USGS Groundwater Data Summary for Pottawatomie County Aquifer N300CNRLOK
The U.S. Geological Survey collected groundwater samples from six wells ranging in depth from 90 to 260 feet within Pottawatomie County’s N300CNRLOK aquifer between August 2011 and March 2013. These samples showed calcium and magnesium hardness concentrations detected in all samples, with a median of 124.6 mg/L and a range from 45.7 to 366.0 mg/L. None of these values exceeded federal water quality thresholds.
Seasonal and Multi-Year Variation Reflected in Sampling Dates and Ranges
Sampling spanned roughly 19 months between late 2011 and early 2013
Hardness levels showed variation from moderate to high within this period
Consistent detection in all six samples indicates persistent mineral presence
Variation is typical for aquifers and can affect scaling rates in equipment over time
Judging Treatment Capacity for Industrial Daily Water Demand
Consider your facility's daily water volume when selecting treatment capacity
450,000 grain capacity of the Nelsen Mineral-Tank system suits substantial industrial flows
Accounting for peak usage and hardness range improves scale control effectiveness
Accurate water testing of your source is essential for sizing beyond regional data
Comparing Public Area Sampling to Private Well Testing
Public sampling provides regional mineral content trends, not site-specific data
Individual well tests establish the actual water conditions impacting your equipment
Area data helps anticipate possible scaling but does not predict exact concentrations
Testing your own water remains necessary for precise treatment planning
Maintenance Routine for the Nelsen 450,000 Grain Mineral-Tank Commercial Water Softener
Requires periodic regeneration cycles timed to throughput and hardness levels
Salt replenishment and tank monitoring maintain treatment capacity
Inspection intervals depend on operation scale and water quality fluctuations
Routine maintenance reduces scale buildup in heaters and associated piping
Equipment and Processes Most Susceptible to Mineral Scale
Water heaters are primary sites for mineral precipitation and scale formation
Heat exchangers and boilers involved in process water heating are vulnerable
Pipes and valves carrying heated water may accumulate scale reducing flow efficiency
Industrial equipment relying on high-temperature water benefits from mineral control
What Not to Conclude From Area Water Data Alone
This regional data reflects six wells sampled over a defined period and does not indicate conditions in your specific well or supply. Detection of minerals at these levels is not a violation or safety concern but signals potential for scale formation. To accurately address your industrial water heating scale issue, testing your own water source is indispensable. The Nelsen 450,000 Grain Mineral-Tank commercial water softener ships ready to configure for large-scale mineral treatment but requires precise capacity matching based on your individual water profile and demand.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2013-03-26. 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 N300CNRLOK aquifer (Pottawatomie County): 6 results from 6 wells, median 124.6 mg/L, range 45.7-366.0 mg/L; none above any federal threshold