THE SOLUBILITY OF HALITE AS A FUNCTION OF TEMPERATURE IN THE HIGHLY SALINE DEAD-SEA BRINE SYSTEM

被引：33

|

作者：

GAVRIELI, I ^{[1
]}

STARINSKY, A ^{[1
]}

BEIN, A ^{[1
]}

机构：

[1] GEOL SURVEY ISRAEL,IL-95501 JERUSALEM,ISRAEL

来源：

LIMNOLOGY AND OCEANOGRAPHY | 1989年 / 34卷 / 07期

关键词：

D O I：

10.4319/lo.1989.34.7.1224

中图分类号：

Q [生物科学];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

引用

收藏

页码：1224 / 1234

页数：11

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[2] SOLUBILITY OF OXYGEN IN THE DEAD-SEA BRINE
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[3] LITHIUM PRODUCTION FROM HIGHLY SALINE DEAD-SEA BRINES
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[4] HEAVY-METALS IN THE DEAD-SEA AND THEIR COPRECIPITATION WITH HALITE
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[5] SURFACE MANIFESTATIONS OF INTERNAL OSCILLATIONS IN A HIGHLY SALINE LAKE (THE DEAD-SEA)
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[6] SOLUBILITIES OF GYPSUM AND HALITE IN THE DEAD-SEA AND IN ITS MIXTURES WITH SEAWATER
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[7] HYPERSALINE BRINE DIAGENESIS AND EVOLUTION IN THE DEAD-SEA LAKE LISAN SYSTEM (ISRAEL)
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[8] THE GEOCHEMICAL EVOLUTION OF HALITE STRUCTURES IN HYPERSALINE LAKES - THE DEAD-SEA, ISRAEL
GANOR, J
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[9] DISSOLUTION, TRANSPORT AND CRYSTALLIZATION OF HALITE IN HYPERSALINE LAKES - THE DEAD-SEA, ISRAEL
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[10] CL-36 IN A HALITE LAYER FROM THE BOTTOM OF THE DEAD-SEA
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LEVY, Y
FINK, D
MEIRAV, O
PAUL, M
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