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WEATHERING
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I. Introduction
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II. Types of Weathering A. Mechanical/Physical B. Chemical
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Mechanical/Physical 1. Thermal Expansion and Contraction
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2. Ice Wedging/Frost Action
Water expands 9% when it freezes 30,000 psi
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3. Exfoliation
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6/19/2018
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4. Action of Organisms
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Biological “Critters”
Burrowing animals Humans
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II B. Chemical Weathering
1. Factors: A. Type of Rock or Mineral
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B. Amount of Surface Area
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C. Presence of Moisture
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D. Effects of Organisms
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E. Air and Water Pollution
Sulfur = acid rain
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II B. Chemical Weathering
2. Mechanisms of Chemical Weathering
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A. Solution“the dissolving of a rock”
CO H2O = H2CO3 Carbon Carbonic Acid Dioxide
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A. Solution“the dissolving of a rock”
CO H2O = H2CO3 Carbon Carbonic Acid Dioxide H2CO CaCO3 = Ca+ + 2HCO3- Carbonic Limestone Bicarbonate Acid
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A. Solution“the dissolving of a rock”
More recently….. 2SO H2O + O2 = H2SO4
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A. Solution“the dissolving of a rock”
More recently….. 2SO H2O + O2 = H2SO4 Sulfur Sulfuric Dioxide Acid
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B. Hydration “chemically adding water to a rock”
CaSO H2O = CaSO4 * 2 H20 Anhydrite Gypsum
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C. Hydrolysis “converting a silicate mineral into a clay via water”
2KAlSi3O H2CO H20 = Orthoclase Carbonic Acid Water Al2Si2O5(OH)4 + 2K+ + 2HCO SiO2 Kaolinite Bicarbonate Quartz
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D. Oxidation: “process of rusting; the taking away of electrons”
Fe2+ >>>> Fe3+ Ferrous Ferric (dark) (red)
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D. Oxidation: “process of rusting; the taking away of electrons”
Fe2+ >>>> Fe3+ Ferrous Ferric (dark) (red) 4Fe O2 = 2Fe2O3 iron hematite ore
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III. Rates of Weathering
A. Climate
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III. Rates of Weathering
A. Climate B. Rock Structure, Size, Composition
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