Understanding Your Local Water Source in Pottawatomie County
The water in Pottawatomie County primarily comes from aquifer 317GBWG. This aquifer is accessed through wells typically ranging from 110 to 200 feet in depth. Water drawn from this source contains varying levels of hardness, which is influenced by dissolved calcium and magnesium minerals. These minerals are naturally occurring in the groundwater and have been documented in area-wide samples collected from six separate wells between 2011 and 2013. The median hardness reported was 76.5 mg/L, with individual results ranging from 25.8 to 190.0 mg/L. These values are below any applicable federal thresholds, indicating no health-based violations in the sampled locations, but they do represent typical mineral concentrations that affect water quality from an aesthetic or operational standpoint.
Steps to Identify Household Water Hardness Problems
When household water treatment equipment fails or the water quality is uncertain, it's important to rule out simpler causes before moving to specialized testing. Begin by reviewing any recent changes in water taste, appearance, or appliance performance that may suggest hardness issues. Next, verify maintenance or operation status of your existing water treatment system. For precise information, submit a water sample from your own supply to a certified laboratory; this test will quantify calcium and magnesium concentrations and confirm actual hardness levels specific to your household. Avoid assuming local aquifer data directly represents your water, as well depth and distribution can impact mineral content.
Consequences of Untreated Water Hardness Over Time
If water hardness remains untreated, calcium and magnesium minerals can accumulate inside household plumbing and appliances. This buildup can lead to scale deposits that reduce water flow, decrease the efficiency of water heaters, and shorten the lifespan of appliances such as dishwashers and washing machines. Additionally, scale can affect water heating times and increase energy costs. While not a health hazard, untreated hardness often results in noticeable wear and maintenance challenges for plumbing infrastructure and water-using equipment.
How Salt-Free Scale Control Technology Works
Salt-free water softening systems use a physical or chemical process to modify hardness minerals, preventing them from forming scale deposits. Unlike traditional salt-based softeners, these systems do not remove calcium and magnesium ions from the water. Instead, they alter the minerals’ behavior so they do not cling to pipes and surfaces. The Pentair Salt-Free Scale Control System, for example, ships ready to configure for household use and is designed to reduce scale buildup without introducing salt or chemicals into your water. This approach maintains essential mineral content while addressing the operational issues associated with hardness.
Interpreting Laboratory Reports on Water Hardness
Certified lab tests report hardness typically as milligrams per liter (mg/L) of calcium carbonate. Reports may include values for calcium and magnesium individually or combined. Understanding these figures allows you to compare your water’s hardness with the regional data for the Pottawatomie County aquifer. Since hardness results are often presented as a range or median from area sampling, your household test result provides a definitive measurement for decision-making about treatment.
Additional Considerations for Commercial or Industrial Water Users
While residential water hardness primarily affects household plumbing and appliances, commercial and industrial operations often face stricter requirements. These may include monitoring for scale buildup in boilers, cooling towers, or other process equipment where hardness impacts operation. Such facilities might require more frequent testing and customized treatment solutions beyond those suitable for a typical household.
Recognizing Seasonal and Multi-Year Changes in Water Hardness
Sampling data from 2011 through early 2013 shows variation in hardness levels among wells in Pottawatomie County’s aquifer 317GBWG. These variations can reflect changes in groundwater flow, recharge, and mineral dissolution over time. Recognizing this variability is important for interpreting test results and anticipating future water quality trends in your household supply.
In conclusion, addressing salt-free water softening in Pottawatomie County requires understanding local aquifer conditions, confirming your own water hardness through testing, and selecting appropriate treatment technologies like the Pentair Salt-Free Scale Control System. This approach helps preserve your plumbing and appliances while maintaining mineral balance in your household water.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2013-03-13. These figures describe groundwater sampled in this area. They are not a test of any individual private well - only a test of that well can establish its own water.
On record: U.S. Geological Survey sampling of Hardness, Ca, Mg in the 317GBWG aquifer (Pottawatomie County): 6 results from 6 wells, median 76.5 mg/L, range 25.8-190.0 mg/L; none above any federal threshold
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