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211.
This paper describes the GPS applicability for detecting the vertical displacements of ground stations caused by ocean tide loading effects. An experiment was carried out using 12 permanent GPS stations located in the coastal area of Korea using data in the period 1 July until 26 August 2003. The relative height differences were calculated from hourly DGPS data processing based on the carrier-phase observation. The power spectra of the M2 and N2 constituents of ocean tide loading were derived using the CLEAN algorithm. The differential vertical displacements generated by the ocean tide loading effect are typically 3–25 mm in coastal area of the Korea. We compared the results from GPS with those of the ocean tide models, NAO.99Jb regional model and GOT00.2, FES99 global models. The M2 (N2) amplitude differences of vertical displacements between GPS and GOT00.2 is 1.22 ± 3.61 mm (1.01 ± 1.48 mm), and that of the M2 (N2) amplitude difference between GPS and FES99 is 0.04 ± 4.64 mm (0.64 ± 1.75 mm), whereas the M2 (N2) amplitude difference between GPS and NAO.99Jb are 0.05 ± 1.03 mm (0.86 ± 1.18 mm). The highest vertical displacements at the PALM station are found for 24.5 ± 0.7 mm from GPS observation, and 22.9 mm from the regional model NAO.99Jb and 13.17 and 10.00 mm from the global models GOT00.2 and FES99, respectively. These values show that the vertical displacements derived from GPS are in good agreement with those of the regional model NAO.99Jb around Korea, more than with the global models. This result indicated that GPS is an effective tool to measure the vertical displacement caused by the ocean tide loading effect in the coastal area, and we need to use the NAO.99Jb ocean tide model rather than the global ocean tide models in and around the Korean peninsula for position determination with permanent GPS installations. This work demonstrates that vertical displacement caused by the M2 and N2 constituents of ocean tide loading can be measured by carrier-phase DGPS.  相似文献   
212.
中层大气中重力波饱和机制的数值分析   总被引:2,自引:1,他引:2       下载免费PDF全文
通过对向上传播的重力波波包在中层大气中的非线性传播过程进行数值模拟,讨论中层大气中重力波的饱和机制.数值模拟结果表明,向上传播的重力波波包的扰动振幅在接近波包的本征水平相速度之前随高度单调增长,而当波振幅接近本征水平相速度时,在对流不稳定区域出现等位温面的翻转,同时波振幅的增长达到饱和(波振幅随高度不发生变化).小尺度对流在等位温面的翻转和波饱和发生后产生,随后波包开始破碎,这些非线性过程的最终结果产生湍流.表明导致重力波饱和的关键因素是等位温面的翻转而不是诸如波破碎、湍流、波-流相互作用等其他的一些物理过程.  相似文献   
213.
分析了造成波浪衰减几种力学机制,并针对不同模型海底底床下的波浪衰减,以及有限深底床和无限深底床的波浪衰减进行了计算比较,认为造成波浪衰减的力学机制直接和底床砂质的性质相关。  相似文献   
214.
解决污水快速渗滤土地处理系统占地突出的新方法   总被引:22,自引:1,他引:22  
根据污水快速渗滤土地处理系统的主要特点和局限 ,针对该系统占地突出这一问题 ,提出了通过采用人工填料 ,提高水力负荷 ,加快污水在系统中的渗透速度 ,从而减小系统占地面积的新方法。对随水力负荷的提高使系统可能产生的出水水质变差、介质堵塞以及投资费用增高等问题进行了分析 ,并且对在涿州进行的现场小型工程的试验进行了验证。得出结论认为改进的人工构建快速渗滤系统切实可行。  相似文献   
215.
In this paper, the response of a visco-elastic half-space subjected to moving loads with static and dynamic components is investigated. Four types of vehicle loads are considered, including the moving point load, uniformly distributed wheel load, elastically distributed wheel load, and a train load simulated as a sequence of elastically distributed wheel loads. In each case, the influence of the moving loads traveling in the subsonic, transonic and supersonic ranges on the dynamic responses of the half-space is studied. The parametric study conducted herein enables us to grasp insight into the mechanism of wave propagation for a visco-elastic half-space under moving loads.  相似文献   
216.
For transient, high frequency, and pulse like excitation of structures in the near field of strong earthquakes, the classical design approach based on relative response spectrum and mode superposition may not be conservative. For such excitations, it is more natural to use wave propagation methods. In this paper (Part I), we review several two-dimensional wave propagation models of buildings and show results for theoretical dispersion curves computed for these models. We also estimate the parameters of these models that would correspond to a seven-story reinforced concrete building in Van Nuys, California. Ambient vibration tests data for this building imply vertical shear wave velocity βz=112 m/s and anisotropy factor βxz=0.55 for NS vibrations, and βz=88 m/s and βxz=1 for EW vibrations. The velocity of shear waves propagating through the slabs is estimated to be about 2000 m/s. In the companion paper (Part II), we estimate phase velocities of vertically and horizontally propagating waves between seven pairs of recording points in the building using recorded response to four earthquakes.  相似文献   
217.
拱坝系统三维非线性地震波动分析   总被引:18,自引:1,他引:18  
本文将显式有限元结合外推人工边界的方法发展应用于三维非线性近场波动问题的研究。首次提出了拱坝-库水-地基系统三维非线性地震反应波动分析方法,并与传统的无质量地基分析方法进行了比较。  相似文献   
218.
Cyclic triaxial tests have been carried out on a skeletal carbonate sand from the west coast of Eire. Results are presented for undrained cyclic shear tests on samples with 80% of relative density consolidated under both isotropic and anisotropic conditions. Failure was defined as a 5% double amplitude cyclic strain and a 5% peak axial strain for stress-reversal and non-reversal stress conditions, respectively. Using this definition the cyclic strength for isotropically consolidated samples was affected by the confining pressure although the angular platey nature of the sand resulted in higher cyclic strengths than for a comparable silica sand. For anisotropically consolidated samples the cyclic strength increased with increasing initial static shear stress while on the other hand the cyclic strength normalised in the usual way with respect to the initial confining pressure decreased as this pressure increased.  相似文献   
219.
不同温压条件下弹性波在岩石中传播速度的实验研究   总被引:10,自引:0,他引:10       下载免费PDF全文
马瑞  卢民杰 《地震地质》1996,18(3):259-265
对以岩浆岩为主的岩石类型进行了不同温压条件下弹性波传播速度的实验研究,结果表明:(1)岩石的物质组成是决定弹性波传播速度的主要因素。以岩浆岩为例,由酸性到基性波速呈增加趋势;(2)岩石中弹性波的传播速度随环境条件改变而变化。一般说来,随温压条件的升高而升高  相似文献   
220.
地震地面运动的转动随机模型   总被引:2,自引:0,他引:2  
李宏男  王苏岩 《地震研究》1992,15(3):334-343
In this paper, the characteristics of rotational power spectra in different sites are analyzed according to the relationship between the rotations and translations of ground motion from the elastic wave theory, and then the unified mathematical model of the spectra (including the torsion and rocking) is presented. Through the use of a lot of earthquake records and curve-fitting of the least square method, the statistical results of rotational power spectral parameters in defferent sites are given.  相似文献   
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