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云南地区氡异常与地震的统计特征分析

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通过梳理 1976-2022 年震例总结报告中云南地区 73 组MS≥5.0 地震的氡测项异常,对其特征予以统计分析.结果表明:73 组地震中有 63 组震前出现水氡异常,震前 6 个月内的短期异常占总异常的 71%,3 个月内的短临异常占总异常的 49%,地震前 3 个月异常数量增加显著;震级越大,异常分布越远离震中,震前 1 个月新出现的异常大部分集中在震中附近.相对而言,由于测点位置和观测技术方面的原因,气氡积累的震例远远少于水氡,但具有短期异常占比较高的优势.随着气氡观测技术的不断改进和观测经验的不断积累,其捕捉地震异常信息的能力也将会不断提升.
Statistical characteristics analysis on the relationship between radon anomalies and earthquakes in Yunnan region
This paper is based on the summary report of Yunnan earthquake cases from 1976 to 2022.It sorts out 73 sets of earthquakes with M≥5.0 one by one,and extracts abnormal information of radon measurement items before earthquakes,then explores the characteristics of radon precursory anomalies.The results are as follows:1)There were 190 water radon anomalies among 63 out of 73 earthquakes.There were a large number of anomalies and a low earthquake missing rate,indicating that water radon obser-vation have good monitoring capability for regional earthquakes.However,the proportion of gas radon anomalies is relatively low by comparison.In our earthquake cases,there were five gas radon anomalies among only four out of 39 earthquakes,showing a higher earthquake miss-ing rate.But as for the measurement sites with good basic conditions,gas radon anomalies have a high repetition rate,and correspond well to earthquakes.Among the five radon anomalies accumulated in historical earthquake cases,three of them were observed by gas radon well Gaoda.2)The water radon anomalies appeared mainly within six months before earthquakes with M≥5.0,accounting for 71%of the total anomalies.Among them,anomalies within three months account for 49%of the total anomalies.Starting from the year before the M5.0-5.9 earthquakes,the number of water radon anomalies in different stages increased significantly.One month before the earthquake,most of the anomalies showed a turning point and then returned to normal level,with a decrease in the number of anomalies.On the other hand,there are not many earthquake cases with abnormal gas radon concentration,but all anomalies are within six months before earthquakes,of which 80%are within three months.3)The spatial distribution of water radon anomalies is different before earthquakes with different magnitudes.Before the earthquakes with magnitude 5.0-5.9,the closer to the time of the earthquake occurrence,the more anomalies are concentrated near the epicenter.During the period of more than six months prior to the earthquake,the anomalies are scattered in space.Starting from six months before the quake,the number of anomalies within a 100 km radius of the epicenter gradually increased.Starting from one month before the earthquake,most of the anomalies outside the 100 km radius of the epicenter showed a turning point and then returned to normal level,the anomalies are concentrated near the epicenter,which can provide reference for location tracking.Before earthquakes with magnitude 6.0 or above,more water radon an-omalies appeared in the areas far from the epicenter,which were relatively scattered.Such an-omalies appearing in a large area may indicate that the stress levels in the entire field were in-creasing.In this state,potential risk of a major earthquake is likely higher.There are relatively few earthquake cases with gas radon anomalies,and the spatial distribution characteristics are not obvious.This paper is based on the summary report of earthquake cases,which shows that there are more anomalies in water radon than in gas radon,and the prediction effect is better than that of gas radon.This is consistent with the practical results reflected by the technical personnel after actual use of the data.Several possible main reasons are:Firstly,the observation sites of water radon are more focused on deep circulating hot spring water,which is more likely to reflect deep tectonic activity.Secondly,the observation methods of water radon and gas radon are dif-ferent.Water radon is observed by manually collecting water samples and detecting,and the technology is relatively stable.However,gas radon is observed automatically,but the stability of the devices for extracting radon gas from water and collecting it has not been fully solved,and the technology from gas collection to automatic detection process is not mature yet.In addi-tion,the efficiency and stability of degassing directly affect the observation quality of data.Thirdly,at some observation sites the escaping gas was extracted from static water level wells to observe the radon concentration,which is difficult to reflect information from deep Earth.Overall,the differences in the effectiveness of water radon and gas radon data in earth-quake prediction are caused by factors such as the location of measurement sites and observa-tion techniques.At present,the observation data of gas radon in Yunnan has not yet achieved the effect of water radon in earthquake prediction.However,gas radon observation has advant-ages that water radon does not have,such as higher automation,faster transmission,higher data sampling rates.Technology-oriented and intelligentization are the main development tend-ency of radon observation.With the improvement of observation technology and the accumula-tion of observation experience,the ability to capture seismic anomaly will also be strengthen.

radonseismic anomalyearthquake predictionstatistical characteristics

李琼、付虹、胡小静、杜家云、杨黎

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中国昆明 650224 云南省地震局

中国云南弥勒 652300 弥勒市地震局

地震异常 地震预测 统计特征

地震科技星火计划公关项目

XH230483C

2024

地震学报
中国地震学会 中国地震局地球物理研究所

地震学报

CSTPCD北大核心
影响因子:1.186
ISSN:0253-3782
年,卷(期):2024.46(2)
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