamy soil
Keep constant:
- plant species
- light
- temperature
- pot size
- initial plant size
Measurements might include:
- plant height
- leaf number
- biomass
- soil moisture
The investigation could then connect observed plant growth to soil properties.
Common Mistakes
Thinking Soil Is Just Dirt
Soil is a complex ecosystem containing minerals, water, air, organic matter, and organisms.
Assuming Clay Soil Is Always Bad
Clay can hold water and nutrients very effectively.
Problems arise when drainage or structure is poor.
Assuming Sandy Soil Is Always Bad
Sandy soils often have excellent drainage and aeration.
Their main limitations may be low water and nutrient retention.
Thinking Fertility Means Only Fertilizer
Fertility also depends on:
- pH
- organic matter
- water
- aeration
- structure
- biological activity
Assuming More Fertilizer Means More Growth
Once nutrient needs are satisfied, additional fertilizer may provide little benefit and can cause environmental damage.
Confusing Soil Texture and Structure
Texture = proportions of sand, silt, and clay
Structure = arrangement of soil particles into aggregates
Thinking Waterlogged Soil Gives Plants More Water
Waterlogged soil may contain plenty of water but insufficient oxygen for healthy roots.
Assuming All Plants Prefer the Same Soil
Different plants are adapted to different:
- pH levels
- moisture conditions
- nutrient levels
- textures
Ignoring Organic Matter
Organic matter influences nutrients, water retention, soil structure, and biological activity.
It is a central component of soil health.
Key Terms
Soil — A mixture of mineral particles, organic matter, water, air, and organisms that develops at Earth's surface.
Soil fertility — The ability of soil to provide suitable conditions and nutrients for plant growth.
Soil texture — The relative proportions of sand, silt, and clay.
Sand — The largest of the three major soil particle-size categories.
Silt — Soil particles intermediate in size between sand and clay.
Clay — The smallest major soil particle-size category.
Loam — Soil containing a useful mixture of sand, silt, and clay.
Soil structure — The arrangement of soil particles into larger aggregates.
Pore space — Spaces between soil particles that can contain air or water.
Organic matter — Material in soil derived from living or once-living organisms.
Humus — Dark, relatively stable organic material produced through decomposition.
Decomposer — An organism that breaks down dead organic material and contributes to nutrient recycling.
Water-holding capacity — The ability of soil to retain water.
Drainage — Movement of excess water through and away from soil.
Aeration — The presence and movement of air through soil.
Soil compaction — Compression of soil that reduces pore space.
Soil horizon — A distinct layer within a soil profile.
Topsoil — Upper mineral soil layer usually containing considerable biological activity and organic matter.
Leaching — Movement of dissolved substances downward through soil with water.
Soil erosion — Removal and transport of soil by water, wind, or other processes.
Compost — Decomposed organic material added to soil.
Crop rotation — Planned sequence of different crops grown on the same land.
Cover crop — Crop planted partly to protect or improve soil.
Key Takeaways
- Soil contains mineral particles, organic matter, water, air, and living organisms.
- Mineral soil particles are commonly classified as sand, silt, and clay.
- Soil texture depends on the proportions of sand, silt, and clay.
- Sandy soils generally drain rapidly but retain less water and nutrients.
- Clay-rich soils retain more water and nutrients but may drain poorly.
- Loamy soils often provide a useful balance of drainage, water retention, and aeration.
- Soil structure describes how particles form aggregates.
- Pore spaces provide both water and air for plant roots.
- Organic matter is extremely important for soil health.
- Humus can improve nutrient retention, water retention, and soil structure.
- Decomposers recycle nutrients from dead organisms.
- Soil fertility depends on more than simply the amount of fertilizer present.
- Nitrogen, phosphorus, and potassium are important plant nutrients.
- Soil pH influences nutrient availability.
- Compaction reduces pore space and can restrict root growth.
- Excess water can reduce oxygen available to roots.
- Erosion can remove fertile topsoil.
- Compost, crop rotation, cover crops, and careful fertilizer use can help maintain soil fertility.
- Soil properties should be evaluated together when predicting plant growth.
A useful way to think about healthy soil is:
MINERALS + ORGANIC MATTER + WATER + AIR + ORGANISMS → HEALTHY SOIL SYSTEM
And successful plant growth requires a balance of:
NUTRIENTS + WATER + OXYGEN + ROOT SPACE + SUITABLE pH.
2. Nutrient Cycles
Learning outcomes
- I can explain how nutrients move through ecosystems.
- I can describe the roles of carbon, nitrogen, and phosphorus cycles.
- I can explain the importance of nutrient recycling.
- I can identify factors that affect nutrient availability.
- I can analyze the relationship between nutrient cycles and agriculture.
3. Fertilizers
Learning outcomes
- I can identify the nutrients supplied by fertilizers.
- I can explain how fertilizers improve crop growth.
- I can compare organic and synthetic fertilizers.
- I can describe environmental impacts associated with fertilizer use.
- I can evaluate the benefits and drawbacks of fertilizer application.
4. Pesticides and Herbicides
Learning outcomes
- I can distinguish between pesticides and herbicides.
- I can explain how these chemicals are used in agriculture.
- I can identify benefits and risks associated with their use.
- I can describe environmental impacts of agricultural chemicals.
- I can evaluate alternatives to chemical pest control.
5. Sustainable Agriculture
Learning outcomes
- I can explain the principles of sustainable agriculture.
- I can identify farming practices that protect soil and water resources.
- I can compare conventional and sustainable farming methods.
- I can evaluate the environmental impacts of agricultural systems.
- I can propose strategies for improving agricultural sustainability.