Calcium and bromide contents of natural waters
January 1, 1966
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.
Citation Information
| Publication Year | 1966 |
|---|---|
| Title | Calcium and bromide contents of natural waters |
| Authors | R.J. Anderson, D. L. Graf, B.F. Jones |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Science |
| Index ID | 70010738 |
| Record Source | USGS Publications Warehouse |