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	<title>Paranormal operator - Revision history</title>
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	<updated>2026-05-25T13:32:19Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<id>https://en.formulasearchengine.com/index.php?title=Paranormal_operator&amp;diff=23677&amp;oldid=prev</id>
		<title>en&gt;Qetuth: more specific stub type</title>
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		<updated>2011-12-18T07:16:04Z</updated>

		<summary type="html">&lt;p&gt;more specific stub type&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;#039;&amp;#039;&amp;#039;Differential stress&amp;#039;&amp;#039;&amp;#039; is the difference between the greatest and the least [[compressive stress]] experienced by an object. For both the [[geology|geological]] and [[civil engineering]] convention  &amp;lt;math&amp;gt;\sigma_1&amp;lt;/math&amp;gt; is the greatest compressive stress and &amp;lt;math&amp;gt;\sigma_3&amp;lt;/math&amp;gt; is the weakest,&lt;br /&gt;
&lt;br /&gt;
&amp;lt;math&amp;gt;\!\sigma_D = \sigma_1 - \sigma_3&amp;lt;/math&amp;gt;.&lt;br /&gt;
&lt;br /&gt;
In other [[engineering]] fields and in [[physics]], &amp;lt;math&amp;gt;\sigma_3&amp;lt;/math&amp;gt; is the greatest compressive stress and &amp;lt;math&amp;gt;\sigma_1&amp;lt;/math&amp;gt; is the weakest, so&lt;br /&gt;
&lt;br /&gt;
&amp;lt;math&amp;gt;\!\sigma_D = \sigma_3 - \sigma_1&amp;lt;/math&amp;gt;.&lt;br /&gt;
&lt;br /&gt;
These conventions originated because geologists and civil engineers (especially [[soil mechanics|soil mechanicians]]) are often concerned with failure in compression, while many other engineers are concerned with failure in [[tension (physics)|tension]]. A further reason for the second convention is that it allows a positive stress to cause a [[Compressibility|compressible]] object to increase in size, making the sign convention self-consistent.&lt;br /&gt;
&lt;br /&gt;
In [[structural geology]], differential stress is used to assess whether [[tensile failure|tensile]] or [[shear failure]] will occur when a [[Mohr circle]] (plotted using &amp;lt;math&amp;gt;\sigma_1&amp;lt;/math&amp;gt; and &amp;lt;math&amp;gt;\sigma_3&amp;lt;/math&amp;gt;) touches the failure envelope of the rocks. If the differential stress is less than four times the [[tensile strength]] of the [[rock (geology)|rock]], then extensional failure will occur. If the differential stress is more than four times the tensile strength of the rock, then shear failure will occur.&amp;lt;ref&amp;gt;Cosgrove. J. W. (1998) The role of structural geology in reservoir characterization. Geological Society, London, Special Publications, v. 127; p. 1-13&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
&lt;br /&gt;
&amp;lt;references/&amp;gt;&lt;br /&gt;
&lt;br /&gt;
{{DEFAULTSORT:Differential Stress}}&lt;br /&gt;
[[Category:Geology]]&lt;br /&gt;
&lt;br /&gt;
&lt;br /&gt;
{{Geology-stub}}&lt;br /&gt;
{{phys-stub}}&lt;/div&gt;</summary>
		<author><name>en&gt;Qetuth</name></author>
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