1996
DOI: 10.2172/266844
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Report on the feasibility of using isotopes to source and age-date groundwater in Orange County water district`s Forebay region

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Cited by 5 publications
(8 citation statements)
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“…In these cases the simulated mean age of groundwater reaching well P6 was never greater than 6 years, certainly much smaller than the 17.7-year isotopically measured age. In addition, these simulations indicated that little, if any, groundwater in this well originated from the Santa Ana River, as has been suggested by the isotopic interpretations of Davisson et al [1996] (Plate 2).…”
Section: Calibration and Specification Of Hydraulic Conductivitysupporting
confidence: 62%
See 2 more Smart Citations
“…In these cases the simulated mean age of groundwater reaching well P6 was never greater than 6 years, certainly much smaller than the 17.7-year isotopically measured age. In addition, these simulations indicated that little, if any, groundwater in this well originated from the Santa Ana River, as has been suggested by the isotopic interpretations of Davisson et al [1996] (Plate 2).…”
Section: Calibration and Specification Of Hydraulic Conductivitysupporting
confidence: 62%
“…In addition, isotopic analyses are now being used to infer historical migra- tion patterns by estimating the composition, sources, and ages of groundwater sampled in production and monitoring wells near the spreading basins [Davisson et al, 1996[Davisson et al, , 1998Williams, 1997]. In this paper we will review some of the isotopic results and present a series of numerical simulations designed to examine residence times, historical or future migration pathways, and mixing and dilution processes in the system.…”
Section: Resource Management Challengesmentioning
confidence: 99%
See 1 more Smart Citation
“…There have been no conclusive monitoring or epidemiological studies relating to the introduction and fate of viruses into the OCWD aquifer system, although viruses derived from similar artificial recharge operations have been observed in a nearby aquifer in Los Angeles County 16 . As a means to assess compliance with the proposed regulations, however, isotopic and modeling analyses have been used in the Orange County system to infer migration patterns of groundwater and estimate the ages and sources of groundwater in production and monitoring wells near the spreading basins [17][18][19][20] . Figure 5 shows a figure from a modeling study 20 that shows approximate flow pathways from three production wells, labeled as 'P5', 'P6', and 'P7', back to their surface water sources.…”
Section: Aquifer Banking In Orange County Californiamentioning
confidence: 99%
“…Notably, from the simulation results, no water entering wells P6 and P7 is younger than 1 year in age, although more than half of the water entering well P5 is. As a result of these observations, a tracer test was conducted during a recharge event in nearby Anaheim Lake to see whether any "first arrivals" would appear in any of the various production wells surrounding the lake within a 1-year time period 17 . A small amount of a Xenon isotope ( 124 Xe) was introduced in the lake as the tracer.…”
Section: Aquifer Banking In Orange County Californiamentioning
confidence: 99%