HR: 1340h
AN: B43C-0290    [Abstracts]
TI: Hydrologic Links Among Urbanization, Channel Morphology, Aquatic Habitat, and Macroinvertebrates in North Carolina Piedmont Streams
AU: * Giddings, E M
EM: giddings@usgs.gov
AF: U.S. Geological Survey, 3916 Sunset Ridge Rd, Raleigh, NC 27607 United States
AB: Landscape changes associated with urbanization have been shown to alter flow regimes of streams that, in turn, alter channel morphology, aquatic habitat, and biological communities. In order to mitigate the effects of urbanization on biological communities, it is important to understand the hydrologic links between these interactions. As part of the U.S. Geological Survey's National Water-Quality Assessment Program, 30 stream sites in the Piedmont of North Carolina (including the cities Raleigh, Greensboro, and Winston-Salem) having a range of watershed urbanization were sampled. To measure urbanization intensity, a multimetric index of watershed and riparian land use, infrastructure, and socioeconomic conditions was used. Population density ranged from 24 to 3,276 people per square kilometer; 75 percent of the sites had less than 2,000 people per square kilometer. At each site, continuous discharge record was estimated for 1 year using continuous stream-stage data, instantaneous discharge measurements, and one-dimensional hydraulic modeling. Hydrologic variability metrics were calculated to compare the magnitude, frequency, and duration of high and low flows among sites. These metrics then were correlated with measures of channel morphology, habitat, a richness-based macroinvertebrate index, and the urban-intensity index. As urban intensity in the watershed increased, the frequency of quickly rising flows increased (R²=0.55, p<0.0001), and the duration of high flows decreased (R²=0.47, p=0.0001). Along with these changes, channels became more incised; bankfull channel depths (normalized by drainage area) increased as the frequency of quickly rising flows increased (R²=0.28, p=0.006) and the duration of high flows decreased (R²=0.17, p =0.04). Additionally, streams with higher frequencies of quickly rising flows had greater percentages of sand as a dominant substrate (R²=0.19, p=0.03) and greater differences between bankfull depth and low-flow depth at summer flows (R²=0.30, p= 0.004), which is considered an indicator of flow stability. A macroinvertebrate index of sensitive taxa (the orders Ephemeroptera, Plecoptera and Trichoptera) to tolerant taxa (the family Chironomid) richness at the sampled streams declined with increases in percentages of sand (R²=0.22, p=0.008) and bankfull channel depth (R²=0.25, p=0.005) and decreases in flow stability (R²=0.43, p<0.0001), illustrating the important hydrologic links among urbanization and channel morphology, habitat, and macroinvertebrates in piedmont streams.
DE: 0493 Urban systems
DE: 1803 Anthropogenic effects (4802, 4902)
DE: 1813 Eco-hydrology
DE: 1825 Geomorphology: fluvial (1625)
DE: 1860 Streamflow
SC: Biogeosciences [B]
MN: Fall Meeting 2005