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Source-time function

Rise time a time interval between the triggering time of AE signal and the time of the peak amplitude is assigned. The rise time is closely related to the source-time function, and applied to classify the tjqie of fracture or eliminate noise signals. [Pg.43]

The M. (, t) terms are the nine time-dependent components of the moment tensor. This equation can be simplified dramatically by assuming that the source time function is an impulse and that all of the moment tensor components have the same time-dependency (synchronous source approximation). In addition, since the equivalent body forces conserve angular momentum. My = only six of the components ate required. Applying these assumptions, Eq. 5.8 reduces to the following linear relationship ... [Pg.88]

By employing a concrete block as shown in Fig. 7.5, AE waves due to surface pulse is detected at the point E. In Fig. 7.6 (a), AE wave detected by AE sensor of resonance frequency 1 MHz is shown, where the force was applied by the same-type sensor driving an electric pulse at the distance R = 6 cm. In this case, the source-time function f(t) was reasonably assumed (Ohtsu 1982),... [Pg.158]

This waveform is simulated by Eq. 7.18, taking into account the location, the crack-opening motion in the xi-direction and the integrated source-time function of Eq. 7.14. Tr is varied to match the waveform with Fig. 7.9 (a). A result with 7> = 14 ps computed in a half space is given in Fig. 7.9 (b). Because the spatial derivatives Gkp q in Eq. 7.18 is computed in a halfspace (Ohtsu 1984), only the first portion of the waveform is synthesized. Still, remarkable agreement is observed. [Pg.162]

Equations 7.15 and 7.18 are represented by the convolution integral with the functions/(Yj and S(t). Thus, inversely solving them, the function can be computed. The procedure is named the deconvolution analysis (Wadley 1981). Conventionally the source characterization of AE implies this procedure. Because the convolution integral in the time domain can be replaced by the multiplication in the fi-equency domain, the deconvolution is mathematically conducted in the fi-equency domain. Thus, the Fourier transform of the detected wave, U(f), is represented as the Fourier transform of the source time function, S(fl, times that of Green s function, G(J),... [Pg.163]

Fig. 7.12. Source-time functions df(t)/dt by deconvolution analysis of Lamb s problem due to a surface pulse. The solid curve is analyzed and the broken is assumed in the synthesized waveform. Fig. 7.12. Source-time functions df(t)/dt by deconvolution analysis of Lamb s problem due to a surface pulse. The solid curve is analyzed and the broken is assumed in the synthesized waveform.
Fig. 7.13. Source-time function S(t) by deconvolution (solid) and assumed in the synthesized (broken). Fig. 7.13. Source-time function S(t) by deconvolution (solid) and assumed in the synthesized (broken).
Eventually AE source is represented by the moment tensor Mpq and the source-time function S(t). This implies that crack kinetics is represented by S(t), which is solved by the deconvolution analysis (Wadley 1981). In contrast, crack kinematics are represented by the moment tensor. In order to characterize crack kinematics, as a conclusion, the determination of the moment tensor is inevitable. [Pg.167]

A pressure source time function reconstructed from these phasors is shown in Figure 5. The corresponding source impedances as a function of frequency are shown in Figure 6. [Pg.105]

Coseismic displacements have been measured for studying geometry of fault surface. The surface displacement of the Earth is associated with the slip on the fault surface through mathematical models. The radiated seismic wave field is dependent on the slip amplitude, mpture velocity, and source time function, whereas the quasi-static displacements depend only on the final slip amplitude. Therefore, the displacements measured with GNSS are complementary constraints on the geometry of fault surface (Segall and Davis 1997). [Pg.1101]

In the second step, the source mechanism and time function are obtained after factorization of the MTRFs into a time constant moment tensor my and a common source time function f(t) ... [Pg.2154]

This means that the same time dependence for all moment tensor components, i.e., a rupture mechanism constant in time, is assumed, which is an acceptable approximation for weak to moderate earthquakes. Only the correlated part of the MTRFs is used in the factorization, thus absorbing the bias due to non-exact Green s functions (Panza and Sarao 2000) the problem is nrmlinear and is solved iteratively by imposing COTistraints such as positivity of the source time function and the requirement of a mechanism consistent with clear readings of at least one first-arrival polarity. [Pg.2154]

In summary, the average mechanism and source time function obtained by the inversion are considered to be basically affected by three kinds of bias, generated, respectively, by (1) the noise present in the data. (2) the horizontal mislocation of the hypocenter, and (3) the epistemic uncertainty in the structural models used to compute the synthetic Green s functions. [Pg.2154]

Figure 20 shows typical waveforms of LMEs at the Sechilieime DSGSD. One type corresponds to impulsive sources similar to small explosions, while another event tyqDe shows mostly emergent onsets and represents source-time functions lasting 5 s, either relatively broadband or low frequency. The LMEs cluster either in the... [Pg.3061]

For a finite excitation pulse width and decay constant Ap (Fig. 7) the observed fluorescence response function f (t) is expressed as a superposition integral of the (true) 8-excitation response function/(f) and the over-all time function of source and detector p(t) according to... [Pg.180]

Moreover, advanced evaluation methods exist to apportion PM levels measured at the receptor site to the trajectory segments (e.g. the residence time weighted concentration method [23]) or to regions (grid cells) hit by trajectory ensembles (e.g. the potential source contribution function, PSCF [24, 25]). Software tools are available which facilitate such calculations and visualisations of the results [26]. [Pg.202]

Being a point source of consciousness, energy, light, and love. Astral travel and other PSI phenomena. Fusion with other entities in time. Functioning in the path mental center in the head. [Pg.230]

Fig. 1. Time course of S. cerevisiae ure2dal80 mutant strain culture in nonbuffered medium containing proline as nitrogen source as function of initial pH. Fig. 1. Time course of S. cerevisiae ure2dal80 mutant strain culture in nonbuffered medium containing proline as nitrogen source as function of initial pH.
This general solution for any time function Q(t) contains special simple cases. The temperature held for a source of constant thermal power Q(t) = Q0 is found... [Pg.189]

Figure 5. Comparison of the computed photosignal and the measured photosignal obtained from a dried multilayered film of oriented purple membranes. The bathing electrolyte solutions contained 0,1-M KCl and 0.01-M L-histidine buffered at pH 2. The measurement was made at an access impedance of 39.2 kil and an instrumental time constant of0.355 fis. The lower trace is the power versus time function of the light source (dye laser output at 590 nm). The inset shows the same data at an expanded time scale. See text for further explanation. Figure 5. Comparison of the computed photosignal and the measured photosignal obtained from a dried multilayered film of oriented purple membranes. The bathing electrolyte solutions contained 0,1-M KCl and 0.01-M L-histidine buffered at pH 2. The measurement was made at an access impedance of 39.2 kil and an instrumental time constant of0.355 fis. The lower trace is the power versus time function of the light source (dye laser output at 590 nm). The inset shows the same data at an expanded time scale. See text for further explanation.
The columns of 4> are then the discrete EOFs and the columns of U are the discrete-time functions. These discrete EOFs can be interpolated in space to obtain the continuous EOFs using, for example, 1 jr- interpolation. Then (26.26) can be applied to obtain the spatial distribution of the source strength. [Pg.1152]

Another meaningful observation is that the Green function convolution (integration) with (source) wave-function is done upon the coordinate only in the basic definition, while the entirely time evolution is contained within the Green function. In relation with this aspect one may establish... [Pg.264]

The calculated arrival time is composed of the travel time t, which is a function of the location of the sensors xt, yt, z,) and the hypocenter (xo, yo, zo), and the source time to. Since this equation consists of four unknowns, at least four arrival times are needed to determine the hypocenter and the origin time three arrival times are necessary if only the epicenter and the arrival time are to be calculated. If n arrival times from n sensors are measured the system is over-determined because there are more knowns than unknowns. The over-determined system has to be solved in a way that the residuals r, between calculated and measured arrival time, at each sensor, are minimized. [Pg.112]

It is not surprising to find that pectin is well suited for low-pH applications considering its source. Pectin functions ideally at pHs near 3.5. Below this pH, it suffers from hydrolysis of both the glycosidic linkage and the ester, and in highly alkaline solutions, hydrolysis of the ester is rapid. Changes in the number of ester groups over time cause unstable viscosities in cosmetic formulations. [Pg.349]

The X dependence of this function has a form similar to g(x,w) shown in Fig. 6.2. In the present case the curves would be drawn for fixed values of time as a parameter. At small values of n(x,0 would show a sharply peaked form much like the shape of (x,mo). This curve would represent the spatial distribution of neutrons soon after their release from the source plane at x = 0. As t increases, the density function n(x,0 flattens much like the curves for Wi, U2, etc., of Fig. 6.2, indicating that as time progresses the neutrons wander farther from the source plane and tend to spread more evenly throughout the medium. One can also sketch from Eq. (6.32) a density-time function for given x analogous to the curve of Fig. 6.3. Such a curve would show how the density at a specified station would vary as the initial neutron burst passes by. In this case the interpretation of the curve would be as follows At short times after the burst, the neutrons have not yet had time to reach point x, and therefore the density would be low very long after the burst, the neutron density has fallen everywhere because of spreading out and absorption. Thus from the viewpoint of an observer at x, a pulse of neutrons passes sometime after the initial burst at the source. The time at which the maximum neutron density occurs at x is... [Pg.279]


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