102 N. Neil Street
We are pleased to have the opportunity to
review and comment on the October 17 report "Aquifer Evaluation and Competing
Use Study" prepared by Malcolm Pirnie, Inc. for the Andersons, Inc. I attach the Water Survey's comments prepared by Dr.
George Roadcap, P.G. and H. Allen Wehrmann, P.E. I will also send this letter and the attachment via
regular mail
Although we
will have improved scientific information about the Mahomet and Glasford
Aquifers after completion of our study in three years, I understand
that decisions about the use of available water resources need to be made
in the immediate future. We currently do not have one single report on
the aquifers that the City of Champaign can turn to as a source of additional
information, but I would like to take this opportunity to
restate and enhance some of the
information that was provided at the Joint Study Session on
September 28. This information reflects a synthesis of data and key findings
from a number of relevant reports and, perhaps more importantly, the
understanding of the aquifers by Water Survey scientists and engineers. Beyond hard scientific data, I
introduced in the Joint Study Session some concepts that are fundamental to
the development of regional water supply plans, as required in Executive Order
2006-01. I would like to reiterate some of these concepts, as I believe they
are relevant to decisions that have to be made about water allocation and
water use in Champaign County and surrounding
areas.
Groundwater is a
renewable resource, but not an infinite resource. As water is withdrawn from
the aquifers the aquifers are
recharged, but water withdrawals cannot continue without creating adverse impacts at some time in the
future. The lowering of water levels in existing wells usually can be
mitigated by lowering pumps or drilling new wells, but ever increasing
withdrawals from the same part of the aquifers will at some point in time lead
to dewatering of the aquifers themselves, a potentially serious situation that
we advise be avoided. A key question for Champaign County is how
much more water can be withdrawn safely before we start dewatering the
aquifers?
From 50 years of data
from continuous monitoring of head (water level) at the Petro North well on
Rising Road, we can determine that as withdrawals from the aquifers have
increased by more than 16 million gallons per day, water level has declined by
almost 50 feet at that location. [It should be noted that we do not have data on
drawdown at the sites of the Illinois American Water wells, as there
are no monitoring wells at these locations. We would expect drawdown to be
greater at these sites. We also believe that the Glasford Aquifer already has
been dewatered within the City of Champaign.] A quick calculation
leads us to conclude that for every million gallons of water that has
been withdrawn, head in the Mahomet Aquifer at Petro North has been
reduced by about 3 feet. Our best estimate is that there is an additional
approximately 50 feet of head before the Mahomet Aquifer would start to be
dewatered in this area. A simple calculation leads to the conclusion that an
additional approximately 16 or 17 million gallons of water per day can be
withdrawn for the Mahomet Aquifer in this area for all
purposes before we start to dewater
the aquifer.
The proposed ethanol
plant will, according to the Malcolm
Pirnie report, withdraw almost 2 million gallons of water per day and
lower the head (water level) by about
4 feet. This will not dewater the Mahomet Aquifer. However,
withdrawing this additional amount of water for any purpose will consume
up to 4 feet of the approximate 50 feet of available head before the Mahomet
Aquifer will start to be dewatered in this area. An additional
approximately 50 feet of drawdown and approximately 16 million gallons per day
of water withdrawals represent finite limits on the amount of additional
water can be withdrawn safely in this area - for all purposes
and for all times. Whether or not the above figures are accurate and
precise is of little consequence. The fact is that, under a business as usual
scenario, at some time in the not too distant future, growth in Champaign
County may be restricted by water
availability.
Implementation of
Executive Order 2006-01 will lead over the next three years to water supply
and demand projections to the year 2050 for East-Central Illinois and
evaluation of management options. Currently, a process for
communities in and around Champaign County to decide how they wish to allocate
available water supplies does not exist. The above analysis is, I believe, the
first time that a finite capacity
to withdraw water from the aquifers in Champaign County has been articulated,
so it is not surprising that there has been no discussion about the allocation
of limited assets.
The Water Survey remains neutral on the allocation and use of
available water. I simply wish to pass on to analysts, decision makers, and
the public our current understanding of the aquifers, future water availability, and water demand. Water
is withdrawn for many purposes including domestic, commercial,
recreational, agricultural, power generation, mining, and other industrial uses. Some of
these users have private wells, but many are dependent on public water
supplies. Knowledge of limited water supplies will, I hope, stimulate
people to set priorities and consider a range of management strategies.
Currently there are many uncertainties, but even with perfect scientific
knowledge and an accurate prediction capability, the key issue will remain the
allocation of scarce resources. Although
the potential sustainable yield of
the entire aquifer is large, water withdrawals in Champaign County already
have created a large cone-of-depression and reversed the east-to-west flow of groundwater. Champaign County is a "hot spot" in need of management
attention.
Please let me
know if we can provide additional information.
Sincerely,
Derek Winstanley, D.Phil.
Chief
Illinois State Water Survey
2204 Griffith Drive
Champaign, IL 61820-7495
Tel: (217) 244 5459
Fax: (217) 333 4983
Attachment (pdf ~68k)