Private Well Water

Arsenic

Naturally occurring, slow-acting, and present in well water across roughly half the United States

EPA MCL
10 μg/L (parts per billion); lowered from 50 μg/L in 2001
Health concern
Bladder, lung, and skin cancer; cardiovascular disease; skin lesions; cognitive effects in children
Testing method
ICP-MS or graphite furnace atomic absorption; $20-40 mail-in

Arsenic is a naturally occurring metalloid present in rocks and soils throughout the world. It's also one of the most consequential drinking-water contaminants on Earth — chronic exposure to even modest levels causes cancer, heart disease, and developmental problems. The most catastrophic case is Bangladesh, where tens of millions of people drink arsenic-contaminated well water and the resulting cancer rate has been called the largest mass poisoning in human history. The United States has its own version of this problem, just at lower concentrations and in less concentrated populations.

Where it comes from

Arsenic in US groundwater is overwhelmingly geologic, not industrial. It leaches from arsenic-bearing minerals — pyrite, arsenopyrite, arsenian iron oxides — under specific water-chemistry conditions:

Industrial sources exist (smelter emissions, chromated-copper-arsenate wood treatment, historical pesticides) but they're localized exceptions. If you have arsenic in your well, geology is the most likely cause.

The numbers

The USGS estimates that about 7% of US private wells exceed the EPA's 10 μg/L MCL for arsenic. That's roughly 3 million Americans drinking water above the legal standard — and many more drinking water at levels (1-10 μg/L) that recent epidemiology suggests still carry meaningful risk.

Hot zones in the US:

Health effects

Arsenic is a confirmed human carcinogen (IARC Group 1). The cancers it's been shown to cause at chronic exposure: bladder, lung, skin, kidney, and liver. Beyond cancer, it causes cardiovascular disease, peripheral neuropathy, skin lesions (the classic clinical sign of chronic arsenic toxicity), diabetes, and developmental and cognitive effects in children.

The dose-response curve is what makes arsenic difficult. There's no obvious "safe" threshold below 10 μg/L — recent meta-analyses suggest measurable bladder cancer risk at 1-10 μg/L. The WHO and EPA standards are not zero-risk levels; they're regulatory compromises between health protection and treatment cost.

Acute arsenic poisoning happens at much higher doses than you'd ever see from drinking water. The well-water concern is chronic exposure measured in years and decades.

Testing

Arsenic doesn't smell, taste, or color the water. The only way to know is to test.

Treatment

Several treatment methods are well-established. Pick based on your concentration, your water chemistry, and your budget:

If your test shows mostly As(III), the treatment system needs to oxidize it to As(V) first (chlorine, ozone, or specific media). Otherwise you'll get poor removal.

If your well tests above 10 μg/L, install treatment and test again. Arsenic levels can vary seasonally, especially in drought-prone areas. One reading doesn't characterize the well; trend over multiple readings does.

If you've been drinking high-arsenic water

The damage from chronic arsenic exposure is cumulative and partially irreversible — past exposure can't be reversed. But future exposure can be eliminated. If you've been drinking elevated-arsenic water for years, talk to your doctor about appropriate cancer screening (especially bladder cancer surveillance) and any skin findings. Arsenic is one of the contaminants where the medical history actually changes the screening recommendations.

Aquifers where this is a concern

Ogallala (High Plains)Denver Basin

Sources