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        <datestamp>2023-07-11</datestamp>
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          <dc:contributor>Parker, Gary</dc:contributor>
          <dc:creator>Czapiga, Matthew</dc:creator>
          <dc:date>2013-05-24T22:18:19Z</dc:date>
          <dc:date>2013-05-24T22:18:19Z</dc:date>
          <dc:date>2015-05-24T10:01:12Z</dc:date>
          <dc:date>2013-05</dc:date>
          <dc:date>2013-05-24T22:18:19Z</dc:date>
          <dc:date>2013-05</dc:date>
          <dc:description>System connectivity is achieved when some intrinsic organization allows inter-medium travel.
Depth connectivity is investigated in alluvial meandering streams as a solution to river
navigability. These types of rivers are naturally ordered systems, which exhibits self-similarity
amongst many scales. Four river sections and four experimental runs were used to investigate
patterns in depth connectivity with varied path dimensions. Dimensions of measured depth and
connective path were made dimensionless through bankfull hydraulic geometry. As these mean
statistics scale with river discharge, connective paths should follow the same trends. Systematic
connectivity was computed through a numerical calculation that determines the success rate for
every combination of dimensionless depth, path width, and path length. Distributions of depth
are presented as hypsometric curves; the standard deviation of these distributions quantifies
depth variability. The experimental runs shows larger magnitude depths and more variability in
depths larger than bankfull channel depth. Experimental runs also display lower internal
connectivity than the rivers. Connectivity results show similarity as a function of dimensionless
path dimensions, a dimensionless threshold depth, and the reach-averaged hypsometric standard
deviation. A first order model is presented which adequately predicts general patterns, but
accuracy decreases through increases to either the width factor or hypsometric standard
deviation.</dc:description>
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Item is restricted until 2015-05-24T22:18:31Z</dc:description>
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Original Data
Group with Access UIUC Users [automated]
Release Date: 2015-05-24 17:18:31 UTC
Reason: Author requested U of Illinois access only (OA after 2yrs) in Vireo ETD system</dc:description>
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          <dc:identifier>http://hdl.handle.net/2142/44498</dc:identifier>
          <dc:language>en</dc:language>
          <dc:rights>Copyright 2013 Matthew Czapiga</dc:rights>
          <dc:subject>River Morphodynamics</dc:subject>
          <dc:subject>Bankfull Hydraulic Geometry</dc:subject>
          <dc:subject>Connectivity</dc:subject>
          <dc:title>Systematic connectivity in single thread meandering alluvial rivers: statistical generalization of hydraulic geometry</dc:title>
          <dc:type>text</dc:type>
          <degree>
            <department>Civil &amp; Environmental Eng</department>
            <departmentCode>1251</departmentCode>
            <discipline>Civil Engineering</discipline>
            <disciplineCode>0106</disciplineCode>
            <grantor>University of Illinois at Urbana-Champaign</grantor>
            <level>Thesis</level>
            <name>M.S.</name>
            <program>PHD:Civil Engineering -UIUC</program>
            <programCode>10KS0106PHD</programCode>
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