The research about subsurface characteristics by using transient electromagnetic method(TEM) and high density resistivity method(HDRM) were already conducted in Ordos. The objective of this research is to detect coalm...The research about subsurface characteristics by using transient electromagnetic method(TEM) and high density resistivity method(HDRM) were already conducted in Ordos. The objective of this research is to detect coalmine goaf areas based on rock resistivity. The data processing using wavelet transform, three point smoothing, RES2 DINV and Maxwell processing software to obtain 2D resistivity structure. The results showed that the layers with maximum resistivity values(30e33 U m on Line 1, 30e31 U m on Line 2, 32e40 U m on Line3) are founded at station 1e7, and 14e20 on Line 1,13e18 on Line 2, and 8e13 and 16e20 on Line 3 which is predicted as goaf layer, and the minimum resistivity values(20e26 U m of TEM, 45e75 U m of HDRM) at the other layers. This resistivity difference was caused by the geology and characteristics of the study area which is located close by the cleugh with rich coal, so the goaf area distinguishable with aquifer layer and coal seam. The results were also significant accidents and serious destruction of ecological environment.展开更多
Based on the relationship between the diameter and buried depth of goaf,the authors establish the forward modeling by Res2dmod and inverse the model by Res2dinv. Thus,three kinds of models are obtained:the model of si...Based on the relationship between the diameter and buried depth of goaf,the authors establish the forward modeling by Res2dmod and inverse the model by Res2dinv. Thus,three kinds of models are obtained:the model of single resistivity anomalous body,model of double different distance resistivity anomalous body,and model of layered resistivity anomalous body. Using forward and inversion,the image of detection is simulated,and the reliability is proved by comparing with the engineering examples.展开更多
The purpose of this research is to explore the spatial distribution and influence range of the mined-out area of a coal mine in Hebei Province,the advantages of ultra-high density resistivity method,such as large data...The purpose of this research is to explore the spatial distribution and influence range of the mined-out area of a coal mine in Hebei Province,the advantages of ultra-high density resistivity method,such as large data volume,high efficiency and high precision,are brought into full play,the abnormal patterns of dislocation and partial drainage area of shallow continuous aquifer caused by subsidence zone are detected,and then the spatial distribution patterns of subsidence and fractures caused by deep mining subsidence zone are deduced,this method not only extends the exploration range of high-density resistivity method in mining subsidence disaster assessment,but also improves the accuracy of measurement,the distribution and influence range of mined-out area are revealed accurately,and good exploration results have been obtained in this project.How to select reasonable geophysical prospecting methods and give full play to the role of geophysical prospecting methods according to the geological characteristics of the study area,this exploration work is not only a good combination of geophysical prospecting methods and actual geological conditions,it also provides a valuable reference version for the exploration work under the same geological conditions.展开更多
As an important geophysical tool,high density electrical technique infers the underground geological structures by processing and inverting the apparent resistivity data.Currently,the false anomalies have been frequen...As an important geophysical tool,high density electrical technique infers the underground geological structures by processing and inverting the apparent resistivity data.Currently,the false anomalies have been frequently occurred in the graph of apparent resistivity pseudo-section or inverted geoelectrical section obtained from high-density electrical technique,and are difficult to remove.In this study,the authors explain the mechanism of the false anomalies and put forward the horizontal differential field method to identify the false anomalies.Based on the analysis of modeling results,this method is applied in the surveying data in Xinlei Quarry of Jiuquan,and the results confirm the effectiveness of the horizontal differential field method.展开更多
【目的】由于天然孔隙介质中存在物理化学非均质性,在这种复杂的非均质性含水层中,以往的现场试验数据显示溶质在非均质介质运移过程中无法用菲克扩散定律对流弥散方程(Advection-Dispersion Equation,ADE)来描述。本研究采用高密度电...【目的】由于天然孔隙介质中存在物理化学非均质性,在这种复杂的非均质性含水层中,以往的现场试验数据显示溶质在非均质介质运移过程中无法用菲克扩散定律对流弥散方程(Advection-Dispersion Equation,ADE)来描述。本研究采用高密度电法证实溶质在非均质介质中非菲克运移。【方法】本研究采用石英砂、沸石两种不同基质构建双重介质物理模型(Models of Dual-Domain Mass Transfer,DDMT),采用高密度电法测定系统ERT21实时检测和采集数据,在实验室利用Nacl溶液开展示踪试验,利用阿尔奇定律分析溶质运移试验研究。【结果】试验结果浓度穿透曲线在后期发生“拖尾”现象;在沸石柱实验中,观察到流体电导率(σ_(f))和体积电导率(σ_(b))之间的滞后现象,这表明流体在不可动领域和可动领域之间的交换。而在沙子柱试验中,未观察到σ_(f)和σ_(b)之间的滞后现象,可以忽略质量传递行为;滞后现象的形状与大小由水动力学特征和基质属性控制,水动力学是影响拖尾时长的因素之一,渗透系数会影响溶质运移的过程。【结论】通过试验观察和地球物理数据分析,直接量化了实验室尺度下的异常质量传递行为,通过地球物理方法测量的导电率(σ_(b))对于移动和不动领域都具有敏感性,从而提供了与标准采样方法相比的独特优势。展开更多
基金supported by the Institute of Seismology Foundation, China Earthquake Administration (201326126)
文摘The research about subsurface characteristics by using transient electromagnetic method(TEM) and high density resistivity method(HDRM) were already conducted in Ordos. The objective of this research is to detect coalmine goaf areas based on rock resistivity. The data processing using wavelet transform, three point smoothing, RES2 DINV and Maxwell processing software to obtain 2D resistivity structure. The results showed that the layers with maximum resistivity values(30e33 U m on Line 1, 30e31 U m on Line 2, 32e40 U m on Line3) are founded at station 1e7, and 14e20 on Line 1,13e18 on Line 2, and 8e13 and 16e20 on Line 3 which is predicted as goaf layer, and the minimum resistivity values(20e26 U m of TEM, 45e75 U m of HDRM) at the other layers. This resistivity difference was caused by the geology and characteristics of the study area which is located close by the cleugh with rich coal, so the goaf area distinguishable with aquifer layer and coal seam. The results were also significant accidents and serious destruction of ecological environment.
文摘Based on the relationship between the diameter and buried depth of goaf,the authors establish the forward modeling by Res2dmod and inverse the model by Res2dinv. Thus,three kinds of models are obtained:the model of single resistivity anomalous body,model of double different distance resistivity anomalous body,and model of layered resistivity anomalous body. Using forward and inversion,the image of detection is simulated,and the reliability is proved by comparing with the engineering examples.
基金This study was supported by the geological project“Shendong-Jindong Large Coal Base 1:50000 Hydrogeological Geophysical Prospecting(G201611-4)”the project“Research on Physical Characteristics of Aquiferous Structure in Areas with Serious Water Shortage in Taihang Mountain(SK201303)”with basic scientific research expense.
文摘The purpose of this research is to explore the spatial distribution and influence range of the mined-out area of a coal mine in Hebei Province,the advantages of ultra-high density resistivity method,such as large data volume,high efficiency and high precision,are brought into full play,the abnormal patterns of dislocation and partial drainage area of shallow continuous aquifer caused by subsidence zone are detected,and then the spatial distribution patterns of subsidence and fractures caused by deep mining subsidence zone are deduced,this method not only extends the exploration range of high-density resistivity method in mining subsidence disaster assessment,but also improves the accuracy of measurement,the distribution and influence range of mined-out area are revealed accurately,and good exploration results have been obtained in this project.How to select reasonable geophysical prospecting methods and give full play to the role of geophysical prospecting methods according to the geological characteristics of the study area,this exploration work is not only a good combination of geophysical prospecting methods and actual geological conditions,it also provides a valuable reference version for the exploration work under the same geological conditions.
文摘As an important geophysical tool,high density electrical technique infers the underground geological structures by processing and inverting the apparent resistivity data.Currently,the false anomalies have been frequently occurred in the graph of apparent resistivity pseudo-section or inverted geoelectrical section obtained from high-density electrical technique,and are difficult to remove.In this study,the authors explain the mechanism of the false anomalies and put forward the horizontal differential field method to identify the false anomalies.Based on the analysis of modeling results,this method is applied in the surveying data in Xinlei Quarry of Jiuquan,and the results confirm the effectiveness of the horizontal differential field method.
文摘【目的】由于天然孔隙介质中存在物理化学非均质性,在这种复杂的非均质性含水层中,以往的现场试验数据显示溶质在非均质介质运移过程中无法用菲克扩散定律对流弥散方程(Advection-Dispersion Equation,ADE)来描述。本研究采用高密度电法证实溶质在非均质介质中非菲克运移。【方法】本研究采用石英砂、沸石两种不同基质构建双重介质物理模型(Models of Dual-Domain Mass Transfer,DDMT),采用高密度电法测定系统ERT21实时检测和采集数据,在实验室利用Nacl溶液开展示踪试验,利用阿尔奇定律分析溶质运移试验研究。【结果】试验结果浓度穿透曲线在后期发生“拖尾”现象;在沸石柱实验中,观察到流体电导率(σ_(f))和体积电导率(σ_(b))之间的滞后现象,这表明流体在不可动领域和可动领域之间的交换。而在沙子柱试验中,未观察到σ_(f)和σ_(b)之间的滞后现象,可以忽略质量传递行为;滞后现象的形状与大小由水动力学特征和基质属性控制,水动力学是影响拖尾时长的因素之一,渗透系数会影响溶质运移的过程。【结论】通过试验观察和地球物理数据分析,直接量化了实验室尺度下的异常质量传递行为,通过地球物理方法测量的导电率(σ_(b))对于移动和不动领域都具有敏感性,从而提供了与标准采样方法相比的独特优势。
