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	<title>File:Newell-Article 1-Fig1r.JPG - Revision history</title>
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	<updated>2026-04-15T13:51:22Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<id>https://www.enviro.wiki/index.php?title=File:Newell-Article_1-Fig1r.JPG&amp;diff=11616&amp;oldid=prev</id>
		<title>Jhurley: 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...</title>
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		<updated>2018-05-09T01:12:43Z</updated>

		<summary type="html">&lt;p&gt;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...&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;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)&lt;/div&gt;</summary>
		<author><name>Jhurley</name></author>
		
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