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Reconstruction of surface

FIGURE 2.3 Burwell mechanism for hydrogenation of alkynes showing reconstruction of surface Pd atom.31... [Pg.34]

The first successful first-principle theoretical studies of the electronic structure of solid surfaces were conducted by Appelbaum and Hamann on Na (1972) and A1 (1973). Within a few years, first-principles calculations for a number of important materials, from nearly free-electron metals to f-band metals and semiconductors, were published, as summarized in the first review article by Appelbaum and Hamann (1976). Extensive reviews of the first-principles calculations for metal surfaces (Inglesfeld, 1982) and semiconductors (Lieske, 1984) are published. A current interest is the reconstruction of surfaces. Because of the refinement of the calculation of total energy of surfaces, tiny differences of the energies of different reconstructions can be assessed accurately. As examples, there are the study of bonding and reconstruction of the W(OOl) surface by Singh and Krakauer (1988), and the study of the surface reconstruction of Ag(llO) by Fu and Ho (1989). [Pg.117]

During the preceding decade the theoretical research has also shifted, possibly as a result of detailed experimental findings. The emphasis is now on microscopic-level reconstruction of surfaces. Advanced surface diffraction and imaging techniques allow detailed characterization of surface morphology at an atomic level. These studies show that metal surfaces contain high concentrations of atomic steps, usually one atom in height, separated by well-ordered terraces. Statistical mechanical theories were developed to explain how atomic-scale processes can lead to the formation of these structures. [Pg.371]

Information about how the ocean circulated during the past is useful in understanding changes in ocean and atmospheric chemistry, changes in the fluxes of heat and freshwater between the ocean and atmosphere, and changes in global wind patterns. The circulation of surface waters in the ocean leaves an imprint on sea surface tempera-mre, and is also inextricably linked to the patterns of oceanic productivity. Much valuable information about past ocean circulation has been inferred from reconstructions of surface ocean temperarnre and productivity, which are covered in separate chapters. Here the focus is on the geochemical tracers that are used to infer the... [Pg.3280]

Die and the nutrient concentration in surface waters (Broecker and Maier-Reimer, 1992), such that even a perfect reconstruction of surface water 13c/12c Yould not provide direct information of surface-ocean nutrient status. In addition, the 13c/12c qP planktonic foraminiferal fossils found in surface sediments appears to be an imperfect recorder of the of DIC in modem surface... [Pg.3357]

Fig. 7. Reconstruction of surface ocean pH over glacial cycles based on 8"B (Honisch Hemming 2005). Fig. 7. Reconstruction of surface ocean pH over glacial cycles based on 8"B (Honisch Hemming 2005).
Atomic force microscopy, often abbreviated as AFM, is one of the elected techniques for fine surface and geometrical characterization. Atomic force microscopes provide three-dimensional reconstruction of surface topographies with subnanometer vertical and lateral resolution, over a range which is typically no larger than a few tens or hundreds of micrometers. [Pg.63]

Figure 2.35. Schematic illustration of the dependence of the surface energy on partial pressure. Surface (2) has surface atoms of lower coordination than surface (1), and hence is most reactive, pc is the partial pressure beyond which there is a driving force for reconstruction of surface (1) to surface (2). Figure 2.35. Schematic illustration of the dependence of the surface energy on partial pressure. Surface (2) has surface atoms of lower coordination than surface (1), and hence is most reactive, pc is the partial pressure beyond which there is a driving force for reconstruction of surface (1) to surface (2).
L. M. Eng, H. J. Giintherodt, G. A. Schneider, U. Kopke, and J. Munoz Saldana, Nanoscale reconstruction of surface crystaUography from three dimensional polarization distribution in ferro electric barium titanate ceramics, Appl Phys. Lett. 74,233 235 (1999). [Pg.19]

In addition to primitive algebraic surfaces, more general surfaces with a simple kinematic generation, such as sweep surfaces, revolved surfaces (rotation sweep), extrusion surfaces (translation sweep), pipe surfaces, are directly compatible to CAD models. Fitting those surfaces to segmented data points or mesh is critical to the reconstruction of surface models and support of parameterization (Lukacs et al., 1998). [Pg.165]

Reconstruction, of surface, 580 Redispersion, 248, 250. See also Peptization, Stability of sols Redistribution. See Reconstruction, of surface. Restructuring Reduced time, 678, 685, 688-689, 696 Reduction, 289 Reedmergnerite, 780 Reesterification. See Esterification Refractive index, 275, 465, 594 film, 790, 852 graded, 844-847 of partially sintered gels, 768 of silica, 766-767 of strontium silicate, 777, 779 silica xerogels, 581, 583... [Pg.458]

Not surprisingly, there are also adsorbate-induced chemical reconstructions of surfaces. A representative example is given in Figure 4.47a showing the result of Hthium adsorption on the Al(lOO) surface. By deposition of a total of 1 ML Li a c(2x2) superlattice results with Li atoms having substituted A1 atoms in a c(2x2) arrangement in both the top and the third layer, so that the Wood notation is Al(100)-c(2x2)-2Li [138]. Accordingly, the surface stoichiometry is as in the AlsLi... [Pg.89]


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See also in sourсe #XX -- [ Pg.315 ]

See also in sourсe #XX -- [ Pg.476 ]




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Reconstruction surface

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