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Title: The Influence of Calcium Carbonate Grain Coatings on Contaminant Reactivity in Vadose Zone Sediments

Technical Report ·
DOI:https://doi.org/10.2172/833529· OSTI ID:833529

Calcium carbonate (CaCO3) is widely distributed through the Hanford vadose zone as a minor phase. As a result of current and past geochemical processes, CaCO3 exists as grain coatings, intergrain fill, and distinct caliche layers in select locations. Calcium carbonate may also precipitate when high-level wastes react with naturally Ca- and Mg-saturated Hanford sediments. Calcium carbonate is a very reactive mineral phase. Sorption reactions on its surface may slow the migration of certain contaminants (Co, Sr), but its surface coatings on other mineral phases may diminish contaminant retardation (for example, Cr) by blocking surface reaction sites of the substrate. This project explores the behavior of calcium carbonate grain coatings, including how they form and dissolve, their reactivity toward key Hanford contaminants, their impact (as surface coatings) on the reactivity of other mineral substrates, and on their in-ground composition and minor element enrichment. The importance of CaCO3 as a contaminant sorbent will be defined in all of its different manifestations in Hanford sediments: dispersed minor lithic fragments, pedogenic carbonate coatings on gravel and stringers in silt, and nodules in clay and paleosols. Mass action models will be developed that allow understanding and prediction of the geochemical effects of CaCO3 on contaminant retardation in Hanford sediments.

Research Organization:
Pacific Northwest National Lab., Richland, WA; Stanford University, Stanford, CA; University of Wyoming, Laramie, WY (US)
Sponsoring Organization:
US Department of Energy (US)
DOE Contract Number:
FG07-99ER15024; FG07-99ER15019
OSTI ID:
833529
Report Number(s):
EMSP-70121-2001; R&D Project: EMSP 70121; TRN: US200430%%1606
Resource Relation:
Other Information: PBD: 1 Jun 2001
Country of Publication:
United States
Language:
English