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Declining
quality of water detected in reservoirs below Fraser Valley, expert says
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How much water is beneath our
feet?
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- Groundwater exists almost everywhere
underground. Water is found in soil, rock fractures, faults
and joints. The level below which all of these spaces are
entirely filled with water is called the water table. This is
also the level to which water will rise in a shallow well.
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- An aquifer is a geological formation
of permeable rock or loose material that can be developed to yield
useful quantities of water. Aquifers range in size from a few
hectares to thousands of square kilometres. They can be a few
metres thick or hundreds of metres thick
- Abbotsford-Sumas
Aquifer
- .
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- Confined aquifers are located beneath
a layer of impermeable materials, so they are more susceptible to
declines in water volumes.
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- Unconfined aquifers - such as the
Abbotsford aquifer - rise up as far as the water table. They
are easier to recharge, but more susceptible to contamination
because they aren't protected by clays or other impermeable layers.
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| Source:
State of the Environment Report for B.C., 1993, published by the federal
and provincial environment departments. |
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Is B.C.'s groundwater
contaminated?
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| Pollution levels
exceed Canadian drinking water guidelines at specific sites within 17 of
the 192 aquifers studied by the municipal, provincial and regional
governments during the 1990s.
Ten of these problem aquifers are in the
Fraser Valley, where the public health guidelines for one or more water
contaminant were exceeded at one or more wells.
Nitrate levels exceed guidelines in nine
of the 17 aquifers, likely because of agricultural fertilizer, manure
and/or septic fields.
Most of the information about aquifers is
collected in areas with large populations. Little is known about
groundwater quality outside these areas.
Source: Groundwater in B.C.,
environment, lands and parks ministry, 1997.
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