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Title: Saline groundwaters and brines in the Canadian Shield: Geochemical and isotopic evidence for a residual evaporite brine component

Journal Article · · Geochimica et Cosmochimica Acta; (United States)
 [1];  [2];  [3]
  1. Atomic Energy Control Board, Ontario (Canada)
  2. Geological Survey of Canada, Ottawa, Ontario (Canada)
  3. Raven Beck Environmental Ltd., Ottawa, Ontario (Canada)

Saline Ca-Na/Cl type groundwaters and brines sampled in deep mines over an extensive area of the Canadian Precambrian Shield have elevated Br/Cl ratios which may indicate that the chlorinity of these waters was derived from the infiltration of residual evaporitic brines, remnants of the great marine incursion of the Paleozoic era. Boron concentrations in these waters are generally low (i.e., < [approximately] 2 mg/L) relative to seawater or Alberta Basin Devonian formation waters. However, the [sup 11]B/[sup 10]B ratios of these waters are significantly greater than the average value for continental crustal rocks with the highest values ([approximately]4.19) approaching that of present-day seawater (4.20). Moreover, the boron isotopic ratios generally trend to higher values with increasing chlorinity which supports the conclusion from the Br-Cl relationship that most of the chloride in shield brines is of marine origin, rather than a product of water/rock interactions. If this is correct, crystalline rocks must then be sufficiently permeable on a regional scale to have allowed the brine to infiltrate to depths of several kilometers where it now resides. The presence of saline groundwaters in crystalline has important implications for the Canadian Nuclear Fuel Waste Management Program, which proposes disposal of waste fuel in a repository constructed at a depth of 500-1000 m in plutonic rock.

OSTI ID:
7040690
Journal Information:
Geochimica et Cosmochimica Acta; (United States), Vol. 58:5; ISSN 0016-7037
Country of Publication:
United States
Language:
English