Use of multiple tracers and geochemical modeling to assess vulnerability of a public supply well in the karstic Floridan aquifer Brian Katz1, Christy Crandall1,

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Presentation transcript:

Use of multiple tracers and geochemical modeling to assess vulnerability of a public supply well in the karstic Floridan aquifer Brian Katz1, Christy Crandall1, Scott McBride2, and Marian Berndt1 U.S. Geological Survey 1Tallahassee, FL 2Tampa, FL Fifth National Monitoring Conference May 8-11, 2006 San Jose, CA U.S. Department of the Interior U.S. Geological Survey

Take Home Messages Public supply well in the karstic Floridan aquifer system is highly vulnerable to contamination due to short circuiting of water from surficial material through a highly transmissive zone in the limestone. Mixing of water in the PSW from the surficial and Floridan aquifers results in elevated concentrations of pesticides, VOCs, nitrate, radon, arsenic and uranium, compared to monitoring wells in the Floridan aquifer.

Floridan Aquifer System- Highly Susceptible to Contamination Mapped karst features Small scale study area Tampa, FL Upper Floridan aquifer

Highly Permeable Surficial material Marine Terrace deposits consisting of highly permeable sands with some clays (intermediate confining unit) Elevations range from 24 to 80 ft above sea level Mean rainfall = 55 in/yr Hillsborough River Mean annual flow (1939- 2000): 450 cfs Interactions between river and surficial and Floridan aquifers Deeply incised river Channel

Vulnerability of ground water to contamination Monitoring Network Area

Monitoring Network Regional ground- water flow 29 monitoring wells installed in 2003-04, based on contributing areas generated using probabilistic, and fracture models. Regional ground- water flow

Putting the pieces together Use of multiple chemical tracers and geochemical modeling to determine: origin of contaminants in PSW movement of contaminants to PSW mixtures of water from different hydrogeologic units in PSW Stable isotopes DOC pesticides Fe major ions Age tracers As, U, 222Rn VOCs Redox TEAPs NO3 Geo- physical logs solid- phase chem. Flow models Geo-chem.

Assessing Ground-Water Age: SF6 and 3H atmospheric input

SF6 and 3H/3He apparent Ages (yrs) much younger in surficial material than Floridan aquifer

Lower specific conductance and much larger open hole in 150-170 ft zone Caliper Depth, ft 110 130 150 170 Geophysical logs of public supply well bore (TTP-4)

Optical Televiewer shots show large openings in limestone in Public supply well bore (TTP-4) 156 ft 148 ft 138 ft 160 ft 164 ft

Pesticides detected in public supply well Atrazine and Deethylatrazine (CIAT) were detected four times in water from PSW (TTP-4) Concentrations were highest in 62SRP POND and surficial well at this site. Surface water

6 VOCs detected in samples from public supply well

Nitrate-N concentrations decrease with depth except for public supply well NO3-N concentrations higher in oxic surficial aquifer system than anoxic Floridan aquifer with exception of TTP-4 and other wells in 150-160 ft depth zone.

Naturally occurring contaminants in public supply well reflect mixing of water

Surficial aquifer water Floridan aquifer water Geochemical Mass-balance mixing models for public supply well (NETPATH) Surficial aquifer water Floridan aquifer water Public Supply Well water TTP-4 Reactions: Mineral dissolution/precipitation Oxidation/reduction of C, S, N, Fe species + Model constraints: C, S, Ca, Mg, Fe, redox Model phases: Calcite, dolomite, gypsum, pyrite, FeOOH, CH2O, CO2

Public Supply well water contains 30-60% water from surficial aquifer TTP-4 Surficial aquifer water 30-60% Floridan aquifer water 40-70% Sensitivity of models evaluated by comparing calculated isotopic compositions to observed compositions +

Conclusions: Public Supply Well Vulnerability Issues Combined chemical, geophysical, and modeling data indicate mixing of water in PSW from surficial aquifer and Floridan aquifer due to short circuiting of water through a highly transmissive zone. Elevated NO3-N conc. (FAS waters typically have much lower NO3 due to denitrification), Numerous detections of VOCs, pesticides at low conc. Elevated As, U, 222Rn conc. compared to water from monitoring wells in the FAS

Acknowledgments: City of Temple Terrace USGS National Water Quality Assessment Program Bruce Bernard Darlene Blum Sandy Eberts Patty Metz Terry Petrosky John Pittman Ann Tihansky City of Temple Terrace Transport of Anthropogenic And Natural Contaminants To Public Supply Wells (TANC) Contact info: bkatz@usgs.gov Brian G. Katz, PhD USGS 2010 Levy Ave. Tallahassee, FL 32310 (850) 942-9500 x3018