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Chat eld C (1970) Statistics for Technology Penguin: Maryland Checkland PB (1981) Systems Thinking, Systems Practice John Wiley: Chichester Chief Scienti c Advisor (undated) CSA Guidelines for Technical Scrutiny, Ministry of Defence Churchman CW and Wagner HM (1972) (compilers) Discussion of the ORSA Guidelines Management Science 18: B608 B629 Churchman CW, Ackoff RL and Arnoff EL (1957) Introduction to Operations Research John Wiley: New York Clark P and Chapman CB (1987) The development of computer software for risk analysis: a decision support system development study European Journal of Operational Research 29: 252 261 Clarke L (1994) The Essence of Change Prentice-Hall: Hemel Hempstead, UK Cleland DI (1984) Matrix Management Systems Handbook Van Nostrand Reinhold: New York Cleland DI and King WR (1988a) Project Management Handbook, 2nd edition Van Nostrand Reinhold: New York Cleland DI and King WR (1988b) Project owner strategic management of projects.

In Project Management Handbook, 2nd edition (eds DI Cleland and WR King) Van Nostrand Reinhold: New York, pp 165 188 Cleland DI, Bursic KM, Puerzer R and Vlasak AY (1998) Project Management Casebook Project Management Institute, Upper Darby, PA Coats PK and Chesser DC (1982) Coping with business risk through probabilistic nancial statements Simulation 44: 111 121 Collins English Dictionary (1986) Second edition, William Collins: London Cooke-Davis T (1996) Learning in a project-based organisation IPMA 96 World Congress on Project Management, Paris, June, pp 421 430..

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In 6, you removed quite a few things from the system and motherboard in order to prepare it for the projects in this and the previous chapter. For this particular project, however, there are a few more modifications to make on top of the ones you ve already done. 1. Start by desoldering and removing the two beige controller connector jacks from the corner of the board. These were identified in 6, and have seven leads each. 2. A thin strip of the main motherboard itself needs to go as well. Use your X-Acto knife to slice several deep grooves along the line of small holes seen in Figure 8-4. You can then snap this piece off the NES board. The removed portion should measure about 1/8 4-3/4 .

(2rnrn- 1).

Let c" denote the code generated by G. The code c" is equivalent to C (see Definition 3.5). The next decoding step is to use the k most reliable elements of v. Let us denote these as i$ = [n2(n1(v))11:k = (;I, 62, . . . , Zk). Since these are the most reliable symbols, these symbols should contain very few errors. Since G is systematically represented, we will take these symbols as the message symbols for a codeword. The corresponding codeword C in c" is obtained by 2 = f k 6 E c". Finally, the codeword P in the original code C can be obtained by unpermuting by both permutations: P = n;'(n,l(q) E c. This gives a single candidate decoded value. Then P is compared with r by computing dE(r, M(P)) (at least, this is the appropriate distance for the AWGN channel).

Figure 1.4 The concept of convection as suggested by Holmes (1928), when it was believed that the oceanic crust was a thick continuation of the continental basaltic layer (a) Currents ascending at A spread laterally, place a continent . under tension and split it, providing the obstruction of the old ocean oor can be overcome. This is accomplished by the formation of eclogite at B and C, where sub-continental currents meet sub-oceanic currents and turn downwards. The high density of the eclogite causes it to sink and make room for the continents to advance. (b) The foundering of eclogite at B and C contributes to the main convective circulation. The eclogite melts at depth to form basaltic magma, which rises in ascending currents at A, heals the gaps in the disrupted continent and forms new ocean oor. Local swells, such as Iceland, would be formed from old sial left behind. Smaller current systems, initiated by the buoyancy of the basaltic magma, ascend beneath the continents and feed ood basalts or, beneath old (Paci c) ocean oor, feed the outpourings responsible for volcanic islands and seamounts (redrawn from Holmes, 1928).

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