| dc.contributor.author | Crouch, Scott Thomas | |
| dc.date.accessioned | 2015-01-27T21:17:51Z | |
| dc.date.available | 2015-01-27T21:17:51Z | |
| dc.date.issued | 1989-12-01 | |
| dc.identifier.uri | https://hdl.handle.net/11244/14148 | |
| dc.description.abstract | The Sundre aquifer was studied in order to determine the source of the sulfate, which occurs in concentrations over 1,000 mgjl. An analytical version of the solutetransport model "Random-Walk" was used to simulate the movement of sulfate in the sundre aquifer. The sulfate was determined to be the result of the oxidation of organic sulfides, present in the till which mantles the bedrock. The analytical version of the solute-transport model was not capable of predicting sulfate levels in the Sundre well field. | |
| dc.format | application/pdf | |
| dc.language | en_US | |
| dc.publisher | Oklahoma State University | |
| dc.rights | Copyright is held by the author who has granted the Oklahoma State University Library the non-exclusive right to share this material in its institutional repository. Contact Digital Library Services at lib-dls@okstate.edu or 405-744-9161 for the permission policy on the use, reproduction or distribution of this material. | |
| dc.title | Hydrogeochemical Interpretation and Computer Simulation of the Sundre Aquifer, Minot, North Dakota | |
| dc.type | text | |
| osu.filename | Thesis-1989-C952h.pdf | |
| osu.accesstype | Open Access | |
| dc.description.department | Geology | |
| dc.type.genre | Thesis | |
