ENST200 chapter 1

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Last updated 10:31 PM on 9/23/26
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30 Terms

1
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Ecological roles of soil in Ecosystems: Medium for plant growth

  • Soils support the plants that make the built environment livable

  • soils grow 95% of the food we eat

  • soils support the plants that we use to make things (EX: Trees for wood)

  • Plants can replace petroleum to make chemicals & fuels to drive our economy


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Ecological roles of soil in Ecosystems: Recycling system for nutrients

  • Carbon and nitrogen cycling

  • Turning organic waste into soil organic matter and then mineral nutrients to be utilized by plants and animals


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Ecological roles of soil in Ecosystems: Modifier of the atmosphere

soils emit and/or absorb

  • dust

  • heat

  • water vapor

  • CO2

  • oxygen

  • methane

  • nitrogen oxides

  • odors

  • other gases


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Ecological roles of soil in Ecosystems: Habitat for soil organisms

  • earth worms

  • microorganisms (fungi, bacteria, etc)


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Ecological roles of soil in Ecosystems: Engineering medium

  • rammed earth houses

  • mud bricks

  • foundation on what infrastructure is built on


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Ecological roles of soil in Ecosystems: System for water supply & purification

  • water purification

  • water runs into bodies of water (rivers, streams, lakes, etc)


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The 6 Ecological roles of soil in Ecosystems

  • Medium for plant growth

  • Recycling system for nutrients

  • Modifier of the atmosphere

  • Habitat for soil organisms

  • Engineering medium

  • System for water supply & purification


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Pedosphere

  • Atmosphere (soil air): gasses- CO2, oxygen, nitrogen

  • Biosphere (organic matter and biomass): plants, animals, microbes, their products and remains

  • Hydrosphere (soil water): water and dissolved substances

  • Lithosphere (soil particles): minerals in rocks, clays, sediments


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Regolith

  • Layer of weathered rock

  • Soft part of the soil


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Solum

O, A, and B horizon portion of soil

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Bedrock

parent material, unweathered rock

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Saprolite

soil that has been weathered to the point that it is loose enough to be dug with a spade

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O horizon

top organic layer at soil surface

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A horizon

layer after O horizon, accumulation of organic matter that has darkened, dominated by mineral particles

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E Horizon

below A horizon (not all soils have them), intensely weathered and leached mineral horizon, light colored, eluvial-washout

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B horizon

accumulation of materials washed down from horizons above, illuvial- wash into

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C horizon

least weathered part of soil profile

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R horizon

hard rock, parent material

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Macronutrients

used in relatively large amounts

mostly from air and water

  • CO2

  • Hydrogen

  • Oxygen


Mostly from soil solids

  • nitrogen

  • phosphorus

  • potassium

  • calcium

  • magnesium

  • sulfur


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micronutrients

used in relatively small amounts

derived from soil solids

  • iron

  • maganese

  • zinc

  • copper

  • cobalt

  • nickel

  • chlorine

  • molybdenum

  • boron

  • silicon


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What plants get from soils

  • air

  • water

  • temperature moderation

  • physical support

  • nutrients

  • medium for bio-signals

  • toxin free medium


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Nutrients obtained from soil minerals

  • phosphorus

  • potassium

  • calcium


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things obtained from air

  • nitrogen

  • co2

  • different gasses


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things obtained from soil organic matter

  • nutrients like nitrogen, phosphorus and sulfur


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soil solution

soil water that contains dissolved organic and inorganic substances

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humus

collection of organic compounds that accumulate in soil when when partially broken down plant and animal matter are protected from complete decay by various factors in the environment

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diffusion

nutrient ions moving from areas of high concentration to nutrient-depleted areas of lower concentration

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root interception

when roots grow and touch soil particles to absorb nutrients’ as they grow (not done on purpose just something that happens)

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mass flow

when dissolved nutrients are carried along with flowing soil water toward a root that is actively drawing water from the soil

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soil colloids

microscopic minerals and organic particles that drive most of the chemical and physical activity in soil