Detailed Information on Publication Record
2011
A Raman spectroscopic study of bukovskýite Fe2(AsO4)(SO4)(OH) . 7H2O, a mineral phase with significant role in arsenic migration
LOUN, Jan, Jiří ČEJKA, Jiří SEJKORA, Jakub PLÁŠIL, Milan NOVÁK et. al.Basic information
Original name
A Raman spectroscopic study of bukovskýite Fe2(AsO4)(SO4)(OH) . 7H2O, a mineral phase with significant role in arsenic migration
Authors
LOUN, Jan (203 Czech Republic, belonging to the institution), Jiří ČEJKA (203 Czech Republic), Jiří SEJKORA (203 Czech Republic, guarantor), Jakub PLÁŠIL (203 Czech Republic), Milan NOVÁK (203 Czech Republic, belonging to the institution), Ray Leslie FROST (36 Australia), Sara PALMER (36 Australia) and Eloise C. KEEFFE (36 Australia)
Edition
Journal of Raman Spectroscopy, 2011, 0377-0486
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10500 1.5. Earth and related environmental sciences
Country of publisher
United States of America
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 3.087
RIV identification code
RIV/00216224:14310/11:00055985
Organization unit
Faculty of Science
UT WoS
000293001000017
Keywords in English
bukovskyite; Raman spectroscopy; arsenate; sulfate; hydroxyl ions; molecular water
Změněno: 14/3/2012 08:15, prof. RNDr. Milan Novák, CSc.
Abstract
V originále
The Raman spectrum of bukovskyite [Fe2(3+)(OH)(SO4)(AsO4) . 7H2O] has been studied and compared with that of an amorphous gel containing specifically Fe, As and S, which is understood to be an intermediate product in the formation of bukovskyite. The observed bands are assigned to the stretching and bending vibrations of (SO4)2- and (AsO4)3- units, stretching and bending vibrations and vibrational modes of hydrogen-bonded water molecules, stretching and bending vibrations of hydrogen-bonded (OH)- ions and Fe3+ -(O,OH) units. The approximate range of O-H ... O hydrogen bond lengths was inferred from the Raman spectra. Raman spectra of crystalline bukovskyite and of the amorphous gel differ in that the bukovskyite spectrum is more complex, the observed bands are sharp and the degenerate bands of (SO4)2- and (AsO4)3- are split and more intense. Lower wavenumbers of delta H2O bending vibrations in the spectrum of the amorphous gel may indicate the presence of weaker hydrogen bonds compared to those in bukovskyite.
Links
MSM0021622412, plan (intention) |
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