Abstract
This paper explores the feasibility of using 14C in dissolved organic carbon (DOC) as an alternative isotopic ground water dating method. Two hydrogeologically contrasting groundwater systems were tested; the Cretaceous age Milk River aquifer, and low‐permeability, organic rich, Wisconsinan age Prairie tills in southern Alberta, Canada. Comparisons of radiocarbon data were made between DOC fractions, dissolved inorganic carbon (DIC), and several DIC geochemical age correction models along well defined flow paths. The data presented demonstrate that 14C dating of DOC fractions can indeed provide an alternative method for determining isotopic groundwater ages, under suitable conditions. However, detailed information may be required regarding (1) the geologic nature of the aquifer and its flow system, (2) the isotopically conservative behavior of DOC, (3) the initial 14C activity of DOC in recharge, and (4) the effect of bacterial redox processes on the 14C activity of DOC. In the Milk River aquifer, DOC 14C ages were successfully used to estimate groundwater residence times, as well as to further refine input parameter assumptions for the DIC method. In the Prairie tills, DOC 14C ages were used to establish a maximum age for the pore waters in an environment where the DIC method is especially problematic.
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