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A standard encryption key for VOD is generated for all set top boxes. The key is changed frequently to avoid unauthorized access to contents. Some DRM implementations will change this key after a few hours; most DRM products will allow a personalized refresh time for the keys. Personal Video Recorder Encrypted content is sent to the set top box and the decryption key for the stream is encrypted using the public key of the set top box as per the digital certificate registered. Only that particular set top box will be able to decrypt the key to access the content, and, moreover, the DRM client will verify the content rights file linked to the movie to determine if there are limits to the number of times the movie can be watched and if there is a time restriction to block access to the movie.

Notes: 1 Observers were asked to pay attention to message duration, response latency, pauses, non uencies, self adaptors and hand gestures; 2 Observers were asked to pay attention to speech errors, pauses, response latency and message duration; 3 Observers

The setLinkTag() function that is called is a local one that reads the new value in the current text box and sets it equal to the corresponding attribute.

can be applied. This is relatively easy to do by the holographic technique of mixing two mutually coherent plane waves on the emulsion. The effective exposure on the

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This security clearly needed to be hedged with options. An optionbased hedge would have provided interest rate protection while controlling for changes in the dollar price of the security. Additionally, even the model that assumed a fast prepayment rate underestimated the actual negative convexity of the security. An option hedge would have been the only type of effective hedge, as any losses on the security due to an unexpected increase in volatility would have been offset by a pro t on the option hedge. As the security paid off in January 1999, this hedging strategy was the only effective one.

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Figure 32-7: Any changes made to a template can be automatically applied to the template s associated files by using the Update Pages command.

4 cup (50 ml) lemon juice (juice of one large lemon) 3 cloves garlic, minced 1 tbsp (15 ml) lemon zest 1 tsp (5 ml) cumin

Conclude that F (z) > 0 whenever z = 0, using the fact that the function n itk x x zk is analytic. k=1 e (b) Deduce that under the hypotheses in part (a), Rice formulas can be applied on any compact interval I and for any k = 1, 2, . . . . 3.5. Assume that the process {X(t) : t R} veri es the hypotheses of Exercise 3.4(a) and moreover, that its paths are C k -functions, k an integer, k 1. Then, for any choice of distinct parameter values t1 , . . . ., tn , the joint distribution of the random variables X(t1 ), . . . ., X(tn ), X (t1 ), . . . , X (tn ), . . . ., X(k) (t1 ), . . . , X(k) (tn ) does not degenerate. Hint: Use the same method as in Exercise 3.4.

Anterior positioning appliances have been shown to reduce TMJ pain, muscle pain, and TMJ noise for many patients. Stabilization appliances similarly improve TMD symptoms for most patients, even if their pain is related to a disccondyle mechanical disturbance or intermittent locking at the opening where the noise occurs.

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Mesozoic Sevier thrust belt (Fig 712) This deformation created a thick pile of weak sedimentary rocks that has contributed to a delocalization of strain (Section 761) during Cenozoic extension (Sonder & Jones, 1999) Some estimates place parts of the province at a pre-rift crustal thickness of 50 km, similar to that of the unextended Colorado Plateau (Parsons et al, 1996) Others have placed it at more than 50 km (Coney & Harms, 1984) This pre-extensional history is one of the most important factors that has contributed to a heterogeneous style of extensional deformation in the Basin and Range The uniformity in size and spacing of normal faults in the Basin and Range, and the apparent uniform thickness of the seismogenic layer, at rst suggests that strain and crustal thinning, on average, might also be uniformly distributed across the province.

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