|
Watershed modeling: Watershed related processes are
non-linear in nature due to complex interactions in pedology, geology,
biology and hydrology and remain all-together a challenging problem with
several societal implications. Some of the perplex questions associated
with watershed processes are the effects of scale in monitoring and
modeling, the integration of all phases (i.e., surface and subsurface)
in monitoring and modeling, and the development of economic and
environmental indicators for alternative scenarios and modeling
assessment purposes. Recognizing the critical
need for developing an integrated and scientifically sound framework in
watershed research, interdisciplinary groups began to emerge, beyond
traditional discipline, some innovative concepts for watershed
modeling. |
| Modeling
the Upper South Amana sub-watershed:
Water
Erosion Prediction Project (WEPP), upland erosion model to predict
sediment erosion rates, was used to model the Upper South Amana
sub-watershed (SAW) of the Clear Creek Watershed. WEPP is a
process-based, event-based, distributed parameter, water flow driven
erosion prediction model. Climatic data and Digital Elevation Models
(DEM) are also incorporated in the model along with the biogeochemical
properties of the soils. Biogeochemical analyses were performed to
characterize soil properties (e.g. organic matter, clay%, sand%, CEC,
pH, etc.) in the Upper South Amana area. These soil properties were
used to calibrate WEPP and to perform a sensitivity analysis to identify
the governing parameters of upland erosion in the Upper South Amana
Area. Simulations of sediment erosion and contaminant transport in the
SAW via WEPP reveal that for high energetic runoff events, terrain
heterogeneity plays a more central role than land use coverage
heterogeneity. Conversely, for low energetic runoff events, the effects
of land use coverage heterogeneity become more pronounced and perhaps
equal to the effects of terrain. |
 |