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Triple exion response, 47 Triplegia, 50, 52 Trisalicylate, for pain, 124t Trismus, 1030 Trisomy 13, 864 Trisomy 18, 864 Trisomy 21, 863 Trochanteric bursitis, 171 Trochlear headache, 164 Trochlear nerve, lesions of, eye movements and, 230, 233 234 Trophic changes, in peripheral nerve disease, 1115 Tropias, 230 Tropical spastic paraparesis (TSP), 647 648, 1059 Troponin, 1094 Trunk muscles, weakness of, 1196 Trypanosomiasis, 344, 625 myopathy associated with, 1203 L-Tryptophan, peripheral neuropathy due to, 1134 Tsutsugamushi fever, 623 Tuberculomas, 611, 611f Tuberculosis, in HIV/AIDS, 647 Tuberculous meningitis, 609 611, 610f clinical features of, 610 laboratory studies in, 611 pathogenesis of, 610 pathologic ndings in, 610, 610f serous, 611 treatment of, 612 Tuberculous myelitis, 1071 Tuberculous spinal osteomyelitis (Pott disease), 1061, 1062f Tuberculum sella, meningioma of, 578 Tuberous sclerosis, 865 868 clinical manifestations of, 866 867, 867f course and prognosis of, 868 diagnosis of, 867, 868f epidemiology of, 866 etiology and pathogenesis of, 866 pathology of, 867, 868f treatment of, 868 Tullio phenomenon, 258 Tumors. See Brain tumors; Metastatic disease; Neoplasms; Paraneoplastic disorders; Spinal tumors; speci c tumors Turner syndrome, 864 Turricephaly, 853 Tussive syncope, 326 Twilight states, 356 Twitch-convulsive syndrome, uremic, 969 971 Two-point discrimination, testing of, 137

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You need only make a small change to the C# portion of the application that assigns the value of the TextBox to the Label control. Note that the only namespace used is System.

List of Commands for Web Templates (continued)

sional of small (and often closely held) rms, the goal of ownership is most frequently achieved by starting up a rm, whether as a sole proprietor or in collaboration with one or two others with common goals and ideally with complementary skills. About a thousand new rms start up each year.

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The righrhand sideof this equationis calledan indefiniteintegraL because limits of inthe tegrationare unspecified. previously This is in contrastto the definite integralsdiscussed in PartFive [compare (PT6.l0) with Eq. (17.5)]. Eq. An analyticalsolutionfor Eq. (PT6.l0) is obtained the irrdefinite if integralcan be evaluatedexactlyin equation fblnr. For this sinrple case, is possible do this witlr the result: it to r ' : - 0 . 5 1 4 * 4 . t 1 - 1 0 . 1+ 8 . 5 . r* C 2

To many algebra students, applications (word problems) seem impossible to solve. You might be surprised how easy solving many of them really is. If you follow the program in this chapter, you will nd yourself becoming a pro at solving word problems. Mastering the problems in this chapter will also train you to solve applied problems in science courses and in more advanced mathematics courses.

carrier and code signals. The tropospheric delay cannot be computed from the GPS observables; therefore, tropospheric e ects are compensated via models. For most users, especially in navigation application, the input parameters for the models are average or typical values for the user location. Users with higher accuracy requirements can add meteorological instruments to sense the model input variables or may use di erential GPS methods. The refractive index is a ected di erently by the water vapor and by the dry components (e.g., nitrogen and oxygen) of the troposphere, so tropospheric models account for these wet and dry pressures separately. The wet component is di cult to predict due to local variations in the water vapor content of the troposphere and accounts for approximately 10% of the tropospheric delay. The dry component is relatively easier to predict and accounts for approximately 90% of the tropospheric delay. Several models exist for the tropospheric wet and dry components [4, 104, 119, 122]. The models contain two parts. The rst part of the model is the estimate of the zenith delay. The second part is a slant factor to account for the satellite elevation. For example, the Chao model is dry Fdry wet Fwet T = = = = = 2.276 10 5 P 1 0.00143 sin(E) + tan(E)+0.0445 4.70 102 sin(E) + e1.46 e1.23 o + 1.705 106 o 3 T2 T 1

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