Urban Impacts on Streams are Scale-Dependent With Nonlinear Influences on Their Physical and Biotic Recovery in Vermont, United States
The physical and biological conditions of stream reaches in 16 watersheds within the Lake Champlain Basin of Vermont, United States, were assessed and analyzed for a response to total impervious area (TIA) at multiple spatial scales. Natural gradients (e.g., channel slope) and human impacts to chann...
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Veröffentlicht in: | Journal of the American Water Resources Association 2012-08, Vol.48 (4), p.679-697 |
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description | The physical and biological conditions of stream reaches in 16 watersheds within the Lake Champlain Basin of Vermont, United States, were assessed and analyzed for a response to total impervious area (TIA) at multiple spatial scales. Natural gradients (e.g., channel slope) and human impacts to channel boundary conditions (e.g., bank armoring) were considered to ensure a robust test of the Impervious Cover Model for upslope TIA. The response of geomorphic stability and sensitive macroinvertebrates to TIA was nonlinear and significant (p < 0.001), decreasing rapidly at 5% TIA. The effect of urbanization on stream condition was shown to interact significantly with drainage area and channel slope using the analysis of covariance (ANCOVA) (p < 0.05). Hydraulic geometry regressions for urban and rural watersheds and ANCOVA were used to describe a significant watershed scale-dependent response of channel width to urbanization (p = 0.001). The analysis of macroinvertebrate data from reaches in different stages of channel evolution indicated that stable reaches supported greater richness of pollution intolerant species (p < 0.001) and overall taxa richness (p < 0.01) than unstable reaches, and that biotic integrity improves as channels regain stability during their evolution into a state of quasi-equilibrium. We conclude that macroinvertebrate communities can respond positively to channel evolution processes leading to natural channel restabilization. |
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Natural gradients (e.g., channel slope) and human impacts to channel boundary conditions (e.g., bank armoring) were considered to ensure a robust test of the Impervious Cover Model for upslope TIA. The response of geomorphic stability and sensitive macroinvertebrates to TIA was nonlinear and significant (p < 0.001), decreasing rapidly at 5% TIA. The effect of urbanization on stream condition was shown to interact significantly with drainage area and channel slope using the analysis of covariance (ANCOVA) (p < 0.05). Hydraulic geometry regressions for urban and rural watersheds and ANCOVA were used to describe a significant watershed scale-dependent response of channel width to urbanization (p = 0.001). The analysis of macroinvertebrate data from reaches in different stages of channel evolution indicated that stable reaches supported greater richness of pollution intolerant species (p < 0.001) and overall taxa richness (p < 0.01) than unstable reaches, and that biotic integrity improves as channels regain stability during their evolution into a state of quasi-equilibrium. We conclude that macroinvertebrate communities can respond positively to channel evolution processes leading to natural channel restabilization.</description><identifier>ISSN: 1093-474X</identifier><identifier>EISSN: 1752-1688</identifier><identifier>DOI: 10.1111/j.1752-1688.2012.00639.x</identifier><identifier>CODEN: JWRAF5</identifier><language>eng</language><publisher>Oxford, UK: Blackwell Publishing Ltd</publisher><subject>Boundary conditions ; Channels ; Drainage ; Earth sciences ; Earth, ocean, space ; Evolution ; Exact sciences and technology ; fluvial processes ; Hydrology. 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Natural gradients (e.g., channel slope) and human impacts to channel boundary conditions (e.g., bank armoring) were considered to ensure a robust test of the Impervious Cover Model for upslope TIA. The response of geomorphic stability and sensitive macroinvertebrates to TIA was nonlinear and significant (p < 0.001), decreasing rapidly at 5% TIA. The effect of urbanization on stream condition was shown to interact significantly with drainage area and channel slope using the analysis of covariance (ANCOVA) (p < 0.05). Hydraulic geometry regressions for urban and rural watersheds and ANCOVA were used to describe a significant watershed scale-dependent response of channel width to urbanization (p = 0.001). The analysis of macroinvertebrate data from reaches in different stages of channel evolution indicated that stable reaches supported greater richness of pollution intolerant species (p < 0.001) and overall taxa richness (p < 0.01) than unstable reaches, and that biotic integrity improves as channels regain stability during their evolution into a state of quasi-equilibrium. We conclude that macroinvertebrate communities can respond positively to channel evolution processes leading to natural channel restabilization.</description><subject>Boundary conditions</subject><subject>Channels</subject><subject>Drainage</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Evolution</subject><subject>Exact sciences and technology</subject><subject>fluvial processes</subject><subject>Hydrology. Hydrogeology</subject><subject>Invertebrates</subject><subject>Nonlinearity</subject><subject>Regression analysis</subject><subject>restoration</subject><subject>Stability</subject><subject>Streams</subject><subject>Urbanization</subject><subject>Variance analysis</subject><subject>Water resources</subject><subject>Watershed management</subject><subject>Watersheds</subject><issn>1093-474X</issn><issn>1752-1688</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNqFkE1v1DAQhiMEEqXwHywhJA4kjD9ix0dY2rLSqq3YLq24RI4z0XpJnMX2ou4f6O9ullY99MJcZqT3mXc-soxQKOgUnzcFVSXLqayqggFlBYDkurh9kR09CS-nGjTPhRI3r7M3MW4AaEkrfpTdrUJjPJkPW2NTJKMnyxTQDJGYgGRpTY_5N9yib9Encu3SmpyPvnceTSBz3_U79Bb_NV6t0QVyud5HN7UR41vy1Y3JWfID7fgXw544T35iGEafPpGVdwnbaZxJGN9mrzrTR3z3mI-z1enJ1ex7vrg4m8--LHLHqUo5QgNWWYqqK9um1FbaStC2a7umslx3AlphDau6VsiGSwsMtBCaKaqZBQB-nH188N2G8c8OY6oHFy32vfE47mJNlWSUC631_1HglaRcyYPr-2foZtwFPx1yoKYVKIiD4YdHysTpQV0w3rpYb4MbTNjXTDJWUi0mLn_gXEx4-6Sb8LuWiquyvj4_q5eX-tdyxm_qBb8HZpidsQ</recordid><startdate>20120801</startdate><enddate>20120801</enddate><creator>Fitzgerald, Evan P.</creator><creator>Bowden, William B.</creator><creator>Parker, Samuel P.</creator><creator>Kline, Michael L.</creator><general>Blackwell Publishing Ltd</general><general>American Water Resources Association</general><scope>BSCLL</scope><scope>IQODW</scope><scope>7QH</scope><scope>7ST</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H97</scope><scope>KR7</scope><scope>L.G</scope><scope>SOI</scope><scope>7TG</scope><scope>7TV</scope><scope>7U6</scope><scope>KL.</scope><scope>7SU</scope></search><sort><creationdate>20120801</creationdate><title>Urban Impacts on Streams are Scale-Dependent With Nonlinear Influences on Their Physical and Biotic Recovery in Vermont, United States</title><author>Fitzgerald, Evan P. ; Bowden, William B. ; Parker, Samuel P. ; Kline, Michael L.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-i317t-e0b0c7c1e7f5db59c6c841dfdfb8c39f40d4ca28fd46b36c020944927192c0003</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Boundary conditions</topic><topic>Channels</topic><topic>Drainage</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Evolution</topic><topic>Exact sciences and technology</topic><topic>fluvial processes</topic><topic>Hydrology. Hydrogeology</topic><topic>Invertebrates</topic><topic>Nonlinearity</topic><topic>Regression analysis</topic><topic>restoration</topic><topic>Stability</topic><topic>Streams</topic><topic>Urbanization</topic><topic>Variance analysis</topic><topic>Water resources</topic><topic>Watershed management</topic><topic>Watersheds</topic><toplevel>online_resources</toplevel><creatorcontrib>Fitzgerald, Evan P.</creatorcontrib><creatorcontrib>Bowden, William B.</creatorcontrib><creatorcontrib>Parker, Samuel P.</creatorcontrib><creatorcontrib>Kline, Michael L.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Pollution Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Environmental Engineering Abstracts</collection><jtitle>Journal of the American Water Resources Association</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fitzgerald, Evan P.</au><au>Bowden, William B.</au><au>Parker, Samuel P.</au><au>Kline, Michael L.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Urban Impacts on Streams are Scale-Dependent With Nonlinear Influences on Their Physical and Biotic Recovery in Vermont, United States</atitle><jtitle>Journal of the American Water Resources Association</jtitle><date>2012-08-01</date><risdate>2012</risdate><volume>48</volume><issue>4</issue><spage>679</spage><epage>697</epage><pages>679-697</pages><issn>1093-474X</issn><eissn>1752-1688</eissn><coden>JWRAF5</coden><abstract>The physical and biological conditions of stream reaches in 16 watersheds within the Lake Champlain Basin of Vermont, United States, were assessed and analyzed for a response to total impervious area (TIA) at multiple spatial scales. Natural gradients (e.g., channel slope) and human impacts to channel boundary conditions (e.g., bank armoring) were considered to ensure a robust test of the Impervious Cover Model for upslope TIA. The response of geomorphic stability and sensitive macroinvertebrates to TIA was nonlinear and significant (p < 0.001), decreasing rapidly at 5% TIA. The effect of urbanization on stream condition was shown to interact significantly with drainage area and channel slope using the analysis of covariance (ANCOVA) (p < 0.05). Hydraulic geometry regressions for urban and rural watersheds and ANCOVA were used to describe a significant watershed scale-dependent response of channel width to urbanization (p = 0.001). The analysis of macroinvertebrate data from reaches in different stages of channel evolution indicated that stable reaches supported greater richness of pollution intolerant species (p < 0.001) and overall taxa richness (p < 0.01) than unstable reaches, and that biotic integrity improves as channels regain stability during their evolution into a state of quasi-equilibrium. We conclude that macroinvertebrate communities can respond positively to channel evolution processes leading to natural channel restabilization.</abstract><cop>Oxford, UK</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/j.1752-1688.2012.00639.x</doi><tpages>19</tpages></addata></record> |
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subjects | Boundary conditions Channels Drainage Earth sciences Earth, ocean, space Evolution Exact sciences and technology fluvial processes Hydrology. Hydrogeology Invertebrates Nonlinearity Regression analysis restoration Stability Streams Urbanization Variance analysis Water resources Watershed management Watersheds |
title | Urban Impacts on Streams are Scale-Dependent With Nonlinear Influences on Their Physical and Biotic Recovery in Vermont, United States |
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