The infrared spectrum of synthetic akaganeite, β-FeOOH

被引:99
作者
Murad, E
Bishop, JL
机构
[1] Bayer Geol Landesamt, D-95615 Marktredwitz, Germany
[2] NASA, Ames Res Ctr, Search Extraterr Intelligence Inst, Moffett Field, CA 94035 USA
关键词
D O I
10.2138/am-2000-5-609
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Fourier-transform infrared spectra of a synthetic akaganeite, beta-FeOOH, were acquired in transmittance, attenuated total reflectance (ATR) and diffuse reflectance. The transmittance spectra showed a distinct dependence on the mode of sample preparation: measurements taken on pellets prepared by pressing the sample with alkali halides (KBr or CsI) displayed bands at 1096, 1050, and 698 cm(-1) that were not observed in spectra of the neat material and must therefore be considered artifacts. Variations in the sampling environment (e.g., water and/or organic volatiles) were also observed to exert a noticeable influence on the development of the IR spectra. Infrared bands due to akaganeite were found at 3480 + 3390 (doublet), 1630, 850 + 820 (doublet), 650, 490, and similar to 420 cm(-1). Diffuse reflectance spectra dominated by volume scattering (loose), diffuse reflectance spectra comprised of both volume and surface scattering (compacted), ATR spectra (surface only), and transmittance spectra (absorbance only, inverse of ATR) showed compatible trends for the akaganeite features both above and below similar to 1000 cm(-1). This indicates that the multiple akaganeite measurements are consistent and confirms the band assignments.
引用
收藏
页码:716 / 721
页数:6
相关论文
共 31 条
[1]  
BISHOP JL, 1996, MINERAL SPECTROSCOPY
[2]   NATURE OF IRON IN AKAGANEITE (BETA-FEOOH) [J].
CHILDS, CW ;
GOODMAN, BA ;
PATERSON, E ;
WOODHAMS, FWD .
AUSTRALIAN JOURNAL OF CHEMISTRY, 1980, 33 (01) :15-26
[3]  
ELLIS J, 1976, CHIMIA, V30, P141
[4]   STRUCTURAL-CHANGES IN BETA-FEOOH CAUSED BY RADIATION-DAMAGE [J].
GALBRAITH, ST ;
BAIRD, T ;
FRYER, JR .
ACTA CRYSTALLOGRAPHICA SECTION A, 1979, 35 (JAN) :197-200
[5]   ATOMIC STRUCTURE OF TUBULAR SUBCRYSTALS OF BETA IRON(III) OXIDE HYDROXIDE [J].
GALLAGHER, KJ .
NATURE, 1970, 226 (5252) :1225-+
[6]   THE POROUS STRUCTURE OF SYNTHETIC AKAGANEITE [J].
GONZALEZCALBET, JM ;
ALARIOFRANCO, MA ;
GAYOSOANDRADE, M .
JOURNAL OF INORGANIC & NUCLEAR CHEMISTRY, 1981, 43 (02) :257-264
[7]   STRUCTURAL-PROPERTIES OF PRECIPITATES FORMED BY HYDROLYSIS OF FE3+ IONS IN AQUEOUS-SOLUTIONS CONTAINING NO3(-) AND CL- IONS [J].
GOTIC, M ;
POPOVIC, S ;
LJUBESIC, N ;
MUSIC, S .
JOURNAL OF MATERIALS SCIENCE, 1994, 29 (09) :2474-2480
[8]  
HENDEL B, 1981, J INFORM REC MATER, V9, P381
[9]   BETA-FEOOH.CLN (AKAGANEITE) AND FE1-XO (WUSTITE) IN HOT BRINE FROM THE ATLANTIS-II DEEP (RED-SEA) AND THE UPTAKE OF AMINO-ACIDS BY SYNTHETIC BETA-FEOOH.CLN [J].
HOLM, NG ;
DOWLER, MJ ;
WADSTEN, T ;
ARRHENIUS, G .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1983, 47 (08) :1465-1470
[10]   FOURIER-TRANSFORM INFRARED-SPECTROSCOPY OF COLLOIDAL ALPHA-FERRIC, BETA-FERRIC AND GAMMA-FERRIC OXIDE HYDROXIDES [J].
ISHIKAWA, T ;
NITTA, S ;
KONDO, S .
JOURNAL OF THE CHEMICAL SOCIETY-FARADAY TRANSACTIONS I, 1986, 82 :2401-2410