Northeastern Section (39th Annual) and Southeastern Section (53rd Annual) Joint Meeting (March 25–27, 2004)

Paper No. 4
Presentation Time: 9:00 AM

SOURCES OF NITRATES AND AGE OF YOUNG FRACTION OF GROUND WATER FROM SILVER SPRINGS, FLORIDA


PHELPS, G.G., U. S. Geol Survey, 224 W. Central Pkwy., Suite 1006, Altamonte Springs, FL 32714, tgphelps@usgs.gov

          Nitrate concentrations in Silver Springs, Florida, have increased from about 0.5 milligrams per liter (mg/L) in the 1970s to about 1.0 mg/L in 2003. During 2001-2002, nitrate concentrations in water from 56 wells in the spring basin ranged from less than 0.02 to 12 mg/L, with a median of 1.2 mg/L. Sources of nitrogen in the basin include atmospheric deposition, fertilizers, and human and animal wastes. Determining the relative influence of the various nitrate sources is problematic. The ratio of 15N/14N in ground-water samples ranged from -0.5 to 11.5 per mil, with a median of 4.9, indicating a mixture of both organic and inorganic sources. Four water samples from the Main Spring of Silver Springs analyzed for 15N/14N showed two distinct values, one (3.8 per mil) indicating inorganic N and the other (8.7 per mil), indicating mixed sources with a strong influence of organic N. The values did not seem to be related to spring discharge. Water samples from 35 wells in the basin and 3 springs of the Silver Springs group were analyzed for a suite of organic compounds commonly found in wastewater. The most commonly detected compound was N,N-diethyl-meta-toluamide (DEET), which was detected in 27 wells and all 3 springs. Samples collected from the three springs in January 2002 also were analyzed for CFCs, SF6, and 3H/3Hetrit. CFC concentrations in the spring-water samples higher than present-day atmospheric levels were indicative of wastewater influence and precluded the use of CFCs for age dating. SF6 and 3H/3Hetrit data yielded apparent ground-water ages (based on a piston-flow model which may not adequately represent the complex flow in the karstic aquifer system) ranging from about 8-27 years for the young fraction of ground water.