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465 Brown Road South - PID: 03-117-23-31-0002
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Last modified
8/22/2023 4:36:25 PM
Creation date
2/5/2016 11:28:53 AM
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x Address Old
House Number
465
Street Name
Brown
Street Type
Road
Street Direction
South
Address
465 Brown Rd S
Document Type
Land Use
PIN
0311723310002
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MINNESOTA DEPARTMENT OF NEALTH <br /> WATER QUALITY PARAMETERS <br /> VOLAT[LE ORGANIC CHEMdU�S (YOC's) are a large group of low boiling point, carbon-containing, predomi- <br /> nantly manmade substances. VOC's are contained in a wide variety of industrial. commercial, and resi- <br /> dential products including: cleaners, degreasers. paints, sotvents, inks, and petroleum distillates. <br /> VOC's do not normally occur in groundwater. Their presence usually signifies contamination from � <br /> improper use, storage. disposal , spillage or leakage of solvenis or petroleum products. VOC's vary <br /> widely in their toxicity anC drinking Nater conCentration standards. <br /> NITRATE AHO NITRITE MITROGEM is used as one of the principal indicators of water quality. Nitrate <br /> is the stable form of nitrogen in oxygenateG groundwater. Nitrite presents a particular health threat <br /> to infants. Sources of nitrogen include: municipal and industrial wastes. landfill leachate, animal <br /> and human wastes. nitrogen fertiliZers, decomposition of organic matter dnC dissolution of nitrogen- <br /> containing soil and rocks. BackgrounG concentrations* in Minnesota groundwaters range from less than <br /> 0.4 mi)iigrams per liter (my/1) to 140 mg/1 with a mean of 2.7 mg/l. A primary drinking water standard <br /> of 10 mg/1 has been established for public aater supplies. <br /> A�MOMIA. a compound of nitrogen and hydrogen, is generally found in low concentrations in groundwater <br /> due to oxidation to nitrate and adsorption to soil particles. High concentrations of artmonia may <br /> represent oxygen depleted water or rapid introduction of ammonia fertilizers. animal or human wastes, <br /> or leaching of solid wastes. <br /> CHLORIDE is one of the major inorganic anions in water. Chloride is very soluble and Nill move through <br /> groundwater with little attenuation. The presence of chloride in groundwater may be due to natural <br /> salts in soils or rocks. or leaching of chemical fertilizers. solid wastes or highway deicing salts. <br /> Background chloride concentrations in Minnesota groundwaters range from 0.3 mg/1 to 490 mg/1 , with <br /> a mean of 19.2 mg/1, The secondary drinking water standard (recommended guiGeline) for public water <br /> supplies is 250 mg/1. <br /> SUIPHATE occurs almost universally in groundwater, Rainfall may contain 10 mg/1 or more sulphate. <br /> Household wastes. includin9 d�tergents. may add 10 mg/1 or more sulphate to sewage. The usual source <br /> in groundwater is naturally occurring suiphates of gypsum or anhydrite. BackgrounC concentrations <br /> of sulphate in Minnesota groundwaters range from 0.5 mg/1 to 1300 mg/1 with a mean of 72 mg/l. The <br /> secondary drinking water standard for public water supplies is 250 mg/1, <br /> IROb is a commonly found constituent in groundwaters, primarily derived from ►�eathering of soil and <br /> rocks. High concentrations can be due to corrosive water or leaching of wastes. Background concen- <br /> trations in Min�esota groundwaters range from less than 0.03 mg/1 to 46 mg/1 with a mean of 1.3 mg/1. <br /> 7he secondary drinking water standard for public water supplies is 0.3 mg/1. <br /> SPECIFIC CONDUCTANCE is a measure of the ability of water to conduct an electric cur�ent. This ability <br /> depends on the presence, concentration, and chemical state of ions. Nastewater and leachate typically <br /> have high concentrations of dissolved material (ions) and therefore high specific conductance. Back- <br /> ground specific ConductanCe in Minnesota groundwaters ranges from 50 to 2500 micromhos per Centimeter <br /> (umho/cm) with a mean of 630 µmho/cm. Specific conductance is often uSeG to estimate total dissolveG � <br /> sotids (TOS) by multiplying specific conductance by .6. The secondary drinking water standard for <br /> public water supplies is 500 mg/1 TDS. <br /> pH is a measure of the hydrogen ion activity of water, pH less than 7 represen[s acid conditions, <br /> pH greater than 1 represents alkaline or basic tonditions. Background pH levels in Minnesota grounG- <br /> wa[ers range from 5.9 to 9.4 with a mean of 7.5. The secondary Arinking water 5[andard for public <br /> water supplies is 6.5 Co 8.5. <br /> *Background co�centrations represent water quality values from 410 welis and springs sampled throughout <br /> Minnesota in the Minnesota Pollution Control Agency'S Ground Nater Quality Monit.orinq Proqram. <br /> MHD 210 LM 19R6 <br />
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