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Tracing Sources of Sulfur in the Florida Everglades

Anne L. Bates*, William H. Orem, Judson W. Harvey and Elliott C. Spiker

United States Geological Survey, 956 National Center, Reston, VA 20192



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Fig. 1. Study areas in the northern Everglades of southern Florida. Surface water flow in the Everglades is generally from north to southwest (from Lake Okeechobee to Florida Bay).

 


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Fig. 2. Sources of sulfate to marshes of the northern Everglades.

 


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Fig. 3. Distribution of average sulfate concentrations (mmol L-1) in surface waters of the northern Everglades.

 


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Fig. 4. Comparison of sulfide concentrations (mmol L-1) in sediment porewater from Water Conservation Area (WCA) 2A and WCA 3A, December 1995 through December 1996. Note the changes in scale: data for August and December 1996, F1 and U3.

 


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Fig. 5. (a) Comparison of total sulfur (% dry weight) and (b) total phosphorus (µg g-1 dry weight) depth profiles in sediment from Water Conservation Area (WCA) 2A at Sites E1 and U3, 1994. Sulfur profile adapted from data in Bates et al. (1998).

 


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Fig. 6. Concentrations of sulfate (mmol L-1) versus {delta}34S values in surface water collected in the northern Everglades from 1995–1999.

 


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Fig. 7. Sulfate in surface water, 1995–1999: Sulfate concentrations versus {delta}34S values in the Everglades Agricultural Area (EAA) canals, the Everglades Nutrient Removal Area (ENR), and the Water Conservation Areas (WCAs) in the northern Everglades.

 


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Fig. 8. (af) Trends in sulfate concentration and {delta}34S values and in {delta}18O values of sulfate and of water, March and July 1995. (h) {delta}34S versus 1/ (as 1/mg L-1), July 1995. Surface water transects are in Water Conservation Area (WCA) 2A and along the Hillsboro Canal.

 


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Fig. 9. Comparison of sulfate concentrations and {delta}34S values in surface and ground water in Water Conservation Area (WCA) 2A and the Everglades Nutrient Removal Area (ENR) of the northern Everglades.

 





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