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Published byBrian Owens Modified over 9 years ago
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Surface-Groundwater interactions on the Eastern Snake River, ID
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Outline Objective: Estimate of seepage loss along a segment of the Eastern Snake river River Channel Generation (RCMM) Unsteady flow simulation(10 non-raining days) Compare the outflow hydrograph with the actual hydrograph Calculate volume of water lost to the aquifer
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Misc. Facts about Idaho 3,100 miles of river, more than any other state 85% of all commercial trouts Number one producer of potatoes Paris and Montpellier 30 miles apart
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Study area Unconfined aquifer Highly fractured basalt Water Supply from snowmelt Precipitation ~8 in/yr
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Human impact on the Eastern Snake system Less surface water irrigation More efficient irrigation Increased pumping (source: IDWR)
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Water Budget
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Increased stress on the aquifer (source: IDWR)
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Eastern Snake aquifer Model
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Eastern Snake aquifer
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River Channel generation
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3D Representation of river reaches Bathymetric data (Expensive, unavailable) 2D 3D representation 2D plan view (DOP) Calculate location of the thalweg Approximate cross-sections with analytical functions
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2D representation of the river segment Calculate Depth/Width for a 2 yr flow Offset the NHD flow line by W/2 to obtain the channel boundary Depth Width 2D Plan view
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River Channel generation (RCMM) REQUIRES: 2D representation of the river segment GENERATES: 3D representation Thalweg: Calculates the radius of curvature Locates the thalweg using the radius of curvature/thalweg relationship Cross-sections: Analytical (Beta functions) from the thalweg location
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Generated cross-sections
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Exporting river channel into HEC- RAS
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Unsteady simulation 10 day simulation Upstream boundary condition: USGS flow hydrograph (@Minidoka) Downstream boundary condition: stage hydrograph (@Kimberley) Compare the calculated/observed hydrograph
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Acknowledgments Dr Merwade (CRWR) Allan Willie (Hydrologist, IDWR)
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Any questions?
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