Titlebook: Eh-pH Diagrams for Geochemistry; Douglas G. Brookins Book 1988 Springer-Verlag Berlin Heidelberg 1988 carbon.chemistry.environment.geochem

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Bismuth, of bismuth are complex. The species Bi.O. is stable with respect to and Bi.,BiO. BiO., and BiOH.based on the avialable thermodynamic data (Table 11). The oxide Bi.O. occupies much of the Eh-pH field above the sulfide- sulfate boundary, and is replaced by Bi.O. at pH between 5.5 and 6 for activities

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Book 1988nt, including transuranic and other radioactive species. For each of these newly calculated diagrams short explanatory texts are added. For the first time the primary elements are considered in water with metal, sulfur, carbon, and other species as appropriate. Furthermore, based on these figures an

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,Univariate H?ufigkeitsverteilungen, of dissolved Bi of 10. and 10., respectively. Under sulfide-stable conditions, Bi.S., bismuthinite, occupies most of the Eh-pH space with a field of native bismuth appearing at high pH, reducing conditions.

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Bismuth, of dissolved Bi of 10. and 10., respectively. Under sulfide-stable conditions, Bi.S., bismuthinite, occupies most of the Eh-pH space with a field of native bismuth appearing at high pH, reducing conditions.

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Book 1988d up-to-date thermodynamic data presented in this reference, researchers can predict the behavior of elements in the surface environment. Geoscientists, chemists and environmental agencies will also benefit from several brief texts on the importance of various elements to problems of radioactive waste disposal.

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