Utilization of Tryptophan-like Fluorescence as a Proxy for E. coli Contamination in a Mixed-Land-Use Karst Basin

Author:

Dapkus Ryan T.1,Fryar Alan E.1ORCID,Tobin Benjamin W.2ORCID,Byrne Diana M.3ORCID,Sarker Shishir K.1ORCID,Bettel Leonie3ORCID,Fox James F.3

Affiliation:

1. Department of Earth and Environmental Sciences, University of Kentucky, Lexington, KY 40506, USA

2. Kentucky Geological Survey, University of Kentucky, Lexington, KY 40506, USA

3. Department of Civil Engineering, University of Kentucky, Lexington, KY 40506, USA

Abstract

Karst aquifers are susceptible to contamination by pathogenic microorganisms, such as those found in human and animal waste, because the surface and subsurface drainage are well integrated through dissolution features. Fecal contamination of water is commonly assessed by the concentration of thermotolerant coliform bacteria, especially E. coli. This method is time-consuming, taking ≥18 h between the start of incubation and subsequent enumeration, as well as the time required to collect and transport samples. We examined the utility of continuous monitoring of tryptophan-like fluorescence (TLF) as a real-time proxy for E. coli in a mixed-land-use karst basin in the Inner Bluegrass region of central Kentucky (USA). Two logging fluorometers were sequentially deployed at the outlet spring. During storm flow, TLF typically peaked after discharge, which suggests that TLF transport in the phreatic conduit is likely related to sediment transport. The ability of TLF and other parameters (48 h antecedent precipitation, turbidity, and air temperature) to predict E. coli concentrations was assessed using the Akaike information criterion (AIC) applied to linear regression models. Because both the models and baseline concentrations of TLF differed between fluorometers, TLF and instrument interaction were accounted for in the AIC. TLF was positively correlated with E. coli and, in conjunction with antecedent precipitation, was the best predictor of E. coli. However, a model that included air temperature and antecedent precipitation but not TLF predicted E. coli concentrations similarly well. Given the expense of the fluorometers and the performance of the alternate model, TLF may not be a cost-effective proxy for E. coli in this karst basin.

Funder

U.S. Geological Survey

Kentucky Senate Bill 271B Water Quality program

National Science Foundation

Kentucky Geological Survey

University of Kentucky College of Agriculture, Food and Environment

Karst Waters Institute

Publisher

MDPI AG

Subject

Earth-Surface Processes,Waste Management and Disposal,Water Science and Technology,Oceanography

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4. Leibundgut, C., Gunn, J., and Dassargues, A. (1997). Karst Hydrology, International Association of Hydrological Sciences Publication 247, IAHS Press.

5. Brahana, J.V., Eckstein, Y., Ongley, L.K., Schneider, R., and Moore, J.E. (1998). Gambling with Groundwater—Physical, Chemical and Biological Aspects of Aquifer-Stream Relations, American Institute of Hydrology.

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