Crystal Face Distributions and Surface Site Densities of Two Synthetic Goethites: Implications for Adsorption Capacities as a Function of Particle Size

被引:31
作者
Livi, Kenneth J. T. [1 ]
Villalobos, Mario [2 ]
Leary, Rowan [3 ]
Varela, Maria [4 ,6 ,7 ]
Barnard, Jon [3 ]
Villacis-Garcia, Milton [2 ]
Zanella, Rodolfo [5 ]
Goodridge, Anna [1 ]
Midgley, Paul [3 ]
机构
[1] Johns Hopkins Univ, Dept Mat Sci & Engn, Baltimore, MD 21218 USA
[2] Univ Nacl Autonoma Mexico, Environm Biogeochem Grp, Geochem Dept, Inst Geol, Cu 04510, Cdmx, Mexico
[3] Univ Cambridge, Dept Mat Sci & Met, 27 Charles Babbage Rd, Cambridge CB3 0FS, England
[4] Oak Ridge Natl Lab, Mat Sci & Technol Div, Oak Ridge, TN 37831 USA
[5] Univ Nacl Autonoma Mexico, Ctr Ciencias Aplicadas & Desarrollo Tecnol CCADET, Cu 04510, Cdmx, Mexico
[6] Univ Complutense Madrid, Dept Fis Mat, E-28040 Madrid, Spain
[7] Univ Complutense Madrid, Inst Pluridisciplinar, E-28040 Madrid, Spain
基金
欧洲研究理事会;
关键词
ALPHA-FEOOH NANORODS; ELECTRON TOMOGRAPHY; AGGREGATION; DISSOLUTION; MECHANISMS; CARBONATE; ARSENATE; PROTON; MODEL;
D O I
10.1021/acs.langmuir.7b01814
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Two synthetic goethites of varying crystal size distributions were analyzed by BET, conventional TEM, cryo-TEM, atomic resolution STEM and HRTEM, and electron tomography in order to determine the effects of crystal size, shape, and atomic scale surface roughness on their adsorption capacities. The two samples were determined by BET to have very different site densities based on Cr-VI adsorption experiments. Model specific surface areas generated from TEM observations showed that, based on size and shape, there should be little difference in their adsorption capacities. Electron tomography revealed that both samples crystallized with an asymmetric {101} tablet habit. STEM and HRTEM images showed a significant increase in atomic-scale surface roughness of the larger goethite. This difference in roughness was quantified based on measurements of relative abundances of crystal faces {101} and {201} for the two goethites, and a reactive surface site density was calculated for each goethite. Singly coordinated sites on face {210} are 2.5 more dense than on face {101}, and the larger goethite showed an average total of 36% {210} as compared to 14% for the smaller goethite. This difference explains the considerably larger adsorption capacitiy of the larger goethite vs the smaller sample and points toward the necessity of knowing the atomic scale surface structure in predicting mineral adsorption processes.
引用
收藏
页码:8924 / 8932
页数:9
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