File:Newell-Article 1-Fig1r.JPG
Revision as of 01:12, 9 May 2018 by Jhurley (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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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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current | 01:12, 9 May 2018 | 650 × 708 (139 KB) | Jhurley (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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