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IDAHO WELLHEAD SURVEY 1993
UPDATE
The Idaho Private Wellhead Sampling program for nitrates was initiated
in 1990 by the Idaho Farm Bureau Federation. This program is a
cooperative effort as seven different government agencies and the Idaho
Farm Bureau have united to make the program a success. The Idaho
Department of Agriculture, Soil Conservation Service, and the
University of Idaho Cooperative Extension System assist with program
logistics, sample bottle distribution, and dissemination of
information. The University of Idaho College of Agriculture's
Analytical Laboratory has major roles in planning and designing the
quality assurance phase of the analytical part of the program and
analyzes all samples for nitrates. The Idaho Division of
Environmental Quality designs the quality assurance plan for the
field effort, the questionnaire, and sampling procedures for the
public. The United States Geological Survey and local health
districts assist with the collection of samples for quality
assurance.

So far, 2,178 samples from private wells and 1,194 control and quality assurance samples have been collected from 18 Idaho counties. County participation to date is as follows: Cassia, Minidoka, and Jerome (September 1990); Canyon (February 1991); Gem and Payette (March 1991); Ada (April 1991); Twin Falls (August 1991); Latah and Benewah (September 1991); Bonner (November 1991); Bonneville (March 1992); Elmore and Owyhee (November 1992); Fremont (April 1993); and Jefferson, Madison, and Teton (October 1993).

What Do the Sampling Results Mean?
This study shows that:
Northern Idaho
According to this sampling, water quality is better in northern Idaho
than other regions of the state. In Benewah, Bonner, and Latah
counties, 142 water samples were collected from wells. Less than 3
percent of the wells contained NO3-N values that exceeded
the drinking water standard. In addition, 76 percent of the wells
contained less than 2.0 ppm NO3-N; 13 percent of the wells
contained NO3-N values between 2.0 and 5.0 ppm; and 11
percent had values greater than 5.0 ppm (50 percent of the drinking
water standard).

Southwestern Idaho
Nitrate values in groundwater were higher in southwestern Idaho than
other regions of the state. Still, 93 percent of the samples did not
exceed the drinking water standard. In Ada, Canyon, Elmore, Gem,
Owyhee, and Payette counties, 1,117 samples were collected from wells.
About 7 percent of the wells exceeded the 10.0 ppm NO3-N
drinking water standard. More than 58 percent of the wells had
NO3-N levels above 2.0 ppm; 36 percent contained
NO3-N values between 2.0 and 5.0 ppm; and 22
percent of the wells had values greater than 5.0 ppm.

Southcentral Idaho
In Cassia, Jerome, Minidoka, and Twin Falls counties, 541 water samples
were collected from wells. Four percent of the wells contained
NO3-N values that exceeded the drinking water standard.
Conversely, 21 percent of the wells contained NO3-N values
less than 2.0 ppm; 54 percent of the wells contained NO3-N
values between 2.0 and 5.0 ppm; and 25 percent had values greater than
5.0 ppm (50 percent of drinking water standard). Ninety-six percent of
the wells meet the drinking water standard in the region; however, man
has impacted the nitrate content in at least 79 percent of the
wells.

Southeastern Idaho
In Bonneville, Fremont, Jefferson, Madison, and Teton counties, 378
water samples were collected from wells. Four percent of the wells
contained NO3-N values that exceeded the drinking water
standard. Conversely, 60 percent of the wells contained
NO3-N values less than 2.0 ppm; 27 percent of the wells
contained NO3-N values between 2.0 and 5.0 ppm; and 13
percent had values greater than 5.0 ppm (50 percent of
drinking water standard). Ninety-six percent of the wells meet the
drinking water standard in the region; however, man has impacted the
nitrate content in at least 40 percent of the wells.

For the most part, the results of this survey are to date reassuring to Idahoans. To deal with specific and geographic problems, use proactive approaches that will protect and enhance water quality while ensuring the survival of Idaho's number one industry -- agriculture. Where NO3-N levels are high, use BMPs to apply N-containing materials.
This program is one of the largest wellhead sampling programs in the
United States. When completed in the next 2 to 3 years, it will provide
an extensive data base for Idahoans to effectively analyze the quality
of groundwater and plan for the future.
(R. L. Mahler)
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HOW EXTENSIVE IS GROUNDWATER
CONTAMINATION?
(This is the fourth in a series of articles on the causes of
groundwater contamination.)
Assessment of the extent of groundwater contamination is difficult, due
to such factors as limited and inconsistent access to the water
(usually dependent on wells and springs), the potential for bias in
existing data (if originally collected to explore a particular water
quality problem), incomplete information about the well (did the well
draw from more than one aquifer?), and inconsistent methods of sampling
and analysis.
It is also important to keep in mind that the trend of increasing reports of detections of contaminants in groundwater is largely due to the intensive search for contaminants now under way by many state agencies, as well as continued improvements in the sensitivity of analytical methods used to measure the concentration of contaminants.
The volume of groundwater within 2,500 feet of the surface has been estimated at 100 quadrillion gallons, or about 16 times the volume of the Great Lakes. Of this amount, at least half is too saline from natural causes to use for drinking water, although some of it may be suitable for other uses. The total amount of the remaining groundwater that is contaminated is unknown, although EPA estimates the amount contaminated by point sources to be 2 to 3 percent.
Recent U.S. Geological Survey studies have made the following assessments:
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FOREST WATER QUALITY VIDEO
AVAILABLE
A new forest water quality videotape is available from the University
of Idaho. "Forest Water Quality" was jointly funded and produced by the
University of Idaho Cooperative Extension System, the Idaho Department
of Lands, and the Idaho Forest Stewardship program. It is targeted at
the thousands of nonindustrial, private owners of woodlands in Idaho.
This group of people owns over 2,000,000 acres of trees in the
state.
"Forest Water Quality" shows the private forest owner ways to improve and maintain water quality during, and after, any forest practice, whether it's timber harvest, road-building, or homesite construction.
"Forest Water Quality" contains two 22-minute segments. Part One shows how water moves through the forest, how forest activities affect that water, and ways to enhance water quality. Part Two takes a close look at the Idaho Forest Practices Act -- the law that sets "Best Management Practices" to guide activities that can affect forest water quality.
Whether you own 5 acres or 5,000, you'll find these programs invaluable for helping you steward one of Idaho's most precious resources. This video is available from the University of Idaho Agricultural Communications Center, University of Idaho, Moscow, Idaho 83844-2332. This VHS format video is priced at $29.95 plus $3.00 for shipping.
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BLUE THUMB FACT
The average family turns on the tap to use water between 70 and 100
times per day.
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IRON BACTERIA IN WELL
WATER
The occurrence of iron bacteria has long been known as a problem for
rural homeowners and for operators of water supplies that rely on
groundwater. Although many other concerns about drinking water have
been in the headlines for the past 20 years, iron bacteria is still a
major headache causing restricted flows as well as taste and odor
problems. Iron bacteria do not make people ill, but they can pit and
corrode pipes, cause discolored, turbid water, and lower the pH of the
water.
Iron bacteria are widespread in the environment. They can be found anywhere that both dissolved iron and dissolved oxygen are present. They occur naturally in soil, streams, cool surface waters, and shallow aquifers. They prefer a pH range of 6 to 10 and a temperature range of 40 to 60 F. Usually the first indication of the presence of iron bacteria is a sudden discoloration or iron staining (rust colored). A rust colored gelatinous slime in the toilet tank or in filter housing is another key indicator of iron bacteria.
If the slime growth is in a water filter or in the pump or pipes, it could cause clogging of the system. If there is any indication that a water supply has iron in it, pressure drops should be investigated to see if iron bacteria are plugging the system.
As a precaution, and to prevent all types of bacterial contamination of wells, all tools and materials should be disinfected with chlorine before they are inserted into a well. After drilling operations or any maintenance on a well, the well and water system should be thoroughly chlorinated.
Once a system has iron bacteria growing in it, periodic shock
chlorination or continuous chlorination may be necessary. Slimy
bacterial growth should be removed from pipes or equipment, and shock
chlorination should follow. A second shock chlorination is recommended
in the case of iron bacteria.
(Ernestine Porter)
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WATER MANAGEMENT BMPs FOR YOUR
GARDEN
Most people intensively manage their backyard flower and/or vegetable
gardens. Inputs such as pesticides, fertilizers, and water when used
incorrectly may adversely impact surface and/or groundwater quality. To
protect the environment and water quality you should use BMPs, which
are defined as implemented strategies that eliminate or minimize
environmental pollution. BMPs are designed to be compatible with garden
ecosystems. BMPs can protect the environment without compromising the
productivity of large or small gardens.
Why should you be concerned about water use in your garden? Americans use a lot of water. In fact, a typical American today uses four times as much water as a great-grandparent did at the turn of the century. In urban areas of the Pacific Northwest water use often doubles when the gardening season arrives.
There are many reasons why water should not be over-used in your garden. Some potential adverse effects include:
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LAND USE PLANNING AS A TOOL TO
PROTECT GROUNDWATER QUALITY
(This is the first in a series of articles on protecting groundwater
quality by managing local land use.)
Since over 90 percent of Idahoans obtain their drinking water from
groundwater it makes sense to consider different options to protect
this resource. One option for county and city governments to consider
is land use planning.
In most areas local land use activities can influence groundwater quality greatly. This close relationship between land use and groundwater quality means that local government, in exercising the traditionally local function of managing land use, can play a significant role in protecting this resource.
Local governments can effectively protect groundwater quality through control of local land use activities. Higher levels of government often are unable to consider unique local characteristics in land use management because of their need to generalize across broad geographic areas. Local governments, however, can attempt to fashion management decisions that do reflect unique local needs.
Developing a groundwater management plan involves many choices. No set formula applies to all local groundwater protection decisions. The variability in the natural resource base, institutional framework, perceptions of groundwater problems, and management and fiscal capabilities suggest the importance of selecting the management technique most suited to the particular setting at hand. Understanding a few general principles, however, can help local governments fashion appropriate management decisions.
Land uses and the pollution sources they generate vary widely in their potential to contaminate groundwater. Substances range from the relatively innocuous to those listed as hazardous by federal and state agencies. There is also wide variability in terms of soil, subsoil, and bedrock conditions affecting the susceptibility of different land areas to contamination. Another factor to consider is the number of people affected.
Regulatory vs. nonregulatory approaches. There are two categories of groundwater protection techniques. Regulatory approaches involve placing a system of legal constraints on land uses and potentially contaminating activities. Nonregulatory approaches include public education and involvement; voluntary best management practices; land acquisition programs; facility siting procedures and capital facility and infrastructure planning; inspection and training programs; monitoring; emergency spill plans; community waste management and minimization programs; and governmental coordination efforts. To be most effective, local protection programs generally should employ a mixture of regulatory and nonregulatory techniques.
Some important potential pollution sources are regulated at the state and federal levels. In these cases, state law sets the basic framework. Local governments must take these regulations into consideration so that their actions complement, rather than conflict with, state regulations.
Local land use controls. Many land use control techniques are important to local groundwater quality protection programs. Such techniques can include prohibiting uses that have the potential to cause serious contamination, permitting other uses only under certain conditions, limiting density of development, and regulating locations within which various uses are permitted.
Measures to require that new land uses protect groundwater quality can
include conventional zoning, flexible zoning devices, subdivision
regulations, and extraterritorial controls. Since these regulations
deal primarily with prospective land uses, however, it may be necessary
to enact special-purpose ordinances that address existing land uses and
specific pollution sources connected with them. Since a number of
pollution sources are controlled at state and federal levels, it is
important to consider whether the local unit is authorized to adopt
source control regulations and how best to coordinate controls at
various governmental levels. Local officials also must consider whether
a proposed ordinance meets state and federal constitutional
requirements.
(Adapted from Groundwater and Public Policy. Series No. 6 by D. A.
Yanggen and S. M. Born from the University of Wisconsin-Madison)
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HARD WATER -- A PROBLEM IN THE
LAUNDRY
Hard water is a water quality problem that may adversely affect the
laundering of clothing. Hard water often results in problems such as:
dinginess or graying, yellowing, general soil buildup, white or gray
streaks on colored fabrics, and/or a stiff, harsh feel to fabrics.
To prevent hard water problems, use adequate amounts of heavy duty liquid detergent and water as hot as is safe for the fabric. Soften the water with nonprecipitating water conditioner or install a water softening system. Note however, that water softening systems may increase the amount of sodium in the drinking water and cause problems for people on salt-restricted diets.
A general prescription to reduce hard water impacts would be as follows: Fill the washer with the hottest water appropriate for the fabric. Add four times the normal amount of liquid laundry detergent and 1 cup of nonprecipitating water conditioner such as Calgon® or Spring Rain®. Agitate just long enough to wet the clothes. Soak overnight or about 12 hours. Drain and spin without agitating. Launder, using regular cycle, no detergent, and 1 cup of nonprecipitating water conditioner. Repeat laundering with no detergent and 1 cup of nonprecipitating water conditioner until no suds appear during the rinses. To remove all dinginess, launder with nonprecipitating water conditioner and bleach safe for the fabric.
A new Pacific Northwest Bulletin, PNW 440, "Stain Removal Guide for
Washable Fabrics," is now available from your local county
Extension office. This guide contains useful hints that will help you
deal with some potential water quality problems as well as stains
caused by everyday activities.
(Ernestine Porter)
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HOW MUCH DO WE DEPEND ON
GROUNDWATER?
According to government figures, nationally groundwater provides an
estimated:
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WATER QUALITY 2000
CONFERENCE
Water Quality 2000, a state-level agricultural water quality
conference, will be held January 24-26, 1994, at the Red Lion-Riverside
in Boise. This conference is co-sponsored by the Idaho Association of
Soil Conservation Districts, the Environmental Protection Agency, and
the University of Idaho Cooperative Extension System. As a follow-up to
the successful 1990 conference this forum will review, examine, and
discuss agricultural nonpoint source pollution control efforts and
programs.
The two-and-one-half day conference will consist of both general sessions and concurrent sessions. General sessions will highlight state water quality objectives, existing programs, emerging initiatives, and technical support.
There will be eight concurrent sessions on the following topics: conservation, monitoring, best management practices (BMPs), watersheds, agrichemical management, state agricultural water quality projects, public policy, and riparian areas and wetlands.
As in 1990, this conference has been designed to benefit a variety of audiences including: farmers and user groups, concerned organizations and citizens, water quality professionals, and local, state, and federal government officials.
Over 500 people are expected in attendance. To receive registration information contact Kathleen Pidjeon at the Idaho Soil Conservation Commission (1215 West State St., Boise, ID 83720; phone 208/334-0220).

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Comments to webmistress: karenl@uidaho.edu
All contents copyright © 1997-2003. College of Agricultural and Life Sciences, University of Idaho. All rights reserved. Revised: January 3, 2003