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A steady-state simulation model for cooling coils with corrugated plate ns has been developed (Yik et al. 1997) and used as a component model in a coupled building and airconditioning system model (Yik et al. 1995). The model can predict sensible and total cooling capacities of cooling coils and the thermodynamic states of the air and chilled water. This section outlines the methods that were used to develop the cooling coil model. Box 4.2 summarises the meanings of symbols used in the coil model. Geometric and ow parameters In the model, a cooling coil is treated as a counter- ow heat exchanger (ARI 1991; ASHRAE 2000) (Fig. 4.12a), which has been shown to be a valid modelling approach if the number of tube passes exceeds three (Stevens et al. 1976). The heat transfer area of a cooling coil (A) is de ned as the total exposed surface area of the ns and the n collars (Fig. 4.12b) (hereafter referred to as the coil surface). The surface factor (Fs) used in evaluating A (A = FsNrAa) is approximated by the ratio of the total exposed surface area of the n and the n collar of a typical cell in the cooling coil (DA) (Fig. 4.12d) to the frontal area of the cell (DAa):

Real-time teleconsultation allows interaction between the transmitter and the recipient of the information and is used when an immediate outcome is needed, eg in an emergency Delays are avoided and the real-time interaction between the patient/healthcare professional and the consultant also provides an educational benefit The cost of these benefits is reflected in the need for higher bandwidth than is required for store-and-forward operation Real-time telemedicine makes use of all of the data types that we have identified Audio data are most commonly transmitted in telephone conversations for a whole raft of purposes ranging from diagnosis through monitoring to patient support Examples of data and text transfer have been given already in our discussion [I 111 on telemonitoring (Section 335) Mobile telephones with graphical displays can now be used to transmit ECGs [1441.

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The magmatism also buries the granitoids to mid-crustal depths where they partially melt due to the build up of radiogenic heat and, possibly, the advection of heat from mantle plume activity Thermal softening and a reduction in mid-crustal viscosity facilitates the sinking of the greenstones, which then squeezes out the underlying partial melts into rising, high-amplitude granitoid domes (Fig 1110c) The convective overturning depresses geotherms in the greenstone tracts, resulting in local cooling and the preservation of kyanite-bearing metamorphic rocks, which equilibrate at moderate-low pressures ( 600 MPa) and temperatures (500 C) This model explains the formation of the dome-and-keel structure without rigid plates or plate boundary forces and is similar to the sinking or sagduction models proposed for the formation of dome-andkeel structures in the Dharwar craton of India (Chardon et al, 1996).

Still image transfer in real time is also apparent in the disciplines noted for store-and-forward operation [145, 1461 including a long-standing telepathology service in Norway [146], and mobile telephones are again having an impact [147] However, it is with video transfer that real-time telemedicine.

Theorem 5.36 Let f (z) and g ( z ) be relativelyprime, monic irreduciblepolynomials over G F(q) of degrees m and n, respectively. Let c be the number of monic polynomials of degree k whose only k k irreducible factors are f (x) and g ( x ) . Then the moment generating function for c is

Listing 12.1 Important source files for the RemoteDBScan project. (continues)

Horizontal tectonic models for the Eastern Pilbara propose that the greenstones were affected by one or more periods of horizontal contraction and extension (Blewitt, 2002) In these interpretations, the contraction results from episodes of Early Archean collision (Sections 104, 105) and terrane accretion (Section 106) Periods of horizontal extension result in the formation of crustal detachments and the emplacement of the granitoid domes Kloppenburg et al (2001) used observations of multiple cross cutting fabrics and unidirectional patterns of stretching lineations to suggest that the Mt Edgar Dome initially formed as an extensional metamorphic core complex (Sections 73, 763, 766) An initial period of terrane collision and thrusting prior to 332 Ga thickens the Early Archean Warrawoona Greenstone Belt and buries granitoid basement to midcrustal levels where it partially melts Partial melting.

Because primitive elements exist, the nonzero elements of the field G F ( q ) can always be written as powers of a primitive element. If a E G F ( q ) is primitive, then 3 &2,-,41 = 1) Ia,a2 , a

3

0 0 1 0 0 1 1 0 0 1 0 0

1 -1 1 -1 -1 -1 1 1 1 -1 1 -1

Summary

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