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Calcium and bromide contents of natural waters

Science

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Abstract

The linear relation observed in a log Ca++ versus log Br - plot for subsurface Cl- waters is attributed to ultrafiltration by shale of sea water and fresh water that have passed through sedimentary rocks since their formation. Reactions between these solutions and sedimentary minerals, particularly dolomitization, must have contributed additional Ca+ + to solution.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Calcium and bromide contents of natural waters
Series title:
Science
Volume
153
Issue:
3744
Year Published:
1966
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Science
First page:
1637
Last page:
1638
Number of Pages:
2