Water in Lawrence County sits in old sandstone and shale layers buried deep underground. These rocks are over 300 million years old and formed from sand and mud deposited in ancient seas. The rock holds water in small cracks and spaces between the grains.
Manganese, iron, and radon all come from the rock itself. As groundwater slowly moves through the sandstone and shale, it dissolves these metals and picks up radon gas. The rock layers also contain sulfate minerals that dissolve into the water over time. There is no protection from these natural sources—the geology simply contains them.
The water here is extremely hard and loaded with minerals. You will see white scale buildup on faucets and inside pipes, and rust-colored stains on sinks and clothes from the high iron content. The very high sodium and sulfate levels mean the water tastes salty and bitter, and the sulfate can cause loose stools. Most well owners need a whole-house treatment system to make the water usable for drinking and laundry.
Iron, manganese, and radon in Lawrence County well water all exceed EPA health standards. This is a serious situation that needs your attention right away. Sulfate levels are also elevated well above what is recommended. Your water quality requires testing and treatment planning.
Long-term exposure to manganese can harm your brain and nervous system, especially in children. Iron causes rust-colored stains on sinks, tubs, and laundry that are hard to remove. The very high sulfate and sodium levels give the water a bitter or salty taste. You will also notice brown or black staining and scale buildup on fixtures and inside pipes.
Get your well tested by a state-certified lab right now. A basic bacteria and nitrate screen costs around fifty to one hundred dollars. A full mineral and metals panel costs two hundred to four hundred dollars. Iron and manganese removal systems can address the staining and taste problems, and radon needs ventilation or aeration treatment.
| Contaminant | Samples ⓘ | % Above MCL ⓘ | Distribution ⓘ | Confidence ⓘ | Risk ⓘ |
|---|---|---|---|---|---|
| Manganese | 20 | 100% | 5% · 0% · 95% | Moderate | High |
| Iron | 34 | 54% | 35% · 12% · 53% | Moderate | High |
| Radon | 2 | 50% | 0% · 50% · 50% | Low | High ⓘ |
| Sulfate | 65 | 31% | 54% · 15% · 31% | Moderate | High |
| Arsenic | 3 | 0% | 100% · 0% · 0% | Low | Low |
| Chloride | 51 | 0% | 96% · 4% · 0% | Moderate | Low |
| Fluoride | 8 | 0% | 100% · 0% · 0% | Low | Low |
| Lead | 3 | 0% | 100% · 0% · 0% | Low | Low |
| Nitrite | 10 | 0% | 100% · 0% · 0% | Low | Low |
| Uranium | 2 | 0% | 100% · 0% · 0% | Low | Low |
| E. coli | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Fecal Coliform | 1 | — | — | Low | Safe |
| Hardness | 47 | — | — | Moderate | Low |
| Nitrate | 1 | 0% | 100% · 0% · 0% | Low | Safe |
| Nitrate | 2 | — | — | Low | Low |
| pH | 14 | — | — | Low | Low |
| Sodium | 24 | — | — | Moderate | Low |
| Total Coliform | 1 | 0% | 100% · 0% · 0% | Low | Safe |
MCL = Maximum Contaminant Level (EPA limit for public water; used as benchmark for private wells). Distribution shows % of sampled wells in each concentration band. Methodology.
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