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Weighted average orientation

The susceptibility tensors give the correct relationship for the macroscopic material. For individual molecules, the polarizability a, hyperpolarizability P, and second hyperpolarizability y, can be defined they are also tensor quantities. The susceptibility tensors are weighted averages of the molecular values, where the weight accounts for molecular orientation. The obvious correspondence is correct, meaning that is a linear combination of a values, is a linear combination of P values, and so on. [Pg.256]

Advanced materials systems based on polymers, ceramics, and composites are constmcted by assembling components to create stmctures whose properties and performance are determined by the form, orientation, and complexity of the composite stmcture. The properties of these assemblages are determined not by the sum of weighted averages of the components but rather by synergistic effects in intercoimected phases. For this reason, the study of fabrication of hierarchical assemblages of materials, as well as the study of mechanisms for repairing defects in assembled stmctures, must be supported by fundamental research. [Pg.88]

Thus, for the general case of a delocalized electron spin, the anisotropic components depend upon the orientation-weighted spatial average of... [Pg.506]

There are three conceivable rotamers for each diastereomer with different relative orientations of the substituents at the atoms C-l and C-2 (for assigning the stereochemical descriptors the fragment L1-C1-C2-L2 is taken as the longest zig-zag chain)368. The experimental NMR parameters, e.g., 3/h,h> are weighted average values ... [Pg.337]

Fig. 46. Tensile strength of highly oriented polyethylene at Young s modulus = 50 GPa versus weight average molecular weight for various polydispersities (indicated in graph). With permission of the publishers John Wiley Sons. Inc. (C)... Fig. 46. Tensile strength of highly oriented polyethylene at Young s modulus = 50 GPa versus weight average molecular weight for various polydispersities (indicated in graph). With permission of the publishers John Wiley Sons. Inc. (C)...
We compare the orientational relaxation of central deuterated part of the PS HDH 188 copoljraer with that of the end part of the PS DH 184 copolymer. Both types of chains have almost the same molecular weight as well as deuterated blocks of comparable length. The master curves of the orientational relaxation average (calculated as the weight average of the measured orientation of each block) can be superimposed as shown in Figure 1. [Pg.44]

For these first experiments, a temperature relatively close to Tg, T=123°C, was chosen with the intention of minimizing the relaxation of stress and chain orientation during the quenching the weight-average relaxation time of sample SI at 123°C is calculated from that at 140°C and the thermal shift factor between 123°C and 140°C Xw(123°C) 380s. On the other hand the cooling time of the stretched specimens can be estimated to a few seconds [19], which is very small compared to the polymer relaxation time at the temperature of the experiments. [Pg.73]

The decomposition of the anisotropic perturbative potential 4>p (7) into its isotropic and anisotropic part suits as an excellent method to include this potential into the formalism. By [14] the separation of the isotropic part weighted averaging s(ri2) = (< p(ri2, Consequently, the molecular DFT approach regards the... [Pg.102]

Figure 27. Analysis of polarized EXAFS data, (a) EXAFS radial structure functions for irom oxide precipitates on quartz single crystal surfaces, r and m refer to the (1011 )and (1120) surface planes of quartz. The parallel and perpendicular refer to the polarization direction of the X-ray beam and thus the probe direction of the EXAFS scattering process, (b) Raw polarized EXAFS and fits for the same samples in (a), (c) Polarized stracture function simulations. Top radial stracture function for a single Fe atom within a 50-atom hematite crystal with [0001] orientation. Middle Same for 20-atom crystal. Bottom Weighted average of all Fe stracture func-tions in the 20-atom crystal. The analysis suggests highly textrrred hematite-like nanocrystals on the quartz surface but no epitaxial relationship. From Waychunas et al. (1999). Figure 27. Analysis of polarized EXAFS data, (a) EXAFS radial structure functions for irom oxide precipitates on quartz single crystal surfaces, r and m refer to the (1011 )and (1120) surface planes of quartz. The parallel and perpendicular refer to the polarization direction of the X-ray beam and thus the probe direction of the EXAFS scattering process, (b) Raw polarized EXAFS and fits for the same samples in (a), (c) Polarized stracture function simulations. Top radial stracture function for a single Fe atom within a 50-atom hematite crystal with [0001] orientation. Middle Same for 20-atom crystal. Bottom Weighted average of all Fe stracture func-tions in the 20-atom crystal. The analysis suggests highly textrrred hematite-like nanocrystals on the quartz surface but no epitaxial relationship. From Waychunas et al. (1999).
Polycrystalline surfaces result from a mixing of all possible crystal orientations. From an energetic point of view, the low index faces discussed above predominate. The work function of the polycrystalline surface reflects a weighted average of the work functions for each crystallographic orientation. In the case of face-centered cubic systems, it falls between that of the (110) and (100) single crystal surfaces. Since polycrystalline metals are involved in most practical applications, the effect of surface structure on the work function is not discussed further here. More information on this topic is available in reviews by Trasatti [G3, 5]. [Pg.401]

The limit of nearly free relative orientations is not of much physical interest in the case of electrostatic forces. The intermolecular interaction is a Boltzmann-weighted average of the form... [Pg.24]

Figure 22. GI-EXAFS model Fourier transform functions for Fe3+ sorption on quartz as small precipitates. Top 47 atom hematite-like cluster with [0001] direction normal to surface plane. Middle analogous 21 atom cluster. Bottom weighted 21 atom cluster, where the EXAFS for each Fe ion has been individually calculated and added as a weighted average. This gives best agreement with observations indicating oriented clusters of average 0.9 nm diameter. Figure 22. GI-EXAFS model Fourier transform functions for Fe3+ sorption on quartz as small precipitates. Top 47 atom hematite-like cluster with [0001] direction normal to surface plane. Middle analogous 21 atom cluster. Bottom weighted 21 atom cluster, where the EXAFS for each Fe ion has been individually calculated and added as a weighted average. This gives best agreement with observations indicating oriented clusters of average 0.9 nm diameter.

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See also in sourсe #XX -- [ Pg.303 ]




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Orientation average

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