| 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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