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Radiocarbon in Dissolved Organic Carbon, A Possible Groundwater Dating Method: Case Studies From Western Canada
Author(s) -
Wassenaar Leonard,
Aravena Ramon,
Hendry Jim,
Fritz Peter
Publication year - 1991
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/91wr00504
Subject(s) - dissolved organic carbon , radiocarbon dating , groundwater , groundwater recharge , aquifer , geology , hydrology (agriculture) , total organic carbon , groundwater flow , geochemistry , environmental science , environmental chemistry , oceanography , chemistry , paleontology , geotechnical engineering
This paper explores the feasibility of using 14 C 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 14 C 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 14 C activity of DOC in recharge, and (4) the effect of bacterial redox processes on the 14 C activity of DOC. In the Milk River aquifer, DOC 14 C 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 14 C ages were used to establish a maximum age for the pore waters in an environment where the DIC method is especially problematic.