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  <titleInfo>
    <nonSort>A </nonSort>
    <title>deterministic model for soil erosion from a small watershed in Nepal</title>
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  <name type="personal">
    <namePart>Anand, Thakur</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
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  </name>
  <name type="personal">
    <namePart>I, Fude</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Apisit Eiumnoh</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Hanaki, K.</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>The Royal Netherlands</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
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  <genre authority="marc">series</genre>
  <genre authority="marc">technical report</genre>
  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">th</placeTerm>
    </place>
    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1987</dateIssued>
    <dateIssued encoding="marc">1986</dateIssued>
    <issuance>continuing</issuance>
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  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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  <physicalDescription>
    <extent>61, [11] p.</extent>
  </physicalDescription>
  <abstract>An effort is mad e to for mutate a soil   loss estimation model applicable to smaller  sized water sheds in the siwalik and middle  mount a in regions of Nepal. The approach is  kept simple by correcting erosion mainly to  hydrological parameter so watershed like  total runoff volume and peak discharge . The  other factors affecting the erosion are  treated as constant , and a watershed constant  is introduced. The watershed constant is  evaluated on similar lines as the Universal  Soil Loss Equation. The model estimates the  loss on the basis of individual storm events.  The result and analys is showed that  there are cerein factors at microscopic  level like effect of electro chemical forces  on soil strength and ground vegetation  inter action, and some macroscopic phenomenon  like mass wasting has to be under stood and  in corporates in the model to improve its  efficiency .  Considering the complexity of erosion  process and the aerial extent of watershed , the predicted value of soil loss using the  formulated soil erosion model showed  consider able agreement with the values  obtained from the field data . In the case  when the effect of mass wasting were reduced  and the early season rains are not  considered , resulted to a fairly good  correlation coefficient . This empirical  model to estimate the soil loss from the  watershed due to a particular storm which  could be correlated to other physical  phenomenon and used for many practical  purposes.</abstract>
  <note>A research study  submitted in partial fulfillment of the requirement for the degree of Master of Engineering, School of Environment, Resources and Development</note>
  <note>Research Studies Project Report (M. Eng.) - Asian Institute of Technology, 1987</note>
  <subject authority="lcsh">
    <topic>Soil erosion</topic>
    <topic>Nepal</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Watersheds</topic>
    <topic>Nepal</topic>
  </subject>
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      <title>Research studies project report ; no. EV-87-1</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=B19011</identifier>
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    <url displayLabel="Full-Text">http://203.159.5.9/ait-thesis/detail.php?q=B19011</url>
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