共查询到7条相似文献，搜索用时 212 毫秒
1.
ＬｉｎｅａｒｉｎｖｅｒｓｉｏｎｏｆｓｅｉｓｍｉｃｍｏｍｅｎｔｔｅｎｓｏｒｓｏｆｇｅｎｅｒａｌｐｏｉｎｔｓｏｕｒｃｅｂｙｕｓｉｎｇｇｅｎｅｒａｌｉｚｅｄｒａｙｔｈｅｏｒｙＲＵＩ－ＦＥＮＧＬＩＵ（刘瑞丰）ＪＩＮＧ－ＰＩＮＧＤＡＮＧ（党京平）ＳＨＡＯ－Ｄ... 相似文献
2.
Ying Hu Hui Chen Hongyan Qian Xinyue Zhou Yuanjun Wang Bin Lyu 《Geophysical Prospecting》2020,68(3):941-954
Improving the seismic time–frequency resolution is a crucial step for identifying thin reservoirs. In this paper, we propose a new high-precision time–frequency analysis algorithm, synchroextracting generalized S-transform, which exhibits superior performance at characterizing reservoirs and detecting hydrocarbons. This method first calculates time–frequency spectra using generalized S-transform; then, it squeezes all but the most smeared time–frequency coefficients into the instantaneous frequency trajectory and finally obtains highly accurate and energy-concentrated time–frequency spectra. We precisely deduce the mathematical formula of the synchroextracting generalized S-transform. Synthetic signal examples testify that this method can correctly decompose a signal and provide a better time–frequency representation. The results of a synthetic seismic signal and real seismic data demonstrate that this method can identify some reservoirs with thincknesses smaller than a quarter wavelength and can be successfully applied for hydrocarbon detection. In addition, examples of synthetic signals with different levels of Gaussian white noise show that this method can achieve better results under noisy conditions. Hence, the synchroextracting generalized S-transform has great application prospects and merits in seismic signal processing and interpretation. 相似文献
3.
For wave propagation simulation in piecewise heterogeneous media, Gaussian-elimination-based full-waveform solutions to the generalized Lippmann–Schwinger integral equation (GLSIE) are highly accurate, but involved with extremely time-consuming computations because of the very large size of the resulting boundary–volume integral equation matrix to be inverted. Several flexible approximations to the GLSIE are scaled in an iterative way to adapt numerical solutions to the smoothness of heterogeneous media in terms of incident wavelengths, with a great saving of computing time and memory. Among various typical iterative schemes to the GLSIE matrix, the generalized minimal residual method (GMRES) is an efficient approach to reduce the computational intensity to some degree. The most efficient approximation can be obtained using a Born series, as an alternative iterative solution, to both the boundary-scattering and volume-scattering waves, leading to the Born-series approximation (BSA) scheme and the improved Born-series approximation (IBSA) scheme. These iteration schemes are validated by dimensionless frequency responses to a heterogeneous semicircular alluvial valley, and then applied to a heterogeneous multilayered model by calculating synthetic seismograms to evaluate approximation accuracies. Numerical experiments, compared with the full-waveform numerical solution, indicate that the convergence rates of these methods decrease gradually with increasing velocity perturbations. The comparison also shows that the BSA scheme has a faster convergence than the GMRES method for velocity perturbations less than 10 percent, but converges slowly and even hardly achieves convergence for velocity perturbations greater than 15 percent. The IBSA scheme gives a superior performance over the other methods, with the least iterations to achieve the necessary convergence. 相似文献
4.
Andrea Cortis Carlos E. Puente Huai-Hsien Huang Mahesh L. Maskey Bellie Sivakumar Nelson Obregón 《Stochastic Environmental Research and Risk Assessment (SERRA)》2014,28(6):1421-1429
In this study, we attempt to offer a solid physical basis for the deterministic fractal–multifractal (FM) approach in geophysics (Puente, Phys Let A 161:441–447, 1992; J Hydrol 187:65–80, 1996). We show how the geometric construction of derived measures, as Platonic projections of fractal interpolating functions transforming multinomial multifractal measures, naturally defines a non-trivial cascade process that may be interpreted as a particular realization of a random multiplicative cascade. In such a light, we argue that the FM approach is as “physical” as any other phenomenological approach based on Richardson’s eddies splitting, which indeed lead to well-accepted models of the intermittencies of nature, as it happens, for instance, when rainfall is interpreted as a quasi-passive tracer in a turbulent flow. Although neither a fractal interpolating function nor the specific multipliers of a random multiplicative cascade can be measured physically, we show how a fractal transformation “cuts through” plausible scenarios to produce a suitable realization that reflects specific arrangements of energies (masses) as seen in nature. This explains why the FM approach properly captures the spectrum of singularities and other statistical features of given data sets. As the FM approach faithfully encodes data sets with compression ratios typically exceeding 100:1, such a property further enhances its “physical simplicity.” We also provide a connection between the FM approach and advection–diffusion processes. 相似文献
5.
G. Ameri A. Oth M. Pilz D. Bindi S. Parolai L. Luzi M. Mucciarelli G. Cultrera 《Bulletin of Earthquake Engineering》2011,9(3):717-739
We exploit S-wave spectral amplitudes from 112 aftershocks (3.0 ≤ ML ≤ 5.3) of the L’Aquila 2009 seismic sequence recorded at 23 temporary stations in the epicentral area to estimate the source
parameters of these events, the seismic attenuation characteristics and the site amplification effects at the recording sites.
The spectral attenuation curves exhibit a very fast decay in the first few kilometers that could be attributed to the large
attenuation of waves traveling trough the highly heterogeneous and fractured crust in the fault zone of the L’Aquila mainshock.
The S-waves total attenuation in the first 30 km can be parameterized by a quality factor QS(f) = 23f
0.58 obtained by fixing the geometrical spreading to 1/R. The source spectra can be satisfactorily modeled using the omega-square
model that provides stress drops between 0.3 and 60 MPa with a mean value of 3.3±2.8 MPa. The site responses show a large
variability over the study area and significant amplification peaks are visible in the frequency range from 1 to more than
10 Hz. Finally, the vertical component of the motion is amplified at a number of sites where, as a consequence, the horizontal-to-vertical
spectral ratios (HVSR) method fails in detecting the amplitude levels and in few cases the resonance frequencies. 相似文献
6.
Raquel Somavilla Cabrillo Cesar González-Pola Manuel Ruiz-Villarreal Alicia Lavín Montero 《Ocean Dynamics》2011,61(9):1215-1235
Mixed layer depth (MLD) variability from seasonal to decadal time scales in the Bay of Biscay is studied in this work. A hydrographic
time series running since 1991 in the study area, a climatology of the upper layer vertical structure based on the topology
of this temperature profile time series and a one-dimensional water column model have been used for this purpose. The prevailing
factors driving MLD variability have been determined with detail, and agreement with observations is achieved. Tests carried
out to investigate climatological profile skill to reproduce the upper layer temporal evolution have demonstrated its ability
to simulate variability at seasonal time scales and reproduce the most conspicuous events observed. This has enabled us to
carry out a reconstruction of the MLD variability for the last 60 years in the study area. Favourable sequence of intense
mixing events explains interannual differences and cases of extraordinary deepening of winter mixed layer. The negative phase
of the Eastern Atlantic pattern seems to determine important interannual variability through intense episodes of cooling and
mixing as in winter 2005 in the Bay of Biscay. Low-frequency variability is also observed. A very striking and unexpected
shallower winter MLD during the 1970s and 1980s than those observed from 1995 has been found. Simulation results support this
counter-intuitive outcome of shallower winter mixed layers concurrent with generalized upper water warming trends reported
on several occasions for the area. The long-term trends in MLD seem related with decadal variability in the North Atlantic
Oscillation, being in phase and opposition with other deepening-shallowing cycles found from subtropical-to-subpolar areas
in the North Atlantic. 相似文献
7.
Siripatana Adil Le Maitre Olivier Knio Omar Dawson Clint Hoteit Ibrahim 《Ocean Dynamics》2020,70(8):1103-1127
Ocean Dynamics - Bayesian inference with coordinate transformations and polynomial chaos for a Gaussian process with a parametrized prior covariance model was introduced in Sraj et al. (Comput... 相似文献