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  <titleInfo>
    <title>Effect of some measurable soil parameters on bubbling pressure</title>
  </titleInfo>
  <name type="personal">
    <namePart>Lin, Ton-tai</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Arbhabhirama Anat</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Ackermann, Norbert L.</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Niwat Daranandana</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>Asian Institute of Technology</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>1971</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
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    <extent>66 p.</extent>
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  <abstract>The bubbling pressure of a porous medium is defined as the capillary  pressure at which the non-wetting fluid is first continuous through  the medium. It is very important soil parameter in characterizing  a partially saturated flow. The purpose of this thesis is to study the  effects of pertinent soil parameters and fluid properties on the bubbling  pressure. A capillary tube model analogy was employed to develop an  equation representing the bubbling pressure as a function of soil  parameters and properties of fluid. The soil parameters being con sidered were porosity, characteristic diameter of soil particle, and a  coefficient which is a function of the pore size distribution index. The  fluid properties were surface tension and specific weight.  Experiments ~'7cre conducted to verify the theoretical equation  and determine tile coefficient. The media \·rnre selected to hav-e wide  ranges of texture, porosity, grain size distrioution and pore size  distribution. The wetting fluid used was distilled water and non wetting fluid was air,</abstract>
  <note>A thesis submitted in partial fulfillment of the requirements for the Degree of master of Engineering of the Asian Institute of Technology, Bangkok, Thailand.</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1971</note>
  <subject authority="lcsh">
    <topic>Soil permeability</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Porous materials</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. 345</title>
    </titleInfo>
    <name type="corporate">
      <namePart>Asian Institute of Technology.</namePart>
      <namePart/>
    </name>
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  <identifier type="uri">http://203.159.5.9/ait-thesis/detail.php?q=B24441</identifier>
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    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B24441</url>
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    <recordCreationDate encoding="marc">011297</recordCreationDate>
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