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A Study on the Characteristics of Electromagnetic Radiation during Deformation and Failure of Different Materials Under Uniaxial Compression 不同材料单轴压缩变形破坏过程中的电磁辐射特性研究
IF 1 4区 工程技术 Q2 Earth and Planetary Sciences Pub Date : 2020-03-01 DOI: 10.2113/JEEG19-044
Qifei Wang, Chengwu Li, Beijing Xie, Yuechao Zhao, Dihao Ai
The detection of electromagnetic radiation (EMR) during the fracture of solid materials such as rocks and coal has been widely used in seismic exploration and mine dynamic disaster prediction. As described in this paper, we conduct uniaxial compression tests on coal, cement, and glass materials to determine the characteristic EMR differences among materials. A band-stop filter based on the Fourier transform and the wavelet packet transform method are used to conduct signal denoising and analysis. Basic analyses of the pulse-time characteristics, energy distribution, cumulative energy, and waveform characteristics of EMR are conducted. The research results show that there is a strong corresponding relation between the loading time, loading stress and EMR energy. A large number of EMR events are released in rapid succession during the main rupture of coal and cement, while the EMR events are evenly distributed throughout the whole loading process of glass. For the same material, the maximum EMR amplitude increases with an increasing peak value of the stress. The EMR pulse waveform of coal and cement agrees well with predictions based on the theoretical formula of the electromagnetic dipole oscillation EMR generation mechanism. The paper provides further theoretical basis for understanding the mechanism of EMR, with great significance for improving coal mining safety.
岩石、煤等固体材料断裂过程中的电磁辐射检测在地震勘探和矿山动力灾害预测中有着广泛的应用。如本文所述,我们对煤、水泥和玻璃材料进行了单轴压缩试验,以确定材料之间的特征EMR差异。采用基于傅里叶变换和小波包变换的带阻滤波器对信号进行去噪和分析。对EMR的脉冲时间特性、能量分布、累计能量和波形特性进行了基本分析。研究结果表明,加载时间、加载应力与EMR能量之间存在较强的对应关系。在煤与水泥主破裂过程中,大量EMR事件快速连续释放,而EMR事件在整个玻璃加载过程中分布均匀。对于同一种材料,最大EMR幅值随应力峰值的增大而增大。煤和水泥的EMR脉冲波形与基于电磁偶极子振荡EMR产生机理理论公式的预测吻合较好。本文为进一步认识电磁共振机理提供了理论依据,对提高煤矿安全生产具有重要意义。
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引用次数: 2
A Weighting Function-Based Method for Resistivity Inversion in Subsurface Investigations 基于加权函数的地下电阻率反演方法
IF 1 4区 工程技术 Q2 Earth and Planetary Sciences Pub Date : 2020-03-01 DOI: 10.2113/jeeg19-029
Nie Lichao, Ma Zhao, Bin Liu, Xu Zhenhao, Zhou Wei, Wang Chengkun, J. Shao, Yin Xin
There is a high demand for high detection accuracy and resolution with respect to anomalous bodies due to the increased development of underground spaces. This study focused on the weighted inversion of observed data from individual array type electrical resistivity tomography (ERT), and developed an improved method of applying a data weighing function to the geoelectrical inversion procedure. In this method, the weighting factor as an observed data weighting term was introduced into the objective function. For individual arrays, the sensitivity decreases with increasing electrode interval. Therefore, the Jacobian matrices were computed for the observed data of individual arrays to determine the value of the weighting factor, and the weighting factor was calculated automatically during inversion. In this work, 2D combined inversion of ERT data from four-electrode Alfa-type arrays is examined. The effectiveness of the weighted inversion method was demonstrated using various synthetic and real data examples. The results indicated that the inversion method based on observed data weighted function could improve the contribution of observed data with depth information to the objective function. It has been proven that the combined weighted inversion method could be a feasible tool for improving the accuracies of positioning and resolution while imaging deep anomalous bodies in the subsurface.
由于地下空间的不断发展,对异常体的探测精度和分辨率提出了很高的要求。本研究重点研究了单个阵列型电阻率层析成像(ERT)观测数据的加权反演,并开发了一种将数据加权函数应用于地电反演过程的改进方法。该方法将加权因子作为观测数据的加权项引入到目标函数中。对于单个阵列,灵敏度随电极间距的增加而降低。因此,对单个阵列的观测数据计算雅可比矩阵,确定权重因子的取值,并在反演过程中自动计算权重因子。在这项工作中,研究了四电极阿尔法型阵列ERT数据的二维联合反演。通过各种综合和实际数据实例验证了加权反演方法的有效性。结果表明,基于观测数据加权函数的反演方法可以提高具有深度信息的观测数据对目标函数的贡献。实践证明,联合加权反演方法是提高地下深部异常体成像定位精度和分辨率的可行工具。
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引用次数: 1
Using an Azimuth Electromagnetic Wave Imaging Method to Detect and Characterize Coal-seam Interfaces and Low-resistivity Anomalies 用方位角电磁波成像方法探测和表征煤层界面及低阻异常
IF 1 4区 工程技术 Q2 Earth and Planetary Sciences Pub Date : 2020-03-01 DOI: 10.2113/JEEG19-041
Gang Chen, Yiren Fan, Quanxin Li
It has been found that the traditionally used electromagnetic wave instruments have limitations in detection depths, as well as a lack of directionality. Therefore, those types of instruments cannot meet the needs of geo-steering applications. However, azimuth electromagnetic wave instruments have shown the ability to quickly acquire effective geo-steering information using a tilt coil design method, which can potentially provide accurate guidance for decision-making in drilling direction adjustments. In this study, a design method for an azimuth electromagnetic wave detection instrument for underground coal mining was proposed. The relationships between the structural parameters of the instrument and installation angles of the coils and the response signals were obtained in this study using simulations. Then, by choosing reasonable instrument spacings, coil installation angles, and transmitting frequencies, the detection performances of the instrument were successfully improved. Also, the basic parameter selections of the proposed logging-while-drilling azimuth electromagnetic wave logging instrument were determined to be suitable for underground coal-mining purposes. It was also found that the symmetric compensation of the instrument was sensitive to the interface responses, and the anti-symmetric compensation was sensitive to the anisotropic responses. In addition, a method of detecting the interface positions and azimuth of coal-seam interfaces using azimuth electromagnetic waves, as well as the potential for the application of the instrument for the detection of low-resistivity anomalies in coal goafs, were effectively demonstrated. The results of this study provided theoretical references for future coal-seam boundary detections and explorations, and also added insight into the development processes of coal-seam bedding.
人们发现,传统使用的电磁波仪器在探测深度上存在局限性,并且缺乏方向性。因此,这些类型的仪器不能满足地质导向应用的需要。然而,方位角电磁波仪器已经显示出利用倾斜线圈设计方法快速获取有效地质导向信息的能力,这可能为钻井方向调整决策提供准确的指导。本文提出了一种煤矿井下方位电磁波探测仪的设计方法。通过仿真得到了仪器结构参数和线圈安装角度与响应信号的关系。然后,通过选择合理的仪器间距、线圈安装角度和发射频率,成功地提高了仪器的检测性能。同时,确定了随钻方位电磁波测井仪的基本参数选择,适合煤矿井下开采。实验还发现,对称补偿对界面响应敏感,反对称补偿对各向异性响应敏感。此外,有效论证了利用方位角电磁波探测煤层界面位置和方位的方法,以及该仪器在采空区低阻异常探测中的应用潜力。研究结果为今后的煤层边界探测和勘探提供了理论参考,也加深了对煤层层理发育过程的认识。
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引用次数: 2
Joint Inversion of Magnetotelluric Impedance and Tipper Data in 3D Axial Anisotropic Media 三维轴向各向异性介质中大地电磁阻抗和倾斜数据联合反演
IF 1 4区 工程技术 Q2 Earth and Planetary Sciences Pub Date : 2020-03-01 DOI: 10.2113/JEEG19-022
Wei Luo, Kunpeng Wang, Hui Cao, Changsheng Duan, Tao Wang, Xingxiang Jian
Magnetotelluric (MT) impedance and tipper data can be utilized to reflect underground structural information. However, when the axial anisotropic property of an abnormal body is marked, it will seriously influence MT measuring data. This study divides the MT field into primary and secondary components and replaces the conductivity parameter in a three-dimensional (3D) governing equation with axial anisotropic conductivity. Analysis of the influence of axial anisotropy on MT tipper data is presented, and a limited-memory Broyden-Fletcher-Goldfarb-Shanno method is then utilized to realize a 3D MT axial anisotropic inversion with impedance and tipper data. The tests presented in this paper show that the resolution of the inverting axial anisotropic model with impedance and tipper data is better than that of only using impedance data.
大地电磁阻抗和自旋数据可以用来反映地下构造信息。然而,当异常体的轴向各向异性被标记时,将严重影响大地电磁测量数据。本研究将大地电磁场划分为一次分量和二次分量,并用轴向各向异性电导率代替三维控制方程中的电导率参数。分析了轴向各向异性对大地电磁学倾斜数据的影响,利用有限记忆Broyden-Fletcher-Goldfarb-Shanno方法实现了阻抗和倾斜数据的三维大地电磁学轴向各向异性反演。试验结果表明,结合阻抗和倾斜度数据的反相轴向各向异性模型的分辨率要优于仅使用阻抗数据的模型。
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引用次数: 1
Ground Penetrating Radar Attenuation Expressions in Shallow Groundwater Research 浅层地下水探地雷达衰减表达式研究
IF 1 4区 工程技术 Q2 Earth and Planetary Sciences Pub Date : 2020-03-01 DOI: 10.2113/JEEG19-039
M. C. Paz, F. Alcalá, L. Ribeiro
The electromagnetic-wave attenuation coefficient determines the overall resolution and effective penetration depth of ground penetrating radar (GPR) surveys. Despite this relevance to the design of proper GPR surveys, the attenuation expressions are rarely used in the applied shallow groundwater research (SGR) literature. This work examines the status of the attenuation expressions in SGR. For this, 73 GPR case studies (in 47 papers), including some information concerning the attenuation variables and parameters, were selected to build a database. From these, 18 cases (in 10 papers) provided attenuation expressions and only 11 cases (in 4 papers) used those expressions. Two types of expressions were identified, physically based global ones that try to solve a broad (but not complete) range of environmental and field technical conditions, and non-global ones adapted for specific geological environments and resolution needed. The database analysis showed that both global and non-global expressions were used exclusively in low-loss media to report an attenuation range of 0.1–21.5 dB m−1 by using common antenna frequencies in the 25–900 MHz range. The range of the attenuation expressions validity in SGR is biased because no surveys in variable-loss heterogeneous media and wider antenna frequency intervals could be compiled. The attenuation database generated seeks to improve the design of GPR surveys in SGR.
电磁波衰减系数决定了探地雷达探测的总分辨率和有效探深。尽管衰减表达式与合理的探地雷达测量设计相关,但在应用浅层地下水研究(SGR)文献中很少使用衰减表达式。本文研究了SGR中衰减表达式的现状。为此,选取了73个GPR案例研究(47篇论文),包括一些有关衰减变量和参数的信息,建立数据库。其中,18例(10篇论文)提供了衰减表达式,只有11例(4篇论文)使用了衰减表达式。确定了两种类型的表达,一种是基于物理的全球表达,试图解决广泛(但不完整)的环境和现场技术条件,另一种是非全球表达,适用于特定的地质环境和所需的分辨率。数据库分析表明,使用25-900 MHz范围内的公共天线频率,在低损耗介质中只使用全局和非全局表达式,报告的衰减范围为0.1-21.5 dB m−1。由于无法编制变损耗非均匀介质和较宽天线频率间隔的调查,SGR中衰减表达式的有效性范围存在偏差。生成的衰减数据库旨在改进SGR中探地雷达调查的设计。
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引用次数: 1
A Theoretical Study of Underground Magnetic Resonance Sounding for the Advanced Detection of Water Influxes in Tunnels 地下磁共振测深超前探测隧道涌水的理论研究
IF 1 4区 工程技术 Q2 Earth and Planetary Sciences Pub Date : 2020-03-01 DOI: 10.2113/JEEG19-021
Yue Zhao, Jun Lin, Chuandong Jiang, Xiaofeng Yi
Based on surface magnetic resonance sounding (MRS), a relationship is proposed to express the MRS response signal with a vertical coil for the MRS method for a whole underground space model. Firstly, the declination and inclination characteristics of the Earth's magnetic field and the coil normal angle are studied by deriving the angle rotation matrix. Surprisingly, the results indicate that the MRS signal can be effectively improved by changing the normal direction of the coil perpendicular to that of the Earth's magnetic field. The advanced detection distance of the underground MRS method is closely related to the exciting pulse moment and the receiving sensitivity. Hence, a larger pulse moment and high receiving sensitivity correspond to a longer advanced detection distance. However, the limited transmitting moment will reduce the advanced detection distance. In the research coincident loop with the coil 2 m by 2 m square is employed. In order to overcome the noises with 1 nV and 100 nV level, the turns of loop should be 100 turns and 400 turns, respectively. Finally, the numerical simulation results verify the feasibility of underground whole MRS theory and resolution analysis method for the advanced detection of water-inrush disasters in mines and tunnels.
在地表磁共振测深的基础上,提出了用垂直线圈表示地表磁共振响应信号的关系式,用于整个地下空间模型的地表磁共振测深方法。首先,通过推导角度旋转矩阵,研究了地磁场的赤斜特性和线圈法向角;令人惊讶的是,结果表明,通过改变垂直于地球磁场方向的线圈的法向,可以有效地改善MRS信号。地下磁振法的超前探测距离与激发脉冲矩和接收灵敏度密切相关。因此,较大的脉冲矩和较高的接收灵敏度对应较长的超前探测距离。然而,有限的发射力矩会减少超前探测距离。在研究中,与线圈重合的回路采用了2m × 2m的正方形。为了克服1 nV和100 nV级别的噪声,回路匝数应分别为100匝和400匝。最后,数值模拟结果验证了井下整体MRS理论和分辨率分析方法在矿井和隧道突水灾害超前探测中的可行性。
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引用次数: 0
Site Characterization of Soil-rock Mixture Sedimentary Stratum Based on HVSR Analysis in the Chinese Loess Plateau 基于HVSR分析的中国黄土高原土石混合沉积层场地特征
IF 1 4区 工程技术 Q2 Earth and Planetary Sciences Pub Date : 2020-03-01 DOI: 10.2113/JEEG19-060
Ruyun Tian, Ma Liwei, Xiaohua Zhou, Wang Junqiu, Jun Lin, Dong-sheng Li
The soil-rock mixture sedimentary stratum is a compound with complex and loose topography, of which the structure is difficult to detect by the ordinary geophysical method. There is a need for a convenient, efficient and effective geophysical method to detect site effects in this area. This paper is an application of the S wave velocity profile inversion for the soil-rock mixture sedimentary stratum, using HVSR (Horizontal to Vertical Spectral Ratio) analysis of ambient noise by some three-component observations in the Chinese Loess Plateau. We carried out the measurement using three nested circular arrays and data recording systems with a spectrum expansion circuit. Inversion of the HVSR curves was performed by a three-layer model. Results of geological observation reveal that the upper part of the sedimentary stratum is Quaternary strata containing a large amount of humus and loess, the middle layer part is the stratum of the loose gravel and the under part is completely weathered granite with homogeneous lithology and fewer rocks. Interpretation results are consistent with previous drilling data, providing a valid geophysical basis for evaluating the stability of the soil erosion and designing a reasonable water and soil erosion control scheme.
土石混合沉积层是一种地形复杂松散的复合地层,其结构难以用普通地球物理方法探测。需要一种方便、高效、有效的地球物理方法来检测该地区的场址效应。本文利用横竖谱比(HVSR)对中国黄土高原部分三分量观测资料的环境噪声进行分析,将S波速度剖面反演应用于土石混合沉积层。我们使用三个嵌套的圆形阵列和带有频谱扩展电路的数据记录系统进行测量。采用三层模型对HVSR曲线进行反演。地质观测结果表明,沉积地层上部为第四纪地层,含大量腐殖质和黄土,中层为松散砾石层,下部为完全风化的花岗岩,岩性均匀,岩石较少。解释结果与以往钻井资料基本一致,为评价水土流失稳定性、设计合理的水土流失防治方案提供了有效的地球物理依据。
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引用次数: 3
2D High-Resolution Crosswell Seismic Traveltime Tomography 二维高分辨率井间地震走时层析成像
IF 1 4区 工程技术 Q2 Earth and Planetary Sciences Pub Date : 2020-03-01 DOI: 10.2113/JEEG19-003
Chuan Li, Jianxin Liu, Jianping Liao, Jianping Liao, A. Hursthouse
This paper presents a method for combining the hybrid eikonal solver and the prior velocity information to obtain high-resolution crosswell imaging. The hybrid eikonal solver in this technique can ensure rapid and reliable forward modeling of traveltime field in an unsmoothed velocity model. We also utilize the sonic well logging curve to properly develop an initial reference velocity model, and use the sonic well logging data as the prior information for the inversion part, which can restrict the problem of non-uniqueness. The results of the numerical experiment of traveltime in multi-layer media showed that the hybrid eikonal solver was more accurate than the finite difference method. The case study of an oil field in eastern China demonstrated that our method can derive a high-resolution reconstruction of the subsurface structure by inverting the primary traveltime datasets. These results suggest that even though the eikonal equation is a high frequency approximation to the wavefield, the hybrid eikonal solver can provide an accurate traveltime field in the forward modelling step of seismic crosswell tomography, which is critical to ensure high-resolution invert imaging in a highly heterogeneous environment.
提出了一种结合混合正交求解器和先验速度信息获得高分辨率井间成像的方法。该方法所采用的混合正交求解器可以保证非光滑速度模型中行时场的快速、可靠的正演建模。利用声波测井曲线适当地建立了初始参考速度模型,并将声波测井数据作为反演部分的先验信息,有效地限制了非唯一性问题。多层介质中行时的数值实验结果表明,混合正交法比有限差分法更精确。对中国东部某油田的实例研究表明,该方法可以通过反演原始走时数据集获得高分辨率的地下结构重建。这些结果表明,尽管eikonal方程是波场的高频近似,但混合eikonal求解器可以在地震井间层析成像的正演模拟步骤中提供准确的走时场,这对于确保在高度非均质环境下的高分辨率反演成像至关重要。
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引用次数: 2
Introduction to the JEEG Special Issue on Geophysics for Urban Underground Space Studies JEEG《城市地下空间地球物理学研究》特刊简介
IF 1 4区 工程技术 Q2 Earth and Planetary Sciences Pub Date : 2019-12-23 DOI: 10.2113/JEEG24.4.V
Lanbo Liu, R. Qian
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引用次数: 0
Integrated ERT, Seismic, and Electrical Resistivity Imaging for Geological Prospecting on Metro Line R3 in Qingdao, China 青岛地铁R3线ERT、地震、电阻率综合地质勘探
IF 1 4区 工程技术 Q2 Earth and Planetary Sciences Pub Date : 2019-12-23 DOI: 10.2113/JEEG24.04.537
Nie Lichao, Ma Zhao, Wang Chengkun, Rentai Liu, Liu Zhengyu, Zhou Wei, Jian Li, S. Ju
Metros are mass rapid-transit systems that have helped solve commuting problems for residents of metropolises throughout the world. However, adverse geological structures, leading to problem such as water inrush and mud gushing, pose a major threat to metro construction. Geophysical survey techniques provide quick and relatively inexpensive ways to detect adverse geological structures ahead of the tunnel face. Left line of the R3 metro tunnel in Qingdao, China will pass an aquifer sand layer under the Wolong River. To map the geological conditions below the river, we proposed a comprehensive prospecting method that would combine the merits of surface electrical resistivity imaging (S-ERT), seismic ahead prospecting, and tunnel-face and borehole electrical resistivity imaging (TBERI). The prospecting scheme was effectively revealed in a numerical model analysis, in which the stratum distribution was reconstructed using S-ERT. Field tests validated the synthetic results. The ahead prospecting scheme was able to reconstruct the distribution of an aquifer sand layer. Based on the results obtained, we believe that, the proposed scheme could play an important role in metro tunnel construction.
地铁是一种大型快速交通系统,它帮助解决了世界各地大都市居民的通勤问题。然而,不利的地质构造导致的突水、涌泥等问题对地铁建设构成了重大威胁。地球物理测量技术为探测巷道前方不利地质构造提供了快速且相对廉价的方法。中国青岛R3地铁隧道左线将通过卧龙河下的含水层砂层。为了绘制河下地质条件图,提出了一种综合地表电阻率成像(S-ERT)、地震超前勘探和巷道面钻孔电阻率成像(TBERI)优点的综合勘探方法。通过数值模型分析,利用S-ERT重建地层分布,有效地揭示了找矿方案。现场试验验证了合成结果。该超前勘探方案能够重建含水层砂层的分布。结果表明,该方案可在地铁隧道施工中发挥重要作用。
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引用次数: 4
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Journal of Environmental and Engineering Geophysics
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