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The U.S. Geological Survey has sampled groundwater in Curry County's aquifer N100HGHPLN, with results showing hardness levels ranging from 151.0 to 747.0 mg/L, median 312.5 mg/L, from 14 wells sampled between 2015 and 2022. No concentrations exceeded federal safety thresholds according to this dataset.
Understanding Laboratory Test Reports for Iron and Hardness
Test results report hardness mainly as milligrams per liter (mg/L) of calcium and magnesium combined
Laboratory reports present hardness figures that represent the concentration of calcium and magnesium ions—key contributors to hardness—typically measured in mg/L. These numbers help determine how 'hard' water is in your household.
Iron presence is tested separately; this dataset focuses on hardness components
While iron is an important factor in water quality, this particular government data set involves hardness components only. To understand iron levels in your water, consult a certified laboratory for direct testing.
Interpreting median and range values helps gauge area-wide variation
The median hardness value provides a central tendency indication, while the range shows the lowest and highest measurements found across the sampled wells in the aquifer.
Household Size and Seasonal Use Impact on Treatment Choices
Larger households may require higher treatment capacity for hardness and iron
More residents increase water demand and the volume of hardness and iron to treat. Understanding household water use helps choose an appropriate system size.
Seasonal or secondary homes might need different service intervals
Properties used intermittently could see variable water quality effects; treatment systems should accommodate fluctuating usage to maintain performance.
Influence of Sample Depth, Well Depth, and Water Source Type
Samples were collected from depths between 110 and 430 feet, reflecting deeper groundwater qualities
Well depth can affect hardness and iron concentrations, with deeper wells often showing different mineral profiles compared to shallow ones.
Groundwater from this aquifer generally contains measurable hardness but no samples exceeded federal limits
This means while hardness is present, it is within acceptable guidelines set for water quality in the region based on government data.
Groundwater Constituents Originate from Regional Geology and Hydrology
Calcium and magnesium derive from natural mineral deposits interacting with groundwater
In Curry County, these minerals leach into water as it moves through local soil and rock formations, contributing to the hardness observed.
Iron may enter groundwater through natural soil and rock dissolution processes
Iron presence typically comes from geologic sources, with variations dependent on aquifer composition and water-rock interaction time.
Sample Size and Data Reliability Considerations
The dataset includes 18 hardness measurements from 14 wells collected over several years
This moderate sample size offers a snapshot of area-wide conditions but does not represent every possible well or household source in Curry County.
Results suggest consistent detection of hardness with concentrations spanning typical regional variability
Regular detection across multiple wells indicates hardness is a common characteristic, reinforcing the need to consider treatment options if household symptoms arise.
After measuring your household water demand and obtaining a certified test report for your own well or municipal supply, consider the Autotrol Iron + Hard Water (Well) System. This system ships ready to configure, with a grain capacity of 32,000, tailored to effectively manage iron and hardness challenges consistent with Curry County's aquifer characteristics.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2022-06-17. 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 N100HGHPLN aquifer (Curry County): 18 results from 14 wells, median 312.5 mg/L, range 151.0-747.0 mg/L; none above any federal threshold