Numerical simulation of the formation of groundwater chemical components in the Mayukou area, Datong, China
The amounts of dissolved primary minerals, precipitated secondary minerals and the aqueous chemical components were determined in groundwater in the Mayukou area, Datong, China by numerical simulation and by using a mathematical model involving the chemical equilibrium for a multiphase, multimineral, multi-component system, and the mass transfer theory developed by Helgeson. The calculated values of chemical components of the groundwater and the determined water chemical type were in concordance with real measured results. This model further simulated and validated the mechanism of the zoning of water chemical types, element transfer, and differentiation, as well as the process controlling the mineral sequence.
W.Zhang Y.Cao J.Jiang W.Wang L.Duan
State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry,Chinese Academy of College of Environment and Resources, Jilin University, Changchun, Jilin Province, P.R.China College of Environment Science and Engineering, Changan University, Xian, Shanxi Province, P.R.China
国际会议
第十二届水-岩相互作用国际研讨会(P0roceedings of the 12th International Symposium on Water-Rock Interaction)
昆明
英文
407-411
2007-07-31（万方平台首次上网日期，不代表论文的发表时间）