相邻两井对大地震的不同水力响应模型研究——页岩影响分析   总被引：1，自引：0，他引：1       下载免费PDF全文

张艳  符力耘  陈学忠  曹呈浩  赵连锋  马玉川 《地球物理学报》2019,62(1):143-158

大地震引起了左家庄和宝坻(相距～50km)两井中截然不同的同震水位响应.我们用水位的气压和潮汐响应来分析解释此现象.结果表明,宝坻井的观测含水层中存在页岩,且此井受裂隙影响很大,储水效应较差.页岩的复杂裂隙或者各向异性可能会导致此井观测含水层处于半封闭状态,从而导致垂直向排水的发生.通过多方计算分析后,我们将这两口井划分为两种模型—1.水平流动模型;2.水平流动+垂直流动的混合流动模型.由于裂隙影响,宝坻井的观测含水层介质与外界的水力沟通性在震前就较强(震前渗透率就比较大),所以宝坻井观测含水层与外界的孔隙压差异较小,导致同震渗透率上升较小甚至没有变化,这些因素是导致该井同震水位变化幅度总是非常微小的原因.  相似文献   

Stability analysis of seabed strata and casing structure during the natural gas hydrates exploitation by depressurization in horizontal wells in South China Sea     

Peng-fei Xie  Lin Yang  Qian-yong Liang  Xu-hui Zhang  Liang-hua Zhang  Bin Zhang  Xiao-bing Lu  Hui-ce He  Xue-min Wu  Yi-fei Dong 《China Geology》2022,5(2):300-309

Natural gas hydrates (NGHs) are a new type of clean energy with great development potential. However, it is urgent to achieve safe and economical NGHs development and utilization. This study established a physical model of the study area using the FLAC^3D software based on the key parameters of the NGHs production test area in the South China Sea, including the depressurization method, and mechanical parameters of strata, NGHs occurrence characteristics, and the technological characteristics of horizontal wells. Moreover, this study explored the law of influences of the NGHs dissociation range on the stability of the overburden strata and the casing structure of a horizontal well. The results are as follows. With the dissociation of NGHs, the overburden strata of the NGHs dissociation zone subsided and formed funnel-shaped zones and then gradually stabilized. However, the upper interface of the NGHs dissociation zone showed significant redistribution and discontinuity of stress. Specifically, distinct stress concentration and corresponding large deformation occurred in the build-up section of the horizontal well, which was thus prone to suffering shear failure. Moreover, apparent end effects occurred at the end of the horizontal well section and might cause the deformation and failure of the casing structure. Therefore, it is necessary to take measures in the build-up section and at the end of the horizontal section of the horizontal well to prevent damage and ensure the wellbore safety in the long-term NGHs exploitation.©2022 China Geology Editorial Office.  相似文献   

Kinetic energy budget and moisture flux convergence analysis during interaction between two cyclonic systems: Case study     

《Dynamics of Atmospheres and Oceans》2019

An analysis of the kinetic energy budget during a case of interaction between middle latitude and extratropical cyclones has been made in this work. Horizontal flux convergence constitutes a major energy sink. Generation of kinetic energy via cross-contour flow is a persistent source throughout the growth and decay periods. Dissipation of kinetic energy from subgrid to grid scales is an important source during the pre-storm period; it acts as a sink during the growth and decay periods. The major contribution to kinetic energy comes from a persistent upper tropospheric jet stream activity throughout the period of the cyclone development. The characteristics of moisture-flux components (divergent and rotational) along with precipitable water content for different tropospheric layers throughout the life cycle of our cyclone are also studied in this work. It is found that most of required humidity for our cyclone are initiated from Arabian Sea and then to some extent are reinforced over Gulf of Aden and east of central Africa and then by passing over Red sea enter to the south and south east of Mediterranean Sea. The rotational component of the moisture transport brings moisture from two regions; the first which is considered the main region is the Indian Ocean, Arabian Sea, Gulf of Aden and north east of Sudan. The second source region is the Atlantic and Mediterranean Sea. In the middle troposphere, the primary moisture source is found over central Africa, which in turn is traced to the Atlantic Ocean, the Indian Ocean, and the Arabian Sea. The upper-level moisture fluxes are weak and play a minor role over the area of interaction between two cyclones.  相似文献   

未知OBS水平方位的SKS分裂参数测量          下载免费PDF全文

司少坤  刘保华  刘晨光  杨挺  封志兵 《地球物理学报》2017,60(3):999-1006

宽频带海底地震仪(OBS)探测是研究海底深部结构最有效的地球物理方法,其中SKS分裂参数测量已被广泛应用于上地幔各向异性的研究.传统的SKS分裂参数测量需要知道确切的OBS水平分量方位,然而OBS的投放过程是自由式的,其两个水平分量在海底的方位是不确定的.本文通过SKS快慢波的运动学特性,发展了一种在未知OBS水平分量方位的情况下直接求取SKS分裂参数的方法,分别用合成地震图和实际观测到的远震资料对该方法进行了数值检验,表明其是一种有效的获得SKS分裂参数的方法,而且相比于传统的先确定OBS水平分量方位,再进行SKS分裂的方法,此方法能够同时获得SKS分裂参数和OBS水平分量方位,应用简便,且减少了累积误差,获得的SKS分裂参数可靠性更高.  相似文献   

注浆技术在砂卵石地层水平（定）导向钻进工程中的应用研究     

梁小强  张可能  赵自亮 《岩土钻凿工程》2011,(2):24-29

本人在借鉴前人成果并结合施工经验的基础上,系统总结了砂卵石地层与非开挖钻进施工的适应性,对非开挖钻进施工中出现的问题进行了归纳和分类,并对其原因进行了分析和探讨。同时,为了解决非开挖导向钻进在复杂地层特别是砂卵石层中的施工难题,考虑采用注浆预加固技术对砂卵石层进行预先加固,以提高其强度,保证非开挖导向钻进的顺利进行。更进一步地,对水平孔中注浆预加固的三种方法（垂直注浆法、导管注浆法、随钻注浆法）在导向钻进工程中的概念、适用范围、优缺点以及实施控制要点等进行了对比和研究。  相似文献   

水平层状岩体边坡动力响应中的结构面效应研究     

周剑  张路青  王学良 《工程地质学报》2011,19(3):352-358

根据应力波传播原理分析了水平层状岩体边坡中应力波传播特征,建立了应力波在该类边坡中传播的模型.利用离散元软件UDEC分析了不同频率垂向压缩应力波作用下边坡动力响应规律中的结构面效应.结果表明:边坡中的水平层面对坡顶的动力响应有明显影响.低频应力波作用下,水平层状岩体边坡坡顶的垂向峰值速度较均质坡体相同部位的峰值速度的增...  相似文献   

鄂尔多斯块体及其周缘上地幔各向异性分析研究   总被引：9，自引：5，他引：4       下载免费PDF全文

胡亚轩  崔笃信  季灵运  郝明 《地球物理学报》2011,54(6):1549-1558

对布设在鄂尔多斯块体及其周缘的固定宽频带地震台网90个台站记录作远震SKS波形资料偏振分析,采用最小切向能量法求得每个台站的SKS快波偏振方向和快慢波时差,获得块体及其周缘上地幔各向异性图像,并结合1999～2007年相对鄂尔多斯块体的GPS水平地壳运动速度场,分析块体及其周缘的各向异性特征和壳幔耦合特征并重新认识块体...  相似文献   

山西临汾中心地震台水平摆倾斜仪对全省及周边地区地震的异常响应     

张红秀  郭国祥  郭林旺  罗振东 《山西地震》2011,(4):1-4

2009年至今,山西境内及周边地区相继发生多次有感地震,文章着重分析几次地震前临汾台水平摆观测资料出现的异常变化和同震响应能力,并对资料在映震中存在的相关问题进行探讨,为准确利用水平摆资料预测、预报地震提供依据。  相似文献   

Dynamic characteristics and horizontal transports of internal solitons generated at the Columbia River plume front     

Jiayi Pan  David A. Jay 《Continental Shelf Research》2009

River plume front-generated internal solitons play an important role in the interaction between the plume and coastal waters. The internal solitons drive a non-harmonic velocity field, resulting in a horizontal transport that carries plume water seaward and redistributes nutrients and sediments. In this study, we present observations of internal solitons generated at the Columbia River plume front that separates the new, tidal plume, older plume and coastal waters. Scale analyses suggest that the plume front-generated internal solitons are highly non-linear waves, and their dynamic properties do not conform to any weakly non-linear theory. Thus, a high-order Korteweg–de Vries (KdV) theory is used to analyze the internal solitons. The comparison between theoretical values and cruise data shows that the high-order KdV model is much better than the weakly non-linear theories for prediction of the soliton dynamic parameters. Based on the model, we develop theoretical and numerical solutions of the soliton-induced upper layer horizontal transport and Lagrangian water parcel transport distance, which shows that the water particle drift, during the internal soliton passage, is as far as 1 km, and demonstrates the role of the internal solitons on the exchange between the plume and ambient coastal water. Energy fluxes caused by the internal solitons are estimated using the high-order KdV theory. The leading soliton fluxes 2.0×10³ W m⁻¹ per unit crest length, and carries energy of 4.2×10⁵ J m⁻¹. The total energy carried by the eight internal solitons is 1.6×10⁶ J m⁻¹, about 70% of the total frontal energy.  相似文献   

水平螺旋度在沙尘暴预报中的应用   总被引：1，自引：0，他引：1  

李岩瑛  张强 《气象学报》2012,70(1):144-154

为了更准确地预报中国北方沙尘暴的强度和范围,应用2002—2010年3—6月逐日08和20时高空流场资料、高空图资料和地面每3 h的天气图资料,计算近地面至500 hPa的水平螺旋度。结果表明,螺旋度负值中心值越大,辐合上升运动越强,风速越大,对应沙尘暴的强度就越强。螺旋度负值中心常常在河西走廊附近最强,沙尘暴发生在螺旋度负值中心附近或下游。在沙尘关键区(40°—48°N,84°—120°E)当出现螺旋度≤-600 m2/s2的负值中心时,6 h内该区或其下游将产生能见度低于500 m的强沙尘暴,螺旋度负值中心与下游沙尘暴发生区有良好的对应关系。通过对中国北方区域性强沙尘暴典型个例、甘肃省河西走廊东部沙尘天气的对比分析,螺旋度有较强的日变化,白天强于夜间,对冬春季中国北方干旱区的冷锋型沙尘暴天气有较强的预报能力。  相似文献