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  <titleInfo>
    <title>Nutrient release from lake sediments</title>
  </titleInfo>
  <name type="personal">
    <namePart>Bautista, Mendeluz B.</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Samorn Muttamara</namePart>
    <role>
      <roleTerm type="text">Chairperson</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Chongrak Polprasert</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Omura, Tatsuo</namePart>
    <role>
      <roleTerm type="text">Examination Committee</roleTerm>
    </role>
  </name>
  <name type="corporate">
    <namePart>US-ASEAN Development Cooperation Program</namePart>
    <role>
      <roleTerm type="text">Scholarship Donor</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <originInfo>
    <place>
      <placeTerm type="code" authority="marccountry">th</placeTerm>
    </place>
    <place>
      <placeTerm type="text">Bangkok</placeTerm>
    </place>
    <publisher>Asian Institute of Technology</publisher>
    <dateIssued>1983</dateIssued>
    <issuance>continuing</issuance>
  </originInfo>
  <language>
    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
  </language>
  <physicalDescription>
    <extent>94 leaves : ill.</extent>
  </physicalDescription>
  <abstract>Diffusional fluxes ranging from 14-30 mg NH4/m2-d and 0.1-0.5 mg P04/m2-d  were computed for Laguna Lake sediments. Laboratory and in situ experimental  results ~ielded rates of release in the order of 5-8 mg TIN/m2-d and 0.5-0.8  mg DIP/m -d. On the other hand, nutrient budget calculations for TIN during  the 1973-1977 period showed slightly lower values, 4-5 mg TIN/m2-d, which are  believed to be overestimates since the larger component would be accounted  for by internal recycling of N in the water column. DIP budget calculations  revealed P uptake by the sediments instead of release over the four-year period  at rates of 0.8-1.0 mg DIP/m2-d. Based on these, Laguna Lake sediments would  not be major sources of nutrients and, as in the case of phosphorus, could  even serve as a nutrient sink.  The transport of N across the sediment-water.interface was not as predo-  minantly controlled by the concentration gradient between the two phases, as  was P flux. This indicates that the mechanism for P release involves mainly  equilibrium-controlled chemical_processes, which are less prevalent in N sedi-  ments enhanced TIN release while DIP release was inhibited under aerobic condi-  tions.  </abstract>
  <note>A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science</note>
  <note>Thesis (M.Sc.) - Asian Institute of Technology</note>
  <subject authority="lcsh">
    <topic>Water</topic>
    <topic>Purification</topic>
    <topic>Filtration</topic>
  </subject>
  <subject authority="lcsh">
    <topic>Filters and filtration</topic>
  </subject>
  <relatedItem type="series">
    <titleInfo>
      <title>Thesis ; no. EV-83-5</title>
    </titleInfo>
    <name type="corporate">
      <namePart>Asian Institute of Technology.</namePart>
      <namePart/>
    </name>
  </relatedItem>
  <recordInfo>
    <recordCreationDate encoding="marc">301098</recordCreationDate>
    <recordChangeDate encoding="iso8601">20260818170321.0</recordChangeDate>
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