Structure of synthetic 2-line ferrihydrite by electron nanodiffraction

被引:120
作者
Janney, DE
Cowley, JM
Buseck, PR
机构
[1] Arizona State Univ, Dept Geol, Tempe, AZ 85287 USA
[2] Arizona State Univ, Dept Chem Biochem, Tempe, AZ 85287 USA
[3] Arizona State Univ, Dept Phys & Astron, Tempe, AZ 85287 USA
关键词
D O I
10.2138/am-2000-8-910
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
Comparison of experimental single-crystal electron diffraction patterns of synthetic two-line ferrihydrite (2LFh) with simulated single-crystal electron-diffraction patterns indicates that a synthetic 21,Fh sample contains highly disordered material and nanocrystals with structures based on hexagonal (ABAB) and cubic (ABC) stacking of close-packed layers of O2- and OH- ions. An apparently continuous variation in ordering exists between the highly disordered material and each of the crystalline structures, suggesting that both nanocrystalline structures represent local extremes of three-dimensional ordering. Experimental diffraction patterns were obtained using electron nanodiffraction, a technique in which the finely focused beam from a field-emission gun in an electron microscope can be used to produce diffraction patterns from areas <1 nm across. Nanodiffraction patterns from the highly disordered material have diffuse streaks rather than distinct reflections, and are consistent with a two-dimensional structure that consists of close-packed anionic layers with essentially complete stacking disorder and nearly random distribution of Fe atoms. The structure with cubic stacking is similar to maghemite and has similar to 25% of the Fe in tetrahedral sites. The structure with hexagonal stacking consists of double chains of face-sharing Fe octahedra; each octahedron shares one face, two edges, and three corners with adjacent octahedra. Previous results from transmission electron microscopy, powder X-ray and electron diffraction, and synchrotron-based techniques reflect the overall high degree of structural disorder rather than the characteristics of the maghemite-like and double-chain structures.
引用
收藏
页码:1180 / 1187
页数:8
相关论文
共 34 条
[1]  
BIRCH WD, 1993, AM MINERAL, V78, P827
[2]  
BLAKE RL, 1966, AM MINERAL, V51, P123
[3]   NATURAL FERRIHYDRITES IN SURFACE DEPOSITS FROM FINLAND AND THEIR ASSOCIATION WITH SILICA [J].
CARLSON, L ;
SCHWERTMANN, U .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1981, 45 (03) :421-429
[4]   FORMATION OF FERRIC OXIDES FROM AQUEOUS-SOLUTIONS - A POLYHEDRAL APPROACH BY X-RAY ABSORPTION-SPECTROSCOPY .2. HEMATITE FORMATION FROM FERRIC GELS [J].
COMBES, JM ;
MANCEAU, A ;
CALAS, G .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1990, 54 (04) :1083-1091
[5]   FORMATION OF FERRIC OXIDES FROM AQUEOUS-SOLUTIONS - A POLYHEDRAL APPROACH BY X-RAY ABSORPTION-SPECTROSCOPY .1. HYDROLYSIS AND FORMATION OF FERRIC GELS [J].
COMBES, JM ;
MANCEAU, A ;
CALAS, G ;
BOTTERO, JY .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1989, 53 (03) :583-594
[6]  
Cornell R. M., 1996, The iron oxides: structure, properties, reactions, occurrence and uses.
[7]  
Cowley JM, 1998, ADV MET SEM, V4, P67
[8]   CONFIGURED DETECTORS FOR STEM IMAGING OF THIN SPECIMENS [J].
COWLEY, JM .
ULTRAMICROSCOPY, 1993, 49 (1-4) :4-13
[9]  
COWLEY JM, 1971, ACTA CRYSTALLOGR A, V29, P529
[10]   STRUCTURAL MODEL FOR FERRIHYDRITE [J].
DRITS, VA ;
SAKHAROV, BA ;
SALYN, AL ;
MANCEAU, A .
CLAY MINERALS, 1993, 28 (02) :185-207