Hydrogeochemical processes in closed and open water-rock systems

被引：3

作者：

Ryzhenko, B. N. ^{[1
]}

Cherkasova, E. V. ^{[1
]}

机构：

[1] Russian Acad Sci, Vernadsky Inst Geochem & Analyt Chem, Moscow 119991, Russia

来源：

PETROLOGY | 2011年 / 19卷 / 01期

关键词：

SALINE GROUNDWATERS;

D O I：

10.1134/S0869591111010073

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Numerical simulations of water-rock systems based on D.S. Korzhinskii's hypothesis of the openness-closedness of natural systems indicates that the composition of groundwaters evolves into Cl-Na-Ca brines at increasing R/W ratios (rations of reacting rock and water masses) and when the system becomes closed (a decrease in the CO(2) partial pressure) or into HCO(3)-Cl-Na brines at a decrease in the R/W ratio and the opening of the system with respect to CO(2) (increase of P (CO) (2)).

引用

页码：26 / 33

页数：8

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