Theoretical analysis of non‐geometric PS‐waves recorded at the water bottom interface          下载免费PDF全文

Guy Drijkoningen 《Geophysical Prospecting》2016,64(3):543-553

When a seismic source is placed in the water at a height less than a wavelength from the water–solid interface, a prominent S‐wave arrival can be observed. It travels kinematically as if it was excited at the projection point of the source on the interface. This non‐geometric S‐wave has been investigated before, mainly for a free‐surface configuration. However, as was shown in a field experiment, the non‐geometric S‐wave can also be excited at a fluid–solid configuration if the S‐wave speed in the solid is less than the sound speed in the water. The amplitude of this wave exponentially decreases when the source is moved away from the interface revealing its evanescent character in the fluid. In the solid, this particular converted mode is propagating as an ordinary S‐wave and can be transmitted and reflected as such. There is a specific region of horizontal slownesses where this non‐geometric wave exists, depending on the ratio of the S‐wave velocity and the sound speed of water. Only for ratios smaller than 1, this wave appears. Lower ratios result in a wider region of appearance. Due to this property, this particular P‐S converted mode can be identified and filtered from other events in the Radon domain.  相似文献   

Non integrability of theJ 2 problem     

Maylis Irigoyen  Carles Simó 《Celestial Mechanics and Dynamical Astronomy》1993,55(3):281-287

We consider the motion of a massless particle around an oblate planet, keeping only in the expression of the perturbing potential the second degree zonal harmonic. We prove the analytical non integrability of this problem, by using Ziglin's theorem and the Yoshida criterion for homogeneous potentials.  相似文献   

Analysis of square and rectangular footings subjected to eccentric-inclined load resting on reinforced sand     

Swami Saran  Surendra Kumar  K.G. Garg  Arvind Kumar 《Geotechnical and Geological Engineering》2007,25(1):123-137

In the present paper, a method of analysis for calculating the pressure intensity corresponding to a given settlement for eccentrically and obliquely loaded square and rectangular footings resting on reinforced soil foundation has been presented. The process has been simplified by presenting non-dimensional charts for the various terms used in the analysis, which can be directly used by practicing engineers. An approximate method has been suggested to find out the ultimate bearing capacity of such footings on reinforced soil. The results have been validated with the model test results. The procedure has been made clear by giving an illustrative example.  相似文献   

静力与非静力平衡模式动力框架对比     

张发波  王斌  李立娟 《气象科技》2018,46(2):267-274

以WRF模式为例,从定性和定量两个方面分别对静力和非静力平衡模式动力框架进行了对比分析。结果表明:大气动力学过程中的非静力平衡特征信息可以由一个控制其打开和关闭状态的开关性变量来予以表示。该变量主要影响大气垂直运动,水平运动受其影响较小,且随着模式分辨率逐步提高,其影响更加显著。因此,可以将复杂耗时的非静力平衡特征信息整合问题转化为开关变量的数学建模问题,从而为解决上述问题开辟了一条可能的新路径。  相似文献   

吉林省农业界限温度条件变化规律研究   总被引：9，自引：3，他引：6  

马树庆  袭著香 《地理科学》1999,19(1):63-68

用线性回归,相对变率,非整数波及小波周期分析等方法,分析了自有气象记录以来,吉林省不同区域日平均气温稳定≥７℃初日,终日、≥１０℃积温及５￣９月平均气温之和等几项与农业生产有密切关系的界线温度条件的长期变化特征,揭示了它们的时间变化趋势和周期变化规律,探讨了未来１０ａ内这些条件的可能变化趋势及农业生产问题。  相似文献   

黄山第四纪泥砾沉积物分形结构特征与沉积环境分析   总被引：13，自引：0，他引：13  

周秉根 《地理科学》1999,19(1):92-94

黄山第四纪泥砾沉积物粒度组成的分维值介于２．７０８￣２．７５３之间,非常接近古泥石流堆积物粒度组成的典型分维值２．７５。结合沉积特征,表明该类沉积物属第四纪间冰缘环境下的稀性泥石流沉积,其形成过程与季风型冰缘环境有关,是两种环境综合作用的结果。  相似文献   

深水压电换能器电声性能的研究     

王清池 《海洋技术学报》1998,17(3):27-30

本文通过电换能器的等效机电图,根据压电陶瓷材料的有关参数随压力的变化关系,研究了深水压电换能器在深水高静压力下的电声性能。  相似文献   

Geostatistical seismic inversion for non‐stationary patterns using direct sequential simulation and co‐simulation          下载免费PDF全文

Hamid Sabeti  Ali Moradzadeh  Faramarz Doulati Ardejani  Leonardo Azevedo  Amilcar Soares  Pedro Pereira  Ruben Nunes 《Geophysical Prospecting》2017,65(Z1):25-48

Geostatistical seismic inversion methods are routinely used in reservoir characterisation studies because of their potential to infer the spatial distribution of the petro‐elastic properties of interest (e.g., density, elastic, and acoustic impedance) along with the associated spatial uncertainty. Within the geostatistical seismic inversion framework, the retrieved inverse elastic models are conditioned by a global probability distribution function and a global spatial continuity model as estimated from the available well‐log data for the entire inversion grid. However, the spatial distribution of the real subsurface elastic properties is complex, heterogeneous, and, in many cases, non‐stationary since they directly depend on the subsurface geology, i.e., the spatial distribution of the facies of interest. In these complex geological settings, the application of a single distribution function and a spatial continuity model is not enough to properly model the natural variability of the elastic properties of interest. In this study, we propose a three‐dimensional geostatistical inversion technique that is able to incorporate the reservoir's heterogeneities. This method uses a traditional geostatistical seismic inversion conditioned by local multi‐distribution functions and spatial continuity models under non‐stationary conditions. The procedure of the proposed methodology is based on a zonation criterion along the vertical direction of the reservoir grid. Each zone can be defined by conventional seismic interpretation, with the identification of the main seismic units and significant variations of seismic amplitudes. The proposed method was applied to a highly non‐stationary synthetic seismic dataset with different levels of noise. The results of this work clearly show the advantages of the proposed method against conventional geostatistical seismic inversion procedures. It is important to highlight the impact of this technique in terms of higher convergence between real and inverted reflection seismic data and the more realistic approximation towards the real subsurface geology comparing with traditional techniques.  相似文献   

Assessing Nutrient,Biomass, and Sediment Transport of Drainage Ditches in the Three Gorges Reservoir Area     

《洁净——土壤、空气、水》2017,45(1)

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