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Geochemistry of Shallow Ground Water in the Fort Union Formation of the Northern Power River Basin, Southeastern Montana
| Content Provider | Semantic Scholar |
|---|---|
| Author | Lee, Roger W. |
| Copyright Year | 1993 |
| Abstract | Abstract. Shallow water in the coal-bearing Paleocene Fon Union Fom1ation of southeastern Montana was investigated to provide a better understanding of the geochemistry. Springs, wells less than 200 feet deep, and wells greater than 200 feet deep were observed to have different water qualities. Overall, the ground water exists as two systems: a mosaic of shallow, chemically dynamic, and localized recharge-discharge cells superimposed on a deeper, chemically static regional system. Water chemistry is highly variable in the shallow system, whereas sodium and bicarbonate waters characterize the deeper system. |
| Starting Page | 249 |
| Ending Page | 265 |
| Page Count | 17 |
| File Format | PDF HTM / HTML |
| DOI | 10.21000/JASMR93010249 |
| Volume Number | 1993 |
| Alternate Webpage(s) | https://www.asmr.us/Portals/0/Documents/Conference-Proceedings/1993/0249-Lee.pdf |
| Alternate Webpage(s) | https://doi.org/10.21000/JASMR93010249 |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |