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Title: Studies of radionuclide sorption by clays in the Culebra Dolomite at the Waste Isolation Pilot Plant site, southeastern New Mexico

Technical Report ·
DOI:https://doi.org/10.2172/6840341· OSTI ID:6840341
 [1]; ;  [2];  [3];  [4]
  1. Sandia National Labs., Albuquerque, NM (USA)
  2. Stanford Univ., CA (USA)
  3. Lawrence Berkeley Lab., CA (USA)
  4. New Mexico Univ., Albuquerque, NM (USA)

The ability of radionuclide-rock interactions to retard the migration of plutonium and uranium within clay-lined fractures in the Culebra Dolomite Member of the Rustler Formation is being estimated in support of the performance assessment of the Waste Isolation Pilot Plant. This paper describes progress in three coordinated studies: characterization of the properties of the groundwater and minerals in the Culebra that will control radionuclide retardation; development of a thermodynamic model for the adsorption of uranium onto corrensite, the mixed chlorite-smectite clay mineral found in Culebra fractures; and development of a data base of equilibrium constants and interaction parameters for calculations of the aqueous speciation of uranium and plutonium in Na--Cl--Ca--SO{sub 4}--CO{sub 3} solutions which contain organic ligands such as EDTA and range in ionic strength from approximately 0.8 to 6.0 molal. 22 refs., 6 figs., 1 tab.

Research Organization:
Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
Sponsoring Organization:
DOE/DP
DOE Contract Number:
AC04-76DP00789
OSTI ID:
6840341
Report Number(s):
SAND-89-2387; ON: DE90013594
Country of Publication:
United States
Language:
English