Titlebook: Kinetics of Water-Rock Interaction; Susan L. Brantley,James D. Kubicki,Art F. White Book 2008 Springer-Verlag New York 2008 Desorption.Dis

RECUR

Kinetics of Mineral Dissolution,ion of contaminants and CO., cycling of metals and formation of ore deposits, and many other geochemical characteristics and phenomena. For example, the weathering rates of Ca- and Mg-silicates influence the concentrations of CO. in the atmosphere over 10.–10. y timescales, impacting the global carb

加劇

廢止

加劇

macabre

Microbiological Controls on Geochemical Kinetics 2: Case Study on Microbial Oxidation of Metal Sulfcally as sources of sulfuric acid and metals, such as Co, Cu, Au, Ni, and Zn that are present either as discrete sulfide phases (e.g., CuS, Gu.S, NiS, ZnS) or coprecipitates with major iron-sulfide phases such as FeS. (e.g., chalcopyrite, CuFeS.). However, in many situations, sulfide minerals (in pa

seroma

有罪

Perennial長(zhǎng)期的

Isotope Geochemistry as a Tool for Deciphering Kinetics of Water-Rock Interaction,f routine techniques of mass spectrometry, an impressive number of studies have used isotopes to constrain water-rock interaction processes. A number of these initial studies were not purposefully designed to determine the kinetics of water-rock interaction, but they demonstrated that isotopic kinet

碳水化合物

車床

Susan L. Brantley,Christine F. Conradinn Féin/Irish Republican Army (IRA) is analyzed as a 2 × 2 game. The unique Nash equilibrium in this game is shown not to predict the recent behavior of and Sinn Féin/IRA, which declared a cease-fire in September 1994, resumed its bombing campaign in February 1996, and reinstituted a cease-fire in