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地下水井水位及化学组分的同震差异响应特征分析--以青白江地震为例 被引量:1
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作者 顾鸿宇 王东辉 +5 位作者 李胜伟 郑万模 刘港 向元英 李丹 陈能德 《水文地质工程地质》 CAS CSCD 北大核心 2021年第6期44-53,共10页
相邻监测井的同震差异响应分析是研究地下水同震响应机理的路径之--。2020年2月3号青白江地震引发了龙泉山地下水监测井水位及水质的异常变化。利用多种水化学组分及水位的自动监测数据分析了相邻两口监测井的同震差异响应特征,讨论了... 相邻监测井的同震差异响应分析是研究地下水同震响应机理的路径之--。2020年2月3号青白江地震引发了龙泉山地下水监测井水位及水质的异常变化。利用多种水化学组分及水位的自动监测数据分析了相邻两口监测井的同震差异响应特征,讨论了水化学组分及水位差异响应机理。在相同能量密度情况下,ZK1水位变幅较ZK6大,表明ZK1对本次地震响应的敏感性高于ZK6。地震主要引起了处于还原环境(E_(h)<0)的第二含水层(主要离子为NH_(4)^(+)和NO_(3)^(-))中地下水向ZK1的排泄,而处于氧化环境(E_(h)>0)的第一含水层(高浓度C1^(-),高TDS及pH)中地下水主要向ZK6排泄。不同含水层水体向井排泄和混合是造成两口井地下水化学组分差异响应的原因。根据震后井水位及水化学组分的趋势变化规律分析,岩体在地震作用下的不排水体积改变是造成地下水水位阶跃变化的主要原因,ZK1周围第二含水层发生了塑性变形,渗透性发生了永久改变,而ZK6周围岩体发生弹性变形,渗透性未发生永久改变。 展开更多
关键词 监测井 水化学组分 水位 同震响应 含水层渗透性
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An Overview of Formation Mechanism and Disaster Characteristics of Post-seismic Debris Flows Triggered by Subsequent Rainstorms in Wenchuan Earthquake Extremely Stricken Areas 被引量:6
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作者 NI Huayong TANG Chuan +3 位作者 zheng wanmo XU Ruge TIAN Kai XU Wei 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2014年第4期1310-1328,共19页
The Wenchuan earthquake induced large amounts of debris flows and catastrophic incidents triggered by subsequent rainstorms occurred frequently in the past 6 rainy seasons, and thus resulted in serious casualties, hug... The Wenchuan earthquake induced large amounts of debris flows and catastrophic incidents triggered by subsequent rainstorms occurred frequently in the past 6 rainy seasons, and thus resulted in serious casualties, huge economic loss and long-term impact. In this paper, post-seismic debris flows distributed in 10 Wenchuan earthquake extremely stricken counties were verified and debris flow database consisting of 609 debris flows was established based on detailed investigation organized by Land and Resources Department of Sichuan Province. Combined with database and related studies, the impact of Wenchuan earthquake on debris flows was analyzed. And then variation of formation conditions including rainfall threshold and landform condition was analyzed by contrasting pre-seismic and post-seismic debris flows. Followed are some typical viewpoints on initiation mechanism of post-seismic debris flows. In the end of this paper, characteristics of postseismic debris flows triggered by subsequent rainstorms were comprehensively summarized, such as regional group occurrence, high frequency, high viscosity, chain effect, huge dynamics, large scale and long duration. We hope this paper will be helpful in understanding the formation mechanism, disaster characteristics and prevention countermeasures of post-seismic debris flows in Wenchuan earthquake extremely stricken areas. 展开更多
关键词 Wenchuan earthquake Post-seismic debris flow Gully-type debris flow Formationmechanism Disaster characteristic
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