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  <titleInfo>
    <title>K determination by hydraulic fracturing</title>
  </titleInfo>
  <name type="personal">
    <namePart>Wang, Wen-tung</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Balasubramaniam, A.S.</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Kazi, Asadullah</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Richardson, A.M.</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Brand, E.W.</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Brenner, R.P.</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Moh, Za-Chieh</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>Ministry of Economic Affairs, Republic of China</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>1975</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
    <form authority="marcform">print</form>
    <extent>95 p.</extent>
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  <abstract>Since most of the laboratory methods of K0 determination are based on no lateral yield principle, any disturbance in the sample could cause significa11.t  error in the estimation of Ko. It is, therefore, important that Ko measurements be made in the field. This research is aimed at confirming the feasibility of the field and laboratory hydraulic fracturing methods for the determination of Ko for Bangkok Clay at Rangsit. Two series of field hydraulic fracturing tests (using BJERRUM and ANDERSEN' s and HILKERS ' methods) have been carried out. The results show that both methods are feasible for the  determination of K0 in Weathered and Soft Bangkok Clay at Rangsit. The opening and closing of fractures and the rate of injection of water do not seem to have noticeable effect in the K0 values determined by the fracturing method. A series of laboratory hydraulic fracturing tests has been carried out,  and the results confirm that the laboratory fracturing method could also be used for the determination of Ko. However, as compared to the field K0 values. the laboratory test results are found to be slightly lower. This may perhaps  be due to sample disturbance.</abstract>
  <note>A thesis submitted in partial fulfilment 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, 1975</note>
  <subject authority="lcsh">
    <topic>Oil wells</topic>
    <topic>Hydraulic fracturing</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Fracture of soils</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Clay</topic>
    <topic>Thailand</topic>
    <topic>Rangsit</topic>
  </subject>
  <relatedItem type="series">
    <titleInfo>
      <title>Thesis ; no. 775</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=B24034</identifier>
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    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B24034</url>
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  <recordInfo>
    <recordCreationDate encoding="marc">080198</recordCreationDate>
    <recordChangeDate encoding="iso8601">20260818144850.0</recordChangeDate>
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