<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>N.D. Hoy</dc:contributor>
  <dc:creator>F. A. Kohout</dc:creator>
  <dc:date>1963</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Investigations of the fluctuations of chloride content&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;wells that tap the zone of diffusion between fresh and salt&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;show that the&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;salty&lt;/span&gt;&lt;span&gt;&amp;nbsp;well&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;behaves erratically when the well is pumped. Frequently, a static distribution of chloride content that ranges from less than 1,000 ppm at the top to more than 10,000 ppm at the bottom is present&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;the open‐hole part of a well. When the well is pumped, the discharge&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;tends to come from the upper part of the open hole because less energy is expended by removal of low‐density&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;from this region than by removal of high‐density&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;from the lower part of the open hole. Where the permeability of strata&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;the deep part of the open hole is greater than that&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;the shallow part, the tendency for natural selection of the less dense, shallow&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;is suppressed, and practically all the&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;the blend comes from the deep part. As a result of this complex interrelation of hydraulics, distribution and density of the salt&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;, and permeability, the depth at which the pumped&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;enters the well bore is indeterminate. This deficiency leads to the use of multiple‐depth‐bottle, windshield‐wiper, and electrical‐conductivity&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;sampling&lt;/span&gt;&lt;span&gt;&amp;nbsp;techniques for collection of data used&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;constructing maps and cross sections that show the areal‐depth relations of salt&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;water&lt;/span&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;in&lt;/span&gt;&lt;span&gt;&amp;nbsp;the Biscayne&amp;nbsp;&lt;/span&gt;&lt;span class="ScopusTermHighlight"&gt;aquifer&lt;/span&gt;&lt;span&gt;&amp;nbsp;of the Miami area, Florida.&amp;nbsp;&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1111/j.1745-6584.1963.tb01903.x</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Wiley  Blackwell</dc:publisher>
  <dc:title>Some aspects of sampling salty ground water in coastal aquifers</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>