Groundwater discharges to the Snake River from numerous volcanic rock springs along the northern canyon wall between Milner Dam and King Hill. Water-resource managers need to be able to quantify the amount of this water to understand the eastern Snake River Plain aquifer's recharge, storage, and discharge. When completed, this study will provide the Idaho Department of Water Resources with an automated method to quantify spring discharge to the Snake River between Milner Dam and King Hill. Updated spring discharge estimates will be useful for developing groundwater management plans and assessing the effectiveness of management actions.
Study Problem
In 1995, the USGS published regression models to quantify discharge from Snake River springs between Milner Dam and King Hill. The models provide estimates of average annual discharge at unmeasurable springs to sum with discharge at measurable springs for an estimate of total annual mean spring discharge to the Snake River between Milner Dam and King Hill. However, changes in land use, water management, and data collection raise questions about whether the regression relationships remain valid. Therefore, it is necessary to update these regression relationships to include data collected in the interim.
Study Objectives
- Identify all available datasets.
- Collect quarterly synoptic spring discharge measurements.
- Assess the uncertainty associated with using measured stream and spring discharge data to estimate reach losses and gains with a water balance approach.
- Assess the uncertainty associated with statistical approaches.
- Compare the uncertainty between the water balance and statistical approaches and report the findings to IDWR with a recommendation for which approach will be most useful for estimating spring discharge into the future.
- Implement an automated method to estimate spring discharge and integrate new data as they are collected.
- Publish methods, data, and software; present details of uncertainty comparisons between water balance and statistical methods and document the methods and accuracy of the approach used to estimate spring discharge to the Snake River.
Site Number |
Site Name |
---|---|
13132800 | Thousand Springs near Hagerman1 |
13089600 | Devil's Washbowl Spring |
13090100 | Devil's Corral Spring |
13091500 | Blue Lakes Outlet |
13093400 | Crystal Springs nr Filer1 |
- | Cedar Draw2 |
13094500 | Clear Lakes Spring at Outlet |
13095200 | Briggs Creek |
13095390 | Snake River abv Blind Canyon Spring |
13095650 | Snake River abv Blue Heart Spring |
13095700 | Blue Heart Spring nr Hagerman |
13132600 | Sand Springs |
13132790 | Bickel Spring |
13133800 | Combo Riley Creek + Brailsford Ditch |
13134600 | Billingsly Creek |
13135100 | Birch Creek |
13152940 | Malad Power Flume |
13153500 | Malad River nr Bliss |
13095300 | Banbury Springs nr Buhl+ |
13093700 | Niagara Springs nr Buhl |
13134800 | Billingsly Creek at Mouth |
1Discharge measurement is the difference between discharge measured at the Snake River upstream and downstream of the spring outlet. |
|
2Discharge is subtracted from measurement at Crystal Springs nr Filer (USGS 13093400). |
The following publications are related to this project.
Methods to estimate annual mean spring discharge to the Snake River between Milner Dam and King Hill, Idaho
Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon
We are conducting this work in cooperation with these partners.
- Overview
Groundwater discharges to the Snake River from numerous volcanic rock springs along the northern canyon wall between Milner Dam and King Hill. Water-resource managers need to be able to quantify the amount of this water to understand the eastern Snake River Plain aquifer's recharge, storage, and discharge. When completed, this study will provide the Idaho Department of Water Resources with an automated method to quantify spring discharge to the Snake River between Milner Dam and King Hill. Updated spring discharge estimates will be useful for developing groundwater management plans and assessing the effectiveness of management actions.
Uppermost vent to Box Canyon Springs near Wendell, Idaho Study Problem
In 1995, the USGS published regression models to quantify discharge from Snake River springs between Milner Dam and King Hill. The models provide estimates of average annual discharge at unmeasurable springs to sum with discharge at measurable springs for an estimate of total annual mean spring discharge to the Snake River between Milner Dam and King Hill. However, changes in land use, water management, and data collection raise questions about whether the regression relationships remain valid. Therefore, it is necessary to update these regression relationships to include data collected in the interim.
Study Objectives
- Identify all available datasets.
- Collect quarterly synoptic spring discharge measurements.
- Assess the uncertainty associated with using measured stream and spring discharge data to estimate reach losses and gains with a water balance approach.
- Assess the uncertainty associated with statistical approaches.
- Compare the uncertainty between the water balance and statistical approaches and report the findings to IDWR with a recommendation for which approach will be most useful for estimating spring discharge into the future.
- Implement an automated method to estimate spring discharge and integrate new data as they are collected.
- Publish methods, data, and software; present details of uncertainty comparisons between water balance and statistical methods and document the methods and accuracy of the approach used to estimate spring discharge to the Snake River.
Synoptic Discharge Measurement Sites
Site Number
Site Name
13132800 Thousand Springs near Hagerman1 13089600 Devil's Washbowl Spring 13090100 Devil's Corral Spring 13091500 Blue Lakes Outlet 13093400 Crystal Springs nr Filer1 - Cedar Draw2 13094500 Clear Lakes Spring at Outlet 13095200 Briggs Creek 13095390 Snake River abv Blind Canyon Spring 13095650 Snake River abv Blue Heart Spring 13095700 Blue Heart Spring nr Hagerman 13132600 Sand Springs 13132790 Bickel Spring 13133800 Combo Riley Creek + Brailsford Ditch 13134600 Billingsly Creek 13135100 Birch Creek 13152940 Malad Power Flume 13153500 Malad River nr Bliss 13095300 Banbury Springs nr Buhl+ 13093700 Niagara Springs nr Buhl 13134800 Billingsly Creek at Mouth 1Discharge measurement is the difference between discharge measured at the Snake River upstream and downstream of the spring outlet.
2Discharge is subtracted from measurement at Crystal Springs nr Filer (USGS 13093400).
- Publications
The following publications are related to this project.
Methods to estimate annual mean spring discharge to the Snake River between Milner Dam and King Hill, Idaho
Many individual springs and groups of springs discharge water from volcanic rocks that form the north canyon wall of the Snake River between Milner Dam and King Hill. Previous estimates of annual mean discharge from these springs have been used to understand the hydrology of the eastern part of the Snake River Plain. Four methods that were used in previous studies or developed to estimate annual mFlow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon
This report is one in a series resulting from the U.S. Geological Survey's Snake River Plain Rasa (Regional Aquifer System Analysis) study that was initiation in October 1979. Purposes of the RASA study were to (1) refine knowledge of the regional ground-water flow system, (2) determine effects of conjunctive use of ground water and surface water, and (3) describe water chemistry. This purpose of - Partners
We are conducting this work in cooperation with these partners.