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Transmission curves through various distances of standard atmosphere (7°C temperature, 85% relative humidity, 3 m above ground) were calculated using MODTRAN [ 21], see Fig. 8(b).
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Based on the relationship between the concentrations of 214Pb and 214Bi in the rainwater and the rainfall rate for an individual rainfall event, the increase in the environmental gamma-ray dose rate from 214Pb and 214Bi deposited on the ground was calculated, and the calculated increase agreed well with that observed by the in situ measurement on flat ground.
Furthermore, the resonant frequency and amplification factor of the ground is calculated.
Analytical results curves are fitted to experimental one and thermal conductivities of ground are calculated for each region.
Furthermore, the echo area of the airborne pulse radar and the echo's Doppler distribution on the ground are calculated in Section 4.
The geoelectric field, at any given position on the ground, is calculated from Eq. (6) with the substituted output parameters (in this case the current strength) obtained after the inversion.
To extrapolate pilot-plant results to larger scale, A ground was calculated including the empty spaces between the photoactive tubes and half the distance between the photoactive loops and the dummy loops from both sides [ 8].
Therefore, the synthetic ground motions were calculated with the assumption that ground motions were only generated within the SMGAs, which were redefined based on asperity location and area information (Kamae and Irikura 1998; Miyake et al. 2003).
Mr Gingrich's attacks on the attempt to build the "Ground-Zero mosque" in Manhattan (in fact, an Islamic study centre some distance from Ground Zero) were calculated to stir up the worst passions.
Structural and conformational, natural bond orbital (NBO) and nonlinear optical (NLO) analysis was performed, and 1H and 13C NMR chemical shifts values of 5- 2-Acetoxyethyl -6-methylpyrimidin-2,4-dione [C9H12N2O4] in the ground state were calculated by using Density Functional Theory (DFT-B3LYP/6-311++G(d,p)) and Hartree–Fock (HF/6-311++G(d,p)) methods.
Site amplifications for the weak ground motions were calculated with respect to a permanent station located at Mt. Kinbo as a reference, and the derived amplifications are relatively variable along the 6-km survey line; however, site amplification factors in the frequency range of 0.5 3 Hz are not large enough to explain the amplitudes produced by the main shock.
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