The Upper Limit Size of Reservoir-Induced Earthquakes     

Huang Fuqiong  Zhang Yan  Wu Zhongliang  Ma Lijie 《中国地震研究》2008,22(2):146-152

We showed the relation between the magnitude of induced earthquake and the reservoir storage and dam height based on the global catalog from 1967 to 1989 compiled by Ding Yuanzhang （1989）. By multiplying reservoir storage with dam height, we introduced a new parameter named EE. We found that the cases with specific EE and magnitude do not exceed a limit. Based on the discussion of its physics, we called EE the equivalent energy. We considered this limit as the upper limit of magnitude for reservoir-induced earthquakes. The result was proved by the recent cases occurring in China. This size limitation can be used as a helpful consideration for reservoir design.  相似文献   

Earthquake detection probability within a seismically quiet area: application to the Bruchsal geothermal field          下载免费PDF全文

Emmanuel Gaucher 《Geophysical Prospecting》2016,64(2):268-286

In applications such as oil and gas production, deep geothermal energy production, underground storage, and mining, it is common practice to implement local seismic networks to monitor and to mitigate induced seismicity. For this purpose, it is crucial to determine the capability of the network to detect a seismic event of predefined magnitude in the target area. The determination of the magnitude of completeness of a network is particularly required to properly interpret seismic monitoring results. We propose a method to compute the detection probability for existing local seismic networks, which (i) strictly follows the applied detection sequence; (ii) estimates the detection capability where seismicity has not yet occurred; and (iii) delivers the results in terms of probabilities. The procedure includes a calibration of a local magnitude scale using regional earthquakes recorded by the network and located outside the monitored area. It involves pre‐processing of the seismograms recorded at each station as performed during the triggering sequence, which is assumed based on amplitude thresholds. Then, the calibrated magnitude–distance–amplitude relations are extrapolated at short distances and combined to reproduce the network detection sequence. This generates a probability to detect a seismic event of a given magnitude at a specified location. This observation‐based approach is an alternative to a fully theoretical detection capability modelling and includes field conditions. Seismic wave attenuation by geometrical spreading and intrinsic attenuation, site effect, and instrumental responses are partly accounted for by the calibration. We apply this procedure on the seismic network deployed in the Bruchsal geothermal field (Germany). Although the system was in good working order, no induced seismicity was identified in the area between June 2010, when monitoring started, and November 2012. The recording of distant seismicity during this time period, however, allowed the application of the proposed procedure. According to the applied network detection parameters, the results indicate that the absence of seismicity can be interpreted as a 95% probability that no seismic event with M_L ≥ 0.7 occurred below the network at 2.4‐km depth, i.e., in the geothermal reservoir.  相似文献   

福建测震台网单台震级偏差与台站场地响应关系的初步分析     

杨贵  许振栋  林彬华 《中国地震》2016,32(4):674-684

利用福建测震台网2008年10月~2015年12月记录的每个事件至少有6个台站测算震级的3069个区域地震事件,进行单台震级与台网平均震级的偏差统计,获得了各台站的总的震级平均偏差为-0.31~0.68,并统计各台站测算震级所量取最大记录振幅相应的周期,获得优势周期为0.06~0.38s;通过Moya方法反演各测震台站的场地响应,获得98个台站对1~20Hz频带的场地响应,结果显示场地对某些频带信息有放大或抑制作用;通过比较Wood-Anderson地震仪摆固有0.8s周期所对应的场地响应、各台样本优势周期所对应场地响应的震级偏差与各台总的震级平均偏差,发现台站测算震级相应优势周期的场地响应的震级偏差与台站震级平均偏差有较好的线性关系,表明单台震级的偏差与测算震级所量取最大记录振幅相应的周期的场地响应有较大关系。  相似文献   

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张为民  王勇 《大地测量与地球动力学》2007,27(4):44-46

??10???????FG5-112?????????????й???????????????????о?????嶯??????????????????????68??????????ι????????????С??2??10 ^-8 ms ^-2???????????????????????С?????????????;????????????????????????????????????仯?????1??10 ^-8 ms ^-2 /a??????????λ???????-0.38 cm/a;??????????λ?仯??????????????????????????????  相似文献   

加蓬G4-188区块钻井技术实践认识     

石强 《海洋地质译丛》2008,(1):82-87

加蓬G4-188区块是一个新的海外勘探区块,在钻井过程中遇到了井壁垮塌、气侵、井斜控制困难等诸多难题,影响了钻井施工的速度。针对这些难题,实施了解决G4-188区块钻井施工难点的各项技术措施,为G4-188区块后续钻井施工提供了有益的技术支持。  相似文献   

基坑及周边建筑物变形监测方案   总被引：1，自引：0，他引：1  

冯文辰  刘欣  王永跃  刘绪广 《测绘与空间地理信息》2009,32(1)

结合某基坑变形监测项目,从观测墩及觇牌的设计、观测方法、精度估计等方面对基坑水平位移观测进行了介绍,并介绍了利用差异沉降量推算法进行倾斜观测的方法.  相似文献   

Research in Astronomy and Astrophysics CONTENTS     

《中国天文和天体物理学报》2014,(12)

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CMIP5模式对辽宁省气温模拟能力及未来2℃升温阈值出现时间评估     

王涛  王乙舒  沈玉敏  王艳  赵连伟  王小桃  沈历都 《气象与环境学报》2020,36(2):49-61

利用全球气候模式、多模式集合和辽宁省气象观测数据,评估了不同典型浓度路径下19个全球气候模式和多模式集合对辽宁省气温变化模拟能力和可信度。结果表明:最优模式模拟结果优于多模式集合,具有较高的可信度。随着全球二氧化碳排放浓度增加,气温变化率和可信度呈增加趋势,首次达到2℃年份呈提前趋势,大部分站点出现在2011年之前,且出现年份越晚,升幅往往越高,反之亦然。大部分站点首次稳定到达2℃阈值开始年份在2022年之前,结束年份出现在2019—2026年,持续时间在13 a以下,开始年份均呈西早—东晚分布形势,结束时间和持续时间分布较均匀,且随着全球二氧化碳排放浓度增加,升温幅度呈上升趋势。不同典型浓度路径下各区域最高温、最低温和平均气温出现年份和变化特征均比较一致。  相似文献   

1989—2019年中国滑雪场时空特征及其演变规律     

颉佳  王世金  窦文康  赵灿文 《地理科学》2022,42(6):1064-1072

滑雪场空间分布特征、集聚演变状况与分布方向性变化深刻影响着中国滑雪旅游乃至冰雪产业的发展。运用地统计学空间分析原理,通过最邻近指数分析、空间自相关分析、核密度分析、标准差椭圆及平均中心分析,对1990年前后每10 a 中国滑雪场空间特征及其演变规律进行了综合分析。结果显示：① 1990年之前,仅在黑龙江和吉林省有7家滑雪场,且分布较为离散。② 1990—1999年,滑雪场数量呈小幅增长,空间上出现向新疆、河北和四川扩散的现象。③ 2000—2009年,滑雪场增速较快,并形成了以哈尔滨?牡丹江、北京?张家口两地区为核心的滑雪场双核驱动模式。④ 2010—2019年,是滑雪场数量增速最快的10 a,期间新增滑雪场522家,并在双核驱动模式基础上,逐步形成了以长白山、燕山–太行山为主要条带的联通南北的滑雪场空间结构。总体上,近30 a中国滑雪场呈现出了“南展西扩东进”的空间演变特征。该研究结果对于未来中国滑雪场空间布局、优化及其区域间的协调发展具有一定的理论指导意义。  相似文献   

关于高精度航空磁测中的磁补偿原理及补偿效果评价的探讨   总被引：1，自引：0，他引：1  

刘浩  卢立波  杨望 《物探化探计算技术》2014,(4):431-435

对于高精度航空磁测来说,飞机磁干扰必须有效的消除,其方法是补偿飞行。补偿效果的好坏直接影响到物探飞行数据的质量,所以有必要采用一些量化指标对磁补偿的效果进行评价,从而对补偿飞行的质量进行有效地控制。这里介绍了飞机磁干扰场的补偿原理及两种评价补偿效果的指标:品质因数(FOM值)和标准差(σc),采用了这两个量化指标对磁补偿的效果进行评价,就能对补偿飞行的质量进行有效的控制。  相似文献