Applications of Aqueous Geochemistry to Weathering Studies - PowerPoint PPT Presentation

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Applications of Aqueous Geochemistry to Weathering Studies

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Title: Applications of Aqueous Geochemistry to Weathering Studies


1
Applications of Aqueous Geochemistry to
Weathering Studies
  • Michael Fortwengler
  • Joniell Borges

2
What is weathering?
  • Physical
  • No chemical change involved
  • Weathering vs Erosion
  • Chemical
  • Chemical change involved
  • Biological
  • Organic acids
  • Chelation

3
Types of Chemical Weathering
  • Hydrolysis
  • 2NaAlSi3O8 2H 9H2O H4Al2Si2O9 4H4SiO4
    2Na
  • Hydration/Dehydration
  • CaSO4.2H2O CaSO4 2H2O
  • Oxidation/Reduction
  • FeSiO3 O2 2Fe2O3 4SiO2
  • Solution
  • H2O CO2 CaCO3 Ca2 2HCO3-
  • Ion Exchange
  • Na-clay H H-clay Na
  • Chelation
  • Metal ions (cations) chelating agent (from
    lichens) H chelateaq

4
Why is chemical weathering important?
  • Climate change
  • Drawdown of greenhouse gases (pCO2)
  • Global Climate Modeling (Past, Present, Future)
  • Anthropogenic vs Natural Weathering
  • Acid Mine Drainage
  • Groundwater Contamination
  • Acid Rain
  • Landscape Evolution (Geomorphology)

5
Climate Change Record
Petit et al., 1999
6
CO2 Sources Sinks
  • Sources
  • Volcanism
  • Respiration
  • Fossil Fuel Burning
  • Sinks
  • Silicate Weathering
  • Photosynthesis
  • Organic Burial

7
Weathering Reactions
  • Silicate Weathering (net pCO2 drawdown)
  • CO2(g) H2O H2CO3
  • CaSiO3 2H2CO3 H2O Ca2 2HCO3- H4SiO4
  • Ca2 2HCO3- CaCO3 CO2 H2O
  • Net Reaction
  • CaSiO3 CO2(g) 2H2O CaCO3 H4SiO4
  • Carbonate Weathering (no net effect on pCO2)
  • CaCO3 CO2 H2O Ca2 2HCO3-
  • Ca2 2HCO3- CaCO3 CO2 H2O
  • Evaporite Weathering
  • NaCl Na Cl-
  • CaSO4 Ca2 SO42-

Urey, 1953
8
Amazon River
Stallard and Edmond, 1993
9
Silicate vs Carbonate Terrains
Stallard and Edmond, 1983
10
Calcite Saturation State
Huh and Edmond, 1999
11
Conclusions
  • Chemical weathering involves a number of aqueous
    geochemistry reactions
  • Silicate weathering and climate change might be
    closely coupled
  • Studying the geochemistry of current river
    systems may allow us to derive silicate
    weathering rates related to climate change
  • Ancient climate systems can be studied by
    discovering sedimentary geochemical tracers
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