When your complete well system can’t keep up with household water needs, you may wonder about the extent and impact of this limitation. Simply put, incomplete water supply can disrupt daily routines and strain existing equipment. The causes vary, but understanding local groundwater conditions is key to addressing the problem effectively.
1. What Happens When This Problem Is Left Untreated for Years
Over time, if your well system's capacity remains insufficient, you may experience inconsistent water pressure and interruptions during peak usage. This can lead to inconvenience and increased wear on your pumping equipment as it compensates for demand fluctuations. While the water quality itself may remain stable, the system's inability to supply enough volume impacts household function directly.
2. How Total Dissolved Solids Enter Groundwater in Whatcom County’s Aquifer 112SUMS
Government groundwater sampling by the U.S. Geological Survey shows that total dissolved solids (TDS) in wells from Whatcom County’s aquifer 112SUMS range broadly from 0.11 to 210.0 mg/L, with a median of 99.0 mg/L. These samples come from wells 18 to 40 feet deep across the area. TDS includes naturally occurring minerals and salts dissolved from soil and rock, introduced gradually over time. These constituents enter the aquifer through natural geological processes and surface water infiltration.
3. Why Aesthetic Secondary Standards Differ from Health-Based Limits, Applied to Total Dissolved Solids
TDS in this aquifer has been consistently measured below all federal health-based limits, meaning no regulatory safety concerns were identified in these samples. However, TDS contributes to the taste, staining potential, and corrosivity of water, which are governed by aesthetic secondary standards rather than enforceable health thresholds. Household water may be affected in appearance or appliance longevity if TDS approaches higher levels, but detection alone does not imply unsafe water.
4. What Changes for a Large Household, a Second Home, or a Seasonal Property
Larger households or multiple-residence properties increase total water demand, which can strain a well system originally sized for fewer occupants. Seasonally used properties may encounter periods of stagnation or variable demand that affect water system efficiency. For properties relying on the same aquifer, these variations make matching pump and treatment capacity to actual water use even more critical to avoid supply shortfalls.
5. The Role of Plumbing Material and Age, Separate from the Source Water
While aquifer water quality remains consistent, plumbing materials and their age impact water safety and taste independently. Older pipes may introduce metals or harbor biofilms unrelated to groundwater TDS levels. These factors should be considered alongside source water conditions but require separate testing and treatment to address properly.
6. What Questions a Commercial or Industrial Operator Adds That a Household Does Not
Commercial and industrial water users must consider factors like process water purity, regulatory compliance for discharge, and large-scale flow consistency. They require detailed constituent testing beyond basic TDS and system capacity calculations tailored to operational demands. Households focus primarily on volume supply and common aesthetic water quality issues.
In summary, government data for Whatcom County’s aquifer 112SUMS show TDS concentrations typical for the region without health violations. When facing capacity limitations in a complete well system, households should test their individual well and consider solutions like the Fleck Complete Well System, which ships ready to configure and offers 32,000 grain capacity to meet increased demand. This path ensures efficient water supply tailored to actual household needs based on local groundwater characteristics.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2018-08-08. 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 Total dissolved solids in the 112SUMS aquifer (Whatcom County): 33 results from 8 wells, median 99.0 mg/L, range 0.11-210.0 mg/L; none above any federal threshold