https://www.heraldandnews.com/members/forum/guest_commentary/state-water-actions-taken-without-first-determining-what-the-actual/article_0a17281d-8157-5d53-82ef-7d3329470455.html
State
water actions taken without first determining what the actual
facts are
Oregon State Senator Dennis
Linthicum, District 28, which includes all or part of Klamath ,
Lake, Jackson, Deschutes and Crook counties, Herald and News
5/15/18
Oregon
Water Resources Department (OWRD) recently shut down 140
irrigation wells in the Upper Klamath Basin. The wells, each
within a 1-mile proximity boundary of the Sprague River,
have been “determined” to impair senior surface water rights
and are being regulated off.
For
some background, water law and theory have linked ground
water to surface water as described in “Arizona Law Where
Ground and Surface Water Meet (1988):”
“When
water is pumped from an aquifer by means of a well, it
creates what is known as a ‘cone of depression.’ This is
caused by the groundwater in the aquifer moving toward the
well. If the material in the aquifer has a high
transmissivity value, the cone of depression will be wide
and shallow. If, on the other hand, the aquifer does not
easily transmit water, the cone of depression will be steep
and narrow.
“If
water is pumped continuously from the well, the cone of
depression will become larger. If the water table is close
enough to the earth’s surface to allow this cone to cut into
a surface stream, water from the stream would directly
infiltrate into the ground, following the slope of the cone
of depression until it reached the well. … This would cause
less water to be available in the stream bed.”
In
Arizona law, the doctrine of prior appropriation applies to
surface waters and extends to another prior appropriation
category known as “subflow.” Historically, this is “those
waters which slowly find their way through the sand and
gravel constituting the bed of the stream, or the lands
under or immediately adjacent to the stream and are
themselves a part of the surface stream.”
Now,
this may be true in the sand and gravel of the Arizona
outback and it may even be true in the geological formations
found within the Upper Klamath Basin, but is it? Logic tells
us that the only way to find out would be to study and
understand the geological and hydrological formations that
are within a specific hydrological zone.
OWRD’s
Division 09 rules (Oregon Administrative Rules — OAR
690-009) were also adopted in 1988, following Arizona case
law. The basis for the OWRD’s regulation of groundwater
occurs whenever OWRD determines that substantial
interference with a surface water supply exists. An OWRD
spokesperson claims, “It is our position that Division 09
governs regulation in the Upper Klamath Basin Area at this
time.”
However, without scientific justification this is nothing
but refutable, theoretical folly.
My
question is, exactly how does OWRD make their
“determination” establishing that substantial groundwater
interference occurs with a surface water right-holder? How
does OWRD determine the transmissivity value or size and
shape of the cone of depression?
Scientific examination would clarify that some wells do
impact surface waters while others do not. OWRD seems to
suggest that in all cases, at all times, and in all
circumstances, groundwater wells impact surface flows.
We
know this can’t be true. After all, some wells are drilled
through solid rock for hundreds of feet while other wells
are not. In other circumstances, a well, even in close
proximity to another, might travel through several different
aquifer layers before arriving at a separate hydrological
zone where irrigation requirements might be met.
First,
OWRD ought to know with certainty that an individual well is
harming a senior water right-holder, before shutting-down
specific water resources.
Second, OWRD needs to establish standards for measuring
distances between wells and surface water sources for the
purpose of determining the probability, or existence of
surface water right impairment.
Third,
OWRD also ought to provide negatively impacted right-holders
with written notice of planned actions so that families have
time to consider their available options.
Fourth, the models used, the facts gained, any legal
theories or existing rulings being used to support the
planned action also need to be made public.
If our
government process is designed around public participation
and transparency, then publishing planned actions and
detailed evidentiary findings produced by a qualified
hydrologist describing specific well site geology and
hydrology should not be a problem for our state government’s
executive agencies.
I am
currently working on legislation that would require OWRD to
follow and adhere to these four suggestions. We must hold
our unelected bureaucracies to the highest bar possible when
their rulings affect the very lives and livelihoods of
hardworking Oregonians.
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