<?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:creator>J.M. Cahill</dc:creator>
  <dc:date>1973</dc:date>
  <dc:description>&lt;p&gt;Hydraulic sand models are useful physical tools in the&amp;nbsp;investigation of the transition zone that occurs between salt and fresh&amp;nbsp;ground water in coastal aquifers. Such models are used to demonstrate&amp;nbsp;the effects of transport mechanisms that influence the dynamic&amp;nbsp;behavior and the shape of the transition zone. The techniques&amp;nbsp;employed in obtaining in-place measurements of solute concentrations&amp;nbsp;are generally the stumbling block in generating data for two-dimensional&amp;nbsp;dispersion systems. Two in-place measurement techniques&amp;nbsp;were used in the studies described: (1) conductivity probes when salt&amp;nbsp;was used as a tracer; and (2) photoelectric cells when organic dye was&amp;nbsp;used as a tracer. Results indicate that conductivity methods are more&amp;nbsp;reliable; however, care must be exercised inasmuch as the probes tend&amp;nbsp;to disturb the fluid flow.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Hydraulic sand-model studies of miscible-fluid flow</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>