Unit 5.1: Introduction to Soil Systems Flashcards
What is soil?
Material composed of five ingredients: minerals, organic
matter, living organisms, gas, and water.
Importance of soil
- food consumed depends upon soil
- plants grow in soil (hold water and mineral nutrients)
- habitat for many organisms
- act as enormous filter for any water that passes through it, altering chemistry of that water (modify the chemical composition by absorbing excess nutrients, such as nitrogen and phosphorus, from agricultural runoff or wastewater)
- store and transfer heat,
eg. moderate temperature fluctuations between day and night. This thermal inertia is important for creating a more stable environment for plants, animals, and humans
eg2. proper management of soil can enhance its ability to act as a carbon sink
The soil system
dynamic ecosystem that has inputs, outputs, storages and flows
storages: organic matter, organisms, nutrients, minerals, air and water
inputs: organic and inorganic matter from precipitation and energy
outputs: uptake by plants and soil erosion
transfers: biological mixing, translocation and leaching
transformations: decomposition, weathering (breaking down rocks naturally) and nutrient cycling
Soil profile
vertical cross-section of the soil, made of layers running parallel to the surface.These layers are known as soil horizons.
Leaching
Natural process by which water-soluble substances such as
calcium are washed out from soil.
- may reduce the fertility of a soil.
- may occur due to rain or irrigation
- fertilizers and chemicals also get washed away with water and reach water bodies causing water pollution
The soil texture triangle
Mineral portion of soil can be divided up into three particles based on size: sand, silt and clay.
Most consist of mixture of soil particles depends on relative proportion of sand, silt and clay particles
Sandy soils
grainy and fall apart easily
Particle diameter:
0.05 - 2 mm
Silty soils
slippery and holds together better than sandy soils
Particle diameter:
0.002 mm - 0.05 mm
Clay soils
sticky and can be rolled up
into a ball easily
Particle diameter:
< 0.002 mm
Minerals
These are derived from the weathering of rocks and include sand, silt, and clay. The proportions of these particles determine the soil’s texture.