Ch.1 The Importance of Soil
Ch. 2 Soil Origin and Development
Ch. 4 Physical Properties of Soil
Ch. 5 Life in the Soil
100

The process by which carbon is recycled directly back to the atmosphere by plants and animals

Respiration

100

Water molecules join with the crystalline structure of minerals

Hydration

100

Soil characteristics that can be seen or felt

Physical property

100

Generate, absorb, or degrade greenhouse gases such as carbon dioxide, nitrous oxide, and methane

Microbes

200

Conversion of dry grasslands to desert

Desertification

200

Organic soils contain ____% or more organic matter.

20

200

Medium-sized particles; silky or powdery to the touch

Silt

200

Fungi that help plants absorb water and nutrients

Mycorrhizae

300

The process of storing carbon in soils, plants, or elsewhere

Carbon sequestration

300

Horizontal layers that develop as a soil ages

Soil horizon

300

Tend to occupy lower B and C horizons; peds are 1/5 to 4 inches, forming angular columns that stand upright in the soil

Prismatic structure

300

The ____ is an area of high biological activity that takes place close to the surface of the soil, near plant roots.

rhizosphere

400

Equal amounts of ____  and water are ideal for plant growth.

air

400

Soil formation

Soil genesis

400

Small particles; many small pores; consisting mostly of tiny sheet-like crystals

Clay

400

A large, diverse group of microscopic segmented worms that are especially numerous in soil.

Nematodes

500

Hardpans, water-logged soil, and ____ prevent roots from growing deeply.

bedrock

500

Minerals react with the hydrogen in water molecules and split the water

Hydrolysis

500

The measure of the rate of water movement through a soil

Hydraulic conductivity

500

Some fix nitrogen and some produce antibiotics

Actinomycetes

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