| Abstract: | During 1983 and 1984, wet precipitation was primarily a solution of dilute sulphuric acid, whereas calcium and bicarbonate were the major ions in springs and ground water in two small watersheds with a deciduous forest cover in central Maryland. Dominant ions in soil water were calcium, magnesium, and sulphate. The relative importance of mineral weathering reactions on the chemical composition of these subsurface waters was compared to the contribution from wet precipitation, biological processes, and road deicing salts. -from Author |
| Genre: | Article |
| ProdID: | 70015613 |
| Citation Author: | Katz, B. G. |
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| Citation End Page: | 202 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Hydrological Processes |
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| Citation Number Of Pages: | 18 |
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| Citation Search Results Text: | Influence of mineral weathering reactions on the chemical composition of soil water, springs, and ground water, Catoctin Mountains, Maryland; 1989; Article; Journal; Hydrological Processes; Katz, B. G. |
| Citation Start Page: | 185 |
| Citation Volume: | 3 |
| Citation Year: | 1989 |
| Type: | citation/reference |
| Text: | Influence of mineral weathering reactions on the chemical composition of soil water, springs, and ground water, Catoctin Mountains, Maryland; 1989; Article; Journal; Hydrological Processes; Katz, B. G. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sun, 1 Jan 1989 00:00 -0600 |
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