山东省地震台站管理与地震仪器运维保障工作的思考

地震台站管理以及地震仪器设备的运维保障工作一直以来都是地震监测台网中十分重要的关键环节,这直接关系到地震观测数据产出的质量,对地震监测与地震预报分析研究工作意义重大。所以如何确保地震仪器设备能够高效率、低故障率的运行就成为人们十分关注的问题。文章分析了山东省地震台站管理的现状以及地震仪器设备运行过程中常见的问题,并针对性地给出了一些意见和建议,希望可以给有关地震工作人员以启发。     

福建省地震台站防雷系统改造分析

对雷电预警、电源分级防雷、信号防雷、地网建设和综合布线等多种综合防雷技术在福建省地震台站推广使用的关键点进行阐述说明,该技术在实际地震监测中取得较好的效果,可有效减轻雷击对地震观测系统仪器设备的损坏。     

全球大震和中国及邻区中强震地震活动（2006年12-2007年1月）.

本目录中的地震参数来自"中国地震台站观测报告"(简称"月报").其中,国内及邻区给出M≥4.7的事件,全球给出M≥6的事件."月报"由中国地震台网中心按月做出.     

对局属地震台站管理工作的思考

介绍了青海省地震台站的现状，对专业地震台站的管理工作，提出了一些建议。     

无人机低空摄影构建影像点云的线路巡检方法

针对当前架空输电线路人工巡检方法存在的劳动强度大、条件艰苦、危险性高且效率低等问题,提出了一种基于无人机低空摄影构建影像点云的输电线路巡检方法。首先阐述了总体技术路线,研究了架空线路无人机影像拍摄方法、航线敷设方法及山区变高飞行航高设计方法,然后利用影像数据进行电力线量测及重建、线路通道场景三维重建以及架空线路障碍物探测,通过试验案例详细对本文方法进行精度分析。试验结果证明,该方法仅依靠低成本设备即可实现可靠的线路巡检,大大降低了现有输电线路的巡检成本,提升树障检测的质量和效率,能保证线路安全运维。     

全球大震和中国及邻区中强震地震活动(2011年7-8月)

本目录中的地震参数来自"中国地震台站观测报告"(简称"月报").其中,国内及邻区给出M≥4.7的事件,全球给出M≥6.0的事件."月报"由中国地震台网中心按月做出.本目录中的发震时刻采用协调世界时(UTC);为了方便中国读者,也给出北京时(BTC).震中位置除给出经     

揭秘日本地震监测系统

2011年3月11日,日本本州三陆冲发生9．0级特大地震,由864个台站组成的高灵敏度测震台网Hi—net、1028个台站组成的强震台网K-net、688个台站组成的基盘强震台网KK—net、83个宽频带地震台站组成的宽频带台网F—net以及205个台站组成的日本气象厅（JMA）地震台网组成的日本地震监测系统,     

一种基于机载激光点云的门型电塔精确提取方法

随着无人机技术的发展,越来越多的电力部门采用机载激光雷达及倾斜摄影测量技术代替传统的人工方法,进行电力巡检、电力部件检修等工作。门型电塔为目前电力走廊中比较常见的一种高压电塔。在无数据标签的电网点云数据中,对门型电塔进行精确点云提取是门型电塔日常维护的重要工作。本文从包含有地面、植被、电力线、门型电塔的电网点云数据入手,首先对点云进行体素化分割,对体素网格进行高程连续与高程阈值的筛选,并对电塔顶部进行扩展搜索,达到去除地面点及植被点的目的。然后根据门型电塔水平投影成条状的特点,利用门型电塔的圆柱杆塔部分得到门型电塔的水平投影直线,再通过距离阈值判断去除点云中多余的电力线点。本文介绍的方法实现了从无标签的电网点云数据中对门型电塔的精确提取,为进一步进行门型电塔的三维建模、维护检修等工作提供了数据基础。     

Did the Ms7.0 Lushan earthquake dynamically trigger earthquakes in the Datong volcanic region （Shanxi Province）？

Immediately following the Ms7.0 Lushan earthquake on April 20, 2013, using high-pass and low- pass filtering on the digital seismic stations in the Shanxi Province, located about 870-1,452 km from the earthquake epicenter, we detected some earthquakes at a time corre- sponding to the first arrival of surface waves in high-pass filtering waveform. The earthquakes were especially noticed at stations in Youyu （YUY）, Shanzizao （SZZ）, Shanghuangzhuang （SHZ）, and Zhenchuan （ZCH）, which are located in a volcanic region in the Shanxi Province,but they were not listed in the Shanxi seismic observation report. These earthquakes occurred 4-50 rain after the passage of the maximum amplitude Rayleigh wave, and the periods of the surface waves were mainly between 15 and 20 s following. The Coulomb stresses caused by the Ray- leigh waves that acted on the four stations was about 0.001 MPa, which is a little lower than the threshold value of dynamic triggering, therefore, we may conclude that the Datong volcanic region is more sensitive to the Coulomb stress change. To verify, if the similar phenomena are widespread, we used the same filtering to observecontrastively continuous waveform data before, and 5 h after, the Ms7.0 Lushan earthquake and Ms9.0 Tohoku earthquake in 2011. The results show that the similar phenomena occur before the earthquakes, but the seis- micity rates after the earthquakes are remarkably increased. Since these weak earthquakes are quite small, it is hard to get clear phase arrival time from three or more stations to locate them. In addition, the travel time differences between P waves and S waves （S-P） are all less than 4 s, that means the events should occur in 34 km around the stations in the volcanic region. The stress of initial dynamic triggering of the Ms9.0 Tohoku earthquake was about 0.09 MPa, which is much higher than the threshold value of dynamic triggering stress. The earthquakes after the Ms9.0 Tohoku earthquake are related to dynamic triggering stress, but the events before the earthquake cannot be linked to seismic events, but may be related to the back- ground seismicity or from other kinds of local sources, such as anthropogenic sources （i.e., explosions）. Using two teleseismic filtering, the small background earthquakes in the Datong volcanic region occur frequently, thus we postulate that previous catalog does not apply bandpass filter to pick out the weak earthquakes, and some of the observed weak events were not triggered by changes in the dynamic stress field.