Details
Originalsprache | Englisch |
---|---|
Seiten (von - bis) | 253-262 |
Seitenumfang | 10 |
Fachzeitschrift | Journal of Contaminant Hydrology |
Jahrgang | 102 |
Ausgabenummer | 3-4 |
Publikationsstatus | Veröffentlicht - 7 Sept. 2008 |
Extern publiziert | Ja |
Abstract
Europium(III) was coprecipitated with the clay mineral hectorite, a magnesian smectite, following a multi-step synthesis procedure. Different Eu(III) species associated with the proceeding synthetic hectorite were characterized by selectively exciting the 5D0→7F0 transition at low temperature (T < 20 K). Fluorescence decay times indicated that Eu(III) ions may be incorporated in the octahedral layer of the brucite precursor as well as in the octahedral sheet of the clay mineral. The excitation spectra indicated that the substitution of the divalent Mg by the trivalent Eu induced local structural deformation. This investigation implements the molecular-level understanding of the f element structural incorporation into the octahedral layer of sheet silicates by coprecipitation with clay minerals from salt solutions at 100 °C.
ASJC Scopus Sachgebiete
- Umweltwissenschaften (insg.)
- Umweltchemie
- Umweltwissenschaften (insg.)
- Gewässerkunde und -technologie
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in: Journal of Contaminant Hydrology, Jahrgang 102, Nr. 3-4, 07.09.2008, S. 253-262.
Publikation: Beitrag in Fachzeitschrift › Artikel › Forschung › Peer-Review
}
TY - JOUR
T1 - TRLFS characterization of Eu(III)-doped synthetic organo-hectorite
AU - Finck, Nicolas
AU - Stumpf, Thorsten
AU - Walther, Clemens
AU - Bosbach, Dirk
PY - 2008/9/7
Y1 - 2008/9/7
N2 - Europium(III) was coprecipitated with the clay mineral hectorite, a magnesian smectite, following a multi-step synthesis procedure. Different Eu(III) species associated with the proceeding synthetic hectorite were characterized by selectively exciting the 5D0→7F0 transition at low temperature (T < 20 K). Fluorescence decay times indicated that Eu(III) ions may be incorporated in the octahedral layer of the brucite precursor as well as in the octahedral sheet of the clay mineral. The excitation spectra indicated that the substitution of the divalent Mg by the trivalent Eu induced local structural deformation. This investigation implements the molecular-level understanding of the f element structural incorporation into the octahedral layer of sheet silicates by coprecipitation with clay minerals from salt solutions at 100 °C.
AB - Europium(III) was coprecipitated with the clay mineral hectorite, a magnesian smectite, following a multi-step synthesis procedure. Different Eu(III) species associated with the proceeding synthetic hectorite were characterized by selectively exciting the 5D0→7F0 transition at low temperature (T < 20 K). Fluorescence decay times indicated that Eu(III) ions may be incorporated in the octahedral layer of the brucite precursor as well as in the octahedral sheet of the clay mineral. The excitation spectra indicated that the substitution of the divalent Mg by the trivalent Eu induced local structural deformation. This investigation implements the molecular-level understanding of the f element structural incorporation into the octahedral layer of sheet silicates by coprecipitation with clay minerals from salt solutions at 100 °C.
KW - Coprecipitation
KW - Europium
KW - Incorporation
KW - Smectite
KW - TRLFS
UR - http://www.scopus.com/inward/record.url?scp=56949088382&partnerID=8YFLogxK
U2 - 10.1016/j.jconhyd.2008.08.003
DO - 10.1016/j.jconhyd.2008.08.003
M3 - Article
C2 - 18845359
AN - SCOPUS:56949088382
VL - 102
SP - 253
EP - 262
JO - Journal of Contaminant Hydrology
JF - Journal of Contaminant Hydrology
SN - 0169-7722
IS - 3-4
ER -