THE OGALLALA AQUIFER
The
Ogallala aquifer (pronounced OH-GA-LA-LA) is one of
the largest aquifer systems in the world. It stretches
across all or portions of eight states generally from
north to south to include South Dakota, Nebraska,
Wyoming, Colorado, Kansas, Oklahoma, New Mexico, and
Texas and underlies about 174,000 square miles. N.H.
Darton is credited with describing and naming the
formation in 1899 after the town of Ogallala,
Nebraska.
The
Ogallala aquifer lies relatively near the land surface
in most of the above-described area with a maximum
thickness of about 1,000 feet with a few hundred feet
more the norm. Even in those areas of only a few feet
of thickness, the aquifer can almost always be counted
on to yield water to a well drilled into it. Some
wells yield only a few gallons of water per minute,
while others yield 1,000 gallons of water per minute
or more. The Ogallala aquifer not only includes the
portion of the Ogallala that is saturated with water,
but may also include saturated portions of the
overlying and underlying formations that are
hydraulically connected to the Ogallala. Water in the
aquifer on the Southern High Plains flows from
northwest to southeast at about 150 feet per year
under natural conditions. This rate of movement can be
altered by discharge from the aquifer by pumping
wells.
Deposition of the Ogallala Formation began 10 to 12
million years ago during late Tertiary
(Miocene/Pliocene) geologic time. Sand, gravel, silt,
and clay eroded from upland areas to the west and
north were deposited over the erosional land surface
of the present-day High Plains by primarily eastward
flowing streams. The surface on which the sediments
were deposited would have been much like the present
area located east of the High Plains escarpment
characterized by low hills, relatively shallow
valleys, and meandering streams. As a result of the
burial of this land surface by predominantly Ogallala
sediments, the Ogallala Formation is thicker where
these sediments filled the old stream channels and
thinner where hills or upland areas were buried. The
uppermost layer of the Ogallala Formation is typically
a caliche layer described as the “Caprock Caliche.”
This layer locally varies in thickness and has been
reported to be as much as 60 feet in thickness in some
areas. The caliche layer formed about one million
years ago after the land surface stabilized and soils
formed.
The
water table is a term used to describe the uppermost
surface of sediments that are 100 percent saturated.
Saturated thickness describes the thickness of an
aquifer. This interval is determined by subtracting
the elevation of the base of the aquifer from the
elevation of the water table at a point of interest.
In some parts of Nebraska, the saturated thickness
exceeds 1,000 feet and generally thins to less than 20
feet in thickness in some areas of the Great Plains.
The
amount of water that may be recovered in an aquifer,
such as the Ogallala, is dependent primarily
on
the areal extent, the saturated thickness, and the
specific yield of the aquifer. Specific yield is a
hydrologic parameter related to the volume of water an
aquifer will yield as a result of gravity drainage. As
an example of this parameter, 15 percent specific
yield is an average value that is customarily accepted
for the Southern High Plains Ogallala aquifer. More
specifically at 15 percent specific yield each cubic
foot of water saturated aquifer volume will yield 0.15
cubic-foot of water as a result of gravity drainage (See
graphic depicting specific yield at right).
In
1990, the Ogallala aquifer in the eight-state area of
the Great Plains contained 3.270 billion acre-feet of
water, of which about 65 percent was located under
Nebraska. Texas had about 12 percent of the water in
storage or approximately 417 million acre-feet of
water. Kansas has 10 percent of the water. About 4
percent was located under Colorado, with 3.5 percent
located under Oklahoma. Another 2 percent was under
Wyoming. The remaining 1.5 percent of the water was
under New Mexico. A recent estimate of the volume of
water in the eight-state Great Plains area was just
under 3 billion acre-feet.
Natural recharge to the Ogallala aquifer occurs
primarily through the percolation of precipitation
through the soils and underlying sediments to the
water table. It is generally recognized that playa
lakes are the primary points of most natural recharge.
The interplaya areas generally contribute a minimum of
the recharge, except for areas of exceptional
accumulation of precipitation with resultant extensive
percolation of water to the water table in locations
where streambeds and dune areas are common. Various
studies of natural recharge have historically
estimated various ranges of average recharge to the
Ogallala aquifer. Recent studies have estimated an
average recharge rate for the entire High Plains
region of approximately 0.5 of an inch per year.
Before the development of irrigation, the discharge
from the aquifer occurred from both saline and fresh
water like basins, from streams, and from seeps and
springs located primarily along the eastern
escarpment. Some of these still flow today; however,
most seeps and springs have ceased to flow due
primarily to lowering of the water table as discharge
has exceeded natural recharge.
Approximately 95 percent of the water pumped from the
Ogallala is for irrigation. The High Plains area
represents 65 percent of the total irrigated acreage
in the United States. The quality of the water pumped
from the aquifer is suitable for irrigating; but in
some places, the water does not meet U.S.
Environmental Protection Agency (USEPA) drinking water
quality standards. For example, some constituents
identified above EPA standards include sulfate,
chloride, selenium, fluoride, nitrate, and total
dissolved solids.
The
Southern High Plains area is characterized as a
semi-arid climate. Average annual rainfall varies
across the region. In the Lubbock, Texas area, the
average annual rainfall is about 18 inches per year.
High evaporation rates are common in the area. The
average annual evaporation rate for the Lubbock area
is about 80 inches per year.
Monitoring of the depth-to-water in the aquifer’s
Southern High Plains revealed rapid declines in the
water table in the early 1950s, 1960s, and the 1970s.
Declines of a foot or more per year were recorded
throughout the 1940s; and during the late 1950s at the
peak of irrigation development, some monitoring wells
indicated as much as five feet of decline in a single
year. The trend of rapid decline started slowing in
the mid-1970s. By 1985, the portion of the Ogallala
aquifer within the service area of the High Plains
Underground Water Conservation District No. 1 began to
stabilize. In some limited or unique areas, water
level rises have been documented. A drought began in
the area in mid-1992, and continued until late 1996.
Agricultural producers, out of necessity, increased
pumpage of water for irrigation to supplement
precipitation. The increased demand for crop water by
irrigation resulted in an increased rate of water
level decline during this period. In subsequent years
of greater precipitation, decreased needs for pumpage
have allowed water level declines to decrease.
Early
settlers believed the water supply that lay beneath
them was inexhaustible. In the 1930s, people had begun
to realize the potential of the vast water supply that
lay beneath them. By 1949, about 2 million acres of
the Southern High Plains were irrigated. Pumpage for
irrigation increased from about 4 million acre-feet in
1949 to nearly 18 million acre-feet in1980.
In
the early days of irrigation on the Texas High Plains,
very little water conservation equipment or technology
was available. As a result, large amounts of water
were lost to evaporation and deep percolation. Open,
unlined ditches were used to transport the water from
the well to the field being irrigated. It was not
uncommon to have water losses ranging from 10 to 30
percent per 1,000 feet of ditch. High pressure,
hand-moved sprinklers had evaporation losses of up to
50 percent.
Throughout the years, irrigation technology has
evolved to allow agricultural producers to apply water
much more efficiently without waste. Irrigation water
escaping from fields into road ditches (“irrigation
tailwater”) is not as common as it once was in the
1960s and 1970s. Improved technologies, spurred on by
incentives such as the Environmental Quality
Incentives Program (EQIP) and low interest
agricultural water conservation equipment loan
programs, have helped improve water use efficiencies.
For example, average water use efficiency within the
High Plains Water District service area improved from
about 50 percent in the mid 1970s to approximately 75
percent in 1990. Current state-of-the-art low
pressure, full dropline center pivot systems, used in
conjunction with furrow dikes, are about 95 percent
efficient, while buried subsurface drip irrigation
lines approach 100 percent efficiency.
Producers are irrigating fewer acres. Land enrolled in
the Conservation Reserve Program (CRP), rising energy
costs, declines in well yields, and low farm prices
also account for part of this reduction.
The
rates of decline in the water levels in the aquifer
continue to be somewhat stable with noted annual
decreases in decline resulting when annual
precipitation is above average and less ground water
needs to be pumped. Researchers continue to work on
methods to increase natural recharge to the aquifer
and to improve water-use efficiency. The prospects
for the future of the Ogallala aquifer ultimately
depend upon its management by each of its water
users.
Additional information is available by contacting
Technical Group Supervisor Don McReynolds at (806)
762-0181.
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