81 Environmental Geoscience; Geology and Health; Public Policy II: Environmental Geology for Public Use and Biogeochemistry (Posters)
Monday, 29 October 2007
8:00 AM - 12:00 PM
THE CORRELATION OF FECAL COLIFORM AND TURBIDITY OF THE LITTLE TALLAPOOSA RIVER IN THE WEST GEORGIA REGION
Paper number: 81-6
Program: Technical Sessions
Time: 8:00 AM – 12:00 PM
Authors
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Brian K. ParrishUniversity of West Georgia, Carrollton, GA
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Curtis L. HollabaughUniversity of West Georgia, Carrollton, GA
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Randa R. HarrisUniversity of West Georgia, Carrollton, GA
Abstract
Turbidity is the cloudiness of water caused by individual particles suspended in the water. A rain event or erosion elevates the amount of sediment in rivers producing an increase in turbidity. A comparison of turbidity and fecal coliform from six sites was conducted using data from 2003 to present along the Little Tallapoosa River. The study proved a direct correlation with an R2 value ranging from 0.6 to 0.8. From the six sites turbidity ranged from 5.7 to 120 NTU with a mean of 12 to 17 NTU. Fecal coliform bacteria ranged from 20 to 25000 col./100mL with a geometric mean of 180 to 340 col./100mL. The direct correlation between turbidity and fecal coliform indicates that as turbidity increases, so does fecal coliform bacteria. The result is significant in obtaining an accurate estimate for fecal coliform before waiting the 24 hour incubation time the procedure requires. As field parameters are taken at a site, increased turbidity values may be used to assume increased levels of fecal coliform bacteria. Therefore, an alert could be made to users of a recreational water body of possible high fecal coliform bacteria values.