5 soil introduction
DESCRIPTION
an introduction to soil geomorphology for college geology students.TRANSCRIPT
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Record the apparent depositional history at a location and
post-depositional development processes.
Soil covers much of the Earth's land surface area, and it iscomprised of minerals, air, water, and organic matter (living
organisms and the remains of plants and animals).
General definition of soil
The unconsolidated mineral and organic matter on thesurface of the earth.
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It is the key to the history of landscapes.
Erosion or sediment deposition changes landscape faster
than Soils mature as their properties are slowly through time.
Mature soil only cover stable landscape that neither erode
nor accumulate sediments.
Chemical and physical weathering convert pre existing
materials into soil.
Valuable minerals?
Geochemical Exploration?
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:
is a natural, 3D body withdefinable boundaries that
occurs on the land surface
composed of solids (mineral
and organic), liquids (water),and gases.
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The soil body begins where the atmosphere meets the soil
surface and ends when bedrock or unweathered parentmaterial is encountered.
In order to study soil, scientists examine the soil pedon. A
pedon is the smallest unit that can be called a soil.
A pedon is a three-dimensional sample that extends from thesoil surface to the deepest roots or genetic soil horizons.
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Parent Material (Rock Type),
Climate,
Topography/Relief,
Organisms (Plants/Animals),
And Time