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Various topics in the field of geochemistry, including the annual input of so4 into the oceans, the calculation of its residence time, the alkalinity of seawater, the charge balance equation, weathering of a sediment, and the precipitation of chemicals in soils. Students can use this document for understanding the principles of geochemistry, calculating residence times, and balancing charge equations.
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1. The oceans a. The annual input of SO 4 2-^ into the oceans by rivers is estimated to be 3 x 10^12 mole/yr. If SO 4 2-^ were at a steady-state concentration in sea water and the only significant sulfate input to the oceans were the river flux, what would the residence time of SO 4 2-^ in the oceans be? The mass of the oceans is 1.4 x 10^24 g and the SO 4 2- concentration in the oceans is 0.028 mol/kg
b. If there were no SO 4 2-^ flux out of the oceans to balance the above input flux, so that its concentration was constantly building up due to the river flux, how long would it take to increase the SO 4 2-^ concentration by 15%
2. Hydrosphere composition a. What is the Alkalinity of seawater of the following composition: Na+^ 0.481 M Cl-^ 0.560 M Mg2+^ 0.0544 M SO 4 2-^ 0.0283 M Ca2+^ 0.011 M HCO 3 -^ 0.00238 M K+^ 0.011 M
b. write the charge balance equation for this solution and substitute in the numbers above. Is this solution balanced? If not, what other ion(s) that are not listed might be present in seawater to help balance the charge?
3 Weathering A sediment has a CEC of 70 meq/100 g. The following exchangeable cations make up the CEC: Ca2+^ , Mg2+^ , Na+^ , K+^ and H+^. The first 4 were measured at concentrations of 19, 5.9, 4.1 and 1.2 meq/100g, respectively. What is the ECS of H+^ on this sediment?
4. Soils a. Name 2 chemicals (or minerals) that precipitate from soil water as the pH changes
b. what is the name of the soil zone where the precipitation occurs?