Dead sea brines: Degree of halite saturation by electrode measurements

Abraham Lerman*, Adam Shatkay

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

13 Scopus citations

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 languageEnglish (US)
Pages (from-to)63-66
Number of pages4
JournalEarth and Planetary Science Letters
Volume5
Issue numberC
DOIs
StatePublished - 1968

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Fingerprint

Dive into the research topics of 'Dead sea brines: Degree of halite saturation by electrode measurements'. Together they form a unique fingerprint.

Cite this