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The Meta object is used to insert tags that provide information for the Web server through the HTTP-equiv attribute, and to include other overall data that you want in your Web page but not made visible to the casual browser. Some Web pages, for example, have built-in expiration dates after which the content is to be considered outmoded. In Dreamweaver, you can use the Meta object to insert a wide range of descriptive data. You can access the Meta object in the Head menu in the Common category of the Insert panel or via the Insert menu by choosing Insert HTML Head Tags Meta. As with all the Head objects, you don t have to have the Head Content visible to insert the Meta object; although you do have to choose View Head Content if you want to edit the object. To insert a Meta object, follow these steps:

There s a good reason not to move string data out of the resource files and into the static data area. CE provides us with a special version of the LoadString() function used to load string resources that allows you to read the string in place. Calling LoadString() like this returns a pointer to the string:

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Figure 16.11shows the factor graph correspondingto aparticular turbo code; see Figure 14.2 for the encoding framework. The form of the graph makes the decoding algorithm clear: the forwardbackward message passing algorithm is used on the first encoder. The resulting messages are interleaved and passed in to the other decoder, where the forwardhackward message passing is again performed. The graph typically has loops in it, through the interleaver, so the decoding algorithm is not exact.

the load and the exural rigidity of the lithosphere. The latter, in turn, is dependent on the effective elastic thickness of the lithosphere, Te (Section 2.11.4). Thus, if the magnitude of the load can be calculated and the amount of exure determined, Te may be deduced. However as indicated above (Section 2.11.6), Te may be determined more generally from the spectral analysis of gravity and topographic data. Results obtained by applying this technique to oceanic areas are very consistent. They reveal that the elastic thickness of oceanic lithosphere is invariably less than 40 km and decreases systematically towards oceanic ridges (Watts, 2001) (Fig. 2.38). By contrast, the results obtained for continental areas vary from 5 to 110 km, the highest values being obtained for the oldest areas the Precambrian cratons. However, McKenzie (2003) maintains that if there are sub-surface density contrasts that have no topographic expression, so-called buried or hidden loads, the technique yields an overestimate of the elastic thickness. Such loads are thought to be more common in continental areas, particularly in the cratons, because of their thick and rigid lithosphere. In oceanic areas loads are typically super-

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In the example discussed here, the oxidation was performed using an O2 -plasma (for more details see Ref. [49]): after the oxidation the static contact angle was below 5 . The very good hydrophilicity suggests the presence of hydroxyl groups at the surface, which are among the most hydrophilic of the O-groups. Fluorescence microscopy with uorescent probes reacting selectively with the hydroxyl groups can be used to assess the availability as well as the reactivity of hydroxyl groups at the surface of O-terminated UNCD lms. The uorescence image in Figure 16.11(a) demonstrates the speci c reactivity of

single symbol might have multiple bits in error - it still is a single symbol error from the perspective of the RS decoder. A single symbol might have up to m bits in error. Under the best of circumstances then, when all the errors affect adjacent bits of a symbol, a RS code may correct up to mt bits in error. This means that RS codes are naturally effective for transmitting over bursty binary channels: since bursts of errors tend to cluster together, there may be several binary errors contributingto a single erroneous symbol. As an example [203, p. 2781, a burst of length 3m 1 cannot affect more than 4 symbols, so a RS code capable of correcting 4 errors can correct any burst of length 3m 1. Or any burst of length m 1 cannot affect more than two bytes, so the 4-error correcting code could correct up to two bursts of length m 1. In general, a t-error correcting RS code over GF(2'") can correct any combination of t 1 U m - 2)/mJ

(gr-1

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Attaching XML data to an XSLT page is just as straightforward as converting the page:

precious = create_masterpiece() location = ask_user() begin File.open(location, w ) do |file| save_work(file, precious)

Summary