https://www.enviro.wiki/index.php?action=history&feed=atom&title=File%3ANewell-Article_1-Fig1.JPGFile:Newell-Article 1-Fig1.JPG - Revision history2026-04-17T01:30:07ZRevision history for this page on the wikiMediaWiki 1.31.1https://www.enviro.wiki/index.php?title=File:Newell-Article_1-Fig1.JPG&diff=11615&oldid=prevJhurley: Jhurley uploaded a new version of File:Newell-Article 1-Fig1.JPG2018-05-09T01:07:31Z<p>Jhurley uploaded a new version of <a href="/index.php?title=File:Newell-Article_1-Fig1.JPG" title="File:Newell-Article 1-Fig1.JPG">File:Newell-Article 1-Fig1.JPG</a></p>
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</td></tr></table>Jhurleyhttps://www.enviro.wiki/index.php?title=File:Newell-Article_1-Fig1.JPG&diff=2877&oldid=prevDebra Tabron: 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...2016-09-02T18:33:45Z<p>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...</p>
<p><b>New page</b></p><div>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)</div>Debra Tabron