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We have calculated the sulphur 1s near edge X-roy absorption fine structure (NEX-AFS) spectra of SO2 adsorbed on Pd( 111 ) in terms of the multiple-scattering Cluster(MSC) method. The origin of the resonances in the NEXAFS spectra has been re-xealed. By the MSC calculation and a (DV)-Xα study we have for the first time iden-tiffed two weak features existing in S K-edge NEXAFS of SO2/Pd(111) system, whichare attributed to the interaction between the adsorbate and the substrate. Moreover,MSC calculation together with the reliability factor (R-.factor) analysis are employedto determine the local adsorption structures. These results are broadly in agreementwith those of Fourier-transform analysis of the surface extended X-ray absorption finestructure (SEXAFS).

参考文献

[1] A Guitiérrez Sosa;J F Walsh;C A Muryn;P Finetti,G Thornton .[J].Surface Science Letters,1996,364:L519.
[2] P Zhu;J C Tang;J P He .[J].Chemical Physics and Physical Chemistry,2000,2:1123.
[3] G J Jackson;J Liidecke;S M Driver;D P Woodruff R G Jones A Chan .[J].Surface Science Spectra,1997,389:223.
[4] S Cao;J C Tang;P Zhu;L Wang .[J].Journal of Physics:Condensed Matter,2001(13):5865.
[5] S. Terada;T. Yokoyama;M. Sakano;M. Kiguchi;Y. Kitajima;T. Ohta .Asymmetric surface structure of SO_2 on Pd(111) studied by total-reflection X-ray absorption fine structure spectroscopy[J].Chemical Physics Letters,1999(5/6):645-650.
[6] J Stohr.NEXAFS Spectroscopy[M].Springer,Berlin,1992
[7] J C Tang;X S Feng;J F Shen;T Fujikawa,T Okazawa .[J].Physical Review B,1991,44:13018.
[8] J C Tang;S B Fu;H Ji;Y B Chen .[J].中国科学A辑(英文版),1992(35):965.
[9] L Wang;F Zhuang;J C Tang .[J].Surface Science Spectra,1999,436:91.
[10] P Zhu;J C Tang;J P He .[J].Journal of Physical Chemistry B,2000(104):10597.
[11] J B Pendry .[J].Journal of Physics C:Solid State Physics,1980(13):937.
[12] B Song;H Nakamatsu;R Sekine;T Mukoyama,K Taniguchi .[J].Journal of Physics:Condensed Matter,1998(10):9113.
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