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Ch 5 Soils

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Regolith - minerals & rock fragments. Humus - organic matter. Gases. Water. Living organisms ... May contain soluble minerals such as calcite in arid climates ... – PowerPoint PPT presentation

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Title: Ch 5 Soils


1
Ch 5 - Soils
  • Important 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

2
What is Soil?
  • Soil consists of
  • Regolith - minerals rock fragments
  • Humus - organic matter
  • Gases
  • Water
  • Living organisms

3
How does soil form?
  • Five factors influencing soil formation
  • Climate
  • Parent rock
  • Organisms
  • Plants
  • animals
  • Topography
  • Time

4
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.

5
Soil Horizons Field
6
Figure 6. 17
7
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.

8
US Soil map
Gray-brown moist
Soft organic rich
Strongly weathered clay rich
9
Soil Orders
10
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

11
Particle Sizes
Loam
12
Loam Combination of Sand, Silt, Clay
Soil's productivity is mainly due to the clays in
the soils
13
Names for Loams
Based on of sand, silt, clay
14
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.

15
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

16

How can we slow soil erosion?
  • Contour plowing
  • Terraces
  • Crop rotation
  • Planting groundcovers
  • Windbreaks
  • Reduce overgrazing
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