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Half-plane

We shall now concentrate on several cases where relations equations (18) and (19) simplify. The most favorable case is where lnreciprocal relations between observable amplitude moduli and phases as in Eqs. (9) and (10), with the upper sign holding. Solutions of the Schiddinger equation are expected to be regular in the lower half of the complex t plane (which corresponds to positive temperatures), but singularities of ln4>(f) can still aiise from zeros of <(>( ). We turn now to the location of these zeros. [Pg.116]

Then, we expect that for this value(s) of the coordinate x, the t zeros of the wavepacket will be located in the upper t half-plane only. The reason for this is similar to the reasoning that led to the theorem about the location of zeros in the near-adiabatic case. (Section rH.E.l). Actually, empirical investigation of wavepackets appearing in the literature indicates that the expectation holds in... [Pg.124]

In the excited states for the same potential, the log modulus contains higher order terms mx(x, x, etc.) with coefficients that depend on time. Each term can again be decomposed (arbitrarily) into parts analytic in the t half-planes, but from elementary inspection of the solutions in [261,262] it turns out that every term except the lowest [shown in Eq. (59)] splits up equally (i.e., the/ s are just 1 /2) and there is no contribution to the phases from these temis. Potentials other than the harmonic can be treated in essentially identical ways. [Pg.128]

The dislocation cannot glide upwards by the shearing of atom planes - the atomic geometry is wrong - but the dislocation can move upwards if atoms at the bottom of the half-plane are able to diffuse away (Fig. 19.2). We have come across Fick s Law in which diffusion is driven by differences in concentration. A mechanical force can do exactly the same thing, and this is what leads to the diffusion of atoms away from the... [Pg.187]

Hertz [27] solved the problem of the contact between two elastic elliptical bodies by modeling each body as an infinite half plane which is loaded over a contact area that is small in comparison to the body itself. The requirement of small areas of contact further allowed Hertz to use a parabola to represent the shape of the profile of the ellipses. In essence. Hertz modeled the interaction of elliptical asperities in contact. Fundamental in his solution is the assumption that, when two elliptical objects are compressed against one another, the shape of the deformed mating surface lies between the shape of the two undeformed surfaces but more closely resembles the shape of the surface with the higher elastic modulus. This means the deformed shape after two spheres are pressed against one another is a spherical shape. [Pg.144]

Ur, Ur, and u- are the cartesian results Ur and u- are the results in cylindrical co-ordinates. Note u is in the direction of positive P, pressing into the half plane for compressive loading. The tangential displacements of the free surface are towards the origin in agreement with our intuition. [Pg.145]

The simplest type of line defect is the edge dislocation, which consists of an extra half plane of atoms in the crystal, as illustrated schematically in Fig. 20.30a edge dislocations are often denoted by 1 if the extra half plane ab is above the plane sp, or by T if it is below. [Pg.1263]

To a good approximation, only atoms within the dotted circles in Figs. 20.30a and b are displaced from their equilibrium position in a real, three-dimensional crystal the diameter d of these circles would be very much less than the length / of the dislocation, i.e. the length, perpendicular to the page, of the extra half plane of atoms ab in Fig. 20.30a, or of the line cd in Fig. 20.306. Dislocations strictly, therefore, are cylindrical defects of diameter d and length / however, since I d they are referred to as line defects. [Pg.1263]

We have seen that the output neuron in a binary-threshold perceptron without hidden layers can only specify on which side of a particular hyperplane the input lies. Its decision region consists simply of a half-plane bounded by a hyperplane. If one hidden layer is added, however, the neurons in the hidden layer effectively take an intersection (i.e. a Boolean AND operation) of the half-planes formed by the input neurons and can thus form arbitrary (possible unbounded) convex regions. ... [Pg.547]

The number of sides of the convex regions is equal to the miinber of half-planes whose intersection formed the decision region, and is thus bounded by the number of input neurons. [Pg.548]

This last representation is completely equivalent to the analytidty of t(ai) in Im 0 and the statement that a,t(a>) go to zero as u - oo. The analyticity property in turn is a direct consequence of the retarded or causal character of T(t), namely that it vanishes for t > 0. If t(ai) is analytic in the upper half plane, but instead of having the requisite asymptotic properties to allow the neglect of the contribution from the semicircle at infinity, behaves like a constant as o> — oo, we can apply Cauchy s integral to t(a,)j(o, — w0) where a>0 is some fixed point in the upper half plane within the contour. The result in this case, valid if t( - oo is... [Pg.591]

Dislocations Dislocations are stoichiometric line defects. A dislocation marks the boundary between the slipped and unslipped parts of crystal. The simplest type of dislocation is an edge dislocation, involving an extra layer of atoms in a crystal (Fig. 25.2). The atoms in the layers above and below the half-plane distort beyond its edge and are no longer planar. The direction of the edge of the half-plane into the crystal is know as the line of dislocation. Another form of dislocation, known as a screw dislocation, occurs when an extra step is formed at the surface of a crystal, causing a mismatch that extends spirally through the crystal. [Pg.421]

Note the initial negative deviation in response to a positive forcing disturbance, caused by the right half plane zero in the transfer function. [Pg.526]

Figure 5.7 Schematic edge dislocation after Peierls. Top part of crystal, T and bottom part B, are joined between planes a and P across a glide plane with an extra half-plane of atoms ending at c. The displacement along the glide plane is b, and the glide plane spacing is a. Figure 5.7 Schematic edge dislocation after Peierls. Top part of crystal, T and bottom part B, are joined between planes a and P across a glide plane with an extra half-plane of atoms ending at c. The displacement along the glide plane is b, and the glide plane spacing is a.
This approach is useful because it allows quantitative analysis via Walsh correlation diagrams to be made without extensive calculations. Figure 5.11 may clarify the approach. Initially the extra half-plane is at x = 0 and atom C is covalently bonded to atom A. When the half plane moves to the mid-glide position, x = b/2, the activation complex, ACB forms (Figure 5.10). Finally, when the half-plane moves to x = b, the pair CB forms a new covalent bond. Symbolically ... [Pg.76]

Figure 31. The stress distributions on a cracked half-plane loaded at infinity. (From Ennis and Sunshine, Tribology Int., 26 319-327, 1993, with kind permission from Elsevier Sciences Ltd., The Boulevard, Langford Lane, Kidlington 0X5 1GB, UK.)... Figure 31. The stress distributions on a cracked half-plane loaded at infinity. (From Ennis and Sunshine, Tribology Int., 26 319-327, 1993, with kind permission from Elsevier Sciences Ltd., The Boulevard, Langford Lane, Kidlington 0X5 1GB, UK.)...
Experimental measurements of DH in a-Si H using SIMS were first performed by Carlson and Magee (1978). A sample is grown that contains a thin layer in which a small amount (=1-3 at. %) of the bonded hydrogen is replaced with deuterium. When annealed at elevated temperatures, the deuterium diffuses into the top and bottom layers and the deuterium profile is measured using SIMS. The diffusion coefficient is obtained by subtracting the control profile from the annealed profile and fitting the concentration values to the expression, valid for diffusion from a semiinfinite source into a semi-infinite half-plane (Crank, 1956),... [Pg.422]


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See also in sourсe #XX -- [ Pg.413 ]




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