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  <titleInfo>
    <title>Flume experiments on sediment bed load in steady non-uniform flow</title>
  </titleInfo>
  <name type="personal">
    <namePart>Rana, Md. Yunus</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Tawatchai Tingsanchali</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Suphat Vongvisessomjai</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>Christoph, Ing. Fried</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>The Canadian International Development Agency</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
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  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">th</placeTerm>
    </place>
    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1986</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
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    <extent>71 p.</extent>
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  <abstract>An experimental investigation on the determination of bed load in  steady non-uniform flow was carried out using one size of uniform coarse  sand. The study is separated into three parts, namely; experiments in  steady uniform flow in the parallel sidewall flume , steady non-uniform  flow in the converging sidewall flume and steady non-uniform flow in t he  diverging sidewall flume. The steady uniform flow experiments were conducted in a flume of 18 m length, 0.82 m width with different depths and  water surface slopes. The measured bed load and flow parameters are  presented in non-dimensional form (u - q curve) for use in determining the  bed load for any given uniform flow condition. The steady non-uniform  flow experiments in the converging sidewall flume were conducted for  contraction ratios of the width from 0 .693 to 0 . 291. The steady  non-uniform flow experiments in the diverging sidewall flume were conducted for expansion ratios of the width from 1.811 to 3.255 .  From the analysis of experimental data on both converging and diverging wall cases, it was found that the correction factor or bed load  ratio (DQS) for the computed bed load using a uniform flow formula based  on energy slope of non-uniform flow depends on two factors namely: the  ratio between the gradient of depth and velocity head over the energy  s lope (DS) and the ratio between the measured and computed velocity gradients (a). The value of DQS can be greater or less than one depending  on the corresponding a value. When a is one, DQS is a l so one . This implies  uniform flow conditions.  Moreover, the ratio of depths in upper and lower uniform sections  in relation with the width ratio when compared with t he theoretical values  indicate that the experimental ranges a re bet ween the conditions of having  clear water scour and scour under full sediment supply . It was found t hat  the sediment supply rates in the experiments are mostly less than the  required rate predicted by the theory.</abstract>
  <note>A thesis submitted in partial fulfilment of the requirements for the degree of Master of Engineering, School of Engineering and Technology</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1986</note>
  <subject authority="lcsh">
    <topic>Flumes</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Bed load</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. WA-86-14</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=B19790</identifier>
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