Abstract
Feldspar minerals are thermodynamically unstable in the
near-surface environment and their surfaces are well known to
react readily with aqueous solutions, leading to incongruent
dissolution at low pH values, but congruent dissolution at
neutral and high pH values. Interactions with mineral surfaces
are an important control on the environmental transport of
trace elements and detrital feldspars are abundant in soils and
sediments.
The interaction of U(VI) ions with the feldspar surface has
been studied. Sorption experiments with uranyl ion (UO2
2+) at
pH 2, 6 and 10 were carried out and measurable uptake,
generally through surface complex formation, was only found
at pH 6 and 10. Reacted surfaces were analysed by X-ray
photoelectron spectroscopy and secondary ion mass
spectrometry. At pH 6 and at an initial U(VI) concentration
above 21.0 μM, precipitation of a surface phase was observed
by atomic force and scanning electron microscopies, and this
was identified as becquerelite (Ca[UO2)3O2(OH)3]2.8H2O) by
grazing incidence X-ray diffraction. Secondary ion mass
spectrometry showed diffusion of uranium into the altered
surface layer.
near-surface environment and their surfaces are well known to
react readily with aqueous solutions, leading to incongruent
dissolution at low pH values, but congruent dissolution at
neutral and high pH values. Interactions with mineral surfaces
are an important control on the environmental transport of
trace elements and detrital feldspars are abundant in soils and
sediments.
The interaction of U(VI) ions with the feldspar surface has
been studied. Sorption experiments with uranyl ion (UO2
2+) at
pH 2, 6 and 10 were carried out and measurable uptake,
generally through surface complex formation, was only found
at pH 6 and 10. Reacted surfaces were analysed by X-ray
photoelectron spectroscopy and secondary ion mass
spectrometry. At pH 6 and at an initial U(VI) concentration
above 21.0 μM, precipitation of a surface phase was observed
by atomic force and scanning electron microscopies, and this
was identified as becquerelite (Ca[UO2)3O2(OH)3]2.8H2O) by
grazing incidence X-ray diffraction. Secondary ion mass
spectrometry showed diffusion of uranium into the altered
surface layer.
Original language | English |
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Title of host publication | GEOCHIMICA ET COSMOCHIMICA ACTA |
Publisher | Elsevier BV |
Pages | A160-A160 |
Number of pages | 1 |
Volume | 71 |
Edition | 15 Suppl.1 |
ISBN (Print) | 0016-7037 |
DOIs | |
Publication status | Published - Aug 2007 |
Event | 17th Annual V M Goldschmidt Conference - Cologne, Germany Duration: 19 Aug 2007 → 24 Aug 2007 https://www.geochemsoc.org/publications/geochemicalnews/gn134jan08/17thvmgoldschmidtconferenc |
Conference
Conference | 17th Annual V M Goldschmidt Conference |
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Country/Territory | Germany |
City | Cologne |
Period | 19/08/07 → 24/08/07 |
Internet address |
Keywords
- Geochemistry & Geophysics