| Abstract: | Combines geochemical mixing theory with the hydrodynamics of fresh-water-salt-water mixing zones in a coupled reaction-transport model. Results from the reaction-path model PHREEQE are used with a variable-density groundwater flow and solute-transport model to simulate an idealized cross section of a coastal carbonate aquifer. The dissolution process is sensitive to fresh-water chemistry, groundwater velocities, and sea-level movement. -from Authors |
| Genre: | Article |
| ProdID: | 70015754 |
| Citation Author: | Sanford, W. E.; Konikow, L. F. |
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| Citation End Page: | 252 |
| Citation Issue: | 3 |
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| Citation Language: | English |
| Citation Larger Work Title: | Geology |
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| Citation Number Of Pages: | 4 |
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| Citation Search Results Text: | Porosity development in coastal carbonate aquifers; 1989; Article; Journal; Geology; Sanford, W. E.; Konikow, L. F. |
| Citation Start Page: | 249 |
| Citation Volume: | 17 |
| Citation Year: | 1989 |
| Type: | citation/reference |
| Text: | Porosity development in coastal carbonate aquifers; 1989; Article; Journal; Geology; Sanford, W. E.; Konikow, L. F. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sun, 1 Jan 1989 00:00 -0600 |
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