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        <identifier>oai:www.ideals.illinois.edu:2142/87761</identifier>
        <datestamp>2023-07-11</datestamp>
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          <dc:title>Experimental Study of Low-Order Models of Highly-Irregular Roughness and Their Impact on Turbulent Boundary Layers</dc:title>
          <dc:type>text</dc:type>
          <dc:contributor>Christensen, Kenneth T.</dc:contributor>
          <dc:creator>Mejia Alvarez, Ricardo</dc:creator>
          <dc:date>2015-09-28T16:23:53Z</dc:date>
          <dc:date>2015-09-28T16:23:53Z</dc:date>
          <dc:date>10000-01-01</dc:date>
          <dc:date>2010</dc:date>
          <dc:date>2010</dc:date>
          <dc:description>The stereo-PIV measurements deep within the roughness sublayer at  y = 0.047delta reveal a wealth of information about roughness-induced effects, including the tendency of the roughness to promote 'channeling' of the flow in the form of low- and high-momentum pathways as noted in contour maps of the mean velocity defect. Similarly, enhanced turbulent and vortical activity is observed both between and along the spanwise boundaries of these streamwise-elongated large-scale pathways. Taken together, these observations support the idea that these persistent low-momentum pathways might represent the statistical imprint of trains of hairpin vortex packets that are channeled along preferred paths over the roughness. Conditional averaging and two-point correlations of velocity further support these structural observations, particularly clear large-scale streamwise coherence of these motions. Of interest, while the M = 5 results show important differences from the full-surface results, the M = 16 results are virtually indistinguishable fromthose of the full surface, including in the single-point turbulence statistics as well as the analysis of the average spatial structure. This consistency is not simply qualitative but is indeed quantitative as the magnitudes of the M = 16 model single-point statistics mirror those of the full surface as do the spatial locations of the low- and high-momentum pathways identified in the mean velocity defect results as well as the enhanced turbulent and vortical activity along the spanwise boundaries of these large-scale motions. Hence, these observations provide significant evidence supporting the importance of the intermediate topographical scales in setting the flow conditions within the roughness sublayer, not only in a statistical sense but also in a structural sense.</dc:description>
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  Previous issue date: 2010</dc:description>
          <dc:description>Embargo set by: Seth Robbins for item 89042
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>183 p.</dc:description>
          <dc:description>Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 2010.</dc:description>
          <dc:identifier>http://hdl.handle.net/2142/87761</dc:identifier>
          <dc:identifier>(MiAaPQ)AAI3455830</dc:identifier>
          <dc:language>eng</dc:language>
          <dc:subject>Engineering, Mechanical</dc:subject>
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            <department>Theoretical and Applied Mechanics</department>
            <discipline>Theoretical and Applied Mechanics</discipline>
            <grantor>University of Illinois at Urbana-Champaign</grantor>
            <level>Dissertation</level>
            <name>Ph.D.</name>
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