Автор |
Turk, L. J. |
Дата выпуска |
1970 |
dc.description |
Evaporation rates were determined for seven brines whose average specific gravities varied from 1.207 to 1.333. Evaporation of the brines ranged from 70% to 9.5%, respectively, of the freshwater evaporation rate. The field data agree exceptionally well with differential vapor pressures over Great Salt Lake brine, measured in the laboratory by Dickson et al. [1965]. Water occasionally condenses on the heavier brines because of an inverted vapor pressure gradient. |
Формат |
application.pdf |
Копирайт |
Copyright 1970 by the American Geophysical Union. |
Название |
Evaporation of Brine: A Field Study on the Bonneville Salt Flats, Utah |
Тип |
shortCommunication |
DOI |
10.1029/WR006i004p01209 |
Electronic ISSN |
1944-7973 |
Print ISSN |
0043-1397 |
Журнал |
Water Resources Research |
Том |
6 |
Первая страница |
1209 |
Последняя страница |
1215 |
Выпуск |
4 |
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Библиографическая ссылка |
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