US Well Water Quality Index 2026: State-by-State Rankings and Contamination Data

Approximately 43 million Americans depend on private wells for drinking water, according to the U.S. Environmental Protection Agency (epa.gov/privatewells). Private wells fall outside the Safe Drinking Water Act, making water quality entirely the homeowner's responsibility. The U.S. Geological Survey's National Water-Quality Assessment program has documented that more than one-third of domestic wells nationally contain at least one contaminant above a human health benchmark (usgs.gov/mission-areas/water-resources/science/national-water-quality-assessment-nawqa-project). The most commonly detected issues are nitrates, arsenic, uranium, radon, and coliform bacteria, with risk distributions shaped by regional geology and agricultural land use. Great Plains states face elevated nitrates from farming. Mountain West and New England states show naturally occurring arsenic and radon in granite and volcanic bedrock. Texas Hill Country wells draw from Edwards Aquifer limestone, encountering hardness, iron, and occasional radium. This index compiles primary-source federal and state data to classify private well water quality risk by state and contaminant, updated for 2026. Verify current figures with the cited primary sources before making any treatment decisions.
Texas well owner? True H2O provides free in-home water testing across San Antonio and the surrounding communities.
Schedule Free Water TestKey findings: US private well water quality by the numbers
The following figures are drawn from the USGS National Water-Quality Assessment program, which has monitored domestic well water quality across the United States since 1991. The primary reference is DeSimone et al. (2009), "Quality of Water from Domestic Wells in Principal Aquifers of the United States, 1991 to 2004," available through the USGS National Water-Quality Assessment project at usgs.gov/nawqa. Verify all figures with that source before citing them, as the NAWQA program continues to update its findings.
- More than one-third of domestic wells nationally contain at least one contaminant above a human health benchmark, based on USGS NAWQA monitoring data (usgs.gov/nawqa).
- Nitrate exceeds the EPA maximum contaminant level of 10 mg/L in approximately 7% of domestic wells nationally, with the highest rates in Corn Belt agricultural states.
- Arsenic exceeds the EPA MCL of 10 micrograms per liter in approximately 6% of domestic wells, with the highest rates in New England, the Mountain West, and parts of the Midwest.
- Radon exceeds the EPA proposed guidance level of 300 picoCuries per liter in an estimated 22% of domestic wells, primarily in the eastern United States and in granite-heavy western states.
- Total coliform bacteria are detected in a significant share of untreated domestic wells, particularly shallow wells and those in karst or fractured-rock geology.
- PFAS are now detected in private wells near military bases, airports, and industrial facilities in states across the country, based on ongoing EPA and state monitoring programs following the 2024 PFAS MCL rule (epa.gov/sdwa).
- Approximately 43 million Americans, or about 13% of the US population, rely on private wells for drinking water, according to the EPA (epa.gov/privatewells).
These national averages mask significant state-by-state variation. A homeowner in rural Iowa faces a very different contamination risk profile than a homeowner in rural Texas or rural Maine. The state-level index below maps those differences using the best available published data.
State-by-state private well water quality risk index
The table below classifies each state into one of three risk tiers based on USGS NAWQA data and state-level monitoring programs. Risk tiers reflect the pattern of documented contamination in domestic wells, not a single numeric score. Elevated means NAWQA or equivalent state data documents multiple contaminants at health benchmarks in a meaningful proportion of wells. Moderate means one primary documented concern is prominent. Lower means limited NAWQA coverage or few documented widespread concerns, though all private wells in every state require annual testing.
| State | Risk Tier | Primary Contaminant Concerns | Data Source |
|---|---|---|---|
| Alabama | Moderate | Bacteria, iron, manganese | USGS NAWQA |
| Alaska | Lower | Bacteria in rural areas; limited NAWQA coverage | USGS NAWQA |
| Arizona | Elevated | Arsenic, uranium, total dissolved solids (Basin and Range geology) | USGS NAWQA |
| Arkansas | Moderate | Bacteria, nitrates (poultry-farming areas) | USGS NAWQA |
| California | Elevated | Arsenic (Central Valley), nitrates (agricultural areas), uranium, PFAS near military sites | USGS NAWQA |
| Colorado | Moderate | Radon, uranium (mountain geology), some arsenic | USGS NAWQA |
| Connecticut | Elevated | Radon, arsenic (granite bedrock), PFAS near manufacturing corridors | USGS NAWQA |
| Delaware | Moderate | Nitrates (agricultural), bacteria | USGS NAWQA |
| Florida | Moderate | Bacteria (shallow Floridan Aquifer wells), saltwater intrusion in coastal areas | USGS NAWQA |
| Georgia | Moderate | Bacteria, uranium (Piedmont granite) | USGS NAWQA |
| Hawaii | Lower | Saltwater intrusion in coastal wells; limited NAWQA data | USGS NAWQA |
| Idaho | Moderate | Nitrates (Snake River Plain agriculture), some arsenic | USGS NAWQA |
| Illinois | Moderate | Nitrates (Corn Belt), bacteria | USGS NAWQA |
| Indiana | Elevated | Nitrates (intensive agriculture), bacteria, arsenic (glacial sediments) | USGS NAWQA |
| Iowa | Elevated | Nitrates (Corn Belt), bacteria, arsenic | USGS NAWQA |
| Kansas | Elevated | Nitrates (agricultural), uranium, arsenic | USGS NAWQA |
| Kentucky | Moderate | Bacteria (karst geography allows rapid surface contamination), some nitrates | USGS NAWQA |
| Louisiana | Moderate | Bacteria, iron, saltwater intrusion in coastal parishes | USGS NAWQA |
| Maine | Elevated | Arsenic (granite bedrock), radon, uranium | USGS NAWQA |
| Maryland | Moderate | Nitrates (Eastern Shore agriculture), radon (Piedmont region), arsenic | USGS NAWQA |
| Massachusetts | Elevated | Radon, arsenic (granite), PFAS near military installations | USGS NAWQA |
| Michigan | Elevated | Arsenic (glacial outwash deposits), bacteria, PFAS near military and manufacturing sites | USGS NAWQA |
| Minnesota | Elevated | Arsenic (glacial deposits), nitrates, radon | USGS NAWQA |
| Mississippi | Moderate | Bacteria, iron, manganese | USGS NAWQA |
| Missouri | Moderate | Bacteria (karst), nitrates, some arsenic | USGS NAWQA |
| Montana | Elevated | Arsenic (volcanic and sedimentary geology), uranium, radon | USGS NAWQA |
| Nebraska | Elevated | Nitrates (Ogallala Aquifer, intensive agriculture), uranium, arsenic | USGS NAWQA |
| Nevada | Elevated | Arsenic, uranium (Basin and Range geology), total dissolved solids | USGS NAWQA |
| New Hampshire | Elevated | Arsenic, radon, uranium (granite bedrock) | USGS NAWQA |
| New Jersey | Moderate | Radon, arsenic, PFAS near chemical manufacturing corridors | USGS NAWQA |
| New Mexico | Elevated | Arsenic, uranium (desert basin geology), total dissolved solids | USGS NAWQA |
| New York | Moderate | Radon, arsenic, PFAS near military and manufacturing sites | USGS NAWQA |
| North Carolina | Moderate | Radon, arsenic, PFAS near Camp Lejeune and other military installations | USGS NAWQA |
| North Dakota | Moderate | Nitrates (agriculture), uranium | USGS NAWQA |
| Ohio | Moderate | Nitrates (agriculture), bacteria, some arsenic | USGS NAWQA |
| Oklahoma | Moderate | Nitrates, arsenic, bacteria | USGS NAWQA |
| Oregon | Moderate | Arsenic (volcanic Cascade geology in some areas), nitrates (Willamette Valley agriculture) | USGS NAWQA |
| Pennsylvania | Elevated | Radon, arsenic (Piedmont crystalline rock), manganese, PFAS near military sites | USGS NAWQA |
| Rhode Island | Moderate | Radon, arsenic (granite), PFAS | USGS NAWQA |
| South Carolina | Moderate | Bacteria, radon (Piedmont), arsenic | USGS NAWQA |
| South Dakota | Moderate | Nitrates (agriculture), uranium, arsenic | USGS NAWQA |
| Tennessee | Moderate | Bacteria (karst geography), nitrates | USGS NAWQA |
| Texas | Moderate | Hardness (Edwards Aquifer limestone), iron, radium, nitrates (West Texas Ogallala), bacteria in rural areas | USGS NAWQA / Texas Water Development Board |
| Utah | Moderate | Arsenic, uranium, total dissolved solids (arid basin geology) | USGS NAWQA |
| Vermont | Elevated | Arsenic, radon (granite and metamorphic bedrock) | USGS NAWQA |
| Virginia | Moderate | Radon, arsenic (Piedmont), bacteria | USGS NAWQA |
| Washington | Moderate | Nitrates (eastern Washington agriculture), arsenic (volcanic geology, some areas) | USGS NAWQA |
| West Virginia | Moderate | Bacteria, arsenic, PFAS near chemical manufacturing facilities | USGS NAWQA |
| Wisconsin | Elevated | Arsenic (Fox River Valley, glacial deposits), nitrates (agriculture), bacteria | USGS NAWQA |
| Wyoming | Moderate | Uranium, arsenic (sedimentary geology), radon | USGS NAWQA |
Risk tiers are based on USGS NAWQA published research and represent documented contamination patterns, not predictions for any individual well. Verify with each cited source. All private wells require annual testing regardless of state risk tier.
What are the most common contaminants in private wells?
Five contaminant categories account for the large majority of health-benchmark exceedances documented in USGS NAWQA monitoring of domestic wells. Each has a distinct geographic pattern tied to geology, land use, or proximity to specific industrial activities. Sourced from the USGS NAWQA program at usgs.gov/nawqa and the CDC private well guidance at cdc.gov/privatewells.
Nitrates
The most commonly detected contaminant above the EPA MCL of 10 mg/L, present in approximately 7% of domestic wells nationally. Nitrate in well water primarily enters from agricultural fertilizers, septic systems, and livestock waste. It is odorless and colorless. High nitrate concentrations pose acute health risk to infants under six months, causing a condition called methemoglobinemia. Agricultural states in the Corn Belt (Iowa, Nebraska, Indiana, Kansas, Illinois) show the highest rates. Testing annually is the only detection method.
Arsenic
A naturally occurring metalloid found in rock formations that groundwater passes through. Exceeds the EPA MCL of 10 micrograms per liter in approximately 6% of domestic wells nationally. Arsenic is odorless and tasteless. Long-term exposure above the MCL is associated with increased risk of bladder, lung, and skin cancers, and cardiovascular effects. Highest in New England granite states (Maine, New Hampshire, Vermont), the Mountain West (Nevada, Arizona, New Mexico, Montana), and parts of the Midwest (Michigan, Wisconsin, Minnesota) with glacial geological deposits.
Radon
A naturally occurring radioactive gas produced by uranium decay in rock. Radon dissolves into groundwater and is released indoors when water is used. The EPA proposed a guidance level of 300 picoCuries per liter for domestic wells; radon is estimated to exceed this level in approximately 22% of domestic wells nationally. Radon has no enforceable federal MCL for private wells. Highest in New England states (Maine, New Hampshire, Vermont, Massachusetts, Connecticut), the Mid-Atlantic (Pennsylvania, Virginia, Maryland), and mountain states with uranium-bearing geology. Mitigation involves aeration of well water and indoor radon ventilation.
Coliform Bacteria
Total coliform bacteria and E. coli are the primary indicators of fecal contamination risk in well water. The EPA MCL for public systems requires zero detection of E. coli; private wells operate without this regulatory standard. Bacteria contamination in private wells typically enters through surface water infiltration (particularly during floods), poorly sealed well casings, and proximity to septic systems or livestock. Karst geology states (Kentucky, Tennessee, Missouri, Florida) are at elevated risk because sinkholes and fractures allow rapid surface water movement into aquifers. UV disinfection and chlorination are the standard treatment options. The CDC recommends testing for bacteria annually at minimum.
PFAS (Per- and Polyfluoroalkyl Substances)
Per- and polyfluoroalkyl substances are a class of synthetic chemicals associated with nonstick coatings, firefighting foam (AFFF), and numerous industrial applications. PFAS are now detected in private wells across the country, with the highest concentrations documented near military installations that used AFFF for firefighting training, near industrial manufacturing facilities, and in areas where PFAS-laden biosolids were applied to agricultural land. The EPA finalized maximum contaminant levels for six PFAS compounds in April 2024, applicable to public water systems. Private wells have no federal regulatory limit. Reverse osmosis and certain activated carbon filters are the EPA-recommended treatment approaches for PFAS in drinking water.
Regional breakdown: where private well water problems are most concentrated
USGS NAWQA has identified four broad regions where well water contamination rates are highest. Each region's problems are driven by the underlying geology and dominant land use, not by industrial activity alone. This regional view helps homeowners understand their baseline risk before ordering specific lab tests. All data cited from the USGS NAWQA program (usgs.gov/nawqa) and the EPA (epa.gov/privatewells).
New England and the northeastern United States
Primary concern: Arsenic and radon from granite bedrock
The granite and metamorphic bedrock underlying Maine, New Hampshire, Vermont, Massachusetts, Connecticut, Rhode Island, Pennsylvania, and parts of New York and Virginia contains naturally occurring arsenic, radon, and uranium. As groundwater moves through fractures in this bedrock over time, it dissolves these elements. NAWQA data documents some of the highest rates of arsenic above the MCL and radon above the proposed guidance level in domestic wells anywhere in the country, concentrated in these states. Maine and New Hampshire in particular have published extensive state-level monitoring data confirming this pattern. Annual arsenic and radon testing is the standard recommendation for any private well in this region.
The Great Plains and Midwest Corn Belt
Primary concern: Agricultural nitrates, arsenic in glacial sediments
Iowa, Nebraska, Kansas, Indiana, Illinois, Wisconsin, Minnesota, Ohio, and surrounding states overlay some of the most productive agricultural land in the world, where nitrogen fertilizers applied at scale over decades have leached nitrate into shallow groundwater. NAWQA identifies this region as having the highest rates of nitrate above the MCL in domestic wells in the country. Additionally, glacial outwash deposits across Minnesota, Wisconsin, Michigan, and Indiana contain naturally occurring arsenic and manganese that dissolve into groundwater over time. Well owners in this region should test annually for nitrates, bacteria, arsenic, and manganese at minimum.
The Mountain West and desert Southwest
Primary concern: Arsenic, uranium, total dissolved solids from arid geology
Arizona, Nevada, New Mexico, Montana, Utah, Wyoming, and parts of California overlie volcanic, sedimentary, and basin-and-range geology that is naturally enriched in arsenic and uranium. Arid conditions concentrate dissolved minerals, and total dissolved solids in many western wells exceed levels that affect taste and appliance longevity. NAWQA documents arsenic and uranium above health benchmarks in a significant proportion of domestic wells in these states, driven by geology rather than agricultural or industrial activity. The U.S. Geological Survey has published specific aquifer-level studies on arsenic and uranium distribution in western groundwater, available through the NAWQA program.
The South and karst regions
Primary concern: Bacteria from rapid infiltration through karst
Karst limestone geology, widespread across Kentucky, Tennessee, Missouri, Florida, and parts of Virginia and Texas, creates a direct pathway from the surface to groundwater. Sinkholes, losing streams, and fractured limestone allow surface runoff, including agricultural runoff carrying bacteria and nitrates, to enter aquifers rapidly with little natural filtration. NAWQA data shows elevated coliform bacteria in domestic wells in karst regions compared to areas with deeper, more protected aquifers. UV disinfection is the standard treatment for bacteria in private wells in karst regions. Florida additionally faces saltwater intrusion in coastal areas as sea levels rise and freshwater aquifer levels decline.
Texas well water quality: Edwards Aquifer, Hill Country, and regional data
Texas has approximately 1.4 million private water wells statewide, according to the Texas Water Development Board (twdb.texas.gov/groundwater). Unlike the New England states where arsenic is the dominant concern, or the Corn Belt where nitrates drive risk, Texas well water quality is highly variable by aquifer and region. The state overlies nine major aquifers, each with a distinct chemistry profile. For homeowners in the San Antonio metro and Hill Country, where True H2O operates, the relevant aquifers are the Edwards Aquifer and the Trinity Aquifer.
The Edwards Aquifer is a karst limestone formation spanning roughly 3,000 square miles beneath central Texas, according to the Edwards Aquifer Authority (edwardsaquifer.org). Water filtering through limestone over geologic time picks up calcium and magnesium, which is why Edwards Aquifer wells are typically very hard at 15 to 25 or more grains per gallon. Hardness is not a health concern but is the single most common water quality problem reported by well owners drawing from the Edwards Aquifer, causing scale buildup, shortened appliance life, and soap efficiency issues. For more detail on how the Edwards Aquifer affects San Antonio water specifically, read our San Antonio water quality guide and our overview of whether San Antonio has hard water.
Beyond hardness, Edwards Aquifer wells in Kendall County and the western Hill Country margin can contain elevated combined radium (radium-226 and radium-228) in some zones. The EPA maximum contaminant level for combined radium is 5 picoCuries per liter for public water systems. Private wells have no federal MCL but the same health reference applies. The Edwards Aquifer Authority publishes groundwater quality monitoring data for the aquifer at edwardsaquifer.org. Iron and hydrogen sulfide (producing a rotten egg odor) are more commonly associated with Trinity Aquifer wells in the Hill Country than with Edwards Aquifer wells.
In West Texas, the Ogallala Aquifer underlies the High Plains agricultural region. Decades of intensive irrigated farming have elevated nitrate concentrations in the Ogallala, making nitrate testing a priority for private well owners in that region. The Texas Water Development Board tracks Ogallala nitrate data through its groundwater quality database at twdb.texas.gov/groundwater.
For Texas Hill Country well owners, the treatment profile typically starts with a whole-home water softener to address hardness, followed by iron and sulfur treatment if those are detected in the specific well, and an under-sink reverse osmosis system for drinking water. The right configuration depends on what a certified laboratory test actually finds in the individual well, not on zone averages. For more on treatment approaches for Texas well water, read our guide to well water treatment options for Texas homeowners. For understanding what signs your home water may have, see our guide to signs of hard water.
True H2O serves private well customers across the San Antonio metro, including the Hill Country communities of Boerne, Helotes, and surrounding Kendall County. For current hardness and water quality data specific to Boerne, see our Boerne, TX water quality article. For New Braunfels, see the New Braunfels water quality guide. Schedule a free in-home well water test at trueh20.net/water-testing.
How to test your private well water
Testing is the only way to know what is in your well water. The CDC recommends annual testing for bacteria and nitrates as a minimum, with a more comprehensive panel every three to five years or after any event that could affect water quality (cdc.gov/healthywater/drinking/private/wells). There are four main approaches:
State-certified laboratory testing is the most reliable option for private well owners. You collect a water sample using the sterile bottles and instructions the lab provides, ship it back via the prepaid label, and receive a detailed report within three to seven business days. A basic bacteria and nitrate panel from a certified lab costs roughly 30 to 60 dollars. A comprehensive heavy metals, arsenic, radon, and VOC panel runs 100 to 200 dollars or more. The EPA maintains a list of state-certified laboratories at epa.gov/privatewells. In Texas, the Texas Commission on Environmental Quality (TCEQ) maintains a database of licensed water testing labs at tceq.texas.gov.
Professional in-home water testing from a water treatment specialist provides an immediate reading for hardness, chlorine (if any), pH, and total dissolved solids at your specific tap using calibrated instruments. The technician interprets the results in the context of your well type, aquifer, and household needs, and recommends treatment only when the data supports it. This is the best first step for Texas Hill Country homeowners who want an expert assessment rather than a mail-in lab number alone. True H2O provides free in-home well water testing across the San Antonio metro and Hill Country communities. Read more about what professional testing involves in our guide on why professional water testing matters.
At-home test strips and meters are useful quick checks but not adequate for treatment decisions. Test strips measure hardness, chlorine, and pH colorimetrically with a resolution too low to size a water softener or confirm safety. TDS meters measure total dissolved solids but do not identify which substances are present. Neither method detects bacteria, arsenic, nitrates, radon, or PFAS. For a full comparison, see our article on how to test water quality at home.
Select your panel based on your region. The state risk index above gives you the starting point. If you are in Maine or New Hampshire, prioritize arsenic and radon. If you are in Iowa or Nebraska, prioritize nitrates and bacteria. If you are in the Texas Hill Country, prioritize hardness, iron, sulfur, bacteria, and radium. Your state health department and the EPA's private wells resources page can help identify any additional locally relevant contaminants to include.
When to treat your well water vs when to connect to municipal supply
Most private well issues are treatable at reasonable cost. The decision to install treatment or connect to a municipal system depends on the specific contaminants found, the severity of contamination, the available treatment technologies, and whether municipal service is accessible.
Treatment is the right choice in most cases. Hardness, iron, sulfur odor, bacteria, nitrates, arsenic at moderate levels, and radon all have well-established treatment approaches. A whole-home water softener addresses hardness and protects appliances. An oxidation filter removes iron and sulfur before the softener. UV disinfection provides chemical-free bacteria inactivation for well water. An under-sink reverse osmosis system reduces nitrates, arsenic, radium, and PFAS at the drinking tap. For most Texas Hill Country homeowners, a softener-plus-RO combination addresses the dominant well water concerns without requiring a connection to municipal supply. For more on how to choose between treatment approaches, see our comparison of reverse osmosis versus whole-house filtration and our guide to water softeners versus water filters.
When to consider municipal connection. Connecting to a public water system is worth evaluating when: (1) multiple serious contaminants are detected that require complex multi-stage treatment, (2) the well has structural issues requiring costly replacement, (3) municipal service is already available at the property boundary and the tap-in fee is competitive with treatment system cost, or (4) the contamination source (agricultural runoff, industrial discharge) is ongoing and unlikely to improve. In many rural Texas areas, municipal service is not available, making treatment the only practical path. Verify availability with your local utility district or the Texas Commission on Environmental Quality at tceq.texas.gov.
True H2O serves well-water homeowners across Bexar County, Kendall County, Comal County, and the surrounding Hill Country communities. We provide free in-home well water assessments and treatment recommendations based on what your actual well test shows. Schedule at trueh20.net/water-testing or see our service areas at Bexar County water testing and Comal County water testing.
Related Guides
- San Antonio Water Quality: What You Need to Know in 2026
- Well Water Treatment Options for Texas Homeowners
- Why Professional Water Testing Matters for Your Family
- 7 Signs You Have Hard Water (And What to Do About It)
- Reverse Osmosis vs Whole-House Filtration: Which Is Right for You?
- San Antonio Water Softener Installation Guide
- Does San Antonio Have Hard Water? 2026 SAWS Data
- PFAS in San Antonio Water: 2026 Test Results
- How to Test Water Quality at Home in San Antonio
- Water Softener vs Water Filter for San Antonio
- Boerne, TX Water Quality 2026: Hard Water Data for Kendall County
- New Braunfels Water Quality 2026: NBU Data and Hardness Guide
- Water Testing Services in Bexar County, TX
- Water Softeners in Bexar County, TX
- Water Testing Services in Comal County, TX
- Schedule a Free In-Home Water Test
Frequently Asked Questions
Which states have the worst well water quality?
Based on USGS National Water-Quality Assessment data, states with the highest documented contamination rates in private wells include Maine, New Hampshire, Vermont, and Massachusetts for arsenic and radon from granite bedrock; Iowa, Nebraska, Indiana, Kansas, and Wisconsin for agricultural nitrates; Arizona, Nevada, New Mexico, and Montana for naturally occurring arsenic and uranium; and Michigan and Minnesota for arsenic from glacial geology. Risk classifications reflect long-term federal monitoring patterns, not a single annual score. All private well owners should test annually regardless of state risk tier.
What is the most common contaminant found in private wells?
Nitrate is the most commonly detected contaminant above health benchmarks in domestic wells, exceeding 10 mg/L in approximately 7 percent of domestic wells nationally, according to USGS National Water-Quality Assessment data (https://www.usgs.gov/mission-areas/water-resources/science/national-water-quality-assessment-nawqa-project). Arsenic exceeds the EPA maximum contaminant level of 10 micrograms per liter in about 6 percent of domestic wells. Radon exceeds the EPA proposed guidance level of 300 picoCuries per liter in an estimated 22 percent of domestic wells, though radon has no federally enforceable MCL for private wells. Total coliform bacteria appear in a significant portion of untreated wells, particularly older and shallow wells.
How often should you test private well water?
The CDC recommends testing private well water at least once a year for bacteria (total coliform and E. coli) and nitrates as a minimum baseline (https://www.cdc.gov/healthywater/drinking/private/wells/index.html). A more comprehensive panel covering arsenic, heavy metals, pH, hardness, and locally relevant contaminants should be conducted every three to five years, or after any of these events: flood or major storm, change in water taste or odor or color, new infant in the household, nearby land-use change such as new agriculture or industrial activity, or well infrastructure work such as pump replacement or new casing.
Is well water safe to drink without treatment?
Well water safety depends entirely on what is in the specific well, which varies by geology, depth, and surrounding land use. The EPA does not regulate private well water under the Safe Drinking Water Act. The USGS National Water-Quality Assessment program has documented that more than one-third of domestic wells nationally contain at least one contaminant above a human health benchmark (https://www.usgs.gov/mission-areas/water-resources/science/national-water-quality-assessment-nawqa-project). Many contaminants that pose health risks, including nitrates, arsenic, uranium, and radon, have no detectable taste or odor. Annual laboratory testing is the only reliable method for confirming safety.
What does the EPA recommend for private well water testing?
The EPA recommends that private well owners test annually for bacteria, nitrates, pH, and total dissolved solids. The EPA also recommends testing for local contaminants of concern: pesticides and nitrates in agricultural areas, radon in radon-prone regions, arsenic in New England and the Mountain West, and PFAS near military installations or industrial sites. For new wells or after infrastructure changes, a comprehensive panel is recommended. The EPA maintains a private well resource guide at epa.gov/privatewells. State health departments and EPA-certified laboratories help identify which contaminants are most relevant for your location.
What are the signs that well water is contaminated?
Many dangerous well water contaminants, including arsenic, nitrates, radon, and low-level bacteria, produce no detectable taste, odor, or color change. Observable signs that may indicate a problem include: rotten egg smell (hydrogen sulfide), orange or reddish staining on fixtures (iron or manganese), cloudy or turbid water (sediment or bacteria), salty or brackish taste (elevated total dissolved solids or saltwater intrusion), or gastrointestinal illness shortly after drinking. However, the absence of these signs does not confirm safety. Annual testing by an EPA-certified laboratory is the only reliable detection method.
Methodology
The US Well Water Quality Index 2026 is a qualitative risk classification, not a numeric score. Each state is placed in one of three tiers (Elevated, Moderate, Lower) based on the pattern of documented contamination in domestic wells as reported by long-term federal and state monitoring programs. The primary source is the USGS National Water-Quality Assessment (NAWQA) program, which has conducted systematic monitoring of groundwater quality across major US aquifer systems since 1991 (usgs.gov/nawqa). The foundational dataset is DeSimone et al. (2009), "Quality of Water from Domestic Wells in Principal Aquifers of the United States, 1991 to 2004."
Secondary sources include: the EPA Safe Drinking Water Information System (SDWIS); CDC private well health guidance (cdc.gov/healthywater/drinking/private/wells); the Texas Water Development Board groundwater quality database (twdb.texas.gov/groundwater); and the Edwards Aquifer Authority water quality monitoring program (edwardsaquifer.org).
Risk tier assignment criteria. A state is classified as Elevated when NAWQA or equivalent state-level data documents two or more contaminants exceeding health benchmarks in a meaningful proportion of domestic wells, or when one contaminant is documented at high rates and backed by dedicated state monitoring programs. A state is classified as Moderate when one primary contaminant concern is prominently documented in NAWQA or state data. A state is classified as Lower when NAWQA coverage is limited or when documented widespread contamination is minimal, which does not imply safety and does not remove the need for annual testing.
Data currency and limitations. Risk classifications were compiled in July 2026 using the most recently available NAWQA publications and EPA data. NAWQA monitoring is ongoing and findings are updated as new aquifer studies are completed. State-level risk can change over time as land use changes, aquifer depletion occurs, or new contamination sources are identified. The PFAS tier for multiple states will likely be revised upward as monitoring under the EPA's April 2024 PFAS rule produces more comprehensive data. Users should verify current state-level data with the cited primary sources before making any treatment or testing decisions. The tier classification reflects published literature patterns at a state scale and does not predict contamination at any individual well.
No numeric scores are assigned. The index uses qualitative tiers rather than numeric scores because the NAWQA data covers domestic wells across principal aquifer systems and does not produce a single comparable state-level index number. Creating a synthetic numeric score from heterogeneous aquifer data would misrepresent the underlying uncertainty. Risk tiers are a descriptive framework for communicating relative concern, not a regulatory determination.
Last updated: July 31, 2026. True H2O compiled this index for informational purposes. Verify all data with the primary sources cited before making treatment, testing, or health decisions.
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