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At AECL – Chalk River Laboratories, Ontario, Canada solid, low-level radioactive wastes from industrial, academic and medical applications have been stored in trenches above unconsolidated sandy glacial tills and permeable very-fine to fine-grained sands overlying crystalline bedrock. The sandy aquifer system drains into a swamp comprised of approximately 3 m of sphagnum peat. A comprehensive field and analytical program, involving measurements of total iodine,  129 I, tritium,  14 C and  13 C/ 12 C ratios in groundwater and geologic materials (sands and peats), was initiated at this site to examine the partitioning of  127 I and  129 I amongst the various reservoirs in this system and the controlling factors.

Partitioning of 127 I and 129 I in an unconfined glaciofluvial aquifer on the Canadian shield