Unit 5.1: Introduction to Soil Systems Flashcards

1
Q

What is soil?

A

Material composed of five ingredients: minerals, organic
matter, living organisms, gas, and water.

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1
Q

Importance of soil

A
  • 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
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2
Q

The soil system

A

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

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3
Q

Soil profile

A

vertical cross-section of the soil, made of layers running parallel to the surface.These layers are known as soil horizons.

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4
Q

Leaching

A

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

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5
Q

The soil texture triangle

A

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

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6
Q

Sandy soils

A

grainy and fall apart easily

Particle diameter:
0.05 - 2 mm

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7
Q

Silty soils

A

slippery and holds together better than sandy soils

Particle diameter:
0.002 mm - 0.05 mm

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8
Q

Clay soils

A

sticky and can be rolled up
into a ball easily

Particle diameter:
< 0.002 mm

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9
Q

Minerals

A

These are derived from the weathering of rocks and include sand, silt, and clay. The proportions of these particles determine the soil’s texture.

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