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Adams and Younger 2001a,b; Nuttall et al 2002), there is no real excuse for continuing to ignore the existence of turbulent ow in certain groundwater ow settings 325 Permeability with respect to saline waters and other uids As was explained in Section 322, the standard formulation of Darcy s Law (Equation 31) assumes that the uid in question is fresh groundwater Where the groundwater is actually saline (total dissolved solids 10,000 mg/L) and/or warm (>40 C), then its density and/or viscosity are likely to be suf ciently different from those of ordinary, fresh, sub-tepid groundwaters that the application of the simple version of Darcy s Law presented above (Equation 31) begins to become untenable Similarly, if we wish to quantify the ow rates of liquids which are considerably more viscous than water (eg.

with A being a positive semidefinite (m x m) matrix and B being an (m x n) matrix, is a bordered Gramian matrix.

Excitement over the dashboard technology is very strong. Everyone recognizes the potential this technology offers to put the right information in the right hands at the right time. However, it is still a new tool, and it will take time to fully realize its true potential. More important than the tool is the culture. To really be effective, senior management must embrace this new technology into their daily decisionmaking process. Strategic goals must be measured using this technology. Until that happens, or more accurately when that happens, the business intelligence vision will not be truly realized.

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oils and other dense liquids), or to quantify gas ow rates, then Equation 31 cannot be used either In such cases, it is necessary to re-cast Darcy s Law in a form which explicitly allows for the viscosity and density of the liquids/gases in question At its simplest, the necessary re-casting can be achieved by substituting a parameter known as the intrinsic permeability ( ) in place of K in Equation 31 To obtain an appropriate value of (in units of m2), it is necessary to multiply K (in m/s) by the kinematic viscosity of the liquid in question (in units of Pa/s), and then divide the product by the acceleration due to gravity (g, ie 981 m/s2) As a nal step, it would be usual practice to multiply the m2 value by 0.

In the case of convolutional codes, the de nition of block length is lost, since it becomes semi-in nite. As we saw above, however, for the current purpose it can be replaced by the decoding length. A given code sequence c generated by a convolutional code converts into a received sequence s r , which is essentially the code sequence c containing some errors, generated by the effect of the channel noise. An optimal decoder will compare the conditional probability P(s r /c ) with the received sequence s r corresponding to one of the possible code sequences c , and will take the decision in favour of that code sequence that has the maximum probability of being s r : P(s r /c) = max s r /c

Fig. 7.9 The curve describes the distribution of distances at which the rst stott was recorded during a chase. Points A and B refer to the median distances at which a gazelle began to ee from a cheetah when, A, the gazelle was caught and B, the gazelle escaped. Point C shows the median 1st stott distance. (Data from Caro 1986. Reproduced with permission of Elsevier.)

987 10 15, in order to obtain a nal value in millidarcies (the unit of intrinsic permeability in widest use in the petroleum industry) Unless you become involved in some of the more complex elds of contemporary groundwater modeling,vii you are unlikely to need to work with intrinsic permeabilities very often If you do get involved in such work, you will need to refer to specialist, advanced texts; Marsily (1986) is a good starting-point Nevertheless, given the abundance of intrinsic permeability data available for various rock types.

Locate your printer s cable (either the USB or 25-pin Centronics style), which should have been included with your printer. If it was not, you need to buy one from a computer or electronics store. Attach one end of the cable to your computer. Attach the other end of the cable to your printer. On the dedicated computer, turn on print sharing. For details on how to do this, see the Enable Print Sharing 5-minute x later in this chapter. For each computer on the network, use Windows to add a shared printer. For details on how to do this, see the Add a Shared Printer 5-minute x later in this chapter. In some cases, you might also need to run a setup CD and install print-server drivers on each computer. Check your printer s instructions to see if you need to do this.

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