2004 Denver Annual Meeting (November 7–10, 2004)

Paper No. 5
Presentation Time: 9:10 AM

COMBINING TRACERS AND HEURISTIC FIELD METHODS TO INFER ANTHROPOGENIC AQUIFER RESPONSES IN NEARSHORE WATERS


BACCHUS, Sydney T., Applied Environmental Svcs, P. O. Box 174, Athens, GA 30603, appliedenvirserv@mindspring.com

Sewage effluent is injected into the karst aquifer along the Florida’s SE coast via >1000 shallow wells (cased depth ~20 m) and numerous high-volume (~200 mgd) deep wells. Harmful macroalgal blooms and coral decline are increasing in those waters. A pilot study evaluated the hypothesis that: 1) deep-aquifer (Floridan) discharges occur in localized areas with dense benthic macroalgae, and coral/seagrass decline, and 2) localized dense benthic macroalgae, associated with submarine groundwater discharges (SGD), exhibit stable nitrogen isotope (δ15N) ratios indicative of sewage effluent. Sites were selected in nearshore (continental shelf) surface waters in Biscayne Bay (vicinity of Black Point deep-aquifer sewage injections); Card Sound/Barnes Sound; Florida Bay (Everglades National Park); and Florida Keys ocean side (vicinity of >1000 shallow aquifer-injection wells). Dissolved helium (He) anomalies in surface waters were used as tracers of groundwater origin. Excesses of 4He indicate deep-aquifer discharges. Greatest 4He excesses were in the Marquesas Keys, associated with localized coral decline and dense benthic macroalgae, and in N Florida Bay, where 1987 seagrass dieoffs occurred. Benthic macroalgal samples from sites with dense macroalgal growth and localized coral decline had δ15N ratios indicative of sewage: 1) where effluent disposal was concentrated into shallow-aquifer sewage wells, and 2) in the Marquesas Keys, ~40 km from shallow-aquifer injection wells, septic tanks, and cess pits. Surfacewater signatures indicative of aquifer-injection zones reconfirm breached aquifer confinement, and are the first report of Floridan-aquifer discharges for the Keys ocean side. Remote sites with deep-aquifer signatures, extensive benthic macroalgal growth, and δ15N signatures indicative of sewage effluent suggest effluent-laden SGD, via karst conduits, may be a significant source of localized nutrients supporting harmful macroalgal blooms.