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WEATHERING. I. Introduction. II. Types of Weathering A. Mechanical/Physical B. Chemical. Mechanical/Physical 1. Thermal Expansion and Contraction. 2. Ice Wedging/Frost Action. Water expands 9% when it freezes 30,000 psi. 2. Ice Wedging/Frost Action. 3. Exfoliation.
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2. Ice Wedging/Frost Action • Water expands 9% when it freezes • 30,000 psi
Other Actions • Burrowing animals • Man
Burrowing animalsgroundhogs “taste like beef”
II B. Chemical Weathering • 1. Factors: • A. Type of Rock or Mineral
E. Air and Water Pollution • Sulfur = acid rain
II B. Chemical Weathering • 2. Mechanisms of Chemical Weathering
A. Solution“the dissolving of a rock” CO2 + H2O = H2CO3 Carbon Carbonic Acid Dioxide
A. Solution“the dissolving of a rock” CO2 + H2O = H2CO3 Carbon Carbonic Acid Dioxide H2CO3 + CaCO3 = Ca+ + 2HCO3- Carbonic Limestone Bicarbonate Acid
A. Solution“the dissolving of a rock” More recently….. 2SO2 + 2H2O + O2 = 2H2SO4
A. Solution“the dissolving of a rock” More recently….. 2SO2 + 2H2O + O2 = 2H2SO4 Sulfur Sulfuric Dioxide Acid
B. Hydration“chemically adding water to a rock” • CaSO4 + 2 H2O = CaSO4 * 2 H20 • Anhydrite Gypsum
C. Hydrolysis“converting a silicate mineral into a clay via water” 2KAlSi3O8 + 2 H2CO3 + H20 = Orthoclase Carbonic Acid Water Al2Si2O5(OH)4 + 2K+ + 2HCO3- + 4 SiO2 Kaolinite Bicarbonate Quartz
D. Oxidation: “process of rusting; the taking away of electrons” Fe2+ >>>> Fe3+
D. Oxidation: “process of rusting; the taking away of electrons” Fe2+ >>>> Fe3+ Ferrous Ferric (dark) (red)
D. Oxidation: “process of rusting; the taking away of electrons” Fe2+ >>>> Fe3+ Ferrous Ferric (dark) (red) 4Fe2+ + 3O2 = 2Fe2O3 iron hematite ore
III. Rates of Weathering A. Climate
III. Rates of Weathering A. Climate B. Rock Structure and Composition
III. Rates of Weathering • A. Climate • B. Rock Structure and Composition • C. Particle Size