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![Page 1: Use of Depth-Dependent Sampling to Determine Source Areas and Short- Circuit Pathways for Contaminants to Reach Public-Supply Wells, High Plains Aquifer,](https://reader031.fdocuments.in/reader031/viewer/2022013101/56649f495503460f94c6ad2b/html5/thumbnails/1.jpg)
Use of Depth-Dependent Sampling to Determine Source Areas and Short-
Circuit Pathways for Contaminants to Reach Public-Supply Wells, High Plains
Aquifer, York, Nebraska
Matthew LandonBrian Clark
Allen Christensen
2006 National Water Quality Monitoring Council Meeting, San Jose, California
May 9, 2006
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Take-Home Messages
• Supply-well vulnerability can be strongly influenced by wellbores that cross confining units
• Sampling from different depths in supply wells, in addition to nearby monitoring wells, improves understanding of contaminant pathways to supply wells
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Objective of Depth-Dependent Measurements
• Develop a refined understanding of where water and contaminants enter supply wells
• Depth-Dependent Sampling:– Provides a more detailed vertical profile
than is possible with a monitoring well cluster
– Is potentially useful for identifying short-circuit contamination pathways to the supply well
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High Plains Aquifer TANC Study Area
TANC Study Area
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Monitoring network
Sites with single wells screened near water table (8)Sites with nested wells (7)
1 km
Regional ground-water flow
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Geology and Well Construction – Supply Well
LoessUnconfined sand & gravel
Clayey till
Confined fine sand
Silty clay
Confined fine sand
Carlile Shale
SupplyWellscreen
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Tracer Pulse Method Conceptual DiagramIzbicki et al. (1999)
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• 25% of flow from bottom half of screen
LoessUnconfined sand & gravel
Clayey till
Confined fine sand
Silty clay
Confined fine sand
Carlile Shale
SupplyWellscreen
Well-Bore Flow Profile
42.7 m
61.0 m
PumpIntake39.6 m
Screen
Cumulative percent of total flow
Preliminary – Subject to Revision
Velocity Measurements
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Depth-Dependent Sampling • Samples
collected using a narrow-diameter pump lowered down an access tube that extends below the pump intake
LoessUnconfined sand & gravel
Clayey till
Confined fine sand
Silty clay
Confined fine sand
Carlile Shale
SupplyWellscreen
Depth-Dependent Samples
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Depth Dependent VOCs
LoessUnconfined sand & gravel
Clayey till
Confined fine sand
Silty clay
Confined fine sand
Carlile Shale
SupplyWellscreen
Depth-Dependent Samples
• Similar results for: TCE, U, major ions, 18O, D, N2
Preliminary – Subject to Revision
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Water18O and Cl
Confined
Supplywell (includesdepth-dependent) Urban confined
mixedAg unconfined
Urban unconfinedshallow
Preliminary – Subject to Revision
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Unconfined-Confined Mixing from D
LoessUnconfined sand & gravel
Clayey till
Confined fine sand
Silty clay
Confined fine sand
Carlile Shale
SupplyWellscreen
Depth-Dependent Samples
Percent unconfined water
Preliminary – Subject to Revision
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Unconfined Mixing Fraction from D Confined Monitoring Wells At Supply Well
Percent unconfined waterPercent unconfined water
Preliminary – Subject to Revision
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• Large vertical head gradients across confining layers
• Irrigation, commercial and old municipal wells are commonly screened in unconfined and confined sand layers
Vertical Leakage Through Wellbores
ConfinedHeads
UnconfinedHeads
Preliminary – Subject to Revision
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Contaminant Pathway HypothesesSupply well (SW)leakage or drawdown induced leakage
SWMWMW
MW – Monitoring WellLW – Leaky Well (Multi-Layer)
Areally uniformleakage through confining unit
SWMWMW SWLW MW
Wellbore leakagein multi-layer wells
MW
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Contaminant Pathway HypothesesSupply well (SW)leakage or drawdown induced leakage
SWMWMW
MW – Monitoring WellLW – Leaky Well (Multi-Layer)
Areally uniformleakage through confining unit
SWMWMW SWLW MW
Wellbore leakagein multi-layer wells
MW
Conceptualbackgroundconfined concentration
Conceptualunconfined concentration(increasing left to right)
Fits measuredchemistry data
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Model Simulations
• Model simulations of ground-water age with MODFLOW-GWT (Ground Water Transport) and the MultiNode Well (MNW) package
• Please see talk by Brian Clark at 3:55 today for more details
• Simulations including wellbore leakage in multi-screen wells and known abandoned wells and test holes have the best match with observed age distribution
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HighPlains TANC Conceptual Model
Denitrification
DenitrificationReductive Dechlorination
Wellboreleakage
Urban chemistry signature(s)Agricultural chemistry signature(s)
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Conclusions
• Supply well vulnerability can be strongly influenced by wellbores that cross confining units
• Short-circuit pathways need to be considered in protecting ground-water supplies
• Sampling from different depths in supply wells, in addition to nearby monitoring wells, improves understanding of contaminant pathways to supply wells
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Acknowlegements
• USGS National Water Quality Assessment Program
• Timothy Boyle• Benjamin Dietsch• Michael Turco
• City of York, Nebraska
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Contact Information
Matthew LandonU.S. Geological Survey
4165 Spruance Road, Suite 200San Diego, CA 92101Tele: 619-225-6109
Email: [email protected] Website:
http://oh.water.usgs.gov/TANCweb/NAWQATANC.htm