File:Newell-Article 1-Fig1.JPG

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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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current01:07, 9 May 2018Thumbnail for version as of 01:07, 9 May 2018650 × 708 (139 KB)Jhurley (talk | contribs)
00:56, 9 May 2018Thumbnail for version as of 00:56, 9 May 2018650 × 708 (92 KB)Jhurley (talk | contribs)Reverted to version as of 12:33, 2 September 2016 (MDT)
00:55, 9 May 2018Thumbnail for version as of 00:55, 9 May 2018550 × 599 (103 KB)Jhurley (talk | contribs)changed Well 2 label
18:33, 2 September 2016Thumbnail for version as of 18:33, 2 September 2016650 × 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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