首页 | 本学科首页   官方微博 | 高级检索  
     


Surface complexation studied via combined grazing-incidence EXAFS and surface diffraction: arsenate on hematite (0001) and (10-12)
Authors:Waychunas G  Trainor T  Eng P  Catalano J  Brown G  Davis J  Rogers J  Bargar J
Affiliation:(1) Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA;(2) University of Alaska Fairbanks, Fairbanks, AK 99775, USA;(3) CARS, Argonne National Laboratory, Argonne, IL 60637, USA;(4) Environmental Chemistry Division, Argonne National Laboratory, Argonne, IL 60637, USA;(5) Stanford University, Stanford, CA 94305, USA;(6) US Geological Survey, Menlo Park, CA 94025, USA;(7) Stanford Synchrotron Radiation Laboratory, Stanford, CA 94305, USA
Abstract:X-ray diffraction [crystal-truncation-rod (CTR)] studies of the surface structure of moisture-equilibrated hematite reveal sites for complexation not present on the bulk oxygen-terminated surface, and impose constraints on the types of inner-sphere sorption topologies. We have used this improved model of the hematite surface to analyze grazing-incidence EXAFS results for arsenate sorption on the c (0001) and r (10–12) surfaces measured in two electric vector polarizations. This work shows that the reconfiguration of the surface under moist conditions is responsible for an increased adsorption density of arsenate complexes on the (0001) surface relative to predicted ideal termination, and an abundance of “edge-sharing” bidentate complexes on both studied surfaces. We consider possible limitations on combining the methods due to differing surface sensitivities, and discuss further analysis possibilities using both methods. An erratum to this article can be found at
Keywords:Crystal truncation rod  GIXAFS  EXAFS  Surface structure  Hematite  Arsenate
本文献已被 PubMed SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号