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Ch 5 - SoilsImportant effect of weathering for people!
Important area of study for geologists.
Objectives • What is soil. • Know soil horizons
and characteristics. • Know 2 types of
soils • Causes &
preventions of soil erosion
What is Soil?Soil consists of: 1. Regolith - minerals & rock
fragments
2. Humus - organic matter
3. Gases
4. Water
5. Living organisms
How does soil form?
Five factors influencing soil formation:
1. Climate
2. Parent rock
3. Organisms• Plants• animals
4. Topography
5. Time
What is a soil profile? A soil profile consists of several soil
horizons.
O horizon – humus on the ground surface.
A horizon – Top soil. – Rich in organic matter. Typically
dark color. – Also called zone of leaching.
B horizon – Subsoil. – Also called zone of accumulation. – May contain soluble minerals such
as calcite in arid climates (caliche). C horizon
– Weathered bedrock (rotten rock). – Bedrock lies below the soil profile.
Soil Horizons – Field
Figure 6. 17
Major Soil Types
• Pedalfer – rich in Al and Fe. – form in humid climates
• Pedocal – rich in Ca. – form in arid climates– commonly contain caliche
(or hardpan), a calcium carbonate deposit which accumulates in the soil.
US Soil mapSoft & organic rich
Strongly weathered & clay rich
Gray-brown & moist
Soil Orders
Have you ever had your soil analyzed? This can be done by county extension
office. Gives you information on: • pH of your soil.
– Is your soil acidic or basic?
• Elements - Plants require – P, K, Ca, Mg – B, Mn, Zn
• Nitrates (fertilizer) – – N, P, K (in that order) – listed as weight percents– Ex. 5-10-5 or 10-10-10.
• Organic matter • Soluble salts
Particle Sizes
Loam
Loam – Combination of Sand, Silt, Clay
Soil's productivity is mainly due to
the clays in the soils
Names for Loams
Based on % of sand, silt, & clay
Soil erosion - (weathering & erosion are different).
• Due to water (runoff) or wind. – transported by streams– deposited on floodplain or
at mouth of river. – trapped behind dams
• reduces beach sand• accelerate beach erosion.
• Dust Bowl of the 1930's - due to wind erosion of soil following extended drought and over-tilling of the soil.
Slopes Make it Worse• 1 % slope = 3 tons soil lost per hectare/yr• 5 % slope = 87 tons lost per hectare/yr
At this rate a 15 cm thickness of topsoil would disappear in about 20 years,
• 15 % slope = 221 tons lost per hectare/yr hectare = 10,000 square meters, or 2.471 acres
• Contour plowing • Terraces • Crop rotation• Planting groundcovers• Windbreaks • Reduce overgrazing
How can we slow soil erosion?