<?xml version="1.0" encoding="UTF-8"?>
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<title>Turbidity</title>
<link href="http://dspace.gcswcd.com:8080/xmlui/handle/123456789/17" rel="alternate"/>
<subtitle/>
<id>http://dspace.gcswcd.com:8080/xmlui/handle/123456789/17</id>
<updated>2026-03-09T15:46:39Z</updated>
<dc:date>2026-03-09T15:46:39Z</dc:date>
<entry>
<title>Variations in sediment sources and yields in the Finger Lakes and Catskills regions of New York.</title>
<link href="http://dspace.gcswcd.com:8080/xmlui/handle/123456789/75" rel="alternate"/>
<author>
<name>Nagle, G.N.</name>
</author>
<author>
<name>Fahey, T.J.</name>
</author>
<author>
<name>Ritchie, J.C.</name>
</author>
<author>
<name>Woodbury, P.B.</name>
</author>
<id>http://dspace.gcswcd.com:8080/xmlui/handle/123456789/75</id>
<updated>2013-10-30T00:40:23Z</updated>
<published>2007-01-01T00:00:00Z</published>
<summary type="text">Variations in sediment sources and yields in the Finger Lakes and Catskills regions of New York.
Nagle, G.N.; Fahey, T.J.; Ritchie, J.C.; Woodbury, P.B.
This study used radionuclide tracer analysis to quantify proportional contributions of land surface and stream bank erosion to fine sediment loads in streams. Results for two streams within the Schoharie Creek basin yielded relatively high rates of bank erosion, indicating the importance of glaciolacustrine deposits as importance sources of stream sediment.
</summary>
<dc:date>2007-01-01T00:00:00Z</dc:date>
</entry>
<entry>
<title>Selected Features of the Character and Origins of Turbidity in the Catskill System.</title>
<link href="http://dspace.gcswcd.com:8080/xmlui/handle/123456789/74" rel="alternate"/>
<author>
<name>Peng, F.</name>
</author>
<author>
<name>Johnson, D.L.</name>
</author>
<author>
<name>Effler, S.W.</name>
</author>
<id>http://dspace.gcswcd.com:8080/xmlui/handle/123456789/74</id>
<updated>2013-10-30T21:53:18Z</updated>
<published>2007-01-01T00:00:00Z</published>
<summary type="text">Selected Features of the Character and Origins of Turbidity in the Catskill System.
Peng, F.; Johnson, D.L.; Effler, S.W.
This report addresses particle composition and transport hypotheses for samples taken at specific high-concentration locations within the NYC water supply system. Emphasis is placed on the nature of turbidity loadings from Schoharie Reservoir.
</summary>
<dc:date>2007-01-01T00:00:00Z</dc:date>
</entry>
<entry>
<title>Testing and application of a two-dimensional hydrothermal model for a water supply reservoir: implications of sedimentation.</title>
<link href="http://dspace.gcswcd.com:8080/xmlui/handle/123456789/73" rel="alternate"/>
<author>
<name>Gelda, K.G.</name>
</author>
<author>
<name>Effler, S.W.</name>
</author>
<id>http://dspace.gcswcd.com:8080/xmlui/handle/123456789/73</id>
<updated>2013-07-02T06:00:27Z</updated>
<published>2007-01-01T00:00:00Z</published>
<summary type="text">Testing and application of a two-dimensional hydrothermal model for a water supply reservoir: implications of sedimentation.
Gelda, K.G.; Effler, S.W.
A hydrothermal model was validated for the Schoharie Reservoir as a means for managing water quality issues such as turbidity and temperature given unusually large constraints due to sedimentation and future supply/demand.
</summary>
<dc:date>2007-01-01T00:00:00Z</dc:date>
</entry>
<entry>
<title>Schoharie Watershed Turbidity Reduction Report: Evaluation of Watershed Management Programs.</title>
<link href="http://dspace.gcswcd.com:8080/xmlui/handle/123456789/72" rel="alternate"/>
<author>
<name>New York City Department of Environmental Protection</name>
</author>
<id>http://dspace.gcswcd.com:8080/xmlui/handle/123456789/72</id>
<updated>2013-07-02T06:00:20Z</updated>
<published>2008-01-01T00:00:00Z</published>
<summary type="text">Schoharie Watershed Turbidity Reduction Report: Evaluation of Watershed Management Programs.
New York City Department of Environmental Protection
NYCDEP performed a combined quantitative and qualitative assessment of turbidity reduction made through the implementation of several existing watershed management programs. A distinction between landscape erosion and in-channel sediment sources is made to effectively gauge the extent of the various programs’ overall impact towards the goal.
</summary>
<dc:date>2008-01-01T00:00:00Z</dc:date>
</entry>
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