| Abstract: | A two-component soil water flow model was used in conjunction with an equilibrium speciation model WATEQF to study aluminum mobility in soils of a forested watershed, White Oak Run, in the Shenandoah National Park, Virginia. The deep soil is a sink for aluminum. Mineral solubility controls water chemistry in the deep soil, while organic substances are the key control in the shallow macropore waters. -from Authors |
| Genre: | Article |
| ProdID: | 70014112 |
| Citation Author: | Cozzarelli, I. M.; Herman, J. S.; Parnell, Jr, R. A. |
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| Citation End Page: | 874 |
| Citation Issue: | 5 |
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| Citation Language: | English |
| Citation Larger Work Title: | Water Resources Research |
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| Citation Number Of Pages: | 16 |
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| Citation Search Results Text: | The mobilization of aluminum in a natural soil system: effects of hydrologic pathways; 1987; Article; Journal; Water Resources Research; Cozzarelli, I. M.; Herman, J. S.; Parnell, Jr, R. A. |
| Citation Start Page: | 859 |
| Citation Volume: | 23 |
| Citation Year: | 1987 |
| Type: | citation/reference |
| Text: | The mobilization of aluminum in a natural soil system: effects of hydrologic pathways; 1987; Article; Journal; Water Resources Research; Cozzarelli, I. M.; Herman, J. S.; Parnell, Jr, R. A. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Thu, 1 Jan 1987 00:00 -0600 |
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