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  <titleInfo>
    <title>Dilatational characteristics of sedimented kaolinite</title>
  </titleInfo>
  <name type="personal">
    <namePart>Roque, Ernesto C.</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Nelson, John D.</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Chai  Muktabhant</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Petersen, Jens L.</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart> United Kingdom</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">th</placeTerm>
    </place>
    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1973</dateIssued>
    <issuance>monographic</issuance>
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  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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    <extent>79 p.</extent>
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  <abstract>A study of the effect of soil structure on dilatation was  carried out on an artificially sedimented kaolinite clay. Various soil structures were produced by the use of different pore fluids i.e. distilled waters, sodium chloride and sodium hexametaphosphate.  Conventional isotropically consolidated undrained triaxial compression tests with pore pressure measurements and oedometer tests were conducted in the investigation. In the oedometer tests, two samples for each soil were consolidated anisotropically at 320 psi and then rebounded at unloading ratios of 1.5 and 3.0 respectively.  In the triaxial tests, the samples for different soil structures were first consolidated to a maximum past pressure of 120 psi and  then allowed to swell under smaller consolidation pressures prior to shear. It was observed that the magnitude of rebound decrements did not affect appreciably the stored strain energy. The strength of the bonds and the tendency of the soil to dilate increased with  higher over consolidation ratios. The greater the amount of locked in strain 'energy released after failure of interparticle bonds, the greater would be the tendency of the soil to dilate. Furthermore, it was observed that the dispersed soil, with weaker bonds, exhibited  slightly greater tendency to dilate than those of the flocculated soils.</abstract>
  <note>A thesis submitted in partial fulfillment of the requirements  for the degree of Master of Engineering at the Asian Institute of Technology, Bangkok, Thailand. </note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1973</note>
  <subject authority="lcsh">
    <topic>Clay</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Soil structure</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Soil mechanics</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. 512</title>
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    <name type="corporate">
      <namePart>Asian Institute of Technology.</namePart>
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    </name>
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  <identifier type="uri">http://203.159.5.9/ait-thesis/detail.php?q=B24250</identifier>
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    <recordCreationDate encoding="marc">221297</recordCreationDate>
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