» Pine Island Sound Water Management, MFLs (Minimum Flows and Levels) and Historical Flow: 

Water Management, MFLs (Minimum Flows and Levels) and Historical Flow

(MFLs: "The limit at which further water withdrawls would cause significant harm to the water resource or ecology of the area" (USGS))

Boggess, D. H. and T. H. O'Donnell.  (1982).  Deep artesian aquifers of Sanibel and Captiva Islands, Lee County, FloridaOpen-file report ; 82-253.  32 pp.  Tallahassee, FL: U. S. Dept. of the Interior, U. S. Geological Survey.

(During the time that the desalination plant has been in operation, questions have been raised by water- management agencies concerning the ability of the deep artesian aquifers underlying Sanibel and Captiva Islands to continue supplying the water needed to meet the increasing demand with a salinity low enough for the desalination plant to operate effectively.  The purpose of this investigation was to evaluate the water- supply potential of the deeper aquifers.  During the 24-month investigation (October 1975-1977) an important objective was to locate and inventory all existing wells that tapped the deep artesian aquifers.  Except for a few, all known wells were found.  Water levels and water samples were obtained at the wells.  No test wells were drilled as part of this investigation, although one observation well was drilled on Sanibel Island as part of a countywide monitoring network.)

Boggess, Durward H.  (1974).  Shallow fresh-water system of Sanibel Island, Lee County, Florida, with emphasis on the sources and effects of saline water.  Report of investigation: State of Florida Bureau of Geology; No. 69.  52 pp. Tallahassee: State of Florida, Dept. of Natural Resources, Division of Interior Resources.

DelCharco, M. J.  (1998).  Tidal flow in selected areas of Tampa Bay and Charlotte Harbor, Florida, 1995-96.  44 pp.  U. S. Geological Survey Water-Resources Investigations Report 97-4265.  Tallahassee, FL: U. S. Dept. of the Interior, U. S. Geological Survey.

(This report presents the results of a study designed to measure and describe flow in selected areas of Tampa Bay and Charlotte Harbor.  A total of 232 measurements of flow were made at the mouth of each estuary and within Anna Maria and Pine Island Sounds.  Data collection included measuring the flows into (flood) and out of (ebb) each estuary and sound under a range of tidal elevation, wind, and freshwater inflow conditions.  Measurements of tidal elevation (water-surface elevation) and wind magnitude and direction were made while flow data were being collected.  Freshwater inflow data from established U. S. Geological Survey gagging sites were used to quantify freshwater inflow.)

Dragovich, A., J. A. Kelly, Jr. and J. H. Finucane.  (1966).  Oceanographic observations of Tampa Bay, Charlotte Harbor, Pine Island Sound, Florida and adjacent waters of the Gulf of Mexico, February 1964 through February 1965.  73 pp.  Washington, DC: U. S. Fish and Wildlife Service.
(The authors present the results of observations made of Tampa Bay, Charlotte Harbor, and Pine Island Sound, Florida, and adjacent waters in the Gulf of Mexico from February 1964 through February 1965.  Includes maps and tables.)

Estevez, E. D, J. Miller and J. Morris.  (1984).  Charlotte Harbor Estuarine Ecosystem Complex and the Peace River.  2 vols.  Fort Myers, FL: Southwest Florida Regional Planning Council.
(This is a 1984 review of published and unpublished scientific information on the Charlotte Harbor estuarine ecosystem complex and the Peace River.  It covers the entire coastal area of the Charlotte Harbor region, including Gasparilla Sound, the Peace and Myakka River estuaries, Charlotte Harbor proper, Matlacha Pass and Pine Island Sound, the Caloosahatchee River estuary, San Carlos Bay and Estero Bay.  A special chapter has been prepared for the Peace River.  Information has been reviewed in the disciplines of meteorology, topography, geology, hydrology, water chemistry, and biology.)

Goodwin, Carl R.  (1996).  Simulation of tidal-flow, circulation, and flushing of the Charlotte Harbor estuarine system, Florida.  Water Resources Investigation Report: 93-4153.  92 pp.  Tallahassee, FL: U. S. Dept. of the Interior, U. S. Geological Survey.
(Examines the simulation of tidal-flow, circulation, and flushing of the Charlotte Harbor estuarine system including the eccect of removing the Sanibel Causeway on flushing of Pine Island Sound and San Carlos Bay.)

Jones, Ronald D. and Joseph N. Boyer.  (2001).  Integrated surface water quality monitoring program for the south Florida coastal waters: FY2000 cumulative report to the South Florida Water Management District (C-10244), and Everglades National Park.  55 pp.  Miami, FL: Southeast Environmental Research Center, Florida International University.

(Covers Cape Romano to Pine Island Sound, providing site-specific information on salinity, temperature, dissolved oxygen, turbidity, total nitrogen and total phosphorous, total organic nitrogen, total organic carbon, alkaline phosphatase activity, chlorophyll a, silicate, nitrate, nitrite, ammonium, total phosphorous and soluble reactive phosphate.)

Missimer and Associates.  (1979).  Hydrologic investigation of the Hawthorn and Suwannee aquifer systems in the central area, Sanibel, Florida.  [Cape Coral, FL: Missimer and Associates.
(In 1978, a site was chosen for exploration of the Suwannee Aquifer System at a location adjacent to the reverse osmosis water treatment plant.  A full hydrologic investigation was completed at the site.  The investigation included test drilling for geologic data, observation and test-production well construction, a 72-hour aquifer test, packer-stem tests, and a water quality test program.  The report includes data, conclusions, and recommendations.)

Missimer and Associates.  (1978).  Hydrologic investigation of the Hawthorn Aquifer system in the northwest area, Sanibel, Florida.  Cape Coral, FL: Missimer and Associates.
(A northwestern Sanibel test site at Bowman's Beach Road was chosen for investigation of the lower Hawthorn Aquifer.  A detailed hydrologic investigation was completed at the site.  The investigation included geologic test drilling, observation and test-production well construction, a 72-hour aquifer test, and the chemical analysis of numerous water samples.  This report includes data, conclusions, and recommendations.)

Post, Buckley, Schuh and Jernigan.  (1999).  Synthesis of technical information.  Charlotte Harbor Estuaries Program.  Technical Report No. 99-02.  2 vols.  North Fort Myers, FL: Charlotte Harbor National Estuary Program.

Vol. 1.  Characterization of water quality, hydrologic alterations, and fish and wildlife habitat

(This document comprises the characterization element of the National Estuary Program process.  It synthesizes available information about the water quality, hydrologic alterations, and fish and wildlife habitat in the Greater Charlotte Harbor watershed.  It covers the Caloosahatchee River, Charlotte Harbor, Estero Bay, Lemon Bay, Myakka River, Peace River,  Pine Island Sound and  Coastal Venice.)

South Florida Water Management District.  (2000).  Caloosahatchee River and estuary salinity profiles.  West Palm Beach, FL: The District.
http://www.sfwmd.gov/lo_statustrends/recessperiod/caloosa/cesprofsal.htm
(Salinity profile for May-June, 2000.  Vertical profiles of salinity as a function of upstream distance from the mouth of the Caloosahatchee River.  Negative distances indicate monitoring sites located in San Carlos Bay.)

Stoker, Yvonne E.  (1992).  Salinity distribution and variation with freshwater inflow and tide, and potential changes in salinity due to altered freshwater inflow in the Charlotte Harbor estuarine system, Florida.  Water-resources investigations report ; 92-4062.  30 pp.  Tallahassee, FL: U. S. Dept. of the Interior, U. S. Geological Survey.

(This report presents the results of a study to define the temporal and spatial salinity variability in Charlotte Harbor, relate this variability to freshwater inflow and tide conditions, and evaluate potential changes in salinity that might result from altered freshwater inflow to the harbor.  The study area includes upper Charlotte Harbor, Pine Island Sound, Matlacha Pass, San Carlos Bay, nearshore waters of the Gulf of Mexico, the tidal Caloosahatchee River, and the lower reaches of the tidal Peace and Myakka rivers.  Data were collected from June 1982 to May 1987.)

Swett, R. A., D. A.. Fann, G. A. Antonini and L. C. Alexander.  (2001).  Regional Waterway Management System for Lee County, Phase 2.  Gainsville, FL: State University System of Florida, Sea Grant College Program.

Swett, R. A., D. A.. Fann, G. A. Antonini and L. C. Alexander.  (2000).  Regional waterway management system for Lee County, Phase 1.  Gainsville, FL: State University System of Florida, Sea Grant College Program.
(The project aims to devise a management strategy that allows for the simultaneous use and protection of coastal waters, while maintaining the economic vitality of the region.)