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Sand/Sediment In Drinking Water
There are three common explanations for sand/sediment (abbreviated S/S)
in drinking water wells as discribed below. The term "sediment" when used
in this fact sheet, means material that is visible but too small to be
felt when rubbed between the fingers. The term "sand" means material that
can be both seen and felt.
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ROCK CUTTINGS OR LOOSE SOILS REMAINING FROM THE INSTALLATION OF A
NEW
WELL.
If a well is newly constructed, particles remaining from the construction
can be removed by pumping the well water to waste; sometimes for an extended
period of time. This flushing procedure is discussed in the fact sheets
concerning wells; WD-WSEB-1-2 through- 1-6. This material will appear as
both a cloudy or muddy condition and, if a bedrock (artesian) well, may
have in part, sharp edges.
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PRECIPITATES FROM CERTAIN DISSOLVED MINERALS IN THE WATER.
Minerals, including iron or manganese (Fe/Mn) are present in well water
in New Hampshire. Methods for treating the rusty brown staining from Fe/Mn
are discussed in fact sheets WD-WSEB-3-7 (Technical
Version) or -3-8 (Summary). The other common
mineral, that possibly could cause sediment in water, is hardness. Hardness
precipitate, by itself, would have a white/yellow color. Hardness removal
is discussed in WD-WSEB-3-6. Fe/Mn precipitates
typically are loose sediments that are too small to be felt between the
fingers. Hardness precipitates typically "plate out" as a solid. Sometimes
this solid may break off and can be captured as irregular sized pieces.
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CONTINUOUS ENTRY OF FINE CLAY OR SAND PARTICLES FROM THE SOIL OR
FROM
POOR QUALITY BEDROCK.
The purpose of this fact sheet, WD-WSEB-3-14, is to discuss
the conditions where either a well defect or an unstable naturally occurring
condition in the bedrock fractures, allows fine sand or sediment to enter
the well. This material generally would have a grit like feel.
ORIGIN OF SEDIMENT
In dug wells (those approximately 3 feet in diameter and 10-15+-feet
deep) sediment entry can occur if the soil backfill passes through the
joints between the sections of well casing or through the perforations
typically presentin the lowest well casing. In fieldstone wells, soils
can migrate into the well throughout the casing circumference and height.
See fact sheet WD-WSEB-1-4 for information concerning proper dug well construction.
Sand could also migrate through the crushed stone around the bottom of
a dug well casing and then into the well. In bedrock wells, sediments can
enter the well from either of the areas; at the interface between the casing
and bedrock or from the unstable soil above the top end a rock fault. These
areas are described below.
Sediment entry can occur at the overlap between the steel well casing
and the socket that has been drilled into the bedrock. This would be considered
a construction defect. In this case the sand entry may possibly be stopped
by setting up the well drilling equipment and repounding the steel casing
into the socket. A more assured method is to install a mechanical seal
inside the well hole. See page 3 for more detail on a Jaswell type mechanical
seal.
Sand entry can occur into the top of any of the bedrock fractures that
the well has encountered. In this case the sand originates at the upper
end of the rock fracture which is covered by loose soil. In this situation,
there is no manmade defect in the well, rather the sand entry is only an
unfortunate aspect of that location's geology. (This situation could also
occur if the rock fault in the rock consisted of highly weathered bedrock.)
IDENTIFYING SAND ENTRY LOCATION IN BEDROCK WELLS
In bedrock wells it is very difficult to determine which of the possibilities
explained immediately above, is the origin of the sand problem.
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In some cases, TV cameras can be lowered into the well to inspect the tightness
of the bottom of the steel casing or to view each intersected rock fracture.
The pump must be pulled to make room for the camera. A budget estimate
for this work would be $1,000.
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Another investigatory method is to install a temporary packer (a device
to close off certain vertical levels of the well) so that each segment
can be pumped individually. The pumpage from each level can then be evaluated
for the presence of sand. A budget estimate for this work would be over
approximately $1,000.
In either case there is only a moderate probability of identifying the
entry location of the sand by this method.
CORRECTIVE ACTION
"In-The-WeIl" Solution for Dug Wells
In dug wells the entry point(s) of the sand should be sealed. However,
this may not be easily accomplished. If impractical, the situation could
be allowed to continue and the pump suction line raised. In the longer
term, the accumulated sand in a dug well can be removed by a 'mudsucker"
construction pump or by clamshell bucket. When raising the suction line
you increase the water systems sensitivity to drought conditions.
Where substantial sand is entering a dug well, bacterial problems are
likely. This is due to the likely short-circuiting of the natural soil
tightness and filtration due to the constant resettlement of the soil outside
of the well casing. In addition, backfill will need to be added around
the top of the well to replace the soil being lost.
"In-The- Well" Solutions for Bedrock Wells
A few devices are available to seal off leakage at either the well
casing/bedrock socket overlap or lower fractures in the well hole. The
best known device of this type is a Jaswell seal. A consequence of installing
a Jaswell seal is the likely loss of a portion of the well's safe yield.
A variation on this approach would be to permanently seal that level of
a bedrock well that has the problem using cement grout. Once the cement
has hardened, a well rig would drill through the sealed area reestablishing
a clear well hole. This approach will also reduce a portion of the well's
safe yield.
More recently, a mechanical system has been developed that can be added
to the intake of your pump to remove sand before it enters the pump.
This system is also costly and requires pulling the pump for retrofit installation.
If major amounts of sand are entering the well, it must be periodically
removed or it will accumulate and will be pulled into the well pump.
"In-The-Home'Solution
Because it is often difficult to pin down the location of the sand
entry and expensive to install a Jaswell seal, some homeowners conclude
that it is more cost effective to leave the well "as-is" and remove the
sand only when the water and sand reach the home.
Two "in-home" treatment options are discussed below. This choice is
possible only if the relative amount of sand entering the well is small.
If the "in-home" option is chosen, it should be recognized that the sand
will cause some continuing damage to the well pump and a shortening of
its life expectancy.
Centrifuge Device
This device removes sand by spinning the water within the housing of
the device. Sand has a greater density than water, and thus accumulates
around the perimeter of the device and is periodically bled off. A disadvantage
is that clay sized particles (which are smaller than sand) may not be totally
removed. The cost of this type of device would be approximately $500. There
is some energy loss with this device.
Sand Filter
This option consists of installing a commercial backwashable filter
that would strain out sand particles. Periodically the device would be
cleaned by backwashing. The cost of such a filter would likely be over
$1000.
FOR MORE INFORMATION
For additional information concerning the purchase of water conditioning
equipment, please see our fact sheet WD-WSEB-2-5.
For more information on sand removal, please call DES's Water Supply Engineering
Bureau at 271-3139. We would appreciate your comments concerning this fact
sheet and the removal of sand. For an overall listing of water supply related
fact sheets, please request fact sheet WD-WSEB-15-2. Drinking water fact
sheets are available through the DES web site at: http://www.des.state.nh.us
then select: publications, fact sheets, water division, water supply.
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