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Vertical time

An estimate of the probability of failure before some chosen specific time is obtained by the following. Suppose that an estimate is desired of the probability of fan failure before 100,000 hours, based on a Weibull fit to the fan data. Enter the Weibull plot on the vertical time scale at the chosen time, 100,000 hours. Go horizontally to the fitted line and then up to the probability scale where the estimate of the probability of failure is read and is 38 per cent. In other words, an estimated 38 per cent of the fans will fail before they run for 100,000 hours. [Pg.1050]

For the purpose of showing how to obtain from an exponential hazard plot an estimate of the exponential mean time to failure, assume that the straight line on Figure 62.9 is the one fitted to the data. Enter the plot at the 100 per cent point on the horizontal cumulative hazard scale at the bottom of the paper. Go up to the fitted line and then across horizontally to the vertical time scale where the estimate of the mean time to failure is read and is 1000 hours. The corresponding estimate of the failure rate is the reciprocal of the mean time to failure and is 1/100 = 0.001 failures per hour. [Pg.1051]

Coupled closely with the effect causing horizontal distributions are the vertical distributions of ozone concentrations. These distributions have an intimate influence on the urban-rural interchange of ozone. Miller and Ahrens presented detailed vertical time and space cross sections of ozone concentrations at altitudes up to 2,500 m. A low-altitude temperature inversion may actually lead to lower concentrations of oxidant, because the destruction rate can be increased by the injection of nitric... [Pg.140]

FIGURE 4 13 Vertical time section for ozone, operation 33, November 5, 1973. Redrawn from Edinger. ... [Pg.147]

Figure 4-14. High-pressure falling-sinker viscometer. Pressure is transmitted to the test liquid through the side arm and acts on the bellows-like reservoir of the viscometer chamber. The instrument is oriented vertically. Time of fall of the sinker is monitored by electrical contact at the top and bottom pins, a Viscometer tube, b Sinker, c Reservoir. d Insulated lead, e Insulated pin. f End plugs, g Terminal plug. After Bradbury, Mark and Kleinschmidt [20]. Figure 4-14. High-pressure falling-sinker viscometer. Pressure is transmitted to the test liquid through the side arm and acts on the bellows-like reservoir of the viscometer chamber. The instrument is oriented vertically. Time of fall of the sinker is monitored by electrical contact at the top and bottom pins, a Viscometer tube, b Sinker, c Reservoir. d Insulated lead, e Insulated pin. f End plugs, g Terminal plug. After Bradbury, Mark and Kleinschmidt [20].
From this map it can be seen that horizontal time is 60 days. In other words, the various processes of gathering materials, spinning, knitting, dyeing, finishing, sewing and so on take 60 days to complete from start to finish. This is important because horizontal time determines the time that it would take for the system to respond to an increase in demand. Hence, if there were to be a sustained increase in demand, it would take that long to ramp up output to the new level. Conversely, if there was a downturn in demand then the critical measure is pipeline volume, i.e. the sum of both horizontal and vertical time, In other words it would take 175 days to drain the system of inventory. So in volatile fashion markets, for instance, pipeline volume is a critical determinant of business risk,... [Pg.134]

Not surprisingly, costs are several times higher than conventional wells. Nevertheless, overall project economics may favour ERD over other development options. For example, BP developed the offshore part of the Wytch Farm Oilfield (which is located under Poole Harbour in Dorset, UK) from an onshore location. The wells targeted the reservoir at a vertical depth of 1,500 meters with a lateral displacement of over 8,000 meters (Fig. 3.20). The alternative was to build a drilling location on an artificial island in Poole Bay. ERD probably saved a considerable amount of money and advanced first oil by several years. [Pg.51]

As object we used a polished diamond oriented with its flat table vertically. Figure 4 shows a radiograph taken with the table plane parallel to the X-ray beam. The magnification is about 50 times. The inset shows the contrast along an horizontal trace, which is also indicated. [Pg.576]

As an extension of Problem 11, integrate a second time to obtain the equation for the meniscus profile in the Neumann method. Plot this profile as y/a versus x/a, where y is the vertical elevation of a point on the meniscus (above the flat liquid surface), x is the distance of the point from the slide, and a is the capillary constant. (All meniscus profiles, regardless of contact angle, can be located on this plot.)... [Pg.380]

Figure Al.6.27. Equipotential contour plots of (a) the excited- and (b), (c) ground-state potential energy surfaces. (Here a hamionic excited state is used because that is the way the first calculations were perfomied.) (a) The classical trajectory that originates from rest on the ground-state surface makes a vertical transition to the excited state, and subsequently undergoes Lissajous motion, which is shown superimposed, (b) Assuming a vertical transition down at time (position and momentum conserved) the trajectory continues to evolve on the ground-state surface and exits from chaimel 1. (c) If the transition down is at time 2 the classical trajectory exits from chaimel 2 (reprinted from [52]). Figure Al.6.27. Equipotential contour plots of (a) the excited- and (b), (c) ground-state potential energy surfaces. (Here a hamionic excited state is used because that is the way the first calculations were perfomied.) (a) The classical trajectory that originates from rest on the ground-state surface makes a vertical transition to the excited state, and subsequently undergoes Lissajous motion, which is shown superimposed, (b) Assuming a vertical transition down at time (position and momentum conserved) the trajectory continues to evolve on the ground-state surface and exits from chaimel 1. (c) If the transition down is at time 2 the classical trajectory exits from chaimel 2 (reprinted from [52]).
Figure 3, Wavepacket dynamics of the photodissociation of NOCl, shown as snapshots of the density (wavepacket amplitude squared) at various times, The coordinates, in au, are described in Figure b, and the wavepacket is initially the ground-state vibronic wave function vertically excited onto the 5i state. Increasing corresponds to chlorine dissociation. The density has been integrated over the angular coordinate. The 5i PES is ploted for the geometry, 9 = 127, the ground-state equilibrium value,... Figure 3, Wavepacket dynamics of the photodissociation of NOCl, shown as snapshots of the density (wavepacket amplitude squared) at various times, The coordinates, in au, are described in Figure b, and the wavepacket is initially the ground-state vibronic wave function vertically excited onto the 5i state. Increasing corresponds to chlorine dissociation. The density has been integrated over the angular coordinate. The 5i PES is ploted for the geometry, 9 = 127, the ground-state equilibrium value,...
A final study that must be mentioned is a study by Haitmann et al. [249] on the ultrafast spechoscopy of the Na3p2 cluster. They derived an expression for the calculation of a pump-probe signal using a Wigner-type density mahix approach, which requires a time-dependent ensemble to be calculated after the initial excitation. This ensemble was obtained using fewest switches surface hopping, with trajectories inibally sampled from the thermalized vibronic Wigner function vertically excited onto the upper surface. [Pg.310]


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