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921.
Decoupling Conditions for Elasto-plastic Consolidation Question Based on Numerical Modeling Method 总被引:1,自引:0,他引:1
Cheng Tao Wang Jingtao Dong Bichang 《中国地质大学学报(英文版)》2005,16(4):363-368
INTRODUCTION Theconsolidationofsaturatedsoilisanimpor tantsubjectingeomechanics.Biot(1941)proposed thethree dimensionalconsolidationtheory,whichis basedontheprincipleofeffectivestress,continuity conditionsandequilibriumequations.Theremarka blesuccessofthistheoryistheanalysisofthetime dependenteffectandcouplingeffectofsoilandpore water.Thus,thetheoryisaclassictheoryinsatu ratedsoilstatistics.Itwasalmostunfeasibletoperformanalysesof thistheorywithoutthedevelopmentofhigh speed computersandnu… 相似文献
922.
923.
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925.
Normalized, coupled governing equations for one-dimensional thermal consolidation problems are established. The non-dimensional coefficients of thermal consolidation and thermal diffusivity are defined accordingly. An analytical solution is deduced by using the Laplace transform and the Gauss–Legendre method of Laplace transform inversion. The responses of saturated porous media subjected to cyclic thermal loading are studied. The evolution of temperature, pore pressure and displacement from instantaneous state to quasi-steady state, with elapsed time, are analysed. The characteristics of cyclic fluctuation and the attenuation of the field variables with increased depth are also analysed. The influences of the permeability of media on thermal responses are discussed. 相似文献
926.
罗德里格矩阵在三维坐标转换严密解算中的应用 总被引:6,自引:0,他引:6
利用反对称矩阵和罗德里格矩阵的性质,把传统的三个旋转角参数用反对称矩阵的三个独立元素代替,推导了用三个公共点计算任意旋转角情况下的7个参数的直接计算公式,井建立了相应的平差模型。 相似文献
927.
In the absence of strong motion records, ground motion during the 26th January, 2001 Kutch, India earthquake, has been estimated by analytical methods. A contour map of peak ground acceleration
(PGA) values in the near source region is provided. These results are validated by comparing them with spectral response recorder
data and field observations. It is found that very near the epicenter, PGA would have exceeded 0.6 g. A set of three aftershock
records have been used as empirical Green's functions to simulate ground acceleration time history and 5% damped response
spectrum at Bhuj City. It is found that at Bhuj, PGA would have been 0.31 g–0.37 g. It is demonstrated that source mechanism
models can be effectively used to understand spatial variability of large-scale ground movements near urban areas due to the
rupture of active faults. 相似文献
928.
E. M. Scordilis 《Journal of Seismology》2006,10(2):225-236
The existence of several magnitude scales used by seismological centers all over the world and the compilation of earthquake catalogs by many authors have rendered globally valid relations connecting magnitude scales a necessity. This would allow the creation of a homogeneous global earthquake catalog, a useful tool for earthquake research. Of special interest is the definition of global relations converting different magnitude scales to the most reliable and useful scale of magnitude, the moment magnitude, M
W. In order to accomplish this, a very large sample of data from international seismological sources (ISC, NEIC, HRVD, etc.) has been collected and processed. The magnitude scales tested against M
W are the surface wave magnitude, M
S, the body wave magnitude, m
b, and the local magnitude, M
L. The moment magnitudes adopted have been taken from the CMT solutions of HRVD and USGS. The data set used in this study contains 20,407 earthquakes, which occurred all over the world during the time period 1.1.1976–31.5.2003, for which moment magnitudes are available. It is shown that well-defined relations hold between M
W and m
b and M
S and that these relations can be reliably used for compiling homogeneous, with respect to magnitude, earthquake catalogs. 相似文献
929.
利用Liner的2.5-D时间域声波方程和高阶有限差分近似,研究了2.5维声波方程在时间-空间域中的衰减特性。简单地质模型(水平二层介质)的数值计算结果证实了下列事实:在Liner的声波方程中的最后一项,即含有1/t2的一项对整个计算结果没有影响,因此可以忽略。这一结论与文献中已经发表的数值结果相吻合。同样的结论对于由Williamson和Pratt提出的2.5-D声波方程也适用。 相似文献
930.
Toshio Fukushima 《Journal of Geodesy》2006,79(12):689-693
By using Halley’s third-order formula to find the root of a non-linear equation, we develop a new iterative procedure to solve an irrational form of the “latitude equation”, the equation to determine the geodetic latitude for given Cartesian coordinates. With a limit to one iteration, starting from zero height, and minimizing the number of divisions by means of the rational form representation of Halley’s formula, we obtain a new non-iterative method to transform Cartesian coordinates to geodetic ones. The new method is sufficiently precise in the sense that the maximum error of the latitude and the relative height is less than 6 micro-arcseconds for the range of height, −10 km ≤ h ≤ 30,000 km. The new method is around 50% faster than our previous method, roughly twice as fast as the well-known Bowring’s method, and much faster than the recently developed methods of Borkowski, Laskowski, Lin and Wang, Jones, Pollard, and Vermeille. 相似文献