A watershed model for a TMDL or a Section 319 plan
The question it answers
How much flow, sediment and nutrient each sub-basin delivers, and how much each practice or land change would cut it.
We deliver
The SWAT+ model of your watershed, calibrated to its USGS gauge; sediment and nutrient loads for each sub-basin; the reduction scenarios your plan asks for; a written report; the model files. Loads are fitted to water-quality samples where you or a public record hold them; elsewhere they use the model’s standard parameters, and the report says which.
Example
Bixler Run (USGS 01567500) and Lycoming Creek (01550000), Pennsylvania: calibrated SWAT+ models scored on years the calibration never saw, daily NSE 0.75 and KGE 0.79 at Bixler Run and NSE 0.63 at Lycoming Creek.
Quoted for your watershed
Request a proposalStreamflow where there is no gauge
The question it answers
How much water flows, day by day and in low-flow and high-flow years, at a stream, intake or outfall that has no gauge.
We deliver
A SWAT+ model calibrated to the nearest USGS gauge, daily flow at every channel in the watershed, the flow statistics you name at your sites, a written report on how far the calibration carries, and the model files.
Example
Lookout Creek, Oregon (USGS 14161500): 63.7 km², 1,316 HRUs and 790 channels, each channel with its own simulated flow.
Quoted for your watershed
Request a proposalGroundwater and streams together
In Michigan Lower Peninsula, Indiana, Minnesota, Ohio, Wisconsin.
The question it answers
How much rain recharges the aquifer, how that compares with pumping, and where groundwater levels and the groundwater flow to streams settle under a dry year’s recharge.
We deliver
The SWAT+ watershed model calibrated to its gauge, a steady-state MODFLOW 6 groundwater model beside it built from the state’s well records, recharge and pumping balances, the scenarios you ask for, a written report and the model files. A run that follows streams and wells through a dry year day by day is further work, quoted on its own.
Example
Our model of the Pentwater River watershed.
Quoted for your watershed
Request a proposalPFAS: how fast it reaches groundwater at a site
The question it answers
How long PFOS takes to pass through the soil to the water table at a site, and how much arrives.
We deliver
Transport through the unsaturated zone for your site’s soil and recharge, with sorption to soil and to the air-water interface, as in our Journal of Contaminant Hydrology paper; arrival times and mass at the water table; a written report. The study runs on your site’s data.
Example
“Vadose-zone control of PFOS delivery to groundwater: explicit unsaturated-zone transport with solid-phase and air-water interfacial sorption”, Journal of Contaminant Hydrology.
Quoted for your watershed
Request a proposal