A Compilation of Rate Parameters of Water-Mineral Interaction Kinetics for Application to Geochemical Modeling

作者: James L. Palandri , Yousif K. Kharaka

DOI: 10.3133/OFR20041068

关键词: Mass transferMineralogyPorosityRate equationAquiferGeochemical modelingChemistryFluid dynamicsVolumetric flow rateReaction rate

摘要: Geochemical reaction path modeling is useful for rapidly assessing the extent of water-aqueous-gas interactions both in natural systems and in industrial processes. Modeling of some …

参考文章(274)
Jacques Schott, Robert A. Berner, Dissolution Mechanisms of Pyroxenes and Olivines During Weathering Springer Netherlands. pp. 35- 53 ,(1985) , 10.1007/978-94-009-5333-8_3
W. J. Ullman, S. A. Welch, Dissolution of Feldspars in Oxalic Acid Solutions ,(1992)
E. Busenberg, L. N. Plummer, The kinetics of dissolution of dolomite in CO 2 -H 2 O systems at 1.5 to 65 degrees C and O to 1 atm PCO 2 American Journal of Science. ,vol. 282, pp. 45- 78 ,(1982) , 10.2475/AJS.282.1.45
H.L. Barnes, Chie Soong, Precipitation and dissolution kinetics of kaolinite under hydrothermal conditions Geological Society of America, Abstracts with Programs; (United States). ,(1992)
Roy A Wogelius, John V Walther, Olivine dissolution at 25°C: Effects of pH, CO2, and organic acids Geochimica et Cosmochimica Acta. ,vol. 55, pp. 943- 954 ,(1991) , 10.1016/0016-7037(91)90153-V
Roland Wollast, Lei Chou, F.J. Huertas, Mechanism of kaolinite dissolution at room temperature and pressure International Clay Conference. ,(1997)
Hubert Lloyd Barnes, Geochemistry of Hydrothermal Ore Deposits ,(1968)