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Latest revision as of 01:07, 9 May 2018
Figure 1. Hydraulic gradient (typically described in units of m/m or ft/ft) is the difference in hydraulic head from Point A to Point B (ΔH) divided by the distance between them (ΔL). In unconfined aquifers, the hydraulic gradient can also be described as the slope of the water table. (Adapted from course notes developed by Dr. R.J. Mitchell, Western Washington University)
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 01:07, 9 May 2018 |  | 650 × 708 (139 KB) | Jhurley (talk | contribs) | |
| 00:56, 9 May 2018 |  | 650 × 708 (92 KB) | Jhurley (talk | contribs) | Reverted to version as of 12:33, 2 September 2016 (MDT) | |
| 00:55, 9 May 2018 |  | 550 × 599 (103 KB) | Jhurley (talk | contribs) | changed Well 2 label | |
| 18:33, 2 September 2016 |  | 650 × 708 (92 KB) | Debra Tabron (talk | contribs) | Figure 1. Hydraulic gradient (typically described in units of m/m or ft/ft) is the difference in hydraulic head from Point A to Point B (ΔH) divided by the distance between them (ΔL). In unconfined aquifers, the hydraulic gradient can also be describ... |
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