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  <titleInfo>
    <nonSort>A </nonSort>
    <title>model for evaporation and transpiration from wetland rice</title>
  </titleInfo>
  <name type="personal">
    <namePart>Rahman, Md. Mazibur</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Jensen, Jens Raunso</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Nielsen, Jens Moller</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Rahman, Md. Ataur</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>DAAD, FRG</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <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>1986</dateIssued>
    <issuance>continuing</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
    <extent>80 p.</extent>
  </physicalDescription>
  <abstract>The study was conducted at the Asian Institute of technology,  Bangkok, Thailand in 1986. Two lysimeters of size 1mx1m with the mariotte  system designed according to TOMAR &amp; O'TOOLE (1980) was used to measure  evapotranspiration, while evaporation &amp; transpiration was measured using a  thin (1mm) transparent PVC tray on the lysimeter. Net radiation and reflected radiation was measured above the crop. All other climatic parameters  were available from the agrometeorological station situated at the site.  The full cover albedo of rice at 14 °04' North and 100° 44' East in  Thailand using exponential relationship was 0.22, that of water surface as  0.08 , and the extinction coefficient for albedo as 0.618. The combination  model was used to develop model for evaporation and transpiration with the  inclusion of estimated correction factor in the wind function of PENMAN  (1954, as cited in PENMAN, 1956) for evaporation from water surface, and on  the wind function of STIGTER (1980) for transpiration from the canopy. For  the period of LAI &lt; 3. 0 a linear relationship varying from 0 to 0. 75 for  transpiration, 1 to 0.32 for evaporation were used on the basis of LAI to  calculate the correction terms in both the wind functions. And for LAI ~  3.0 both the correction terms were estimated to be constant; 0.32 for evaporation and 0.75 for transpiration. The estimated E was within 1mm of E  observed during the initial period, thought to be associated with the error  in measurement of evaporation while the evaporation in the later period could  be estimated within 0.2mm of accuracy. Estimated T was higher In the initial  period by 1mm on average and later within 0.5mm. Finally ET could be estimated within o.5mm accuracy on average.</abstract>
  <note>A research study submitted in partial fulfillment of the requirements for the degree of Master of Engineering, School of Environment, Resources and Development</note>
  <note>Thesis (M.Eng.) - Asian Institute of Technology, 1986</note>
  <subject authority="lcsh">
    <topic>Plants</topic>
    <topic>Transpiration</topic>
  </subject>
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    <titleInfo>
      <title>Thesis ; no. AE-86-07</title>
    </titleInfo>
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      <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=B19568</identifier>
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