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US states digging deep to monitor water
Published in Saudi Press Agency on 05 - 07 - 2009


About a quarter mile (half
a kilometer) into dense woods, geologists watch as a
drilling rig twists a shaft deep into the granite bedrock
of southeastern New Hampshire. They are searching for water
_ not to drink _ but to watch, AP reports.
State and federal agencies have been watching, or
monitoring, lakes and rivers for more than a century, but
less attention has gone to vast amounts of water in cracks
and rock fissures deep underground, leaving a void in
understanding a resource growing in importance as demands
for water increase and surface water sources are being used
to the fullest in many areas.
New Hampshire is drilling a series of wells to monitor
groundwater in cracks in granite hundreds of feet below the
surface. The goal is to allow scientists to check for
contamination; learn about how long it takes for rainfall
or melting snow to make its way into the supply; and keep
tabs on how climate change, population growth and
development affect the water.
State Geologist David Wunsch would like to share the
information as part of a nationwide network.
«In the future, your water may come from hundreds of
miles away, so in order to get that national picture of
'Are we depleting some area for the sake of another
region?,' you need to have that national picture,» said
Wunsch, who represented state geologists on a national
committee that has developed a national groundwater
monitoring plan.
Groundwater provides drinking water for 130 million
Americans and 42 percent of the nation's irrigation water,
and while many states have monitored groundwater, they have
done so for state-specific reasons, using different
criteria. So, while groundwater supplies spread beneath
large regions, monitoring generally stops at state lines.
«Some states have several hundred wells and sample them
four times a year. Others have absolutely nothing,» said
Wunsch.
The goal of forming a network got a boost this year as
Congress approved the SECURE Water Act, directing the U.S.
Geologic Survey to work with states to develop a national
monitoring program for underground water supplies, known as
aquifers.
There is no national big picture on groundwater levels or
quality because the information exists only «in bits and
pieces,» said Christine Reimer of the National Ground
Water Association.
She emphasized that a national monitoring effort would not
put the government in charge of groundwater management, but
said information showing trends or changes in groundwater
quality or levels could help guide local decisions.
Montana approved groundwater monitoring in 1991 because
its water information was inconsistent and not part of any
system, said Thomas Patton, the state's groundwater
assessment program manager.
«If you are going to relate precipitation to water levels
in wells, you've got to collect precipitation over time and
water levels over time,» Patton said. «If you are going
to compare water levels to development, you've got to have
the water levels, over time.»
Information collected from 900 Montana wells has been
valuable, especially in watching how groundwater levels
responded to six or seven years of drought and to
irrigation or rainfall, he said.
Patton and Wunsch said ideally, states will gain
information valuable to their own water planning and share
with the federal government, which will share the cost of
the monitoring.
Wunsch said monitoring will be a great help in New
Hampshire, where more than a third of the state's
population gets drinking water from bedrock wells. Before
work began on the current network of 10 wells, the state
had only one bedrock monitoring well. He hopes for
significantly more.
Contamination is a particular concern around the country,
he said, because homeowners are not required to test their
wells. About 20 percent of New Hampshire's bedrock wells
contain arsenic levels above the government standard.
Bedrock water also contains uranium and radon, even unsafe
levels of fluoride.
Another major concern is just how long it takes for
rainfall or melting snow to flow down to, or recharge, the
aquifer.
«We don't know how quickly rain gets to bedrock,» Wunsch
said. «It might take a day, a week, a year for it to
migrate down.»
Monitoring that process, over time, might show how climate
change and development affect levels and quality.
For instance, rainfall that now percolates into the ground
gets diverted by the paved surfaces of development and is
carried away by storm drains.
And climate change may mean less snow around the country,
with more rain, in more severe storms, Wunsch said, which
could mean more groundwater, but at different times of the
year.


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