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Fractions of river water in groundwater range from 0 to 72 percent and average 10 percent. Plummer,.N., Busenberg,., Drenkard,., Schlosser,., McConnell,.B., Michel,.L., Ekwurzel,., and Weppernig,., 1998, Flow of river water into a karstic limestone aquifer2. The influence of river-water discharge on the quality of water in the Upper Floridan aquifer was traced from the sinkhole area on the Withlacoochee girl River 25 km dating southeast in the direction of regional groundwater flow. This led to him talking to me on the phone one night from 7pm to 4am. I just wanted to say thank you for bringing us together.
Dissolved Cl-, 18O, D, CFC-12, and the quantity (3H3He) are stable in water from the Upper Floridan aquifer, whereas DOC, DO, H2S, CH4, 14C, CFC-11, and CFC-113 are affected by microbial degradation and other geochemical processes occurring within the aquifer. Data on transient tracers and other natural substances, including dissolved chloride (Cl- tritium (3H tritiogenic helium-3 (3He chlorofluorocarbons (CFC-11, CFC-12, CFC-113 dissolved organic carbon (DOC dissolved oxygen (DO dissolved hydrogen sulfide (H2S dissolved methane (CH4 oxygen-18 ( 18O deuterium ( D and carbon-14 (14C) were. Publications: Plummer,.N., McConnell,.B., Busenberg,., Drenkard,., Schlosser,., and Michel,.L., 1998, Flow of river water into a karstic limestone aquifer1. Tritium/helium-3 (3H/3He) and chlorofluorocarbon (CFCs, CFC-11, CFC-12, CFC-113) data were used to date the young fraction in groundwater mixtures from a karstic limestone aquifer near Valdosta, Georgia, where regional paleowater in the Upper Floridan aquifer receives recharge from two young sources- flow of Withlacoochee River. The fractions of regional paleowater, regional infiltration water, and Withlacoochee River water in the groundwater mixtures were determined from Cl- and 18O data for water from the Upper Floridan aquifer at Valdosta, Georgia (Plummer., 1998). Location map for Valdosta, Georgia, and wells sampled. Map showing contours of CFC-11 concentration in ground water at Valdosta (as log pg/kg). I am so glad he didn't because we have now been married for 2 1/2 years.
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Map showing calculated islam percent of Withlacoochee river water in ground water. Map showing contours of CFC-113 concentration in ground water at Valdosta (as log pg/kg). I just wanted to let you know that I am grateful for this site. Groundwater mixing fractions were determined by using dissolved Cl- and 18O data, recognizing three end-member water types in the groundwater mixtures: (1) Withlacoochee River water ( 18O-2.50.3 per mil, Cl-12.22 mg/L (2) regional infiltration water ( 18O-4.20.1 per mil, Cl-2.30.1 mg/L and (3) regional paleowater. Tritium data and dating based on both CFC-11 and CFC-12 in Type-1 mixtures indicate that travel times of infiltration water through the overlying Post-Eocene semi-confining beds exceed 35 years.
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Of the 41 water samples measured for 3H/3He back dating, dilution of 3H and low 3H concentration limited 3H/3He dating to 16 mixtures in which 3H/3He ages were defined with errors ranging from 2.5 years (1 s ). Tracing the young fraction in groundwater mixtures in the Upper Floridan aquifer near Valdosta, Georgia. The concentrations of all tracers were affected by dilution and mixing. After correction for dilution with (assumed) CFC-free regional infiltration water and regional paleowater in the Upper Floridan aquifer, adjusted CFC-12 ages agreed with 3H/3He ages within 5 years or less in 7 of the 9 co-dated Type-2 france mixtures.
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This site is amazing. An average lag time of approximately 10 to 25 years was determined for discharge of groundwater from the surficial and intermediate aquifers above the Upper Floridan aquifer to the Withlacoochee River. I wish others the same happiness as we have found. Few domestic and municipal supply wells sampled intercept water younger than 5 years.