2009
DOI: 10.1111/j.1745-6584.2008.00504.x
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Vulnerability of a Public Supply Well in a Karstic Aquifer to Contamination

Abstract: To assess the vulnerability of ground water to contamination in the karstic Upper Floridan aquifer (UFA), age-dating tracers and selected anthropogenic and naturally occurring compounds were analyzed in multiple water samples from a public supply well (PSW) near Tampa, Florida. Samples also were collected from 28 monitoring wells in the UFA and the overlying surficial aquifer system (SAS) and intermediate confining unit located within the contributing recharge area to the PSW. Age tracer and geochemical data f… Show more

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Cited by 19 publications
(10 citation statements)
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“…Redox conditions are also important for understanding occurrences of elevated arsenic concentrations in the lower intermediate aquifer. Previous studies have attributed relatively high arsenic concentrations to the infiltration of surface water and subsequent oxidation of pyrite in these formations (Katz et al ; Katz et al ; Ayotte et al ). Although the present model predicted that surface water would have reached lower intermediate aquifer wells by the early 2000s (~28–31 m; Figure C), oxygen was predicted to have been consumed prior to this depth.…”
Section: Discussionmentioning
confidence: 97%
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“…Redox conditions are also important for understanding occurrences of elevated arsenic concentrations in the lower intermediate aquifer. Previous studies have attributed relatively high arsenic concentrations to the infiltration of surface water and subsequent oxidation of pyrite in these formations (Katz et al ; Katz et al ; Ayotte et al ). Although the present model predicted that surface water would have reached lower intermediate aquifer wells by the early 2000s (~28–31 m; Figure C), oxygen was predicted to have been consumed prior to this depth.…”
Section: Discussionmentioning
confidence: 97%
“…The highest groundwater arsenic concentrations historically occurred in the surficial aquifer beneath the Main Plant Area and the primary process water pond (P1) (Figure ), with concentrations predominantly greater than 0.01 mg/L (the EPA Maximum Contaminant Level, or MCL) at these locations. In deeper groundwater, arsenic concentrations have generally been within the expected natural background range (0.001–0.02 mg/L) (Katz et al , ; Ayotte et al ).…”
Section: Site Backgroundmentioning
confidence: 99%
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“…A public-supply well located within the Rio Grande principal aquifer in Albuquerque, New Mexico, was studied as part of the NAWQA program's "Transport of Anthropogenic and Natural Contaminants (TANC) to supply wells" topical team (Bexfield and others, 2012). Samples for 3 H, 14 C, and chlorofluorocarbons (CFCs) were collected in June and December 2007, November 2008, and May 2009 The data in this report are from the studied supply well or SSW in Bexfield and others (2012). All 14 C measurements were corrected for dilution from non-radioactive ("dead") carbon sources by using PHREEQC and NetpathXL (Parkhurst and Appelo, 1999;Plummer and others, 1994).…”
Section: Example 2: Public-supply Well In Albuquerque New Mexicomentioning
confidence: 99%
“…The situation is heavier and heavier, which is concerned by many scholars [1][2][3], especially in the oilfield [4].…”
Section: ⅰ Introductionmentioning
confidence: 99%