Gaylussite formation at mono lake, california

The salinity of Mono Lake has steadily increased since 1941 from 50%. to about 90%. due to diversion of tributary streams. This increase has resulted in the newly discovered precipitation of gaylussite (Na 2Ca(CO 3) 2 · 5H 2O). Chemical modeling of the lake water using Pitzer equations suggests that...

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Veröffentlicht in:	Geochimica et cosmochimica acta 1991-06, Vol.55 (6), p.1743-1747
Hauptverfasser:	Bischoff, James L., Herbst, David B., Rosenbauer, Robert J.
Format:	Artikel
Sprache:	eng
Schlagworte:	580000 - Geosciences ALKALI METAL COMPOUNDS ARAGONITE CALIFORNIA CARBON COMPOUNDS CARBONATE MINERALS CARBONATES CHEMISTRY DEVELOPED COUNTRIES GEOCHEMISTRY GEOLOGIC DEPOSITS GEOSCIENCES LAKES MINERALIZATION MINERALS NORTH AMERICA OXYGEN COMPOUNDS PRECIPITATION SALINITY SALT DEPOSITS SATURATION SEPARATION PROCESSES SODIUM CARBONATES SODIUM COMPOUNDS SUPERSATURATION SURFACE WATERS USA
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