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Language: English

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Pages: 558

Publisher: Springer; Softcover reprint of the original 1st ed. 1987 edition (November 20, 2011)

ISBN: 3642711391

Groundwater Geochemistry and Isotopes

For example, if a and b are both 2 then j is 2 and and are both 1. In other words, the isotopic compositions of mixtures are intermediate between the compositions of the endmembers. Note that a total sulfur concentration of 0.002 molal units is about 200 mg/l which is higher than normal ba about a factor of 4 but the total inorganic carbon concentration is about average. 3) Pb(OH)2 + 2H+ = Pb2+ + 2H2O; log K3 = 8.2 8) HS- + H+ = H2So; log K8 = 7.0 9) SO42- + 9H+ + 8e- = HS- + 4H2O; log K9 = 34.0 13) 2H+ + 2e- = H2; log K13 = 0 14) O2 + 4H+ + 4e- = 2H2O; log K14 = 83.1 As previously shown the retardation factor for the downstream movement of the concentration front of contaminant A can be predicted using a mass balance across the front.

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Petroleum Geochemistry and Geology (A Series of books in geology)

Mineralium Deposita, International Journal for Geology, Mineralogy and Geochemistry of Mineral Deposits. Official Bulletin of the Society for Geology Applied to Mineral Deposits, 2003, Mineralium Deposita, Volume 38, Number 6 : .

Mineralium Deposita, International Journal for Geology, Mineralogy and Geochemistry of Mineral Deposits. Official Bulletin of the Society for Geology Applied to Mineral Deposits, 1997, Mineralium Deposita, Volume 32, Number 3 : .

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Mineralium Deposita, International Journal for Geology, Mineralogy and Geochemistry of Mineral Deposits. Official Bulletin of the Society for Geology Applied to Mineral Deposits, 1973, Mineralium Deposita, Volume 8, Number 4 : .

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