CCl4 chemistry on the magnetite selvedge of single-crystal hematite:: competitive surface reactions

被引:29
作者
Adib, K
Camillone, N
Fitts, JP
Rim, KT
Flynn, GW
Joyce, SA
Osgood, RM
机构
[1] Columbia Univ, Dept Appl Phys & Appl Math, Mat Sci Program, New York, NY 10027 USA
[2] Columbia Univ, Environm Mol Sci Inst, New York, NY 10027 USA
[3] Pacific NW Natl Lab, Environm Mol Sci Lab, Richland, WA 99352 USA
基金
美国国家科学基金会;
关键词
molecule-solid reactions; thermal desorption spectroscopy; surface chemical reaction; surface relaxation and reconstruction; iron oxide; single crystal surfaces;
D O I
10.1016/S0039-6028(01)01635-1
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Temperature programmed reaction/desorption (TPR/D) studies were undertaken to characterize the surface chemistry which occurs between CCl4 and the Fe3O4 (111) selvedge of single crystal alpha-Fe2O3 (0 0 0 1). Six separate desorption events are clearly observed and four desorbing species are identified: CO4, OCCl2, C2O4 and FeCl2. It is proposed that OCCl2, CCl4 and C2O4 are produced in reactions involving the same precursor, CCl2. Three reaction paths compete for the CCl2 precursor: oxygen atom abstraction (for OCCl2,), molecular recombinative desorption (for CCl4) and associative desorption (for C2Cl4). During the TPR/D temperature ramp, the branching ratio is observed to depend upon temperature and the availability of reactive sites. The data are consistent with a rich site-dependent chemistry. (C) 2001 Published by Elsevier Science B.V.
引用
收藏
页码:127 / 138
页数:12
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