Stability of U(VI) solid phases in the U(VI)-Ca2+-SiO2-OH system

Verfasser / Beitragende:
[B. Ritherdon, C. Phelps, H. Neff, A.G. Sowder, S.B. Clark]
Ort, Verlag, Jahr:
2003
Enthalten in:
Radiochimica Acta/International journal for chemical aspects of nuclear science and technology, 91/2/2003(2003-02-01), 93-96
Format:
Artikel (online)
ID: 378877038
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024 7 0 |a 10.1524/ract.91.2.93.19992  |2 doi 
035 |a (NATIONALLICENCE)gruyter-10.1524/ract.91.2.93.19992 
245 0 0 |a Stability of U(VI) solid phases in the U(VI)-Ca2+-SiO2-OH system  |h [Elektronische Daten]  |c [B. Ritherdon, C. Phelps, H. Neff, A.G. Sowder, S.B. Clark] 
520 3 |a Synthetic metaschoepite was altered at 70°C, for 30days in silicate solutions of varying compositions to study alteration reactions and to compare experimental observations with a thermodynamic model of stability of the uranyl minerals metaschoepite ([(UO2)8O2(OH)12](H2O)10), becquerelite (Ca[(UO2)3O2(OH)3]2(H2O)8), α-uranophane (Ca[(UO2)(SiO3OH)]2(H2O)5) and soddyite ((UO2)2(SiO4)· (H2O)2). Powder X-ray diffraction analysis, scanning electron microscopy and solution chemistry were used to monitor the alteration of the initial metaschoepite. In general, the secondary phases predicted by the thermodynamic model formed. However, an unexpected mineral (a calcium uranate) was observed above pH 8. Also, within the timeframe of these experiments, U(VI) silicate phases only formed at Si concentrations much higher than the lower field boundaries for uranophane and soddyite. 
540 |a © 2003 Oldenbourg Wissenschaftsverlag GmbH 
690 7 |a Laboratory techniques, experiments  |2 nationallicence 
690 7 |a Analytical chemistry  |2 nationallicence 
690 7 |a Inorganic chemistry  |2 nationallicence 
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