The effects of urbanization on the streambed sediment characteristics in a ridge and valley watershed /
Abstract (Summary)
Urbanization causes flow and sediment regime changes, which leads to alterations
in the bed sediment characteristics and degradation of the ecological habitat. Evidence
shows that changes in the characteristics of streambed sediment occur in urbanized
watersheds; however a link between urbanization and changes in streambed sediment is
not well established in the literature. Limited support in the literature does suggest that
urbanization is linked to a decline in the diversity of algae, invertebrate, and fish
populations. Relationships between urbanization and bed sediment characteristics were
explored by three studies using the AnnAGNPS and CONCEPTS models. AnnAGNPS
is a GIS-based sediment delivery model with land erosion rates determined by the revised
Universal Soil Loss Equation (RUSLE) and sediment yield rates determined by the
Hydrogeomorphic USLE (HUSLE) for watersheds primarily dominated by agricultural
land use. CONCEPTS is a sediment transport and channel adjustment model that routes
sediment input from AnnAGNPS and sediment inputs from channel bed and bank
erosion. Both models were developed by the United States Department of Agriculture –
Agricultural Research Service (USDA ARS). The research objectives for this project
included: 1) conducting a sensitivity analysis of the AnnAGNPS and CONCEPTS
models to evaluate the significance of various model inputs that incorporate the mosaic of
urban land use and require field measurements for the non-urbanized and urbanized
subwatersheds, 2) producing and executing several combinations of model run
simulations with altered runoff and erosion from the hillslope using the entire
AnnAGNPS-CONCEPTS modeling couple to simulate varying levels of urbanization,
and 3) evaluating AnnAGNPS model results of 15 urban and non-urban subwatersheds
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across Beaver Creek watershed to gain insight to dominant sediment delivery dynamics
resulting from urbanization using a multivariate cluster analysis between the model
output, field measurements, stream power, subwatershed area, and percent urbanization.
The studies addressing the first and second research objectives were conducted using the
geographic data in two subwatersheds of the Beaver Creek watershed in Knox County,
Tennessee, whereas the third study used data across the entire Beaver Creek watershed.
The two subwatersheds include Hines Branch, which is a highly disturbed urban
subwatershed, and Cox Creek, which is a subwatershed with minimal urban development.
The results from the three studies included the following main conclusions: 1) the
AnnAGNPS and CONCEPTS models were fairly insensitive to the model input
parameters tested in the sensitivity analysis on an individual basis; however, when
comparing the sensitivities between the urban and non-urbanized subwatersheds for the
AnnAGNPS analysis, the percent difference between the sensitivity slopes for each
model input parameter ranged from 150 to 300 percent; 2) simulations with altered
runoff and erosion from the hillslope showed that altered runoff had a greater impact on
the bed sediment characteristics and sediment yield; and 3) the cluster analysis of the
five watershed characteristics illustrated that percent urbanization of each subwatershed
and suspended sediment from AnnAGNPS model output over subwatershed stream
power and total subwatershed area were the most related to the bed sediment size
distributions collected at each site. Assuming the AnnAGNPS-CONCEPTS modeling
couple represents the physical watershed and channel processes, then this thesis shows
that urbanization does impact bed sediment characteristics, and it appears hydrology is
more of a controlling factor to bed sediment characteristics than hillslope erosion.
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Bibliographical Information:
Advisor:
School:The University of Tennessee at Chattanooga
School Location:USA - Tennessee
Source Type:Master's Thesis
Keywords:river sediments sediment transport control tennessee
ISBN:
Date of Publication: