作者: James L. Palandri , Yousif K. Kharaka
DOI: 10.3133/OFR20041068
关键词: Mass transfer 、 Mineralogy 、 Porosity 、 Rate equation 、 Aquifer 、 Geochemical modeling 、 Chemistry 、 Fluid dynamics 、 Volumetric flow rate 、 Reaction 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 …