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Lateral shift

FIGURE 1.7 Construction of a master curve of dynamic modulus /a versus log (frequency) by lateral shifting of experimental results made over a small frequency range but at several different temperatures. [Pg.10]

Position of the coastline. The position of the coastline with reference to the position of the aquifer intake area should remain constant. This is particularly critical along coastlines with gently sloping topography and shallow water on the continental shelf. In such areas, lateral shifts of the shoreline of more than 200 km have been common during the past 20,000 years. [Pg.216]

Figure 6 shows the size distributions for the samples taken from one of the runs, presented as the cumulative number oversize per ml of slurry. From the lateral shift of the size distributions, the growth rate can be determined. Figure 7 shows values of growth rate, G, supersaturation, s, and crystal content determined during the run. As a material balance check, the crystal contents were evaluated from direct measurements, from solution analyses and from the moments of the size distribution. The agreement was satisfactory. No evidence of size dependent growth or size dispersion was observed. [Pg.301]

The entire construction was accomplished without incident the conventional equipment and techniques worked as well as with Sulphlex binders as with asphalt. After 2.5 years service, at a traffic volume of 1000 ADT (10 percent trucks), distress is evident in a number of sections. In general, the distress has been primarily attributed to poor subgrade drainage placement of certain sections with mix at extremely low temperature (below 65C (150F)) ravelling of dry mixtures and lateral shifting of lifts due to the absence of adequate tack between them. None of the distress is uniquely related to the use of Sulphlex binders in lieu of asphalt cement in the pavement. [Pg.219]

Cofacial diporphyrins can be bridged by one, two, three, or four links. In each case, the relative arrangement of the two bound metal atoms (one per porphyrin) can be described by the interplanar distance (P-P), the metal-center-to-metal-center distance (Ct-Ct), and the lateral shift (LS) of the metal centers with respect to each other (76), as shown in Fig. 6. Variations in these structural parameters should markedly affect the reactivity of the dimetallodiporphyrin. [Pg.285]

The first (imaginary) exponential term in (9.18) is responsible for the lateral shift of the reflected wave in the direction x of its propagation (Fig. 9.8). [Pg.279]

Lateral shifts are also due to depth penetration and refer to a shift in the exit location of an X-ray at the crystal surface. This results in a transverse shift at the detector, typically 10%-100% of refractive index corrections [20]. While ray-tracing can adequately describe geometrical effects outside the crystal, the effects of depth penetration and lateral shifts require full dynamical diffraction theory. [Pg.704]

Amplitude a, period Xc, mean separation l, lateral shift b. [Pg.113]

When comparing with the location of the true fibre edge, the general conclusion is that the fibre-polymer borderline as defined by the current criterion exhibits a small lateral shift towards the polymeric material. Consequent-... [Pg.139]

Pt (110) (fee) (2x1) Missing-row model with the top layer expanded by 23% to l.A A from bulk value of 1.387 A. Lateral shift of second layer rows of 0.05 A. LEED/12/... [Pg.134]

This model involves buckling in layers 2 to 6 of up to 0.27 A and small lateral shifts in the first six layers. [Pg.154]

Fig. 13 Power distribution P as a function of the lateral coordinate. A phase shift in the wave representing the sensing branch causes a lateral shift of the interference pattern on the CCD detector... Fig. 13 Power distribution P as a function of the lateral coordinate. A phase shift in the wave representing the sensing branch causes a lateral shift of the interference pattern on the CCD detector...
Overall, the Late Ordovician extinction appears to be the result of purely terrestrial phenomena. High sea-level stands of the early Paleozoic allowed for animal diversification on shallow-water, epicontinental carbonate platforms that proved, however, to be highly sensitive to glacio-eustatic effects on ecospace availability and lateral shifts in the oxic-anoxic interface. Tectonic activity facilitated the establishment of Gondwanan ice sheets which robbed the shallow seas of water, leading to extinction, establishment of recovery ecosystems, and then the destruction of these as the ice sheets melted, perhaps catastrophically. [Pg.3821]


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Lateral Nuclear Shifts

Lateral shift absorption

Lateral shift mechanism

Lateral shift transit time

Planar waveguides lateral shift

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