共查询到19条相似文献，搜索用时 187 毫秒
1.
山西奇村井水汞动态的映震能力与特征分析 总被引：1，自引：0，他引：1
山西奇村水汞动态受忻定盆地区域水化学特征控制,水汞映震灵敏,对山西境内ML≥4.0级地震有很好的前兆异常反应。水汞异常多为短临异常,对地震的时间预测有较好的参考价值。水汞异常反应与地震活动水平、震源深度等相关。 相似文献
2.
汞测量用于地震预报研究实例剖析 总被引：1，自引：1，他引：1
本文着重对1986—1988年先后在云南、北京、四川开展水汞测量的8个测点汞量变化与10次地震的关系进行了分析研究。获得的大量数据表明:水中汞测量受干扰少、正常情况下背景稳定、在地震前反应灵敏、变化幅度大、异常易于识别,汞量测量将成为短临预报的有效新方法。本文将介绍这一批实际资料。 相似文献
3.
详细阐述了微地震注水前缘监测的原理。应用微地震注水前缘监测系统,通过微地震信息的现场监测和解释,结合生产动态及其他监测资料综合分析,并以秦家屯地区的QK 3-5井为例,描述了秦家屯地区注水开发状态下水井水驱前缘位置,研究了地下油水运动规律,证明了方法的可靠性和实用性。结果表明,对于油田注水分析与研究微地震监测技术可以取得很好的效果。 相似文献
4.
5.
屋顶雨水回灌裂隙岩溶含水层连通示踪试验 总被引：1，自引：0，他引：1
雨水回灌后对岩溶水的影响分析和效果需要对回灌井和下游的观测井监测数据说明。由于岩溶含水层中岩溶发育极不均匀,在测定地下水位并判定出地下水流向的基础上,连通示踪试验是选择与回灌井相对应的观测井的有效办法。用氯化钠作为示踪剂,监测不同测井不同埋深地下水电导率随时间变化的方法确定了岩溶水观测井选址、岩溶含水层的结构及水文地质条件。示踪试验结果表明,3#观测井(西院井)可用来监测雨水回灌效果,并计算出该地区的地下水势流速在9 m/h～20 m/h之间。该成果对北方地区岩溶含水层回灌和环境评价具有重要的参考价值。 相似文献
6.
7.
在安徽省南部山区林竹村现场测定50个水样的pH值、电导率和水温,结合9个水样的室内分析结果,分析了该地区的地下水化学类型、水质,指出当地的水体没有受到酚、氰、汞、砷、铬等成分的污染,但受生活污水的影响较大,可属Ⅱ类水;少数水样受农药化肥残留物的影响较大,属Ⅲ类水。并提出钻探一眼更好的深机井、注意生活用水的排放等措施,以提高当地的饮用水安全。 相似文献
8.
A．Ferretti 《地壳构造与地壳应力》2004,(3):1-4
尽管D—INSAR技术有定期常规精确监测滑坡的巨大潜力，但对于监测火山和地震断层的活动仍然面临着挑战。时间去相关和大气异质性构成了主要的限制。时间去相关使。INSAR测量在植被覆盖地区无法应用，通常这些地区的电磁剖面或每个分辨率单元内散射体的位置会随时间而变化。另一方面，在估算DEM和形变模式时，大气异质性引起的低波数变化也会受人为因素的影响。 相似文献
9.
垃圾堆放场氯代脂肪烃对浅层地下水的污染特征初步分析 总被引：12，自引：2，他引：12
研究区是浅层地下水主要补给区，通过区内地下水监测说明，受垃圾淋滤液影响的地下水中氯代烃高值点主要集中在研究区中部；地下水中氯代烃检出值和检出率有季节性变化特征，与垃圾堆放时间和该井距垃圾场堆放场距离有密切关系，堆放时间越长，离垃圾堆放场越近，检出率、检出值越高；对地下水污染的敏感性和影响氯代烃迁移的机理方面进行了分析。 相似文献
10.
采用井下地震仪可监测到许多地面地震台未记录到的微弱地震波,可减小地面噪声干扰,大大提高震源定位精度。介绍了武汉甚宽频带数字地震监测1井的设计以及钻井和固井的关键技术。在项目实施过程中采用合理的钻井工艺和专门设计的单向注浆装置等技术满足了地震监测井的特殊技术要求。 相似文献
11.
Water level fluctuations in twenty-one observation wells have been monitored for the last 10 years around the seismically active Koyna–Warna region, western India where earthquakes continue to occur even after four decades of the initiation of the seismic activity in the region. Fourteen of the observation wells act as volume strain meters as their water levels show earth tidal signals. Our analysis suggests three types of response of the well water levels to seismo-tectonic effects, i) one to local earthquakes, ii) to regional and teleseismic events, and iii) to local fluctuations in rock strain on regional scale. We observed five cases of co-seismic step-like well water level changes, of the order of few centimeters in amplitude, related to earthquakes in the magnitude range 4.3 ≤ M ≤ 5.2. All these earthquakes occurred within the network of wells drilled for the study and within 25 km distance of the recording wells. In three cases, drop in well levels preceded co-seismic step-like increases, which may be of premonitory nature. The second type of response is observed to be due to the passing of seismic waves from regional and teleseismic earthquakes like the M 7.7 Bhuj event on January 26, 2001 and the M 9.3 December 26, 2004 Sumatra earthquake. The third type is a well level anomaly of centimeter amplitude coherently occurring in several wells. The anomalies are similar in shape and last for several hours to days.From our studies we conclude that the wells in the network appear to respond to regional strain variations and transient changes due to distant earthquakes. The two factors which are important to co-seismic steps due to local earthquakes are the magnitude and epicentral distance. From the limited number of events we found that all local earthquakes exceeding M ≥ 4.3 have produced co-seismic changes. No such changes were observed for earthquakes below this magnitude threshold. 相似文献
12.
Earthquakes cause a variety of hydrological phenomena, including changes in the ground water levels in bore wells. The Koyna
region in the peninsular shield of India, hitherto considered stable in terms of seismic activity, has been active since 1967.
More recently, the earthquakes have been localized to the newly impounded Warna reservoir, which is located south of Koyna,
where a burst of seismicity occurred in 1993. The region continues to remain seismically active even after four decades. Twenty-one
bore wells were drilled around the seismic source volume in the region to observe water level changes resulting from earthquake
phenomena. Our studies have shown coseismic anomalous water level changes to be associated with the moderate earthquakes of
April 25, 1997 and February 11, 1998. Our results show that changes in the ground water level in bore wells are correlated
with micro-earthquake activity, both preceding and following moderately sized earthquakes. The results have implications in
enhancing our understanding of earthquake mechanisms. 相似文献
13.
New factual materials on methane eruptions into the water of Lake Baikal in August 1912 are considered. The regional press
is used as the information source. The spatio-temporal relationship between the gas eruptions and earthquakes, observed in
South Baikal in 1912, is revealed, which permits us to consider this effect as a consequence of seismic activity intensification.
Intensive methane discharge into water is a potential danger for the lake’s ecosystem as was proved by massive death of water
organisms in South Baikal in 1912 during the described phenomena. 相似文献
14.
Bodrum Peninsula is located between Hellenic Trench in the west and Gökova Fault Zone in the east which is affected by hundreds of earthquakes every year. Because of its active environment is allowed to monitor tracers/precursors continuously to analyse natural processes. This study focused on the determination of ground water radon (222Rn) concentrations in the Bodrum Peninsula in terms of seismic activities. Radon levels of ten ground water wells were measured periodically throughout the peninsula and these wells were divided into two groups according to the number of earthquakes they are exposed. Radon variations in second group stations are fairly significant as a result of high number of earthquakes. In these stations, radon continuously increased before the seismic storm and then decreased step by step. The results indicated that radon variations in ground waters of Bodrum Peninsula can be a good indicator for seismic storms instead of one specific event. 相似文献
15.
Lee Soo-Hyoung Lee Jae Min Moon Sang-Ho Ha Kyoochul Kim Yongcheol Jeong Dan Bi Kim Yongje 《Hydrogeology Journal》2021,29(4):1679-1689
Hydrogeological responses to earthquakes such as changes in groundwater level, temperature, and chemistry, have been observed for several decades. This study examines behavior associated with ML 5.8 and ML 5.1 earthquakes that occurred on 12 September 2016 near Gyeongju, a city located on the southeast coast of the Korean peninsula. The ML 5.8 event stands as the largest recorded earthquake in South Korea since the advent of modern recording systems. There was considerable damage associated with the earthquakes and many aftershocks. Records from monitoring wells located about 135 km west of the epicenter displayed various patterns of change in both water level and temperature. There were transient-type, step-like-type (up and down), and persistent-type (rise and fall) changes in water levels. The water temperature changes were of transient, shift-change, and tendency-change types. Transient changes in the groundwater level and temperature were particularly well developed in monitoring wells installed along a major boundary fault that bisected the study area. These changes were interpreted as representing an aquifer system deformed by seismic waves. The various patterns in groundwater level and temperature, therefore, suggested that seismic waves impacted the fractured units through the reactivation of fractures, joints, and microcracks, which resulted from a pulse in fluid pressure. This study points to the value of long-term monitoring efforts, which in this case were able to provide detailed information needed to manage the groundwater resources in areas potentially affected by further earthquakes.
相似文献16.
Pradeep Talwani 《Engineering Geology》1976,10(2-4):239-253
Following the McCormick County, South Carolina, local magnitude 4.3 earthquake on August 2, 1974, continuous seismic activity has been observed in the area. The epicenters are located within 3 km from the Clark Hill reservoir. The shallow seismic activity appears to be related to water level fluctuations in the reservoir, and follows them by about two days. The frequency of earthquakes is related to the rate of change of water level, while the energy release is seen to depend on the water level itself. Pore pressure fluctuations at focal depths in a regime of high tectonic stresses is the suggested cause for the triggering of earthquakes. 相似文献
17.
Filling of McNaughton Lake, with a capacity at full load of25 · 109m3 and maximum depth 191 m, was initiated on March 29, 1973. An earthquake swarm of 747 events (ML > 0) with largest eventML = 4.7 occurred within 17 km of the reservoir just prior to loading. Subsequent to this, three swarms of 194, 292 and 22 events with maximumML = 4.1 occurred in the same region; however, no earthquakes have occurred between the reservoir and the swarm area. The level of regional seismic activity is similar to that observed prior to loading. The distribution of this activity, excluding swarm events, exhibits a spatial pattern similar to that recorded earlier by regional seismic stations, except that several events appear to be associated with the fault underlying the Rocky Mountain Trench in which the lake is formed. During a loading-unloading cycle in which the maximum water depth varied from 98 m to 171 m to 131 m, the change ofvp was less than 2%. This indicates that no significant change in dilatancy or degree of water saturation occurred in the upper crustal layer during this cycle. 相似文献
18.
以热水及矿水的水文地球化学场为主要标志,以构造格局和构造活动性、历史地震活动规律为主要划分依据,再结合地球物理场、地温场及区域地层的组合分布状况,进行了地震危险区带的划分。将中国大陆划分为6个地震危险区、23个危险亚区和30个危险带,并对各个危险亚区和危险带的主要水文地球化学特征及构造进行了论述。通过对地下水水文地球化学特征和水文化学场的研究,分析构造特征及其活动性,确定地震与水文地球化学特征及化学场的耦合关系。这对地震水文观测孔的布置和地震预测具有重要意义。通过长期监测地下水中水化学成分的变化,就有可能为预测预报地震提供一种新的前兆信息。 相似文献
19.
Mohammad Mokhtari 《Natural Hazards》2010,52(2):351-368
Iran has long been known as one of the most seismically active areas of the world, and it frequently suffers destructive and catastrophic earthquakes that cause heavy loss of human life and widespread damage. The Alborz region in the northern part of Iran is an active EW trending mountain belt of 100 km wide and 600 km long. The Alborz range is bounded by the Talesh Mountains to the west and the Kopet Dagh Mountains to the east and consists of several sedimentary and volcanic layers of Cambrian to Eocene ages that were deformed during the late Cenozoic collision. Several active faults affect the central Alborz. The main active faults are the North Tehran and Mosha faults. The Mosha fault is one of the major active faults in the central Alborz as shown by its strong historical seismicity and its clear morphological signature. Situated in the vicinity of Tehran city, this 150-km-long N100° E trending fault represents an important potential seismic source. For earthquake monitoring and possible future prediction/precursory purposes, a test site has been established in the Alborz mountain region. The proximity to the capital of Iran with its high population density, low frequency but high magnitude earthquake occurrence, and active faults with their historical earthquake events have been considered as the main criteria for this selection. In addition, within the test site, there are hot springs and deep water wells that can be used for physico-chemical and radon gas analysis for earthquake precursory studies. The present activities include magnetic measurements; application of methodology for identification of seismogenic nodes for earthquakes of M ≥ 6.0 in the Alborz region developed by International Institute of Earthquake Prediction Theory and Mathematical Geophysics, IIEPT RAS, Russian Academy of Science, Moscow (IIEPT&MG RAS); a feasibility study using a dense seismic network for identification of future locations of seismic monitoring stations and application of short-term prediction of medium- and large-size earthquakes is based on Markov and extended self-similarity analysis of seismic data. The establishment of the test site is ongoing, and the methodology has been selected based on the IASPEI evaluation report on the most important precursors with installation of (i) a local dense seismic network consisting of 25 short-period seismometers, (ii) a GPS network consisting of eight instruments with 70 stations, (iii) magnetic network with four instruments, and (iv) radon gas and a physico-chemical study on the springs and deep water wells. 相似文献