HECTOR O. CONDE
CAGRD, Attn. Cliff Neal
Comments: CAGRD Draft Plan of
Operation
Although the plan presented
September 28 seems to allow continuance with the present recharge and
replenishment established goals for the Tucson AMA, the truth of the matter is
that the availability of water for the population in the future will not be met
with the present recharge methods.
The water should be recharged
where the wells are located. The particular topography of the northern part of
the Tucson AMA is such that there is a 1800 feet
altitude drop between
To illustrate the point I
refer to fig. 1 that shows the altitude changes. Fig. 2 shows a partial map (1)
of the area that depicts the depth of the saturated zone. Fig. 3 shows the
general direction of the underflow (2). Notice that the subsurface water will
flow from
The example of
Fig. 4 shows what the
development would do to safe yield in the area. It is clear that there is a
water deficit from the start. Data is 2002.
At a water roundtable in
Oracle in 2001, Erroll Montgomery stated that the
area was not sufficiently studied, but his estimate was a capacity of 1,500,000
Acre feet. He also pointed out that the number could be half of that.
Fig. 5 shows an estimate of
the aquifer use in 100 years. Assuming that build-out would occur in 50 years
the column called “cumulative” that shows the total water use in the area,
indicates that in 53 years the aquifer would be depleted. This also shows that
there is no compliance with the 100 year assured water supply statutory
requirement. Of course if the aquifer is half the stated capacity, it would be
25 years.
One example of politicians
voting on the wrong side of the issue is
The CAGRD is an elected body.
As such it is supposed to act in defense of the voter’s interest. For starters,
it would be appropriate that the board recommend to the legislature that all
recharges take place in the areas where the wells are drilled. It will be a
step to assure the population that their properties would not have zero value
some day, either because of subsidence or lack of drinking water or both.
Sincerely,
Hector Conde
1 Cooley, 1973, Alluvial deposits…USGS 1-844-C
2 Osterkamp, 1974, Ground water velocities… USGS i-844-K








