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Call 911 to report Hazards, Toxic Spills or
Threats to Basin
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FACTS
Size: 11,500
square miles of south-central Kansas. Includes
all or parts of 20 counties.
Population:
Has the second largest population of all the twelve
major river basins, with an estimated 641,000
residents in the year 2000. The population is
projected to grow to nearly 813,000 in the year
2040.
Flow: The
Arkansas River flows generally southeast across
the basin. Major tributaries entering the river
along its course are Rattlesnake Creek, Cow
Creek, Little Arkansas River, Ninnescah River
and Slate Creek. Other major streams in the
basin that join the Arkansas River in Oklahoma
are the Chikaskia River, Medicine Lodge River
and Salt Fork. For real-time information on
water levels in the river basin click on the
following website:
http://waterdata.usgs.gov/ks/nwis/rt
Reservoirs:
The major reservoir in the basin is Cheney
Reservoir in Reno County M75. To locate Cheney
Reservoir see the following website:
http://www.kgs.ku.edu/Hydro/lake_maps.html
Topography and Soil:
The topography in the basin varies from
flat, undulating plains of slight relief to
rolling uplands and, in places, steep bluffs and
hills. Sandy soils and sand dunes are prevalent,
mostly in the river valleys, but fine textured
soils, tight clays and many other soil types are
also represented.
Economy: The general economy of the basin is
diversified, with farming throughout the area
and industrial activity most heavily
concentrated in the Wichita-Newton-Hutchinson
vicinity. Corn, wheat and livestock are the
principal agricultural products. Many kinds of
industries are represented in the basin, with
the aircraft and oil and gas industries being of
major importance. The salt mines of the state
are located largely in this basin. There is a
sizable gypsum production west of Medicine
Lodge.
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Usage of Water
Surface water provides 8% of supply for
all reported uses in 1997.
Groundwater is the source for 92 percent
of supply for all reported uses in 1997.
Groundwater sources for the Lower Arkansas Basin
include the Ogallala (also called the High
Plains Aquifer) and Equus Beds Aquifers. To find
the locations of these subsurface water bearing
units, and the organizations that manage
groundwater districts, click on the following
website:
http://www.ksda.gov/Default.aspx?tabid=180&mid=2311&ctl=Download&method=attachment&EntryId=217
Reservoir
Information: Cheney Reservoir
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CONSUMERS
Agriculture: Irrigation accounted for
about 71 percent of all reported water pumped or
diverted (1997).
Industry: Industry accounted for over 9
percent; recreation and stock water combined
about 1.5 percent (1997).
Municipal: Municipal use accounted for
about 19 percent of water used in the basin.
The City of Wichita takes 60% of its water from
the Lake Cheney reservoir and 40% from ground
water of the Equus Beds. It adopted an
Integrated Local Water Supply Plan in 1993 to
meet the projected water needs of the City and
surrounding communities through 2050. A key
component of the plan is a recharge, storage and
recovery project involving the use of water from
the Little Arkansas River to recharge the Equus
Beds Aquifer. For more information on the Equus
Bed Artificial Recharge Project see websites in
subsurface Quality section that follows.
The use of Cheney Reservoir is also a part of
the Wichita water plan. Information on Cheney
water usage can be found in the following site:
http://www.usbr.gov/dataweb/html/wichita.html
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THREATS AND HAZARDS
Quality
Ground Water (subsurface)
High Plains Aquifer: For specific
information about groundwater quality contact:
Stafford Groundwater
Management District at
Big Bend Groundwater Management District #5
125 South, Main St
Stafford, KS 67578
Phone: (620) 234-5352
Fax: (620) 234-5718
http://www.gmd5.org/
The following
websites contain general information about the
High Plains Aquifer and threats to groundwater
quality from salt contamination and total
dissolved solids (TDS):
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EQUUS BEDS
ACQUIFER
(perched above High Plains Aquifer
in subsurface)
Equus Beds Groundwater
Management District No. 2
313 Spruce Street
Halstead, KS 67056
phone: (316) 835-2224
fax: (316) 835-2225
http://www.gmd2.org/
The following
websites and summaries provide information on
the artificial recharge project in the Equus
Beds. Water quality is an issue with artificial
recharge (i.e, flood water from the Arkansas is
pumped or seeped into ground water system).
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> WATER QUALITY
Each Public Water System
should provide a Consumer Confidence Report of
water quality to the KDHE and the EPA:
Information
about Kansas public water supplies can be found
at:
To find out
what is in your local drinking water follow the
websites below:
Drill down’ from the top using EPA websites that
follow:
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WATER QUANTITY
Groundwater: For current information about groundwater levels
and water rights, see WIMAS website:
http://hercules.kgs.ku.edu/geohydro/wimas/index.cfm
KGS - water level decline in high plains aquifer
http://www.kgs.ku.edu/HighPlains/2000-29B/Decdir.htm
KGS -supply and demand needs on high plains
aquifer
http://www.kgs.ku.edu/HighPlains/2000-29C/needdir.htm
Surface Water:
Streams:
Flood and Drought Information: for real
time water levels on the Lower Arkansas River:
http://waterdata.usgs.gov/ks/nwis/rt
Drought Assessment:
http://www.kwo.org/reports%20&%20publications/drought/kwo%20drought%20report.htm
Kansas Water Office reports on drought:
http://koufax.kgs.ku.edu/kars/kars_map.cfm
Weekly
interactive maps showing vegetation conditions
across the State of Kansas. The maps are derived
from NOAA satellite data that measures how green
vegetation is. Vegetation stress is a proxy
measure of drought. Flood Information:
Contact the National Weather
Service http://www.nws.noaa.gov/
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ADDITIONAL LINKS
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