Weathering - PowerPoint PPT Presentation

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Weathering

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... Africa) Chemical weathering an important means of denudation Soil Based View of Weathering: Chemical Mass Balance (Brimhall and others) ... – PowerPoint PPT presentation

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Title: Weathering


1
Weathering
  • Types
  • Physical or mechanical (increases surface area)
  • Chemical (chemical transformations)
  • Congruent (complete dissolution)
  • Incongruent (solids dissolved products)

2
Factors Controlling Chemical Weathering Rates
  • Mineralogy
  • Surface area
  • pH
  • Temperature
  • Organic acids
  • Rate d(mineral mass)/dt -KA
  • Where A surface area and Kparameter reflecting
    all other controls

3
Effect of Mineral Type
  • In general, rate decreases with
  • Increasing tetrahedral linkages
  • 2. Less Al for Si.

Faster than olivine
Slower than olivine
4
Measuring Weathering Rates
  • Streams
  • Instantaneous measures
  • Integrates area
  • Soils
  • Integrates time
  • Site specific

5
EBMUD Water Chemistry and Mineral Weathering
6
Sierran Spring Chemistry and EBMUD Water
  • Lafayette 2.4 1.1 0.4 0.13 2.8
  • Orinda 3.3 1.8 0.6 0.15 5.4

7
Typical Weathering Reactions
  • Reaction medium consists of water and CO2
  • Products kaolinite and gibbsite plus dissolved
    products

8
Sierran Spring Chemistry and EBMUD Water
  • Lafayette 2.4 1.1 0.4 0.13 2.8
  • Orinda 3.3 1.8 0.6 0.15 5.4
  • Subtract contribution from rain (i.e. assume all
    Cl and SO4 from rain - balanced by Na)
  • Assume all Mg derived from biotite
  • .15(B).15(H2CO3).15(.5H20).15(K).15(3Mg).15(7
    HCO3).15(2H4SiO4).15(.5 Kaol)
  • Assume all K from K spar

9
Chemical vs. Mechanical Weathering Role of
Climate and Geology
  • Recently glaciated, tectonically active areas
    have high chemical weathering rates
  • Areas of long term stability (and long weathering
    history have lower rates (Aust, Africa)
  • Chemical weathering an important means of
    denudation

10
Soil Based View of Weathering Chemical Mass
Balance (Brimhall and others)
  • Give soil profile based perspectives
  • Depth variations
  • Climate variations
  • Age variations
  • Gives us view of both physical and chemical
    changes in soils during development
  • Soils commonly undergoe initial expansion
    followed by collapse
  • Soils, given enough time, can become chemically
    depleted and must rely on atmospheric inputs
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