1996
DOI: 10.1021/es950745i
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Speciation of Uranium in Fernald Soils by Molecular Spectroscopic Methods:  Characterization of Untreated Soils

Abstract: ES950745IX Abstract published in Advance ACS Abstracts, May 15, 1996.

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Cited by 114 publications
(83 citation statements)
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“…Uranyl oxyhydroxide minerals such as compreignacite are formed easily from oxidation of reduced U minerals (compared to uranyl phosphates and silicates) and precipitate readily from saturated solutions (Morris et al, 1996;Hunter and Bertsch, 1998;Kanematsu et al, 2014). Their fast dissolution rates in natural waters, especially in the presence of high dissolved carbonate, compared with uranyl phosphate and silicate phases emphasizes the need for quantification of coupled reaction and transport processes that control the concentration and fate of U in surface and subsurface environments.…”
Section: Discussionmentioning
confidence: 99%
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“…Uranyl oxyhydroxide minerals such as compreignacite are formed easily from oxidation of reduced U minerals (compared to uranyl phosphates and silicates) and precipitate readily from saturated solutions (Morris et al, 1996;Hunter and Bertsch, 1998;Kanematsu et al, 2014). Their fast dissolution rates in natural waters, especially in the presence of high dissolved carbonate, compared with uranyl phosphate and silicate phases emphasizes the need for quantification of coupled reaction and transport processes that control the concentration and fate of U in surface and subsurface environments.…”
Section: Discussionmentioning
confidence: 99%
“…In the absence of dissolved phosphate or silicate, U(VI) has been observed to form a variety of crystalline and amorphous oxyhydroxide mineral phases in oxic subsurface environments (Morris et al, 1996;Hunter and Bertsch, 1998) and in synthetic acidic-tocircumneutral wastewaters (Kanematsu et al, 2014). The first oxidized alteration phase from the weathering of synthetic or natural UO 2 (s) is typically a simple oxyhydroxide, either schoepite ((UO 2 ) 8 O 2 (OH) 12 Á12H 2 O) or metaschoepite ((UO 2 ) 4 O(OH) 6 Á5H 2 O) (Finch and Ewing, 1992).…”
Section: Introductionmentioning
confidence: 99%
“…8-10H 2 O) and soddyite (UO 2 ) 2 SiO 4 . 2H 2 O) (Buck et al 1996;Morris et al 1996). These solids in particular, the U-phosphates, are often difficult to leach (Buck et al 1996;Morris et al 1996).…”
mentioning
confidence: 99%
“…2H 2 O) (Buck et al 1996;Morris et al 1996). These solids in particular, the U-phosphates, are often difficult to leach (Buck et al 1996;Morris et al 1996). Due to the heterogeneous nature of soil and sediment materials, and the possible formation of numerous slightly soluble U solids, leach-based remediation is often less efficient than that observed for U ore bodies.…”
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confidence: 99%
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