2006 Philadelphia Annual Meeting (22–25 October 2006)

Paper No. 11
Presentation Time: 11:10 AM

USE OF POLYDISPERSE MICROSPHERES AND SIZE- AND FLUORESCENCE-DISCRIMINATION FLOW CYTOMETRY TO ESTIMATE THE VULNERABILITY TO CRYPTOSPORIDIUM PARVUM OF A SOLE-SOURCE, KARST-LIMESTONE AQUIFER IN SOUTHEASTERN FLORIDA


HARVEY, Ronald W.1, METGE, David W.2, SHAPIRO, Allen M.3, RENKEN, Robert A.4, OSBORN, Christina L.5, RYAN, Joseph N.6, CUNNINGHAM, Kevin J.7 and LANDKAMER, Lee L.1, (1)U.S. Geological Survey, 3215 Marine Street, Boulder, CO 80303, (2)US Geological Survey, 3215 Marine, Marine Street Science Ctr, Boulder, CO 80303, (3)U.S. Geological Survey, 12201 Sunrise Valley Drive, Mail Stop 431, Reston, VA 20192, (4)3110 SW 9th Avenue, Fort Lauderdale, FL 33315, (5)Department of Civil, Environmental, and Architectural Engineering, Univ of Colorado, Boulder, CO 80309, (6)Civil, Environmental, and Architectural Engineering, University of Colorado, 428 UCB, Boulder, CO 80309-0428, (7)U.S. Geological Survey, 3110 SW 9th Ave, Fort Lauderdale, FL 33315, rwharvey@usgs.gov

Municipal well vulnerability in the Northwest Well Field in Miami-Dade County in southeastern Florida to potential contamination by oocysts of the protozoan pathogen, Cryptosporidium parvum, was assessed in a large-scale, forced-gradient (convergent) injection and recovery test. The field study involved a simultaneous pulse introduction of a conservative tracer (SF6, an inert gas) and a polydispersed suspension of oocyst-sized (1.6 ìm, 2.9 ìm, and 4.9 ìm diameter), carboxylated polystyrene microspheres into a section of Biscayne aquifer karstic limestone characterized by complex, triple (matrix, touching-vug, and conduit) porosity. Recoveries 97 m downgradient from the injection borehole were inversely related to diameter and ranged from 2.8 to 5.6%, respectively. The centers of mass for the microspheres arrived at the pumping well ~3-fold earlier than that of the SF6 further underscoring the need for use of colloid tracers and field-scale tracer tests for evaluating time-of-travel well-field protection zones in the Biscayne. In a bench-scale test involving a modified triaxial cell using near in-situ chemical conditions, the microspheres underestimated by several fold the transport potential of the less-electronegative oocysts within interparticle matrix porosity of limestone core samples. Field-scale microsphere test results and the aforementioned bench-scale comparisons of microsphere and oocyst transport behaviors collectively suggest buffer areas much larger than 100 m are required to achieve a ten-fold reduction of oocysts, even though the limestone surfaces exhibit a substantive capability for their sorptive removal. The study further demonstrated the utility of size- and fluorescence-discrimination flow cytometry and the use of large quantities of microspheres in a polydispersed suspension as oocyst surrogates in field-scale assessments of well vulnerability, provided that electrochemical differences between oocysts and microspheres are taken into account.