Abstract
Measurements of the sodium and chloride ions activity product in Dead Sea brines before and after their equilibrium with halite show that the upper 40 m of the brine column are undersaturated, whereas the brine below 100 m is uniformly very close to saturation with respect to halite. The 40-100 m layer exhibits strong saturation gradients. Independent calculation of the ion activity products produces a similar picture although the results are consistently higher than the measured values by 15-20 percent.
Original language | English (US) |
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Pages (from-to) | 63-66 |
Number of pages | 4 |
Journal | Earth and Planetary Science Letters |
Volume | 5 |
Issue number | C |
DOIs | |
State | Published - 1968 |
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology
- Earth and Planetary Sciences (miscellaneous)
- Space and Planetary Science