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本文研究了代县台地电阻率在正常年变背景上出现有叠加地震的短临异常。认为它们与代县台周围150km范围内发生的四次5.1—6.1级地震有关。通过研究再次表明地电阻率方法预报地震的重要性和有效性。 相似文献
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利用乾陵地震台地电数字观测资料,分析了该台地电阻率变化与降雨的关系,认为两者之间存在着一定的相关关系,降雨是造成地电阻率突变的主要原因,并且通过相关分析校正较好地剔除了降雨对地电阻率变化的影响。 相似文献
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本文定量分析地温、地下水位变化对视电阻率的影响。首先建立与地温、地下水位变化相应的地电断面,这种断面的电性不是分层均匀的,然后用有限单元法计算视电阻率。计算结果表明,对与临沂地电台相近的地电断面,地下水位的变化对视电阻年变的影响大于地温年变的影响,前者约为后者的两倍。基岩对年变大小有强烈的控制作用,基岩浅,年变明显,基岩深,年变大为减弱。 相似文献
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通过数值模拟及褶积滤波方法，对甘肃省定西台地电阻率两测道“冬低夏高”的反向年变形态进行分析，并利用自适应计算变化幅度法提取该台地电阻率资料的中短期异常数据。结果表明，定西地电阻率的年变形态主要受地表薄层介质电阻率季节变化和降雨影响；褶积滤波法可以拟合短期降雨影响，并且可以过滤地电阻率的年变形态，但2021年出现的趋势性转折下降的低值破年变与降雨量和薄层季节干扰关系不大；九寨沟7.0级和门源6.9级地震前出现较为显著的中短期下降异常变化，最大下降率为0.983%;2022年门源6.9级地震后的两测道去年变趋势变化幅度中的异常形态依然存在，且并未恢复。因此定西台地电阻率对甘东南和祁连山中东段具有指示意义，有必要利用该方法进一步重点关注该区域的强震危险性。 相似文献
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2001年8～9月间,江油地电台N10°E测向视电阻率ρs值出现持续下降,变化形态打破年变,降幅约3%,很像是一次孕震异常。但经现场核实为供电电源极性接反漏电所致,与理论计算出的漏电影响系数相反。 相似文献
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隆尧地电阻率与地下水位关系分析 总被引：2，自引：0，他引：2
利用线性回归法,分析河北省隆尧地电阻率和地下水位的关系,发现该地区地电阻率季节性年变和近年来显著的趋势上升变化与地下水位动态变化相关.调查发现,年降雨量减小和农业用水量增大引起该区地下水位下降,从而导致地电阻率发生趋势上升变化. 相似文献
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APPARENT RESISTIVITY TEMPORAL VARIATION CHARAC-TERISTICS AFFECTED BY THE FIXED DISTURBANCE SOURCE ON SURFACE OF MEASURING AREA 
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下载免费PDF全文 Current leakage,metallic conductor,and local anomalous resistivity body are main disturbance sources which affect the successive observation of apparent resistivity in stations,besides the observing system failure.We construct a finite element model using a 3-layered horizontal medium to discuss the dynamic characteristics of disturbances caused by metal conductor and local anomalous resistivity body in the measuring filed.The numerical results show that low resistivity source which is located in areas where the sensitivity coefficient is positive will cause decline on apparent resistivity observation.While low resistivity source will cause increase when it is located in areas where the sensitivity coefficient is negative.Disturbance caused by high resistivity source is opposite to the one from low resistivity source.The general dynamic feature of disturbance is that the disturbance amplitude increases as the resistivity of shallow layer decreases,while the amplitude declines when the shallow layer's resistivity increases.For the measuring direction which has normal annual variation form,low resistivity source which is located in area where the sensitivity coefficient is positive will increase the annual variation amplitude,while it will reduce annual amplitude when it is in a negative sensitivity coefficient area.Annual amplitude changes caused by high resistivity source are opposite to the changes caused by low resistivity source.For the measuring direction which has abnormal annual variation form,dynamic annual feature is opposite to the one in direction of normal annual variation form.If the dynamic feature is opposite to the annual variation and disturbance amplitude is also greater than annual amplitude,the annual variation will change direction.Disturbance amplitude from metallic conductor is affected by the resistivity and cross-section area,the lower of the resistivity and the larger of the cross-section area,the greater of the disturbance amplitude. 相似文献
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Parts of the consecutive apparent resistivity monitoring stations of China have recorded clear diurnal variations. The relative amplitudes of diurnal variations at these stations range from 1.3‰ to 5.8‰. The daily accuracies of apparent resistivity observation are better than 1‰, because the background electromagnetic noise is rather low at these stations. Therefore, the diurnal variations of apparent resistivity recorded at these stations are real phenomena. The diurnal variation shapes can be divided into two opposite types according to their characteristics. One type is that the apparent resistivity data decreases during the daytime but increases during the nighttime(Type 1). The other type is the apparent resistivity data increases during the daytime but decreases during the nighttime(Type 2). There is a correspondence between the diurnal and annual variation patterns of apparent resistivity. For the monitoring direction with diurnal variation of Type 1, the apparent resistivity decreases in summer and increases in winter. However, for the monitoring direction with diurnal variation of Type 2, the apparent resistivity increases in summer and decreases in winter.
We take an analysis on the mechanism of apparent resistivity diurnal variation, combining the influence factors of water-bearing medium's resistivity, the electric structure of stations, and the apparent resistivity sensitivity coefficient(SC)theory. Intuitively, diurnal variation of apparent resistivity is caused by diurnal variation of medium resistivity in the measured area. The diurnal variation of medium resistivity will inevitably be caused by the factors with diurnal variation. Among the possible factors, there is diural variation in earth tide and temperature.
Our analysis displays that apparent resistivity diurnal variation is not caused by the usually-believed earth tide, but by the ground temperature difference between daytime and nighttime. The earth tide strain is too small to cause remarkable effects on the apparent resistivity data. On the other hand, the daily tide strain has two peak-valley variations, and its phase and amplitude has a period of approximate 28 days. However, the apparent resistivity data do not show these corresponding features to earth tide. Furthermore, the detection range of current apparent resistivity stations is within a depth of several hundred meters. Within this depth range, the medium deformation caused by solid tide can be regarded as uniform change. Therefore, all monitoring directions and all stations will have the same pattern of diurnal variation.
In general, the temperature increases in the daytime but decreases in the nighttime. For most water-bearing rock and soil medium, its resistivity decreases as temperature increases and increases as temperature decreases. Diurnal temperature difference affects about 0.4m of soil depth. Therefore, resistivity of this surface thin soil layer decreases in the daytime while increases in the nighttime. Under layered medium model, SC of each layer represents its contribution to the apparent resistivity. For the stations with positive SC of surface layer, apparent resistivity decreases in the daytime but increases in the nighttime. While for the stations with negative SC of surface layer, apparent resistivity diurnal variations display the opposite shape. 相似文献
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近年来安徽地区地电阻率观测多次出现异常数据, 同期间省内发生了多次MS3.0以上地震, 我们对安徽省观测较好的几个台站数据进行年变化特征、 干扰因素的分析, 发现水位、 降雨是影响地电阻率数据变化的主要因素, 通过以月为窗长的回归拟合分析进行水位的干扰消除, 计算的残差值能有效地消除地电阻率年变化干扰, 运用消除干扰后的曲线对近期发生的地震进行分析, 发现霍山MS4.3和阜阳MS4.3等地震前未出现明显趋势性前兆异常, 临近台站出现的异常变化可能与该区域的地下水位干扰性变化有关。 相似文献
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台址下表层介质电阻率变化对视电阻率观测值影响特征的初步研究 总被引：2，自引：0，他引：2
气候的交替变化将导致大地表层含水量发生变化，从而使该层介质的电阻率发生变化，进而使得观测结果(即视电阻率)发生变化，显然这对地震前兆观测而言是一种干扰。目前我国绝大多数前兆地电阻率台采用单极距观测方式，因此观测到的视电阻率变化应是表层变化(主要是干扰)和观测范围内深部变化(地下介质应力与应变状态发生变化)的综合反映。作先依据台址下的水平层状模型进行了模拟计算研究，发现大地表层含水量的变化对单极距四极装置视电阻率观测值的影响有两个特征：(1)无论台址下电阻率结构是下伏低阻还是下伏高阻，表层介质电阻率升高对观测值的影响都很小；(2)表层电阻率降低对观测值的影响很明显，且对下伏高阻结构的影响大于对下伏低阻结构的影响。然后用视电阻率实际观测资料说明了将其特征用于预报的可能性。 相似文献