| Integration of GIS and
Watershed Modeling of Runoff and Infiltration |
These figures illustrate the integration
of runoff/infiltration modeling into a GIS framework.
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To incorporate bedrock geology, soil
depth, soil type, and geomorphic features, a grid was generated
in a GIS framework. The upper figure shows the grid overlaid on the
the bedrock geology. |
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The lower figure shows the spatial distribution of excess
infiltration, which reflects runoff from upgradient areas that
infiltrates in a downgradient grid element.
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The blue areas denote infiltration greater than precipitation, and the brown areas denote
infiltration less than precipitation.
Channel infiltration is not included in
this figure. |
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Southwest Research Institute |
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Sponsor: U.S. Nuclear Regulatory Commission |
| Principal Investigators:
Randall Fedors and David Woolhiser |
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Program Brief
Statement of Problem: The client
required an evaluation of lateral flow on hillslopes and its effect on
the distribution of shallow infiltration. The potential focusing of
infiltration was expected to affect the performance of an underground
high-level waste storage site. Data from a wide variety of field and
literature sources needed to be integrated into the Geographic
Information System (GIS) to develop model input and to analyze results
of surface water and infiltration modeling for a small watershed.
Approach and Accomplishments: The
KINEROS2 watershed model, developed by the U.S. Department of
Agriculture for surface water runoff and infiltration, was used to evaluate
the spatial heterogeneity of shallow infiltration in a 0.25 km2
watershed. Field measurements, an ortho-rectified air photograph, a
geo-located image of soil depth, a bedrock geologic map, a soil type
map, and a geomorphic feature map were assembled in a GIS framework.
After a grid was generated, plane and channel element geometric
information and hydraulic properties were estimated for each element as
input to KINEROS2. Simulations of storm events were aggregated for a 10-year period to evaluate the interplay between geomorphic features, soil
depths, and bedrock geology. The results clearly showed that focusing of
shallow infiltration in areas below steep slopes would significantly
enhance channel infiltration; thus, a broad zone of focused infiltration
was likely occurring. A likely zone of focused infiltration on the broad
sloping crest of the ridge at the uppermost portion of the watershed also
was identified.
Client Benefits: Integration of
GIS with numerical process models like KINEROS2 is an efficient approach
for generating grid and model hydraulic properties and evaluating model
simulation results using all geologic, geomorphic, and topographic
information. |