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  <titleInfo>
    <title>Dispersive soils in Northeastern Thailand</title>
  </titleInfo>
  <name type="personal">
    <namePart>Kim, Gyo Won</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Prinya Nutalaya</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Balasubramaniam, A.S.</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Yudhbir</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>Government of Thailand</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <originInfo>
    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1982</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <physicalDescription>
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    <extent>vii, 73 p.</extent>
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  <abstract>Tests on the physical, chemical and mineralogical properties on the  soils from 3 selected sites of dispersive soils and 1 selected site of nondispersive soil are carried out in the field and laboratory during this study. In order: to find out the relationship between clay  contents and dispensability of the soil, some specimens are  artificially mixed with a certain amount of clay in the  laboratory and tested by means of pinhole tests. The artificial soils are dispersed in pinhole tests regardless of its clay content.  For the relationship between the dispersity and a water content and/or a density of the specimen on natural soils, pinhole tests are also carried out  at a different water content and different tamps per layer.  Natural soils are dispersed in pinhole tests regardless of their water content and a number of tamps per layer.  Chemical properties on the soil saturation extract and  reservoir water are also determined by means of sodium  adsorption ratio(SAR), exchangeable sodium percentage(ESP) and  pH.   The dispersive soils in the region have ranges of 1.8-6.7  SAR, 1.4-7.9 ESP and 5.4-9.0 pH, while a nondispersive soil  has only 0.5 SAR, no ESP and 4.3 pH. The main minerals of the  clay fraction in the soil are montmorillonite, kaolinite and  illite which are analyzed by the X-ray diffraction method. The dispersive soils in this region have somewhat higher  SAR, ESP and pH value chemically, and higher content of a montmorillonite mineralogically than those of the   nondispersive soil. The dispersive soil area has distinct  features, i.e., a pseudocarps and cloudy water which are good  indicators of the dispersive soil area in the field. </abstract>
  <note>A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science, School of Engineering and Technology</note>
  <note>Thesis (M. Sc.) - Asian Institute of Technology, 1982</note>
  <subject authority="lcsh">
    <topic>Soils</topic>
    <topic>Thailand, Northeastern</topic>
    <topic>Testing</topic>
  </subject>
  <identifier type="uri">http://203.159.5.9/ait-thesis/detail.php?q=B21240</identifier>
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    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B21240</url>
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