多道瞬变电磁法共中心点道集数据联合反演   总被引：2，自引：2，他引：0       下载免费PDF全文

李海  薛国强  钟华森  底青云 《地球物理学报》2016,59(12):4439-4447

多道瞬变电磁法是目前地面资源勘查领域的研究热点,开展该方法观测数据的一维反演对完成装备研发及技术推广具有积极的推动作用.针对多道瞬变电磁法特殊的源波形和数据采集方式,本文对多道瞬变电磁数据的响应提取和一维反演进行了研究.首先,采用反卷积方法从伪随机二进制序列全波形响应数据中提取大地脉冲响应.为了避免脉冲响应中空气波的干扰,提出采用反向积分算法,把脉冲响应转换成下降沿阶跃响应,并将其整理成共中点道集.最后,为充分利用各个偏移距下的响应数据对不同深度范围目标体的分辨能力,采用基于OCCAM算法的联合反演方法对共中心点道集数据进行联合反演.结果表明在不同目标体深度以及有噪声干扰的情况下,共中心点道集数据联合反演计算均可获得较好的结果.  相似文献   

Improvements for the smooth joint contact model of the particle flow code and its applications     

《Computers and Geotechnics》2017

This paper deals with two shortcomings of the smooth-joint contact model (SJCM) used in the particle flow code (PFC). The first shortcoming is the increase of the shear strength of the joint when the shear displacement of the joint exceeds a specific value that is related to the particle size. This problem is named as the interlocking problem, which is caused by the interlocking particles. It occurs due to a shortcoming of the updating procedure in the PFC software related to the contact conditions of the particles that lie around the intended joint plane during high shear displacements. This problem also increases the dilation angle and creates unwanted fractures around the intended joint plane. To solve this problem two new approaches are proposed in this paper: (1) joint plane checking (JPC) approach and (2) joint sides checking (JSC) approach. These approaches and the regular approach are used to model: (a) the direct shear test using the PFC^2D and PFC^3D, (b) the biaxial test on a sample having a persistent joint with a dip angle varying from 0° to 90° at an interval of 15° using the PFC^2D and (c) the polyaxial test on two samples, one of them having a joint with a dip direction of 0° and the dip angle varying from 0° to 90° at an interval of 15°, and the other sample having a joint with a dip angle of 60° and the dip direction varying from 0° to 90° at an interval of 15° using the PFC^3D. All numerical results show that the JPC and JSC approaches can solve the interlocking problem. Also, they proved to be more consistent with the theory compared to the regular approach. However, the JPC approach leads to a slightly softer joint. Therefore, the JSC approach is suggested for jointed rock modeling using the PFC. The other shortcoming of the SJCM dealt within this paper is its inability to capture the non-linear behavior of the joint closure varying with the joint normal stress. This problem is solved in this paper by proposing a new modified smooth-joint contact model (MSJCM). MSJCM uses a linear relation between the joint normal stiffness and the normal contact stress to model the non-linear relation between the joint normal deformation and the joint normal stress observed in the compression joint normal stiffness test. A good agreement obtained between the results from the experimental test and the numerical modeling of the compression joint normal test shows the accuracy of this new model.  相似文献   

江苏中、南部及邻区地震重新定位及在断层研究中的应用   总被引：1，自引：0，他引：1       下载免费PDF全文

刘建达  李清河  张元生  金淑梅 《地球物理学进展》2009,24(1):58-66

本文分析了地震相对定位的双差法和地壳结构与定位联合反演方法的优势与局限性,在联合反演中用遗传算法最优化,将上述两种方法结合,对江苏省中南部和相邻地区进行地震重新精定位.先对研究区进行地壳结构与定位联合反演,然后用得到的地壳结构,用双差法进行相对定位.就该区主要断层的平面分布及与地震的关系,溧阳6.0级地震、南黄海6.2级地震、常熟-太仓5.1级地震的震源深度与发震构造,常熟一张家港间震群的震源深度进行了分析讨论.  相似文献   

海上多次波的联合衰减法   总被引：1，自引：0，他引：1       下载免费PDF全文

王建立  王真理  张洪宙  方正茂  李学良  杨长春 《地球物理学进展》2009,24(6):2070-2078

地震勘探尤其是海上地震勘探中存在着各类多次波,由于多次波的存在严重影响了速度分析、叠加、偏移成像等地震资料处理,海上多次波主要有全程多次波和层间多次两大类,为了压制海上不同类型的多次波,本文首先分析波场外推、预测反褶积和拉东变换衰减不同多次波的理论基础,然后联合采用这些方法,分别衰减全程多次波和层间多次波;即：首先对炮记录或者接收点记录进行波场外推,建立海底多次波模型,预测并减去全程多次波,然后利用预测反褶积衰减掉周期性明显的多次波,最后将数据转换到τ-p域,用拉冬变换根据同一时间多次波和有效波在速度等方面的差异,进一步分离层间多次波和剩余的全程多次波,并在该域中切除分离出的多次波,从而实现联合多次波衰减处理.通过对悉尼海区和里海等实际地震资料的处理证明,文提出的联合多次波衰减方法在海洋地震资料的处理中有着广泛的应用,联合衰减多次波处理流程具有快速、简洁、易于实现的特点,经处理后的地震资料有效信号损失小、保福性好的特点,有利于速度分析、叠加、叠前偏移等的后续处理工作.  相似文献   

Constraining the anisotropy structure of the crust by joint inversion of seismic reflection travel times and wave polarizations   总被引：2，自引：0，他引：2  

Jingyi Chen  Jiwen Teng  José Badal 《Journal of Seismology》2009,13(2):219-240

In the context of wide-angle seismic profiling, the determination of the physical properties of the Earth crust, such as the elastic layer depth and seismic velocity, is often performed by inversion of P- and/or S-phases propagation data supplying the geometry of the medium (reflector depths) or any other structural parameter (P- or S-wave velocity, density...). Moreover, the inversion for velocity structure and interfaces is commonly performed using only seismic reflection travel times and/or crustal phase amplitudes in isotropic media. But it is very important to utilize more available information to constrain the non-uniqueness of the solution. In this paper, we present a simultaneous inversion method of seismic reflection travel times and polarizations data of transient elastic waves in stratified media to reconstruct not only layer depth and vertical P-wave velocity but also the anisotropy feature of the crust based on the estimation of the Thomsen’s parameters. We carry out a checking with synthetic data, comparing the inversion results obtained by anisotropic travel-time inversion to the results derived by joint inversion of seismic reflection travel times and polarizations data. The comparison proves that the first procedure leads to biased anisotropic models, while the second one fits nearly the real model. This makes the joint inversion method feasible. Finally, we investigate the geometry, P-wave velocity structure and anisotropy of the crust beneath Southeastern China by applying the proposed inversion method to previously acquired wide-angle seismic data. In this case, the anisotropy signature provides clear evidence that the Jiangshan-Shaoxing fault is the natural boundary between the Yangtze and Cathaysia blocks.  相似文献   

新疆柯坪块体震源参数的初步研究与应用   总被引：1，自引：0，他引：1       下载免费PDF全文

潘振生  刘辉  谷美菊  李晓东  沈琦 《地震工程学报》2010,32(4):357-362,410

采用多台多地震联合反演的方法得到了新疆柯坪块体2006-2008年53次MS≥3.0中小地震的震源谱,进而计算了103次MS≥2.5地震的应力降、地震矩、震源破裂半径、视应力等震源参数,并讨论了它们与震级之间的关系。在此基础上分析了2006年以来柯坪块体上普昌断裂两侧区域及整个块体上应力降和地震视应力空间演化特征,并结合柯坪5.2级地震对研究结果应用于地震趋势预测和短临跟踪的可行性进行了探讨。  相似文献   

4 种重金属离子对中华鳖(Trionyx sinensis)稚鳖的急性致毒效应   总被引：1，自引：0，他引：1       下载免费PDF全文

王志铮  吕敢堂  施建军  申屠琰  毛文举 《海洋与湖沼》2009,40(6):745-752

以5日龄中华鳖稚鳖为实验动物,采用静水停食实验法,在水温(27.4±1.3)℃条件下,开展了Hg2+、Cr6+、Cu2+、Zn2+对中华鳖稚鳖的急性毒性和加和等毒性强度联合毒性试验。结果表明,4种重金属离子对中华鳖稚鳖均呈现以蓄积为主导的急性毒发效应,Cr6+、Zn2+对中华鳖稚鳖的急性致毒高峰期明显滞后于Hg2+、Cu2+;4种重金属离子毒性大小依次为Hg2+、Cu2+、Cr6+、Zn2+,其对中华鳖稚鳖96h的半致死质量浓度分别为5.98、16.42、28.90和91.88mg/L;所构建的中华鳖稚鳖累积死亡概率与重金属质量浓度和实验时间之间的数学模型,以及半致死时间-质量浓度回归方程,可作为侦查和分析重金属离子排放时间和致中华鳖稚鳖大量死亡时间的重要计算工具;Hg2+、Cr6+、Cu2+、Zn2+离子两两组合在加和等毒性强度下对中华鳖稚鳖96h联合急性毒性所呈现的致毒特征与离子种类及其毒性强度匹配情形密切相关。  相似文献   

论渔业法之违反捕捞许可规定到共同管理渔区作业行为的法律责任          下载免费PDF全文

洪洁  裴兆斌 《海洋开发与管理》2022,39(1):38-42

近年来我国渔业作业群体的数量明显增多,同时违反捕捞许可到共同管理渔区作业的违法行为也日益严重。在《中华人民共和国渔业法》及相关渔业立法中已经存在明确界定,但是对于法律责任没有具体阐明,严重影响了渔业活动的正常秩序与渔业资源的可持续发展。文章根据违反捕捞许可到共同管理渔区作业的现状出发,结合渔业法等相关规定,分析增设法律责任的必要性与可行性,提出完善相关法律责任,细化责任认定;加大惩治力度,提高违法成本等建议。  相似文献   

基于流程控制的国际气象通信数据收集管理系统的设计与实现          下载免费PDF全文

顾文静  王鹏  戴晴  韩鑫强 《气象科技》2023,51(1):31-39

近年来,天气和气候业务对国外数据种类和时效要求不断提高,为解决大量数据的收集分发压力以及管理问题,设计并实现了基于流程控制的国际气象通信数据收集管理系统。系统应用数据收集器Logstash、Inotify监听机制与分析平台Kibana等技术,支持多种通信协议,扩展Scrapy网络爬虫功能,通过流程控制、任务调度等方式实现大量数据快速高效收集和集成管理,有效提高数据并行处理能力和可扩展性,且设计了全流程监视,保障数据时效。系统已经上线提供服务,为业务/科研用户提供全球观测数据、国外卫星数据和数值预报产品等300余种,日收集数据量约2 TB。  相似文献