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WEATHERING.

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Presentation on theme: "WEATHERING."— Presentation transcript:

1 WEATHERING

2 I. Introduction

3 II. Types of Weathering A. Mechanical/Physical B. Chemical

4 Mechanical/Physical 1. Thermal Expansion and Contraction

5 2. Ice Wedging/Frost Action
Water expands 9% when it freezes 30,000 psi

6 3. Exfoliation

7

8 6/19/2018

9 4. Action of Organisms

10 Biological “Critters”
Burrowing animals Humans

11 II B. Chemical Weathering
1. Factors: A. Type of Rock or Mineral

12

13 B. Amount of Surface Area

14 C. Presence of Moisture

15 D. Effects of Organisms

16 E. Air and Water Pollution
Sulfur = acid rain

17 II B. Chemical Weathering
2. Mechanisms of Chemical Weathering

18 A. Solution“the dissolving of a rock”
CO H2O = H2CO3 Carbon Carbonic Acid Dioxide

19 A. Solution“the dissolving of a rock”
 CO H2O = H2CO3 Carbon Carbonic Acid Dioxide H2CO CaCO3 = Ca+ + 2HCO3- Carbonic Limestone Bicarbonate Acid

20 A. Solution“the dissolving of a rock”
More recently….. 2SO H2O + O2 = H2SO4

21 A. Solution“the dissolving of a rock”
More recently….. 2SO H2O + O2 = H2SO4 Sulfur Sulfuric Dioxide Acid

22 B. Hydration “chemically adding water to a rock”
CaSO H2O = CaSO4 * 2 H20 Anhydrite Gypsum

23 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

24 D. Oxidation: “process of rusting; the taking away of electrons”
Fe2+ >>>> Fe3+ Ferrous Ferric (dark) (red)

25 D. Oxidation: “process of rusting; the taking away of electrons”
Fe2+ >>>> Fe3+ Ferrous Ferric (dark) (red) 4Fe O2 = 2Fe2O3 iron hematite ore

26 III. Rates of Weathering
A. Climate

27 III. Rates of Weathering
A. Climate B. Rock Structure, Size, Composition


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