Calcium and bromide contents of natural waters
Science
By: R.J. Anderson, D. L. Graf, and B.F. Jones
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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.
Suggested Citation
Anderson, R., Graf, D.L., and Jones, B., 1966, Calcium and bromide contents of natural waters: Science, v. 153, no. 3744, p. 1637-1638, https://doi.org/10.1126/science.153.3744.1637.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Calcium and bromide contents of natural waters |
| Series title | Science |
| DOI | 10.1126/science.153.3744.1637 |
| Volume | 153 |
| Issue | 3744 |
| Year Published | 1966 |
| Language | English |
| Publisher | American Association for the Advancement of Science |
| Description | 2 p. |
| First page | 1637 |
| Last page | 1638 |