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Title: Natural radionuclides in groundwaters from J-13 well at the Nevada Test Site

Conference ·
OSTI ID:138088

The concentrations of U-238 and Th-232 chain members are extremely low in J-13 water, suggesting that their concentrations in groundwaters are largely governed by sorption/desorption processes. Relative to radon (gas), uranium, thorium, radium, and polonium radionuclides are highly sorbed in a tuffaceous matrix, and the retardation factors range from 10{sup 2} to 10{sup 5}. Uranium, unlike Th, is in the +6 state and is soluble as carbonate complex (UO{sub 2}CO{sub 3}), and the aquifer`s environment is oxidizing. There is no colloidal effect down to <0.10 {mu}m. 15 refs., 1 fig., 2 tabs.

Research Organization:
Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
Sponsoring Organization:
USDOE, Washington, DC (USA)
DOE Contract Number:
AC06-76RL01830
OSTI ID:
138088
Report Number(s):
PNL-SA-17572; CONF-900406-83; ON: DE91011817; TRN: 91:018473
Resource Relation:
Conference: 1. international topical meeting on high-level radioactive waste management, Las Vegas, NV (United States), 8-12 Apr 1990; Other Information: PBD: Apr 1990
Country of Publication:
United States
Language:
English