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  <titleInfo>
    <title>Numerical simulation of sand terrace formation at a river mouth</title>
  </titleInfo>
  <name type="personal">
    <namePart>Qin, Huimin</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
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  </name>
  <name type="personal">
    <namePart>Tanaka, Hitoshi</namePart>
    <role>
      <roleTerm type="text">Chairpeson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Suphat Vongvisessomjai</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
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  </name>
  <name type="personal">
    <namePart>Tawatchai Tingsanchali</namePart>
    <role>
      <roleTerm type="text">Examintion Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>CIDA</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
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  <originInfo>
    <place>
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    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1992</dateIssued>
    <issuance>monographic</issuance>
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  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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    <extent>86 leaves</extent>
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  <abstract>In this study the results of numerical simulation of sand terrace formation in front of a river  mouth are presented. A finite difference leap-frog scheme is applied as a method for the time  integration procedure.  A process of sand terrace formation in the conditions of different jetty length and steep slope  longshore bed as well as constant in time solid and fluvial runoff have been investigated.  The flow velocities and bed elevations from the numerical model are compared with the  experimental results. The available two-dimentional depth-averaged hydrodynamic model is used  to compute the velocity field and water surface elevation by solving the continuity and momentum  equation of flow. For the morphological model, the sediment balance equation and sediment transport  formula are solved to simulate the morphological process. Besides employing uniform  schematization, a mixed schematization in the computation is attempted.  The hydrodynamic and morphological model are found to give good prediction for the relevant  geometrical shape of sand terrace with respect to time.</abstract>
  <note>A thesis submitted in partial fulfillment of the requirement for the degree of Master of Engineering, School of Engineering and Technology</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1992</note>
  <subject authority="lcsh">
    <topic>Sediment transport</topic>
    <topic>Mathematical models</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Hydrodynamics</topic>
    <topic>Simulation methods</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. WA-92-23</title>
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    <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=B17285</identifier>
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