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A cryogenic XPS study of Ce fixation on nanosized manganite and vernadite: Interfacial reactions and effects of fulvic acid complexation

Yu, Changxun, 1983- (författare)
Linnéuniversitetet,Institutionen för biologi och miljö (BOM)
Boily, Jean-François (författare)
Umeå universitet,Kemiska institutionen,Umeå University, Sweden
Shchukarev, Andrey (författare)
Umeå universitet,Kemiska institutionen,Umeå University, Sweden
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Drake, Henrik, 1979- (författare)
Linnéuniversitetet,Institutionen för biologi och miljö (BOM)
Song, Z. L. (författare)
Tianjin University, China
Hogmalm, Johan, 1979 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences,University of Gothenburg, Sweden
Åström, Mats E., 1963- (författare)
Linnéuniversitetet,Institutionen för biologi och miljö (BOM)
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 (creator_code:org_t)
Elsevier BV, 2018
2018
Engelska.
Ingår i: Chemical Geology. - : Elsevier BV. - 0009-2541 .- 1872-6836. ; 483, s. 304-311
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • This study investigated interfacial reactions between aqueous Ce(III) and two synthetic nanosized Mn (hydr-) oxides (manganite: gamma-MnOOH, and vernadite: delta-MnO2) in the absence and presence of Nordic Lake fulvic acid (NLFA) at circumneutral pH by batch experiments and cryogenic X-ray photoelectron spectroscopy (XPS). The surfaces of manganite and vernadite were negatively charged (XPS-derived loadings of (Na+ K)/Cl > 1) and loaded with 0.42-4.33 Ce ions nm(-2). Manganite stabilized Ce-oxidation states almost identical to those for vernadite (approximately 75% Ce(IV) and 25% Ce(III)), providing the first experimental evidence that also a Mn (III) phase (manganite) can act as an important scavenger for Ce(IV) and thus, contribute to the decoupling of Ce from its neighboring rare earth elements and the development of Ce anomaly. In contrast, when exposed to Ce (III)-NLFA complexes, the oxidation of Ce by these two Mn (hydr-) oxides was strongly suppressed, suggesting that the formation of Ce(III) complexes with fulvic acid can stabilize Ce(III) even in the presence of oxidative Mn-oxide surfaces. The experiments also showed that Ce(III) complexed with excess NLFA was nearly completely removed, pointing to a strong preferential sorption of Ce(III)-complexed NLFA over free NLFA. This finding suggests that the Ce(III)-NLFA complexes were most likely sorbed by their cation side, i.e. Ce(III) bridging between oxide groups on the Mn (hydr-) oxides and negatively-charged functional groups in NLFA. Hence, Ce(III) was in direct contact with the oxidative manganite and vernadite but despite that not oxidized. An implication is that in organic-rich environments there may be an absence of Ce(IV) and Ce anomaly despite otherwise favorable conditions for Ce(III) oxidation.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Kemi -- Oorganisk kemi (hsv//swe)
NATURAL SCIENCES  -- Chemical Sciences -- Inorganic Chemistry (hsv//eng)

Nyckelord

Cryogenic XPS
Manganite
Vernadite
Oxidative scavenging
Ce anomaly
frozen hematite colloids
biogenic mn oxides
l-iii-edge
reaction-mechanism
gamma-mnooh
structure spectroscopy
organic-compounds
mn(ii) oxidation
chloride-ions
strain sg-1
Geochemistry & Geophysics
hindler pw
1990
reviews in mineralogy
v23
p281
Cryogenic XPS
Natural Science

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