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Material Type: Assignment; Class: CHEMICAL OCEAN; Subject: Oceanography; University: University of Washington - Seattle; Term: Winter 2009;
Typology: Assignments
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Propose an approach to calculate how much CO 2 (atm) is consumed by weathering of b) carbonate rocks (CaCO 3 ) c) silicate rocks hint: Assume all Si comes from silicate rocks. Calculate the HCO 3 -^ that weathering produces. Then calculate the HCO 3 -^ that comes from weathering of carbonate rocks. As a check, if all the Ca2+^ comes from weathering CaCO 3 then Ca should equal 0.5 x HCO 3 - from carbonate weathering. You will find that it doesn’t. The reason is that some carbonate rocks are MgCO 3 or CaMg(CO 3 ) 2.
d) From your model, what is the total amount of CO 2 consumed by weathering (in PgC y -1^ )? Use a total world river flow of 3.7 x 10^16 L y-^.
e) How does your rate compare with that of Sarmiento and Gruber (2002) as shown in their Figure 1.
f) How does the weathering ratio of CaCO 3 /silicate rocks compare with the outcrop abundance of carbonate sedimentary rocks to silicate rocks. See the attached table from Meybeck (1987, American Journal of Science, 287, 401-428). If the weathering ratio differs from the outcrop ratio, suggest why.