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  <titleInfo>
    <title>Characteristics of flow and salinity intrusion in the Mekong delta</title>
  </titleInfo>
  <name type="personal">
    <namePart>Ngo The Khai</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Suphat Vongvisessomjai</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Gupta, Ashim Das</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Tawachai Tingsanchali</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Preecha Kamronrithisorn</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>The Government of Australia</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>1988</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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    <extent>104 p.</extent>
  </physicalDescription>
  <abstract>Characteristics of flow velocity and salinity intrusion into the  estuarine system are a problem of great important for development of Mekong  river. During t he dry season, about 1.5 million hectares of fertile land  suffer from the l ack of fresh water source.  This study presents different methods for the data analyse, analytical  solution for velocity field and salinity intrusion. The study formulates the  expression for longitudinal dispersion coefficient of the estuary and  applies the mathematical model of one-dimensional. unsteady salinity  intrusion in the Mekong river estuary . The model results were calibrated  with observed values at different stations along the four main branches of  the Mekong river. In regard of the problem of downstream boundary salinity  and upstream constant source discharge , it becomes an important step for  prediction possibility of the model.  It is found that the daily average river discharge is too small in  comparison with tidal one. The strong influence of "temporary storage" on  average values of water level and discharge, and also of discharge  distribution . The magnitude of dispersion coefficient is very high due to  extreme slope and large specific discharge of the Mekong river. </abstract>
  <note>A thesis submitted in partial fulfilment of the requirement for the degree of Master of Engineering, School of Engineering and Technology</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1988</note>
  <subject authority="lcsh">
    <topic>Saltwater encroachment</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Mekong Delta</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. WA-88-10</title>
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      <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=B18858</identifier>
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