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Hydraulic Conductivity of Ohio's Glaciated Soil, Its Implications, and Suggestions for Future Studies
Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/23940
| Files | Size | Format | View |
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| V102N5_106.pdf | 364.6Kb |
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| Title: | Hydraulic Conductivity of Ohio's Glaciated Soil, Its Implications, and Suggestions for Future Studies |
| Creators: | Fisher, Henry H. |
| Issue Date: | 2002-12 |
| Citation: | The Ohio Journal of Science. v102, n5 (December, 2002), 106-109 |
| Abstract: | Since 1999, hydraulic conductivity values in till have been measured by the laboratory standard test method ASTM D 5084 on undisturbed soil samples taken at depths between 3.0 m to 6.0 m (10 to 20 ft) in glacial till soils in western Ohio. Their rates on uncracked soil vary from 106 cm/sec to 109 cm/sec. Measurements made on till with cracks vary from 105cm/sec to 10 8 cm/sec. Suggestions are made for future studies. |
| URI: | http://hdl.handle.net/1811/23940 |
| ISSN: | 0030-0950 |
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