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Published byMelvyn Simpson Modified over 9 years ago
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Surface Water & Groundwater Interactions Middle Reach of Russian River
Marcus Trotta, PG, CHg Water Agency Hydrogeologist
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Riverbank Filtration System
Russian River Riverbank Filtration System One of the largest riverbank filtration systems in the world Treatment accomplished via natural filtration. Only chlorine added as a disinfectant 6 Collector Wells 7 Vertical Wells 5 Infiltration Ponds Inflatable Dam
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Groundwater Movement Between Recharge and Discharge
U.S. Geological Survey Circular 1139
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Groundwater Basin Characteristics
Unconfined alluvial aquifer filled with highly transmissive sands and gravels Hydraulically connected with Russian River Alluvial sediments Up to ~100 feet thick near River Bounded on West by low permeability Franciscan bedrock Bounded on East by older and less transmissive fluvial deposits (correlative with Glen Ellen Fm)
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US Geological Survey Circular 1139
Gaining and Losing Streams Stream gains water from groundwater Stream loses water to groundwater Groundwater Mounds beneath the stream US Geological Survey Circular 1139
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Assessment Techniques and Methods
Temperature based streambed conductance estimates Water-Level measurements & vertical gradient analysis Seepage meters Surface and groundwater quality studies Riverbed sediment sampling program In-situ microsphere studies Geophysical Methods to Evaluate SW-GW Interactions Electrical Resistivity Spontaneous Potential
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Measurement of Temperature to Characterize Surface and Groundwater Interactions
Since 1998, SCWA/USGS have measured temperature trends of Russian River & shallow groundwater Estimate hydraulic conductivity & streambed conductance using VS2DH (USGS) Able to evaluate seasonal trends Cost-effective method Results compare favorably with seepage meters
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Temperature data showing upward gradient
Water level data showing upward gradient
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Groundwater Flow Models
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Questions/Discussion
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