WSP Whole House Chlorination System - Well Water

WSP Whole House Chlorination System - Well Water

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Myth: Chloride Levels in Local Wells Define My Home's Corrosive Water Condition

Many assume that chloride measurements from area wells directly reflect their own household water corrosiveness. However, the U.S. Geological Survey groundwater sampling in Los Angeles County shows wide variation in chloride concentrations across 179 wells, with a median of 65.6 mg/L but ranging from 0.83 to 18,200 mg/L. These samples come from wells 6 to 3,945 feet deep throughout the local aquifer. This range indicates significant differences across locations. Importantly, detecting chloride—even above the secondary standard of 250 mg/L—is an aesthetic indicator related to taste and staining, not a safety concern or corrosivity violation. Therefore, individual household water corrosivity cannot be assumed from this data alone without specific water testing.

Myth: Household Signs Like Minor Pipe Discoloration or Slight Taste Changes Confirm Corrosive Water

While some household signs can hint at water corrosivity, not all visible effects confirm it. Corrosive water can contribute to pipe metal leaching, discoloration, and metallic taste, but these symptoms may also arise from other causes unrelated to water chemistry, such as plumbing materials or water age. Conversely, the absence of obvious symptoms does not guarantee non-corrosive water. To identify corrosive water effects thoroughly, observe persistent staining, repeated pipe issues, or changes linked directly to water use, and compare those with laboratory water chemistry analysis.

Myth: Immediate Treatment Advice Can Be Given Without Detailed Household Water Data

Before seeking advice or considering solutions, it's important to document household water characteristics. This should include recent water testing results measuring parameters that influence corrosivity (for example, pH, alkalinity, hardness, and chloride), as well as observations of equipment performance and any unusual water behaviors. Such detailed records enable accurate understanding and tailored recommendations. Without this information, treatment options may not fully address the underlying causes of corrosive water conditions.

Myth: Corrosive Water in Los Angeles County Aquifers Remains Constant Over Time

The USGS sampling data spans from March 24, 2011, to February 24, 2025, showing chloride detections in 223 of 231 samples. Such a wide time range captures seasonal and multi-year variations in water chemistry. Chloride levels and thus water corrosivity may fluctuate due to aquifer recharge, rainfall patterns, or human activities impacting groundwater quality. Recognizing these temporal changes helps in understanding the persistence and variability of corrosive water concerns and informs periodic reassessment of household water conditions.

Myth: Treated Water With Corrosive Water Filters Is Indistinguishable at the Tap

When a suitable filtration system designed to address corrosive water is in use, the treated water delivered to the household tap typically shows marked improvements. This system operates by reducing the elements that contribute to pipe corrosion and associated damage, thereby enhancing water stability and reducing staining or metallic tastes that signal corrosivity. While the tap water’s fundamental chemistry is altered to mitigate corrosive effects, no significant negative impact on water quality or safety occurs. Regular monitoring remains advisable to confirm continued efficacy.

For households in Los Angeles County facing limitations with existing equipment handling corrosive water, the Autotrol Corrosive Water Damaging Pipes Filter ships ready to configure for direct purchase. This equipment is designed specifically to address pipe-damaging corrosivity by managing water chemistry factors tied to local groundwater data and measured household demands.

Where this information comes from

Source: USGS groundwater sampling. Sampled 2025-02-24. 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 Chloride in the aquifer (Los Angeles County): 231 results from 179 wells, median 65.6 mg/L, range 0.83-18200.0 mg/L; 44 above an AESTHETIC secondary standard only (secondary standard 250.0 mg/L (aesthetic)) - not a health finding

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