My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
1987-11-25 Water Quality Report
Orono
>
Property Files
>
Street Address
>
B
>
Brown Road South
>
760 Brown Road South - PID: 03-117-23-43-0004
>
Misc.
>
1987-11-25 Water Quality Report
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
9/18/2024 3:32:04 PM
Creation date
9/18/2024 3:28:17 PM
Metadata
Fields
Template:
x Address Old
House Number
760
Street Name
Brown
Street Type
Road
Street Direction
South
Address
760 Brown Road South
PIN
0311723430004
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
2
PDF
View images
View plain text
MINNESOTA DEPARTMENT OF HEALTH <br />WATER QUALITY PARAMETERS <br />VOLATILE ORGAKIC CHEMICALS (YOC*s) are a large group of low boiling point, carbon-containing, predomi <br />nantly manTK»de substances. V0C*s are contained in a wide variety of industrial, coffiTK?rcial, and resi <br />dential products including: cleaners, degreasers, paints, solvents, inks, and petroleum distillates. <br />VOC's do not nonn.rlly occur in groundwater. Their presence usually signifies contamination from <br />improper use, storage, disposal, spillage or leakage of solvents or puroleum products. VOC’s vary <br />widely in their toxicity and drinking water concentration standards. <br />NITRATE AND NITRITE NITROGEN is used as one of the principal indicators of water quality. Nitrate <br />is the stable form of nitrogen in oxygenated 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 and dissolution of nitrogen- <br />containing soil and rocks. Background concentrations* in Minnesota groundwaters range from less ihan <br />0.4 milligrams per liter (mg/1) to 140 mg/1 with a mean of 2.7 mg/1. A primary drinking water standard <br />of 10 mg/1 has been established for public water supplies. <br />AlflONIA, 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 ammonia may <br />represent oxygen depleted water or rapid introduction of aimonia 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 will 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 (reconmended guideline) for public water <br />supplies is 250 mg/1. <br />SULPHATE occurs almost universally in groundwater. Rainfall may contain 10 mg/1 or more sulphate. <br />Household wastes, including detergents, may add 10 mg/1 or more sulphate to sewage. The usual source <br />in 9’^oundwater is naturally occurring sulphates of gypsum or anhydrite. Background concentrations <br />cf sulphate in Minnesota groundwaters range from 0.5 mg/1 to 1300 mg/1 with a mean of 72 mg/1. The <br />secondary drinking water standard for public water supplies is 250 mg/1. <br />IRON is a commonly found constituent in groundwaters, primarily derived from weathering of soil and <br />rocks. High cc..centrations can be due to corrosive water or leaching of wastes. Background concen <br />trations in Minnesota groundwaters range from less than 0.03 mg/1 to 46 mg/1 with a mean of 1.3 mg/1. <br />The secondary drinking water standard for public water supplies is 0.3 mg/1. <br />SPECIFIC CONDUCTANCE Is a measure of the ability of wat«»r to conduct an electric current. This ability <br />depends on the presence, concentration, and chemical state of ions. Wastewater and leachate typically <br />have high concentrations of dissolved icaterial (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 pmho/cm. Specific conductance is often used to estimate total dissolved <br />solids (TDS) 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 represent; acid conditions, <br />pH greater than 7 represents alkaline or basic conditions. Background pH levels in Minnesota ground- <br />waters range from 5.9 to 9.4 with a mean of 7.5. The secondary drinking water standard for public <br />water supplies Is 6.5 to 8.5. <br />•Background concentrations represent water quality values from 410 wells and springs sampled throughout <br />Minnesota in the Minnesota Pollution Control Agency’s Ground Water Quality Monuonng Piogram. <br />Mill) 710 IM I9R6
The URL can be used to link to this page
Your browser does not support the video tag.
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).