Reference Library

Contaminant Guides

Plain-English explanations of the most common U.S. drinking water contaminants — what they are, where they come from, health effects, and how to address them.

Heavy Metals

Lead

high

Lead enters drinking water primarily through corrosion of lead service lines and lead-containing plumbing fixtures — not typically from the water source itself. There is no safe level of lead exposure for children. The EPA's 2024 Lead and Copper Rule Improvements require utilities to replace all lead service lines within 10 years.

EPA limit: 15 ppb (action level)

Arsenic

moderate

Arsenic is a naturally occurring metalloid found in geological deposits across the western United States, New England, and the Midwest. It can also enter water through industrial processes. Long-term exposure is strongly linked to bladder, lung, and skin cancer. The EPA reduced the arsenic MCL from 50 ppb to 10 ppb in 2001, though some researchers advocate for an even lower limit.

EPA limit: 10 ppb

Chromium-6

high

Chromium-6 (hexavalent chromium, or Cr-6) is a carcinogenic form of chromium that occurs both naturally from serpentinite rock weathering and from industrial contamination. It was brought to widespread public attention by the Hinkley, California case documented by Erin Brockovich. The EPA has no specific federal MCL for chromium-6 — only a combined 100 ppb limit for total chromium. California attempted to set a state-specific 10 ppb limit for Cr-6 before it was rescinded following industry litigation.

EPA limit: 100 ppb (total chromium)

Copper

moderate

Copper enters drinking water primarily from copper household plumbing and service lines — not from the water source itself. It is regulated under the same Lead and Copper Rule as lead. At low levels, copper is an essential nutrient. At elevated levels (above 1.3 mg/L), it causes gastrointestinal symptoms acutely and liver and kidney damage with chronic exposure. Blue-green staining on sinks and fixtures is the most common sign of elevated copper. Corrosive (low-pH, low-alkalinity) water dramatically accelerates copper leaching.

EPA limit: 1.3 mg/L (action level)

Cadmium

moderate

Cadmium is a toxic heavy metal that enters drinking water primarily from industrial contamination, mining operations, and corrosion of galvanized steel pipes — not typically from natural geological sources. The EPA MCL is 5 ppb. Cadmium is an IARC Group 1 human carcinogen and accumulates in kidney tissue over decades, causing irreversible kidney damage. It is one of the most persistent environmental contaminants because it remains toxic in the body for 10–30 years after exposure stops.

EPA limit: 5 ppb (0.005 mg/L)

Mercury

moderate

Mercury is a toxic heavy metal that occurs naturally and from industrial sources. In drinking water, the concern is inorganic mercury from industrial contamination, mining, and geological sources — distinct from the methylmercury exposure that comes from eating fish. The EPA MCL for inorganic mercury is 2 ppb. Chronic exposure damages the kidneys and nervous system. Mercury violations in public water systems are rare; the greater concern is private wells near gold and mercury mining sites and industrial facilities.

EPA limit: 2 ppb (0.002 mg/L)

Barium

low

Barium is a naturally occurring alkaline earth metal found in sedimentary rock formations across the United States. It enters groundwater through natural geological weathering and from oil and gas drilling operations that produce barium-containing brine. The EPA MCL is 2 mg/L. At elevated levels, barium raises blood pressure and can cause cardiovascular and kidney effects. Barium violations in public water systems are uncommon but occur in parts of the Midwest and Southeast where sedimentary geology concentrates barium in deep aquifers.

EPA limit: 2 mg/L

Minerals

Hard Water

low

Hard water contains elevated levels of dissolved calcium and magnesium. It is not a health risk and is associated with some cardiovascular benefits, but it causes scale buildup in pipes and appliances, soap scum, and reduces the effectiveness of detergents. Approximately 85% of U.S. homes have hard water. It is an aesthetic and infrastructure issue, not a regulatory one.

EPA limit: No federal limit

Fluoride

low

Fluoride is added to most U.S. public water supplies at low levels to reduce tooth decay — a practice called water fluoridation. At the EPA's enforceable limit of 4 mg/L, fluoride causes skeletal fluorosis. At higher natural levels (above 2 mg/L), it causes dental fluorosis (tooth mottling) in children. The current recommended fluoridation level is 0.7 mg/L. Naturally elevated fluoride in groundwater affects well owners in the western U.S., parts of New Mexico, Nevada, and some Texas formations.

EPA limit: 4 mg/L (MCL) / 2 mg/L (Secondary MCL)

Iron & Manganese

low

Iron and manganese are naturally occurring minerals found in groundwater across the United States — they are the most common aesthetic problems reported by private well owners. Iron causes red-brown staining and a metallic taste; manganese causes black-brown staining and at high levels poses a genuine neurological health concern, particularly for infants and children. Neither has a federal health-based MCL (only aesthetic standards), but manganese above 0.3 mg/L warrants health attention beyond aesthetics.

EPA limit: 0.3 mg/L iron / 0.05 mg/L manganese (aesthetic SMCLs)

Selenium

low

Selenium is a naturally occurring mineral essential to human health in trace amounts but toxic at elevated levels — it has one of the narrowest margins between beneficial and harmful dose of any element. In drinking water, selenium exceeds the EPA's 50 ppb MCL primarily near coal mining operations, coal-fired power plant sites, and in naturally selenium-rich agricultural soils of the western United States. Chronic high exposure causes selenosis, characterized by hair loss, nail brittleness, and neurological effects.

EPA limit: 50 ppb (0.05 mg/L)

Radioactive Contaminants

Radon

moderate

Radon is a naturally occurring radioactive gas that dissolves into groundwater from uranium-bearing rock and soil. It is primarily a concern for private well owners — public water systems remove most radon before distribution. The main health risk is not from drinking radon-contaminated water, but from breathing radon gas that off-gasses when the water is used for showering, dishwashing, or laundry. Radon in water contributes to indoor air radon levels, which cause approximately 21,000 lung cancer deaths in the U.S. each year.

EPA limit: No finalized MCL

Uranium

moderate

Uranium is a naturally occurring radioactive heavy metal found in rock and soil across the western United States. It enters groundwater through natural geological weathering and from uranium mining legacy sites. The primary health concern from uranium in drinking water is not radiation but kidney toxicity — uranium acts as a chemical nephrotoxin at concentrations found in some wells. The EPA MCL is 30 µg/L (ppb). An estimated 2 million private well users drink water with uranium above this limit.

EPA limit: 30 µg/L (30 ppb)

Radium

moderate

Radium is a naturally occurring radioactive element found in rock formations across the central and eastern United States. It enters drinking water by dissolving from uranium- and thorium-bearing rock. Radium is a bone-seeking element — it accumulates in bone tissue, delivering ongoing radiation dose from within. The EPA MCL covers combined radium-226 and radium-228 at 5 picocuries per liter (pCi/L). Radium is primarily a concern for public water systems in the Midwest, Gulf Coast, and parts of New England drawing from deep confined aquifers.

EPA limit: 5 pCi/L (combined Ra-226 + Ra-228)