Skip to content

Private Well Water in South Dakota

South Dakota is split between people whose water is tested for them and people whose water is not. Enter your ZIP below to see which principal aquifers USGS maps under your county, how many neighbours USGS counted on wells, and where the state well program and testing guidance live. Every figure here is USGS's, from 2015, and none of it is a statement about your water.

about 129,000 people in South Dakota drink from private wells, 14.6 percent of the state, with nobody testing them
People on private wells
128,711
Share of the state
14.6%
Counties in the USGS file
66
Required water tests
None

What is under your South Dakota well?

USGS county estimates, 2015

South Dakota is where USGS’s aquifer attribution breaks down hardest: the by-aquifer release accounts for only about a quarter of the state’s 129,000 self-supplied residents, so most South Dakota counties here list their principal aquifers without any population divided among them, and the report says exactly that rather than pretending the people are not there. Lincoln County south of Sioux Falls carries the most at about 35,000, more than a quarter of the state total.

Private wells and the law

Nobody is testing South Dakota's private wells

The Safe Drinking Water Act regulates community water systems. It does not regulate your well, and neither, in most respects, does South Dakota. There is no Consumer Confidence Report for a private well, no required sampling schedule, no violation record and no agency that would notice if something changed. EPA says it plainly:

“The quality and safety of drinking water from private domestic wells are not regulated by the Federal Government under the Safe Drinking Water Act nor by most state governments and laws.”

US EPA, Private Drinking Water Wells

“Private well owners are responsible for delivering safe drinking water to their households.”

US EPA, Private Drinking Water Wells

The two halves of South Dakota's drinking water

On a community water system

  • Sampling schedule set by federal rule
  • Violations reported to EPA and public
  • An annual Consumer Confidence Report by law
  • A primacy agency reviewing the results

On a private well, like 128,711 people here

  • No required test, ever
  • No record anyone can look up
  • No report in the mail
  • Nobody reviewing anything

This page covers the well side. South Dakota drinking water quality covers the other: what EPA lists for the systems that do report, which stops at the property line of everyone on this page.

By USGS's 2015 count, South Dakota ranks 24 of 50 by the share of its population on self-supplied water and 45 of 50 by the raw number of people. The national share is 13.2 percent. That puts South Dakota in the middle band, where the well side of the state and the served side are both large enough to be invisible to each other.

A flowing artesian well head in a grassland, water rising from the pipe under its own pressure
A flowing artesian well at the Baca National Wildlife Refuge in Colorado, where the aquifer is under enough pressure to push water out without a pump. Most private wells are nothing like this: a pump, a pressure tank and a cap in the yard, and no way to see what is coming up. “BacaFlowingWell” by Fred Bauder, CC BY-SA 3.0
Advertisement
USGS principal aquifers

South Dakota well water mostly comes from the Lower Cretaceous aquifers

USGS attributes each county's groundwater to the principal aquifer or aquifers it draws from. A principal aquifer is USGS's own category, defined this way:

“A principal aquifer is defined as a regionally extensive aquifer or aquifer system that has the potential to be used as a source of potable (drinkable) water. For study or mapping purposes, aquifers are often combined into aquifer systems.”

USGS, Principal Aquifers of the United States

In South Dakota, USGS's by-aquifer release is incomplete in a specific and important way: the state Water Science Center that built this part of it reported the self-supplied population as zero on most aquifer rows, so only about 25 percent of the state's 128,711 well users are attributed to any aquifer at all. The ZIP report says so on those counties rather than showing a zero. The aquifers below are the ones USGS did attribute people to.

Lower Cretaceous aquifers

21,000

self-supplied residents USGS attributed to it in South Dakota, across 16 counties. Nationally it supplies about 90,000 people in 7 states.

USGS 2015

Upper Cretaceous aquifers

3,596

self-supplied residents USGS attributed to it in South Dakota, across 7 counties. Nationally it supplies about 25,000 people in 4 states.

USGS 2015

Sand and gravel aquifers (glaciated regions)

3,508

self-supplied residents USGS attributed to it in South Dakota, across 15 counties. Nationally it supplies about 8.3 million people in 22 states.

USGS 2015

Other aquifers

2,206

self-supplied residents USGS attributed to it in South Dakota, across 7 counties. Nationally it supplies about 2.2 million people in 37 states.

USGS 2015

These counts are of people, not of wells, and they come from an estimate rather than a census. USGS built them county by county from population and water use records; there is no national well registry to count against, which is itself the point. Read a large figure as a large number of households in the county drawing from that aquifer, and nothing more precise than that.

Our summary of information published by USGS estimated groundwater withdrawals from principal aquifers, county level data for 2015

A pile of rounded sorted gravel from Pleistocene glacial outwash in an Ohio gravel pit
Glacial outwash gravel exposed in a pit in Licking County, Ohio. Sand and gravel aquifers in the glaciated regions supply more self-supplied Americans than any other principal aquifer in USGS's file, and this rounded, sorted material is what they are made of: pore space between stones, filled with water. “Glacial outwash (Pleistocene; St. Louisville gravel pits, Licking County, Ohio, USA) 16 (45402436985)” by James St. John, CC BY 2.0
County by county

South Dakota well water by county

The table below is USGS's 2015 record for every county in South Dakota, sorted by the number of people on self-supplied water. The largest is Lincoln County at about 35,000 people. It is an inventory of use, not a ranking of anything: a county with more well users is a county where more households are on their own, which says nothing about the water in any of them.

Loading the county table from the committed USGS snapshot.

128,711
People on self-supplied water
rank 45 of 50
14.6%
Share of the state
rank 24 of 50, national figure 13.2%
5.6 Mgal/d
Domestic groundwater withdrawn
USGS estimate for 2015
6
Principal aquifers carrying people
USGS attribution, statewide
The part that is yours

Testing a well in South Dakota

Here is EPA's baseline, in EPA's own words:

“Test your private well annually for total coliform bacteria, nitrates, total dissolved solids, and pH levels. If you suspect the presence of other contaminants, you should test for those also. You can also contact your local health department to find out what substances may be common in your area’s groundwater.”

US EPA, Protect Your Home’s Water

“You may want to test more frequently if small children or elderly adults live in your house or if someone in your house is pregnant or nursing. These segments of the population are often more vulnerable to pollutants than others.”

US EPA, Protect Your Home’s Water

Beyond that baseline the list is local, and South Dakota DANR, private well sampling is where South Dakota publishes it. Your county health department usually knows the local answer better still, and in many states will run or subsidise the test. CDC Private Wells and EPA Protect Your Home’s Water cover the general case. Laboratory, test kit and treatment choices follow from a test result and a licensed installer, so the state program and your county health department are the next step.

What state programs typically do regulate is construction, not water: who may drill, how a well must be cased and sealed, and what record gets filed afterwards. EPA's own summary of the national picture:

“While most states have zero or limited regulations for private drinking water wells, states do have programs to assist well-owners.”

US EPA, Private Drinking Water Well Programs in Your State
A USGS continuous water monitoring station cabinet at an observation well in a Georgia forest
A USGS observation well and continuous monitoring station in Georgia. This is the kind of well the federal government does watch: an instrumented hole recording an aquifer's water level for the national record. Nothing like it exists for the well in anyone's yard. “Stephen C. Foster State Park USGS observation well, continuous water monitoring station” by Michael Rivera, CC BY-SA 3.0

One last framing, from USGS, about why the absence of a test is not the same as the absence of a problem:

“Typically, the water supplied by domestic wells is not routinely tested. As a result, people using domestic-supply wells could be drinking water with elevated concentrations of some contaminants.”

USGS, Domestic (Private) Supply Wells
Common questions

South Dakota well water FAQ

Keep going

The rest of South Dakota's water picture

Well water in nearby states

Advertisement

Population, withdrawal and aquifer figures are USGS's, from its estimated use of water in the United States county level data for 2015 (published June 2018 (v2.0)) and its estimated groundwater withdrawals from principal aquifers county level data for 2015 (published February 2020 (v1.0)). ZIP to county resolution uses the Census Bureau's ZCTA relationship file. All are US Government works in the public domain. In EPA's words: "Private well owners are responsible for delivering safe drinking water to their households." National picture: private wells in every state