BEHAVIOR OF MAJOR SOLUTES DURING CLOSED-BASIN BRINE EVOLUTION

被引：293

作者：

EUGSTER, HP ^{[1
]}

JONES, BF ^{[1
]}

机构：

[1] US GEOL SURVEY,RESTON,VA 22092

来源：

AMERICAN JOURNAL OF SCIENCE | 1979年 / 279卷 / 06期

关键词：

D O I：

10.2475/ajs.279.6.609

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The pronounced chemical fractionation that takes place in hydro logically closed basins between dilute inflow and concentrated brines can be accounted for by a variety of mechanisms. These include mineral precipitation, selective dissolution of efflorescent crusts and sediment coatings, sorption on active surfaces, degassing, and reactions. Major solutes are differentially affected by these mechanisms, and their response may differ from basin to basin. Using data from Lake Magadi, Kenya; Lake Abert, Oreg; Devils Lake, N. Dak; Deep Springs Lake, Calif.; Basque Lake, British Columbia; and Great Salt Lake, Utah, some of these differences can be delineated. -from Authors

引用

页码：609 / 631

页数：23

共 51 条

[1]

ALDROUBI A, 1976, 46 U L PAST MEM

[2] ADSORPTION AND DESORPTION OF SULFATE IONS BY SOIL CONSTITUENTS [J].