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  <titleInfo>
    <nonSort>An </nonSort>
    <title>analysis of dam breaching caused by flow overtopping</title>
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  <name type="personal">
    <namePart>Sompong Chamgramol</namePart>
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  <name type="personal">
    <namePart>Tawatchai Tingsanchali</namePart>
    <role>
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  </name>
  <name type="personal">
    <namePart>Kubo, Naritaka</namePart>
    <role>
      <roleTerm type="text">Examination committee           </roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Sutat Weesakul</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>
  <name type="corporate">
    <namePart>Royal Thai Govenment</namePart>
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      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
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  <originInfo>
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    <place>
      <placeTerm type="text">Pathum Thani</placeTerm>
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    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1998</dateIssued>
    <issuance>monographic</issuance>
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  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
    <extent>106 leaves</extent>
  </physicalDescription>
  <abstract>Flood waves due to sudden outflow through dam breach section cause severe damages  downstream of the dam. An accurate estimation of outflow through the dam breach section is  important as it is the upstream boundary condition for flood routing toward the downstream  direction. The height of peak of flood wave and travel time of the flood wave, if known  properly, can be used as a guide for evacuation preparation which can significantly reduce the  downstream damage and losses of lift.  Model dam made of medium sand with Dso = 0.65 mm. was built in a 1 m. wide and 40  m long flume with horizontal bed and transparent walls on both sides. Six experimental runs  were conducted. The upstream slope of the dam is fixed at 1V:3H but the downstream slope is  varied from 1V:3H to 1V:2.5H and 1V:2H for Run No.I, 2 and 3 in which the height of the  dam is 0.55 m. In Run No.4, the setup is the same as Run No.2 but the dam height is changed  to 0.80 m. In Run No.5 and 6, sand of D50 = 0.85 mm. is used and the dam height is 0.55 m.  The downstream slope is 1 V:3H and 1 V:2H. The upstream inflow to the reservoir is 9. 3 lps for  Run No. 1to4 and 7.8 lps for Run No.5 and 6.  The physical model dam shows that the breach starts at the center of dam crest and the  overtopping flow causes the breach channel along the downstream face of the dam to enlarge  to a larger channel. In addition to the effect of breach enlargement, the collapse of the breach  side wall or mass failure accelerates the lowering of the dam crest and the total failure of the  dam. During the erosion process, the dam crest propagates in the upstream direction in which  the crest elevation reduces exponentially with time and distance. The geometry of breach  section and the overtopping discharge can be correlated by a power law. Lastly, the MIKE-11  dambreak model developed by the Danish Hydraulic Institute is used to simulate the dam  breaching section geometry and the overtopping discharge. It is found that the MIKE-11 model  gives a very underestimated result compared to the experiments. </abstract>
  <note>A thesis submitted in partial fulfillment of the requirements for the degree of Master of Engineering, School of Civil Engineering </note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1998</note>
  <subject authority="lcsh">
    <topic>Dam failures</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. WM-97-25</title>
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      <namePart>Asian Institute of Technology.</namePart>
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  <identifier type="uri">http://203.159.5.9/ait-thesis/detail.php?q=B13344</identifier>
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