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        <identifier>oai:www.ideals.illinois.edu:2142/83217</identifier>
        <datestamp>2023-07-11</datestamp>
        <setSpec>col_2142_5131</setSpec>
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        <thesis xmlns="http://www.ndltd.org/standards/metadata/etdms/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/" xsi:schemaLocation="http://www.ndltd.org/standards/metadata/etdms/1.1/ http://www.ndltd.org/standards/metadata/etdms/1.1/etdms11.xsd http://purl.org/dc/elements/1.1/ http://www.ndltd.org/standards/metadata/etdms/1.1/etdmsdc.xsd">
          <dc:contributor>Rood, Mark J.</dc:contributor>
          <dc:creator>Kus, Pinar</dc:creator>
          <dc:date>2015-09-25T21:03:37Z</dc:date>
          <dc:date>2015-09-25T21:03:37Z</dc:date>
          <dc:date>10000-01-01</dc:date>
          <dc:date>2003</dc:date>
          <dc:date>2003</dc:date>
          <dc:description>This study summarizes the evaluation of closure when measuring and modeling aerosol optical properties as a function of RH in a laboratory and reports measured ambient aerosol optical and chemical properties for an anthropogenically perturbed continental US site from 1995 to 2000. The optical closure experiment was completed in a laboratory set-up for NaCl, (NH4)2SO 4 and NH4NO3 aerosol using an RH scanning nephelometry system. Correcting for nephelometer non-idealities and RH of the sample improved the agreement between measured and predicted total scattering coefficients (sigmasp) at RH = 80% from 35% to 11%. The closure experiment revealed the importance of keeping the nephelometry system isothermal when measuring particle scattering coefficients as a function of RH or as particles exist in the ambient environment. Corrections based on the laboratory results were applied to ambient optical measurements. The averaged hygroscopic growth factor (f(RH = 82%)) at 550 nm was 1.74 +/- 0.31 for sub-micrometer particles for the site. Chemical analysis of submicrometer particles revealed that approximately 50% of the ambient aerosol mass was SO4 and NH4. Direct aerosol radiative forcing (DARF) for the site was estimated to be -1.3 W/m2 at an ambient RH of 72%. Therefore the net effect of ambient aerosols at the site is to cool the atmosphere.</dc:description>
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  Previous issue date: 2003</dc:description>
          <dc:description>Embargo set by: Seth Robbins for item 84498
Lift date: Forever
Reason: Restricted to the U of I community idenfinitely during batch ingest of legacy ETDs</dc:description>
          <dc:description>Restricted to the U of I community idenfinitely during batch ingest of legacy ETDs</dc:description>
          <dc:description>U of I Only</dc:description>
          <dc:description>123 p.</dc:description>
          <dc:description>Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 2003.</dc:description>
          <dc:identifier>http://hdl.handle.net/2142/83217</dc:identifier>
          <dc:identifier>(MiAaPQ)AAI3101891</dc:identifier>
          <dc:language>eng</dc:language>
          <dc:subject>Engineering, Environmental</dc:subject>
          <dc:title>Physical and Chemical Properties of Laboratory and Ambient Aerosols Related to Climate Change</dc:title>
          <dc:type>text</dc:type>
          <degree>
            <department>Civl and Environmental Engineering</department>
            <discipline>Civl and Environmental Engineering</discipline>
            <grantor>University of Illinois at Urbana-Champaign</grantor>
            <level>Dissertation</level>
            <name>Ph.D.</name>
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