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{{Multiple issues| |
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{{external links |date= June 2012}} |
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{{self-published |date= June 2012}} |
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{{confusing|date=September 2012}} |
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{{original research|date=September 2012}} |
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{{undue|date=September 2012}} |
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}} |
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[[File:Peaceflrivermap.png|thumb|200px|]] |
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[[File:Kissengen Springs Painting.jpg|thumb|Painting Kissengen Springs]] |
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[[File:Kissengen Spring flooded from Peace River backflow after 3 hurricanes passed through the area, October, 2005.jpg|thumb|Backflow from [[Peace River (Florida)|Peace River]] after hurricanes]] |
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'''Kissengen Spring''' (also spelled Kissingen) was a venue for recreation until it dried up in 1950. Hundreds of wells drilled into the [[Floridan Aquifer]] may have caused the demise of the springs. The spring was located near the northern end of [[Peace River (Florida)|Peace River]]. |
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==History== |
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Kissengen's springwater rose from the Floridan Aquifer at the rate of 20 million gallons a day.<ref>[http://www.tampabay.com/news/perspective/hope-lives-even-as-marker-notes-polks-kissengen-springs-dry-since-1950/1193065 Kissengen Spring Dry Since 1950]</ref><ref>[http://www.tampabay.com/news/perspective/hope-lives-even-as-marker-notes-polks-kissengen-springs-dry-since-1950/1193065 Kissengen Spring Dry Since 1950]</ref> Kissengen Spring was once a [[Spring_(hydrology)#Classification|second magnitude spring]].{{cn|date=July 2012}} |
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It is believed that Kissengen Spring was fed by pressurized waters from the Upper Floridan Aquifer System and perhaps other local aquifers.{{fact|"other local aquifers" too vague. maybe whole sentence should be dropped|date=July 2012}} |
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In 1886, the Burr family moved near the spring to farm.<ref>[http://www.robertburr.com/bunburr.html 1886 Burr Family and Kissingen Springs]</ref><ref>[http://www.robertburr.com/bunburr.html 1886 Burr Family and Kissingen Springs]</ref> |
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It was once a featured subject in news articles from the late 19th century.{{fact|date=July 2012}} |
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Increased groundwater withdrawal, beginning in the late 1930s, lowered the [[potentiometric surface]] of the aquifers. Kissengen Spring gradually ceased flowing. The spring was publicly declared inactive in 1950 as the result of overpumpage.{{cn|date=July 2012}} |
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Until 1950, tourists used the area for picnicking, boating, and swimming.<ref>[http://www.theledger.com/article/20110823/COLUMNISTS/108235000?p=1&tc=pg Kissingen Spring Was Spot For Fun]</ref><ref>[http://www.floridamemory.com/solr-search/results/?q=kissengen+springs+ Florida Archive Photos]</ref> There was a pavilion for parties and dancing.<ref>[http://www.polkcountyhistory.org/pdf/dec75.pdf Activities That Were In The Pavillion]</ref> The waters were thought medically beneficial to those with various ailments. |
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In 1962 a sinkhole filled in the spring vent with clay.<ref>[http://itech.fgcu.edu/faculty/ndemers/Mining/kissengen%20Springs%20may%2008.htm Kissingen Spring was much enjoyed and now is dried up.]</ref><ref>[http://itech.fgcu.edu/faculty/ndemers/Mining/kissengen%20Springs%20may%2008.htm Kissingen Springs was much enjoyed and now is dried up.]</ref> |
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===Historical Marker=== |
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<!---probably should be shortened---> |
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A historical marker was funded by the Florida Humanities Council.<ref>[http://www.polkarts.org/2011/08/16/kissengen-spring-historical-marker-dedication/ Kissengen Spring Historical Marker Presentation]</ref> The Polk County Museum had a Historical Marker Ceremony in August 2011. The marker has now been placed at the Mosaic Peace River Park.<ref> |
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[http://www.theledger.com/article/20110823/COLUMNISTS/108235000?p=1&tc=pg Kissingen Spring Was Spot For Fun]</ref> |
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==Hydrology== |
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In 1962 a [[sinkhole]] formed near the site of Kissengen Spring and a flow of clay filled in the flow vent and probably the underground channels. This is a problem in restoring flow to the springs.<ref> [http://www.dep.state.fl.us/water/mines/docs/prbmac/kissengen-response.pdf The Spring Vent Plugged with Clay]</ref> |
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[[File:Streamflow changes along upper Peace River, Fl 3.JPG|thumb|left|Flow changes along upper Peace River]] |
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===Florida Aquifers=== |
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<!---may need background under hydrology. But this is not an article about Floridan Aquifer which has it's own article---> |
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[[Image:Floridan Aquifer USGS.gif|thumb|right|300px|The Floridan aquifer underlies portions of five states. Source: USGS]] |
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Most spring water comes from the [[Floridan Aquifer]]. <ref>[http://sofia.usgs.gov/publications/papers/pp1403a/flaqsys.html Florida Aquifers]</ref> This water enters the aquifer from groundwater recharge areas across the Southeast. The water is under pressure |
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and this force pushes water out of spring vents. <ref>[http://plants.ifas.ufl.edu/guide/aquifers.html Florida Aquifers] </ref> |
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===Peace River=== |
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<!---needs rewriting.---> |
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Kissingen Spring used to put {{convert|20|e6USgal|m3}} of water into [[Peace River (Florida)|Peace River]]. The river had a year round flow. Lacking the spring water and {{convert|11|e6USgal|m3}} going down into large sinks causes the upper river to go dry in the spring. Peace River sometimes goes dry and flows into several sinks around the riverbed. Water flows into openings to the underground [[karst]] conduits.<ref>[http://gallery.usgs.gov/tags/PeaceRiver/thumb/_/1 Peace River Is Sometimes Dry And Flows Underground]</ref> |
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<ref>[http://gallery.usgs.gov/tags/NR2009_09_30 Find Picture Of Water Gauge Being Placed In The Mud]</ref> |
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[[Image:AlapahaRiver2002.jpg|thumb|Image of the entire [[surface water]] flow of the [[Alapaha River]] near [[Jennings, Florida]] going into a sinkhole leading to the [[Floridan Aquifer]] [[groundwater]].]] |
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Progress is being made to control the |
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draining of the [[aquifer]]. <ref>[http://soundwaves.usgs.gov/2010/02/research.html 11 Million Gallons of River Water Goes Underground]</ref> |
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There are a number of cracks and sinks in the Peace River. The water flows down into |
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undergroundcaverns that can hold millions of gallons of water.<ref>[http://pubs.usgs.gov/sir/2009/5140/pdf/sir2009-5140.pdf Karst Features of Upper Peace River]</ref><ref>[http://pubs.usgs.gov/sir/2009/5140/pdf/sir2009-5140.pdf USGS Publications]</ref> |
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A hydrology report on Peace River points to efforts to repair damage done by lowering the water table.<ref>[http://www.gohydrology.org/2011/02/second-life-of-kissengen-spring.html Hydrology Report On Peace River]</ref><ref>[http://www.collinscenter.org/resource/resmgr/our_florida/FloridaWaterEthic.pdf Cynthia Barnett and the Vanishing Water]</ref><ref>[http://license.icopyright.net/user/viewFreeUse.act?fuid=MTM5NzMyODY= Hope lives, even as marker notes Polk's Kissengen Springs, dry since 1950]</ref> |
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===Peace Creek=== |
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Located in [[Polk County, Florida]], Peace Creek joins with Saddle Creek to form the headwaters of the |
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Peace River. This stream and its watershed have been altered from their natural state. |
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==Role of government== |
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Water regulation did not start until the early 1960s. |
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The [[Florida Department of Environmental Protection]] (DEP) protects natural resources, including springs. <ref>[http://www.dep.state.fl.us/springs/ Department of Environmental Protection]</ref> |
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The [[Southwest Florida Water Management District]] has developed a plan to restore waterflow to Kissingen Springs.<ref>[http://www.swfwmd.state.fl.us/documents/plans/swuca_recovery_strategy.pdf South Water Use Caution Area Recovery Strategy]</ref> |
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==Restoration== |
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It is not known whether the water shortage at Kissengen Spring is real and permanent, or the result of a period of lower than average rainfall coupled with decades of pre-regulatory overdrafting of the aquifer.{{fact|date=July 2012}} |
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[[File:Streamflow changes along upper Peace River, Fl.JPG|thumb|Streamflow changes along upper Peace River]] |
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There is a project to raise the level of Lake Hancock and start a larger flow towards Peace River.<ref>[http://www.enviro-net.com/story.php?id=17&month=10&paper=fl&year=2008 Lake Hancock Project]</ref> |
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To restore Kissengen Spring, the [[aquifer]] must be recharged with enough water to recreate the original spring pressure.{{cn|date=July 2012}} Peace River will have to be restored to the year round minimal flow. During May, much of the upper Peace River goes dry. This dry period is hindering the aquifer recharge and revitalzation of Kissengen Spring.<ref>[http://peacecreek.org Peace Creek Alliance: Peace River Source Gains New Ally]</ref> |
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The intent of these two projects is to increase the clean flow of Peace River and recharge the aquifer around the Kissengen Spring area. |
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===Lake Hancock Outfall Wetland Project=== |
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The Lake Hancock Outfall Wetland Project (LHOWP) is a large-scale, flow-through, wetland to improve the quality of water that discharges from Lake Hancock to Saddle Creek and ultimately to the [[Peace River (Florida)|Peace River]] and [[Charlotte Harbor]]. The project site is located adjacent to and south of [[Lake Hancock]] in [[Bartow, Florida|Bartow]], [[Polk County, Florida]]. |
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The finished project is expected to consist of a {{convert|1008|acre}} treatment wetland located on former reclaimed [[phosphate]] mine clay settling areas now owned by the [[Southwest Florida Water Management District]]. |
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On the south end of Lake Hancock is a structure called P-11. It can be raised or lowered to control the level of water in Lake Hancock. |
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Water will be pumped from the southern shore of the lake through three wetland cells. The cells will incorporate narrow planting strips separated by larger natural recruitment zones. The treated water will discharge from the Cell 3 wetland outfall structure into Lower Saddle Creek, which is downstream of the lake outfall structure (P-11). |
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The project includes construction of an inlet pump station, instrumentation, controls, control structures, earthwork, embankment, slurry cut-off wall, channels, aeration structure and access road. |
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The plan is to raise the level of the lake about {{convert|1|ft}} and making the lake a natural storage area for water. The result would increase flow into the Peace River. Part of the project is to filter the water through marsh areas before releasing it. |
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Peace River has several openings into the karst conduits and millions of gallons of water flow underground instead of down the riverbed. This project will attempt to create berms around these holes and limit the amount of water being lost. |
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The water cannot be directly discharged into Peace River because of the polluted condition of the water.{{cn|date=July 2012}} |
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The LHOWP project should be completed by 2013.<ref>[http://www.swfwmd.state.fl.us/files/database/site_file_sets/88/lake_hancock_outfall_alt_treatment2007-09.pdf Lake Hancock Outfall Wetland Project]</ref><ref>[http://rondrake.com/spring.html LHOWP Maps Pictures]</ref> |
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===Peace River Project=== |
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A second project is being built on the Old Plantation property to clean the water and send it to Peace River. |
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==References== |
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{{Reflist|2}} |
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==External links== |
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*[http://capp.water.usgs.gov/aquiferBasics/floridan.html USGS Aquifer study] |
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*[http://itech.fgcu.edu/faculty/ndemers/mining/kissengen%20Springs%20may%2008.htm Kissengen Spring among the lost resources] |
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*[http://www.tampabay.com/news/perspective/hope-lives-even-as-marker-notes-polks-kissengen-springs-dry-since-1950/1193065 Hope lives, even as marker notes Polk's Kissengen Springs, dry since 1950] |
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*[http://rondrake.com/spring.html Kissengen Spring] |
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*[http://www.theledger.com/article/20110823/COLUMNISTS/108235000 Polk Chronicles: Kissengen Spring Was Spot For Fun] |
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*[http://www.theledger.com/article/20110825/NEWS/110829601 Historical Marker Unveiled in Bartow For Kissengen Spring] |
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{{coord missing|Florida}} |
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[[Category:Regional geology]] |
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[[Category:Springs of Florida]] |
Revision as of 13:05, 10 September 2012
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