soil horizons and profiles
Called the A-horizon, the topsoil is usually the darkest layer of the soil because it has the highest proportion of organic material. The topsoil is the region of most intense biological activity: insects, worms, and other animals burrow through it and plants stretch their roots down into it. Plant roots help to hold this layer of soil in place. In the topsoil, minerals may dissolve in the fresh water that moves through it to be carried to lower layers of the soil. Very small particles, such as clay, may also get carried to lower layers as water seeps down into the ground.
soil horizons and profiles
A residual soil forms over many years, as mechanical and chemical weathering slowly change solid rock into soil. The development of a residual soil may go something like this. 1. 2. 3. 4. 5. The bedrock fractures because of weathering from ice wedging or another physical process. Water, oxygen, and carbon dioxide seep into the cracks to cause chemical weathering. Plants, such as lichens or grasses, become established and produce biological weathering. Weathered material collects until there is soil. The soil develops soil horizons, as each layer becomes progressively altered. The greatest degree of weather- ing is in the top layer. Each successive, lower layer is altered just a little bit less. This is because the first place where water and air come in contact with the soil is at the top. A cut in the side of a hillside shows each of the different layers of soil. All together, these are called a soil profile (Figure 1.1). The simplest soils have three horizons. Soil is an important resource. Each soil horizon is distinctly visible in this photo- graph.
The C-horizon is a layer of partially altered bedrock. There is some evidence of weathering in this layer, but pieces of the original rock are seen and can be identified. Not all climate regions develop soils, and not all regions develop the same horizons. Some areas develop as many as five or six distinct layers, while others develop only very thin soils or perhaps no soils at all. Click image to the left or use the URL below. URL:
The B-horizon or subsoil is where soluble minerals and clays accumulate. This layer is lighter brown and holds more water than the topsoil because of the presence of iron and clay minerals. There is less organic material. Figure A soil profile is the complete set of soil layers. Each layer is called a horizon.
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to make a soil
a) mechanical weathering processes break up bedrock. b) chemical compounds cause chemical weathering. c) plants break up rock and chemically alter rock. --> d) all of the above
going down in a soil, each soil horizon downward becomes
a) more altered from the original rock. --> b) less altered and more like the original rock. c) darker and more organic rich. d) a & c
if the plants are removed from a slope, that slope is more likely to erode in the next rain.
--> a) true b) false
this layer of soil has the highest proportion of organic material.
--> a) topsoil b) subsoil c) c-horizon d) bedrock
this layer of soil grades into the parent rock below.
a) topsoil b) subsoil --> c) c-horizon d) bedrock
the zone where iron oxide and clay accumulate.
a) topsoil --> b) subsoil c) c-horizon d) bedrock
what organic material is added to the topsoil?
--> a) humus b) clay c) altered rock d) a & b
what can cause chemical weathering?
a) water b) oxygen c) carbon dioxide --> d) all of the above
all climate regions develop soil, and all regions develop the same horizons.
a) true --> b) false
in soil, water is held by carbonate minerals.
c) true d) false
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