PEE 1.0 Flashcards
(49 cards)
It takes about two hundred to a thousand years to form and develop a few centimetres of fertile top soil.
Soil
Contents that affect soil fertility
Mineral nutrients, air, water
Components of fertile soil
Nitrogen, potassium, phosphorus
Stages of soil formation
-Bedrock begins to disintegrate
-Organic materials facilitate disintegration
-Horizons form
- developed soil supports thick vegetation
Bedrock begins to disintegrate as it is subjected to freezing-thawing cycles, rain, and other environmental forces
Bedrock begins to disintegrate
The rock breaks down into parent material, which in turn breaks into smaller mineral particles.
Organic materials facilitate disintegration
The organisms in an area contribute to soll formation by facilitating the disintegration process as they live and adding organic matter to the system when they die. As soil continues to develop, layers called
Horizons form
The A horizon, nearest the surface, is usually richer In organic matter, while the lowest layer, the C horizon, contains more minerals and still look much like the parent material. The soll will eventually reach a point where it can support a thick cover of vegetation and cycle its resources effectively.
Developed soil supports thick vegetation
Soil is formed by
parent material, climate, topography; time, biological.
the original “Mom & Pop” soil transported from elsewhere, usually by wind or water, at different speeds
Parent material
the amount, intensity, timing, and kind of precipitation that breaks dowr parts of ecosystem (i.e. rocks, trees) into soil
Climate
Slope and Aspect affect the angle of the land and position toward/away from the sun that soil will be exposed to
Topography
Plants, animals, microscopic organisms, and humans interact w soil in different ways
Biological
the amount of time it takes for the four factors (above) to interact each other
Time
Soil plays important roles and these include:
Serving as a foundation Emitting and absorbing gases Providing habitat
Interacting with water
Recycling nutrients
Supporting human settlements
Soil characterizations
- Soil profile
- Soil texture
- Soil color
- Soil consistency
- Acidity is affected by the chemical nature of parent rock material, the kind of water it absorbs and the natural and man
Is a vertile cross-section of layers of soil found in given area
Soil profile
Each layer is called?
Horizon
topmost layer; made up of organic materials and other newly decomposing surface litter; usually present in areas with many trees and plants
O horizon
also known as top soil. Since it receives the nutrients from decaying litter of O horizon, it is usually made up of humus which makes it fertile. With the help of plant roots water is absorbed by humus thus preventing flood
A horizon
materials from A and O horizons accumulate here. Thus it is rich in clay, organic matter and other mineral components. It is lighter in color with reddish brown shades
B horizon or subsoil layer
is usually made up of massive bedrock of the original parent material and it does not undergo much change.
C horizon
At depths of 48+ feet, deepest soil horizon in the soil profile,
no rocks or boulders, only a continuous mass of bedrock, colors are those of the original rock of the area
R horizon or bedrock
This pertains to how much sand, clay, or silt is present in the soil. these 3 kinds of soil vary in size.
Soil texture
Sand-particles measure up to 2 mm
Clay-particles are smaller than 002 mm
Silt-particles measure between 0.05 to 0.002 mm