Title: Arsenic in Minnesota Groundwater
1Arsenic in Minnesota Groundwater
- Mindy Erickson, P.E.
- Water Resources Science
- University of Minnesota
- Funding provided by CURA, MDH, WRC and USGS
2Why Arsenic? Why Now?
- In 2001, MCL changed from 50 ug/L to 10 ug/L
- Public Water Suppliers (PWS) must comply by
January 1, 2006 - About 40 MN PWS affected
- Treatment plants for arsenic are expensive
3Why the Change?Arsenic and Health
- Exposure
- Living with a smoker
- Arsenic at 50 ug/L
- Contaminant (EPAs standard threshold)
Arsenic is classified by EPA as a known human
carcinogen. It can cause skin, lung, prostate,
and bladder cancers skin lesions nerve damage
and other health effects.
4Arsenic Occurrence
- Arsenic naturally present in rock and sediment at
1 to 100s mg/Kg - Crustal average is 1.8 mg/Kg
- At 1.8 mg/Kg, solubilization of lt0.1 yields 10
ug/L arsenic in water - Certain geochemical conditions leach arsenic into
groundwater - Arsenic in mid-western groundwater is widespread
and naturally occurring
5Arsenic Chemistry
- Arsenate (As5 ? H2AsO4-, HAsO4-2)
- Oxidized form
- Adsorbs to metal oxides
- Arsenite (As3 ? H3AsO3)
- Reduced form more toxic inorganic form
- Adsorbs to iron oxides
- Organic Arsenic (many forms)
- In foods highest in seafood
- Uncommon in groundwater
6Arsenic Release Mechanisms
- Reductive Desorption
- Reductive Dissolution
- Anion Competition
- Mineral Oxidation (often pyrite)
7Project Goals
- Characterize arsenic variability
- Spatial
- Temporal
- Investigate geochemical connections and
mechanisms - Provide information for developing regulations
and guidelines
8Research Tasks
- Database building
- PWS Sampling
- Sediment Sampling
- Private Well Sampling
- Statistical Analysis
- Geochemical/hydrological modeling
9Database Building
- Quaternary geology information
- Water quality data
- Sediment geochemical data
- Well construction information
10Minnesota Arsenic Data
- National Uranium Resource Evaluation
- Public Water Supplies
- Centers for Disease Control
- MN Pollution Control Agency GWMAPS
- Minnesota Arsenic Study (MARS)
- Minnesota Geological Survey
- Other
11Minnesota Arsenic and Geology
12Recent Glacial History
13Regional Arsenic and Geology
14Arsenic and the Des Moines Lobe Till
- 10 of PWS within the Des Moines lobe footprint
exceed 10 ug/L - 2 of PWS outside of Des Moines lobe footprint
exceed 10 ug/L - 3,200 measurements
15Arsenic in Sediment
- Sediment arsenic concentrations vary from lt1 to
50 mg/Kg in the region - Average sediment arsenic concentrations are
similar across the region - No direct link between sediment arsenic
concentration and water arsenic concentration - Des Moines lobe till is not the source of arsenic
in groundwater
16As and Well Characteristics
Till
Sand
17As and Well Characteristics
Description Avg As As gt 10 Count
Screen 8 feet Clay 4 feet 20 60 224
All others 17 49 606
Screen gt 8 feet Clay gt 4 feet 12 40 71
18Research Tasks
- Database building
- PWS Sampling
- Sediment Sampling
- Private Well Sampling
- Statistical Analysis
- Geochemical/hydrological modeling
19PWS Sampling
- Arsenic Variability
- Local Private well sampling
- Temporal sampling of city well(s)
- Filtered/Unfiltered pairs (selected sites)
- Water analyzed for metals, arsenic species, major
anions, TOC, ammonium
20Participating Communities
21Nielsville SI Wells
22Nielsville SI Wells
23Long-Term Temporal Results
24Long-Term Temporal Results
25Short-Term Temporal Results
26PWS Results
- No difference between raw water filtered and
unfiltered arsenic concentrations - Significant difference between chlorinated
filtered/unfiltered arsenic concentrations - No long-term trends
- Some significant short-term variability
- Low arsenic private wells identified near some
high arsenic PWS wells
27PWS Results Implications
- Most water arsenic is dissolved
- Four quarterly samples from an old well is likely
representative - Short-term temporal sampling is worthwhile for
wells with As close to the MCL - Site investigation is worthwhile
- Low cost
- Quick implementation
- Significant potential cost savings
28Research Tasks
- Database building
- PWS Sampling
- Sediment Sampling
- Private Well Sampling
- Statistical Analysis
- Geochemical/hydrological modeling
29Sediment Sampling
- Sediment and water samples from 8 new private
wells, mud-rotary drilling - Sediment and water samples from 2 new monitoring
wells, rotasonic drilling - Sediment analyzed for metals, organic carbon,
carbonate - Selected sediment samples sequentially extracted
- Water analyzed for metals, major anions, arsenic
species, ammonium, and TOC
30Mud-Rotary Water Results
31 Mud-Rotary Results
- No direct correlation between sediment arsenic
concentration and water arsenic concentration - Arsenic concentration in till averaged 6 mg/Kg,
Fe 2 - Arsenic in aquifer sediment averaged 1.5 mg/Kg,
Fe 0.8 - High arsenic concentration increases over time in
new wells
32Monitoring Wells
33Monitoring Wells
34Monitoring Wells
35Preliminary Rotasonic Results
- Organic layer observed between the till and sand
- 0.5 0.7 mg/Kg arsenic is adsorbed to the
sediment grains - Broad sediment and water geochemistry yet to come
36Research Tasks
- Database building
- PWS Sampling
- Sediment Sampling
- Private Well Sampling
- Statistical Analysis
- Geochemical/hydrological modeling
37Private Well Sampling
- 60 private wells selected based on well
characteristics and arsenic concentration - Water analyzed for metals, major anions, arsenic
species, ammonium, and TOC - Filtered/unfiltered pairs at 20 wells
38Private Well Sampling Results
39Private Well As Speciation Results
40Preliminary Private Well Sampling Results
- Arsenic concentration is not directly correlated
to TOC or ammonium concentration - Most arsenic is As3
- Most arsenic is dissolved, not particulate
- Well water with a rotten egg smell has
relatively low arsenic about 10 ug/L
41Research Tasks
- Database building
- PWS Sampling
- Sediment Sampling
- Private Well Sampling
- Statistical Analysis
- Geochemical/hydrological modeling
42Outcomes
- Quantify arsenic phases
- Support or refute preliminary observation of
increasing arsenic concentration in new wells - Narrow potential geochemical mechanisms and
geological/hydrogeological controls - Characterize arsenic variability
- Provide MDH with info for developing guidelines
and regulations