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wavelength 532 nm. CS2 as reference material with the highest known Brillouin gain shows a much smaller threshold. The difference between stationary and nonstationary SBS re ection can be much more easily detected by the temporary pro les of the re ected light in comparison with the incident light as shown in Fig. 2.18. As can be seen from this gure showing two re ectivity situations with roughly the same energy re ectivity value in case of more stationary scattering as obtained for Freon-113 (tB 0.84 ns), the pulse of the re ected light is much more symmetric than nonstationary scattering in SF6 (tB 17.3 ns). The onset at the beginning of the re ectivity is just a small part of the pulse, and overall the re ected light is almost not delayed to the incident light. In the case of SF6, much more delay occurs. The onset of the re ected light occurs much later. Here the long lifetime of the SBS material is the prominent value causing this effect. Whereas the pulse seems to be delayed compared to the input pulse, the trailing edge of the re ected light is almost identical with the incident pulse.

for which ( , ) is on the line segment that joins the points (x0 , t0 ), and (x, t). Proof Omitted. The reader can now easily imagine that any attempt to apply this approach for m > 2 will be quite tedious. Thus, we shall not do this here. We will restrict ourselves to stating a few facts. Applying the method to m = 3 (i.e., the generation of third-order Runge Kutta methods) leads to algorithm coef cients satisfying six equations with eight unknowns. There will be 2 degrees of freedom as a consequence. Fourth-order Runge Kutta methods (i.e., m = 4) also possess two degrees of freedom, and also have a truncation error per step of O(h5 ). One such method (attributed to Runge) in common use is xn+1 = xn + where h [k1 + 2k2 + 2k3 + k4 ] , 6 (10.80)

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Figure 5-17: To change the size, shape, and hardness of the current brush, click its icon in the Options bar.

If this were not the case then a gap could develop between the ions which would stop the current being carried altogether. The relationship described in Equation 5.12 results in a zone sharpening effect. Ions which diffuse into a zone with higher mobility will be slowed because of the weaker electrical eld. Conversely, ions diffusing into a zone of

Figure 19-19: Click the Output Settings button in the Save For Web dialog box to uncover additional Web-related options.

1 where RIF is a fixed rate increase factor and its default value is also 16 . If NI s 1, no increase is allowed. The source simply makes sure ACR is no less than MCR but no more than ER,

Note that themes can also be internationalized just like labels. You can create a language-specific theme properties file by appending the language code to the theme name. This can be handy for internationalizing images. To serve a French logo, you d add another theme properties file and name it theme_fr .properties. This file s site.logo key can then point to a translated logo.

This example shows you how the pieces can fit together in a simple application. The next section delves deeper into the XSQL classes used programmatically. You will use these same classes when, in s 18 and 19, you develop custom action handlers and serializers.

B z = [ 0 0 O]B, 1 1 0 1 0

Table 1.2 (continued ) Identi ed Cause 1. Creates urban smog which is unsightly and presents a health hazard. Effects Relevance to Plastics

After you set polar tracking settings, discussed earlier in this chapter in the Polar tracking section, you can snap to increments along the polar angles you have set. When PolarSnap is on, the polar tooltip only shows distances in increments of the snap setting. When you see the distance you want, just click. PolarSnap makes it easy to draw accurately without having to type coordinates. To use PolarSnap, follow these steps: 1. Right-click the SNAP button on the status bar and click Settings to open the Drafting Settings dialog box with the Snap and Grid tab displayed, as just explained. 2. Check PolarSnap in the Snap type & style section of the dialog box (refer to Figure 4-18). 3. Type a number in the Polar Distance text box. 4. Click OK to close the dialog box. 5. Click SNAP on the status bar. Note that PolarSnap and Grid snap are mutually exclusive. If PolarSnap is on, the cursor will not snap to the grid. Used with polar tracking, PolarSnap is a powerful tool. Remember that you can polar track along orthogonal as well as other angles.

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Table 11.7 (continued )

Bear in mind that when you download a file from the FTP tab to the Files tab, the downloaded file replaces the file on your hard drive.

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