The sensor design was integrated on the optical fiber by utilizing the evanescent wave produced on the fiber surface to react with sensing reagents.
This indicates that EMC or shielding characteristics can only be designed either by utilizing the phenomenon of wave reflections, or by equipping the panels with additional foils on surfaces or absorbing foams in air volumes.
The SV-wave velocities were obtained by using the Multichannel Analysis of Surface Waves (MASW) method while the SH-wave velocities were extracted by utilizing the Multichannel Analysis of Love Waves (MALW) technique.
Dispersion equations of Love waves in double porosity medium are obtained by utilizing the usual assumption of Love waves in elastic solid with the coupling mass coefficient ρ23 and coupling permeability term k(12) being equal to zero.
After the reduction of this equation by utilizing the Lie symmetries, the traveling wave solutions are first discussed in Reduction 1.
Against this background, this paper aims at assessing potential migration flows to the EU from the countries with which the EU is intensifying cooperation – recent entrant Croatia, several candidate countries and members of the EaP program – by utilizing the experiences of the enlargement wave of 2004.
The angle gather data with free noise (Fig. 2a) were synthesized with Zoeppritz equations in the time domain by utilizing the real well logs of P-wave velocity, S-wave velocity, and density and a 35 Hz Ricker wavelet for incident angles ranging from 0° to 35°. Figure 2b d displays the log curves of Young's modulus, Poisson's ratio, and density.
The new approach presented here describes the ( overrightarrow{E} ) components of the characteristic waves by utilizing the Forsterling functions discussed above.
Considering these facts, the 1D S-wave velocity model depicted in Fig. 5c was constructed by trial and error to reproduce the peak period on the long-period side (1 10 s) of the H/V spectral ratios for coda waves by utilizing the available geological and geophysical information discussed above.
The mixing ratio of H2SO4 vapor around 35 50 km altitude can be measured by radio occultation by utilizing the fact that attenuation of radio waves occurs in the Venus atmosphere primarily due to H2SO4 vapor in this altitude region, with smaller contributions from CO2 and SO2 (Jenkins and Steffes, 1991; Jenkins et al., 1994).
