Whitewater Watershed “Paired-Watershed” Monitoring
Project
John Nieber, Professor
Bradley Hansen, Senior Scientist
Gregory Johnson, Minnesota Pollution Control Agency
Funding Source
Minnesota Pollution Control Agency
Objective
To assess the differences of runoff, sediment yield,
and nutrient yield from two small watersheds located in southeast
Minnesota
and to evaluate the ability of the complex hydrologic simulation
model, GSSHA, to simulate the hydrology of those two watersheds.
Need
or Impact
With the need to develop Best Management Practices
(BMPs) for land uses and Total Maximum Daily Loads (TMDLs)
for streams
in Minnesota, it is necessary to acquire hydrologic and water
quality data from areas of critical interest. A TMDL for the
Whitewater River Watershed is sediment. It is therefore necessary
to quantify runoff and sediment concentrations/yield from
different areas within the watershed. To extrapolate the experimental
results from the small watershed sites, it is necessary to
test
and calibrate hydrologic/water quality models for the watersheds.
Project Status
This study involves the continuation of a monitoring
program for acquisition of field data. We will continue to
monitor the
watersheds through 2006. We now have data from 1997. We have
processed all precipitation, water flow, and water quality
collected since the beginning of the project up through 2005,
and these
data have been summarized into the US-EPA STORET system. The
GSSHA (Gridded Surface Subsurface Hydrologic Analysis) model
has been set up for the two watersheds. This has consisted
of generating the gridded surface from a digital elevation model
and entering the grid cell dependent properties of soil characteristics
and land cover types. The model is being used to simulate
the
storm runoff hydrographs measured for these watersheds and
ground water contributions to sustained flows. The surface runoff
portion
of the model is being calibrated using a subset of stormflow
hydrographs, and the ground water component is being calibrated
using baseflow recession data. The calibrated model will be
verified with an independent subset of stormflow hydrograph
data. The calibrated model will be used to evaluate proposed
changes in land use within the watershed and to simulate nitrate
and phosphorus export from the watersheds. In addition to
the modeling activity, the flow and water chemistry data are
being
used to characterize the source waters of the paired watersheds.
Data used include nitrate and phosphorus concentrations, water
temperature, and stable isotope (deuterium and oxygen-18)
concentrations. Preliminary analysis has shown that the two
watersheds, while
they are side-by-side, behave differently in terms of their
ratios of surface and subsurface contributions to runoff.
One of the watersheds has runoff dominated by surface runoff,
while
the other watershed has runoff dominated by ground water.
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