Monitoring Saturated and Un-saturated Zone Processes for Improving Integrated Modeling
Patrick Tara, Jeff Vomacka, Mark RossCenter for Hydrologic Modeling and Aquatic Systems
Jeff Geurink, Ron Basso
Why Collect Data?Determine Water Budget TermsET budget?Vadose zone ETGroundwater ETSurface water runoff?Infiltration excessSaturation excessBaseflow flux?Surface water storage releaseGroundwater storage release
Why Collect Data?Answer Fundamental Groundwater upward flux (capillary fringe)?Vadose zone or water table recharge?Variable specific yield?Air entrapment
Site LocationHillsborough CountyReservoir Site LocationF L O R I D AReservoir Site Location
Instrument Locations
Installed InstrumentationWeatherRainfallContinuous tipping bucket rain gages (3 gages)Standard NWS manual rain gages (3 gages)Pan evaporationWind speed / wind directionTemperature / humidity / solar radiation
Installed Instrumentation HydrologicStreamflow (5 installations)Complex V-notched weirsContinuous stage recordersWellsContinuously recorded (12 gages)Weekly manually recorded (83 wells)Runoff test-bed (1 installed, 1 in progress)Continuous soil moisture probes (6 installations)
Streamflow Monitoring
Streamflow Analysis
Well Transects
Well Transect Data
Runoff Test-bedSize 100ft x 20ft (30.5m x 6.1m)Flashed to prevent inflows/outflowsGutter captures runoffWeir with continuously logged precision level gage allows accurate flow measurementRain gageWellsSoil moisture probes
Runoff Test-bedATION in Feet
Runoff Test-bed SchematicMonitoring wellsSoil moisture probesWeir10020Perimeter FlashingGutterOverland Flow
Runoff Test-bed Flow MeasurementCross-section of runoff gutter which captures the overland flow and discharges to a weir in order to measure flowOverland FlowV-Notched Weir plateDischarge to Land Surface via conduit
Runoff Test-bed Photographs
Runoff Test-bed DataJune 25-26, 2002
Soil MoistureFrequency domainContinuously monitors wetting as well as dryingCaptures upward fluxCaptures air entrapmentTypical probe includes 8 transducers spaced at 10, 20, 30, 40, 50, 70, 100, 150cm below land surface
Soil Moisture Probes Installation Photographs
Soil Moisture Probes Photographs
Geo-probe Soil Sampling
Soil Texture Analysis
Soil Moisture Profiles
Soil Moisture Profiles
Variable Specific Yield
Preliminary ResultsAir entrapment is an important processEvent pressurizationProlonged encapsulationSpecific yield is not constant (shallow water table)Small ET and recharge fluxes result in significant water table fluctuationsSaturation excess is dominate runoff processMaybe controlled by air entrapment?Vadose zone moisture deficit controls rechargeRainfall intensity effects all above processes
Soil Moisture Profiles
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