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The presence of chloride (Cl-) where it does not occur naturally indicates possible
water pollution. Chloride does not affect plant and algae growth and is not toxic to
aquatic organisms at most of the levels found in Wisconsin. Chloride is not common in
Wiscons soils, rocks or minerals, except in areas with limestone deposits. Figure 7 shows the geographic distribution of chloride in Wisconsin
lakes.
Sources of chloride include septic systems (chloride values of 50 to 100 mg/l are
common in septic tank effluent), animal waste, potash fertilizer (potash = potassium
chloride), and drainage from road-salting chemicals. Increases in chloride, either
seasonally or over time, can mean that one or more of these sources is affecting the
lake. An increase in chloride from human or animal waste suggests that other nutrients are
also entering the lake. Higher chloride concentrations from spring to fall may be the
effect of lawn fertilizer runoff or septic systems during heavy use by summer residents.
Higher values in spring after the snow melts may signify runoff from drainage basins or
highways as a major source of chloride. Since lakes vary in their natural chloride
content, it is important to have background data or a long term database to document
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Next For more information on this topic, contact: James Vennie Lakes Partnership |
Watershed Management |
Fish Wisconsin |
Fisheries ManagementFIGURE 7. Generalized distibution gradients of chloride in the
surface waters of Wisconsin Lakes. (Adapted from Lillie and Mason, 1983(Exit DNR))
Note:This figure's key is corrected from the printed book
Watershed Management
(608) 266-2212