|本期目录/Table of Contents|

[1]段元泽,付虹,白宝荣,等.云南云县地震台形变观测的降水效应分析*[J].地震研究,2017,40(02):241-247.
 DUAN Yuanze,FU Hong,BAI Baorong,et al.Precipitation Effect Analysis with Deformation Measured Value in Yunxian Seismic Station in Yunnan[J].Journal of Seismological Research,2017,40(02):241-247.
点击复制

云南云县地震台形变观测的降水效应分析*(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
40
期数:
2017年02期
页码:
241-247
栏目:
出版日期:
2017-04-23

文章信息/Info

Title:
Precipitation Effect Analysis with Deformation Measured Value in Yunxian Seismic Station in Yunnan
作者:
段元泽1付虹2白宝荣1杨春华1李智蓉2
(1.普洱市地震局,云南 普洱 665000; 2.云南省地震局,云南 昆明 650224)
Author(s):
DUAN Yuanze1FU Hong2BAI Baorong1YANG Chunhua1LI Zhirong2
(1. Pu’er Seismological Bureau,Pu’er 665000,Yunnan,China)(2. Earthquake Administration of Yunnan Province,Kunming 650224,Yunnan,China)
关键词:
洞体应变 水管倾斜 降水影响 异常提取 云县地震台
Keywords:
the cavity strain inclined pipe precipitation effect anomaly extraction Yunxian Seismic Station
分类号:
P315.725
DOI:
-
摘要:
对云南云县地震台洞体应变和水管倾斜观测值与降水量的对比分析,结果表明,云县年降水总量每增加200 mm,洞体应变和水管倾斜的增量分别约为4 000×10-8和90″; 月降水增加100 mm,云县洞体应变和水管倾斜月变幅的增量分别约为38×10-8和2.5″。构建月降水和月增量的线性方程,求取测值与理论值的残差,发现当残差量大于1倍均方差后,短期内台站周边500 km范围内均有5.5级以上地震发生。距离台站最近的昌宁5.1级地震前,异常幅度最大,表明排除降水干扰后的变形增大,多与构造活动有关。
Abstract:
In this article,through comparative analysis on the cavity strain and inclined pipe observation value and precipitation in Yunxian seismic station,we found that there have a certain correlation between each other.Quantitative analysis result shows,the total annual precipitation increased by 200 mm,the influence on the cavity strain is 4 000×10-8 and the influence on the inclined pipe observation value is 90″; The monthly precipitation increased 100 mm,the cavity strain and inclination observation value increase monthly in amplitude,are respectively 38×10-8 and 2.5″. After constructing the linear equation of monthly precipitation and monthly increment,the residual of measured value and theoretical value are obtained.When the residual quantity is 1 times more than the mean square deviation,there are M≥5.5 earthquakes occurred in the vicinity of 500 km from station in the short term.The nearest distance station from Changning MS5.1 earthquakes shows the maximum amplitude of anomaly,which shows that the deformation increases after the precipitation disturbance,and are related to the tectonic activity.

参考文献/References:


陈金海,晏枫桐,韩新民,等.1979.龙陵地震前兆异常特征及其前兆场理论初探[J].地震研究,2(1):1-10.
陈立德,付虹.2010.汶川8.0级地震前兆异常对比研究[J].内陆地震,24(4):289-297.
梁楠.2012.差分曲线关系与地震前兆数据特征研究[J].陕西教育学院学报,28(4):81-85.
刘序俨,张雁滨.1991.排除形变观测数据中降水干扰的数学物理方法的研究[J].地震形变与地震,11(1):36-40.
卢艳清,王贤仁.1992.澜沧—耿马大震的短临形变特征[J].内陆地震,6(4):377-382.
邱桂兰.2015.芦山M7.0 级与汶川M8.0 级地震前兆异常对比[J].四川地震,(1):14-20.
孙伶俐,罗俊秋,龙涛,等.2010.大气降水对数字化地倾斜观测干扰特征分析[J].大地测量与地球动力学,30(增刊1):105-110.
杨继登,唐吉阳.1988.富民5.2级地震的前兆异常与监测预报[J].地震研究,11(5):455-462.
杨婕,占惠,凌学才,等.2009.强降水对厦门地震台伸缩仪的影响[J].大地测量与地球动力学,29(增刊1):76-79.
张晶,牛安福,高福旺,等.2003.数字化形变观测提取的地震短临异常特征[J].地震,23(1):70-76.
张燕,吴云.2010.2008年汶川地震前的形变异常及机理解释[J].武汉大学学报·信息科学版,35(1):25-29.
赵慈平,虎雄林,付 虹,等.2003.2001年10月27日云南永胜6.0级地震的前兆异常特征[J].地震研究,26(2):126-135.

备注/Memo

备注/Memo:
收稿日期:2016-12-13
基金项目:地震科技星火计划项目(XH13022)资助.

更新日期/Last Update: 2017-06-10