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  <titleInfo>
    <title>Assessing potential salt-vulnerable areas through terrain analysis using remote sensing and GIS - the Vientiane Plain case study</title>
  </titleInfo>
  <name type="personal">
    <namePart>Nokeo Ratanavong</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Lukens, John E.</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Prinya Nutalaya</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Motti, Etienne</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>SIDA ( Swedish International Development Agency)</namePart>
  </name>
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  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">th</placeTerm>
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    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1991</dateIssued>
    <issuance>monographic</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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    <extent>119 p.</extent>
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  <abstract>Salt-affected areas in the Vientiane Plain have been created  by a salinization process operating primarily via saline  groundwater. They are characterized by the occurrence of highly  saline barren patches with few halophiles, surrounded by  apparently less or non - saline areas. The saline patches show an  uneven distribution within t he topographically low-lying  terrains.  Salt- affected areas can be observed o n remotely-sensed  images with the help of secondary indicators and verified by  ground truth surveys. Besides soils affected by salt at present,  potential salt-vulnerable soils must also be distinguished. Soils  considered potentially salt-vulnerable are those that are not, or  only to a mi n o r degree, saline at present, but with environmental  changes could become salt-affected.  Potential salinity classes are based on a combination of  factors rather than t he presence of surface salt occurences only.  Highly salt- vulnerable areas are located within low- lying areas  with shallow watertables, of saline quality, underlain by the Tha  Ngone salt-bearing Formation, with fine textured soils a nd  inefficient drainage, and covered with sparse vegetation. A sandy  soil is rarely a salt- affected soil because t he soil is well drained a nd the salt can be leached out easily. A clayey soil is  likely to be salt-affected if t he salts are introduced by surface  water. A loamy soil is likely to be affected if t he ground water  is saline because the capillary rise is higher than in other  soils. Paddy fields may favor the development of salinization.  These fields  need poor drainage conditions for rice cultivation,  which is one of the factors favoring salinization if combined  with other environmental factors.  Potential salt-vulnerable areas could be assessed at a  reconnaissance level by integrating and analyzing the necessary  environmental data and information. Further field and analytical  data are needed for more adequate modeling.</abstract>
  <note> A thesis submitted in partial fulfillment of the requirement for the Degree of Master of Science, School of Environment, Resources and Development</note>
  <note>Thesis (M.Sc.) - Asian Institute of Technology, 1991</note>
  <subject authority="lcsh">
    <topic>Salinization</topic>
    <topic>Vientiane Plain</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Salinization</topic>
    <topic>Remote sensing</topic>
  </subject>
  <subject authority="lcsh">
    <topic>GIS (Computer program)</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. NR-91-04</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=B17692</identifier>
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