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Call 911 to report Hazards, Toxic Spills or
Threats to Basin
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FACTS
Size:
The Marais des Cygnes basin covers 4,304 square
miles in east central and southeast Kansas (see
Figure 1). It is known as the Lake District.
Population: There
were an estimated 125,000 residents in the basin
in the year 2000, and the population is
projected to grow to nearly 178,000 by the year
2040.
Flow:
The Marais des Cygnes River Basin rises near
Eskridge in Wabaunsee County, Kansas and flows
east and south to join the Little Osage in Bates
County, Missouri. Below this junction the
stream becomes the Osage River, which continues
eastward through Truman Lake and Lake of the
Ozarks to its juncture with the Missouri River a
short distance below Jefferson City. Major
tributary streams include Pottawatomie Creek and
the Marmaton River.
Information on water levels in the river basin
click on the following website:
http://waterdata.usgs.gov/ks/nwis/rt
Reservoirs:
The Corps of Engineers operates three large
reservoirs in the Marais des Cygnes Basin.
These are Pomona Lake, Melvern Lake and
Hillsdale Lake.
To locate
these reservoirs see the following website:
http://www.kgs.ku.edu/Hydro/lake_maps.html
Topography and Soil:
Surface elevations in the Marais des Cygnes
Basin range from about 742 feet to 1,475 feet.
The climate of the Marais des Cygnes Basin is
humid, with average annual total precipitation
ranging between 35-40 inches.
Economy:
The local economy is based primarily on general
manufacturing. The production of oil and gas is
a relatively small but important component of
the economy.
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Usage of Water
The majority of water used in the basin is from
surface sources. Municipal and industrial
supply is the predominant use of water. For
information on water Appropriation see:
http://www.drought.unl.edu/plan/handbook/nds8.pdf
Groundwater
Ground water is readily available throughout the
Flint Hills region. Most wells produce 10 to 100
gpm, although the eastern crest of the Flint
Hills is not so productive. Well yields of 100
to 500 gpm are common in portions of central
Marion and western
Butler counties (KGS Map M-4a). Principal
aquifers in the Flint Hills are the Nolands,
Winfield, and Barneston Limestones. Springs
emerge from these units in valleys and stream
channels Crystal Spring, near Florence, is one
of the largest single springs in the Flint
Hills. This spring supplies water for the city
of Florence; the spring house has a pumping
capacity of 370 gpm, and excess water flows into
a nearby stream (O'Conner and Chaffee 1983). The
spring emerges near the base of the Barneston
Limestone on the northern side of the Cottonwood
River valley.
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CONSUMERS
Agriculture
Irrigation accounted for a small percent of all
reported water pumped or diverted (1997).
Industry
Most water withdrawals for municipal and
industrial supply in the Marais des Cygnes Basin
come from surface sources.
Municipal
Municipal and industrial supply is the
predominant use of water.
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Water Management
The State of Kansas has purchased water
marketing or water assurance storage in each of
the federal reservoirs in the basin. Two
reservoirs Hillsdale and Melvern contain
state-owned water marketing storage. Two
multipurpose small lakes, Bone Creek and Xenia
have been constructed in this basin. Two
additional lakes, Cedar Creek and Little Sugar
Creek are under development. Eight watershed
districts and one drainage district have been
organized in the Marais des Cygnes Basin,
primarily for flood control.
Marais des Cygnes River Water Assurance District
No. 2 was organized in 1990 and became
operational in 1995 with the signing of a
contract and operations agreement. Seven
municipal and industrial water right holders
along the Marais des Cygnes River are members.
State-owned water assurance storage is located
in Melvern and Pomona lakes
Conservation Districts
are part of a nationwide grass roots
organization made up of people that collectively
promote the wise management of our natural
resources for sustained use. There are 105
Conservation Districts across Kansas, one for
each county in Kansas. Each district is lead by
a board of five supervisors that are locally
elected. These supervisors are not paid for
their service on the board.
Each conservation district has developed
programs aimed to address priority concerns for
their county. If you own land in Kansas, it is
best to contact the district in the county you
own the land. This will insure you the best in
assistance and knowledge of local conditions.
http://www.cjnetworks.com/~sccdistrict/dist_ks.htm
The Army Corps of Engineers
is responsible for the operation of Melvern,
Hillsdale and Pomona and lakes is an important
water manager in the basin. To contact the Army
Corps of Engineers see the following:
http://www.nwk.usace.army.mil/regulatory/boundary.htm
Topographic Maps of Kansas dams
http://www.topozone.com/states/Kansas.asp?feature=Dam
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Threats and Hazards
Quality
Ground Water (subsurface)
Ground water of the Flint Hills region generally
has high total dissolved solids and high total
hardness concentrations. The ionic composition
of well water is dominated by Ca2+
and HCO3-, as expected for
weathering of limestone by precipitation
containing CO2. Magnesium, sodium,
chloride, and sulfate are also added by
weathering. The relatively high concentrations
of calcium and magnesium exceed the recommended
limit for hardness in drinking water in most
cases. Ground water from Smith Cave is sampled
regularly as part of the Groundwater Quality
Monitoring Network (site I.D. 00017602) of the
Kansas Department of Health and Environment.
Nitrate contamination of ground water is a
serious problem throughout Kansas, believed to
be the result of excessive fertilizer
application rather than from natural weathering.
The concentrations of nitrite plus nitrate vary
from below the detection limit to above the
drinking water standard within the Flint Hills.
Dissolved iron and manganese exceed secondary
drinking water standards at many sites. Although
minerals containing these elements are abundant
in the region, they become soluble only under
reducing conditions. It is interesting to note
that samples high in iron or manganese are
usually low in nitrate; the same reducing
conditions promote denitrification of nitrate to
nitrogen gas or ammonia (Schroeder 1990).
Solutions now in effect to slow or prevent
surface or ground- water pollution:
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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:
Surface Water Quality:
Reservoir Quality:
Melvern and
Hillsdale and Pomona Reservoirs
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WATER QUANTITY
Groundwater:
Surface Water
Streams:
Flood and Drought Information:
For real time water levels on the Lower
Arkansas River click on the following website:
http://waterdata.usgs.gov/ks/nwis/rt
USGS
monthly water flow: real time
http://ks.water.usgs.gov/Kansas/history/kswater.hist.html
NOAA advance prediction service for MDC river
http://www.crh.noaa.gov/ahps2/hydrograph.php?wfo=top&gage=qnmk1&view=1,1,1,1,1,1
Drought Assessment:
Kansas Water Office reports on drought
http://www.kwo.org/reports%20&%20publications/drought/kwo%20drought%20report.htm
KGS--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.
http://koufax.kgs.ku.edu/kars/kars_map.cfm
Army Corps of Engineers drought management plan
1994:
http://www.drought.unl.edu/plan/handbook/nds8.pdf
Flood Information:
NOAA Contact the National Weather Service:
http://www.nws.noaa.gov/
Reservoir Quantity Information:
Redman, Council Grove and Marion Reservoirs:
USGS real time water data for reservoirs
http://waterdata.usgs.gov/ks/nwis/current?type=lake&type=none&search_site_no_station_nm
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