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在假设声场不受电磁场影响的前提下,将Pride声电耦合方程组化为具有电流源的麦克斯韦方程组.与空间位置固定的电流源产生的电磁场不同,孔隙地层中声波诱导的电磁场是由空间波动的电流源产生的.通过引入赫兹矢量,将求解麦克斯韦方程组问题转化为求解关于赫兹矢量的非齐次矢量赫姆霍兹方程组.通过求解该方程组,得出电磁场表达式.利用此方法,针对声电效应测井,分别计算了由单极声源、偶极声源、四极声源激发的井内声场及其诱导电磁场的全波波形.
关键词:
孔隙介质
诱导电磁场
测井
多极声源 相似文献
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由于孔道的双电层结构和流体-固体耦合运动, 弹性波在孔隙地层中传播时会引起电磁场. 前人提出了基于这种耦合效应的震电测井方法, 但对井中震电波的特性缺少细致的分析. 本文对孔隙地层充流体井孔中点声源激发的震电耦合波的分波进行分析, 证明了井孔流体电磁波波数不是井内震电波场支点, 计算了地层电磁波支点、横波支点和快纵波支点对应的侧面波. 在利用辐角原理求出震电波场函数的复极点之后, 针对典型砂岩地层计算了震电波场模式波(包括泄漏模式)的频散曲线和声压、电场激发曲线. 计算了各个侧面波和模式波的电场激发强度与声压激发强度的比值(电声激发比), 发现纵波的电声激发比相对于横波和模式波更高, 而Stoneley波电声激发比的辐角对渗透率敏感, 其敏感性会随频率增大而增加, 随孔隙度增大而降低. 相似文献
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水下目标的前向声散射会引起声波传播过程中的简正波耦合效应,使得接收声场结构发生变化,研究目标前向散射引起的垂直阵列上空域响应变化特征,可实现对直达波强干扰背景下的前向散射检测。通过将垂直阵波束形成技术分别用于信道中目标散射场理论模型计算数据和湖上实验验证数据,分析了等声速环境中目标前向声散射简正波耦合的垂直阵空域响应特征。结果表明,目标靠近接收端时前向散射引起的声波垂直达到结构与无目标时相比差异显著,高阶简正波向低阶简正波转化导致信号到达时延宽度展宽,采用指向水平方向的窄波束可显著提取目标前向散射引起的接收声波变化特征。 相似文献
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“储层声学”属于多相孔隙固体介质声学的研究范畴,它是研究声波在储层中的产生、传播、接收及声波与储层相互作用及应用等的一门学问。储层声学从提出到现在有十多年的发展历史,它虽是一个年轻的声学分支,但它是在面向地震勘探和地震储层预测等基础问题上发展起来的,且在实际需求的驱动下发展迅速。储层声学要回答以下问题:声波是如何在孔隙性、裂缝性及各向异性的多相储层介质中传播的,组成储层的各组分及特性等对声波的传播是如何影响的,如何利用这些声学特征来描述储层的组分和特性以及声波引起的各种物理效应与储层是如何相互作用的。 相似文献
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致密储层声波性质受骨架矿物组成及孔隙类型影响较大,为更准确进行气层识别,本文给出了一种综合模型,和利用纵横波速度信息进行致密气层识别的方法:其首先利用Voigt-Reuss-Hill平均模型,求取岩石骨架等效弹性模量,消除岩性影响;根据综合模型和岩石剪切模量计算孔L隙纵横比(或裂隙密度),消除孔隙性质影响;利用DEM和K-T模型计算干燥岩石弹性模量,得到不受孔隙流体性质影响的弹性模量;将实测岩石弹性模量减去干燥岩石弹性模量定义为含气性因子;同时利用最小二乘法和体积模量,进行气层识别。本文含气分析方法考虑因素全面,干燥岩石纵横波速度比非定值,为具有复杂岩性和低孔低渗等特征的致密岩石气层识别提供技术支持。 相似文献
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对于常规储层,核磁共振是一项十分有效的解释-评价技术,它既能评价岩石物性与孔隙结构,又能评价孔隙流体分布与饱和度,且具有快速、无损、经济等特点;而对于页岩储层,其核磁共振受纳米级孔隙、复杂矿物成分、特殊孔隙结构、较高有机质含量、超低渗透性及内部梯度和受限扩散等因素的影响,面临探测分辨率低、解释模型不适用等瓶颈.为了发挥该项技术在页岩油气勘探开发中的作用,将国内外的页岩油气层核磁共振分析、评价技术与相关的页岩油气层实验室微观分析成果相结合,进行了系统梳理,从探测分辨率的提高、孔隙结构与岩石物性评价模型的建立、孔隙流体分布与识别模型的建立等方面进行了综述,提出需加强纳米孔的核磁共振弛豫机理和提高 D-T2二维谱分辨率两个基础研究,在此基础上,进一步完善岩石物理及孔隙流体两个评价模型. 相似文献
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声波测井时孔隙地层中的声波首波平行于井轴沿井壁传播,它既有轴向位移分量,又有垂直于井壁的位移分量.这种以快纵波速度传播的波, 不仅含有由快、慢纵波势给出的梯度场,而且还含有由横波势给出的旋度场.慢纵波势的梯度是渗流位移首波的主要构成成分, 也是声电效应测井响应中存在伴随声波首波电场的主要原因.首波包含有旋度位移场,是存在伴随声波首波磁场的原因.
关键词:
孔隙介质
声波首波
诱导电磁场
测井 相似文献
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Numerical Simulation of Shear-Horizontal-Wave-Induced Electromagnetic Field in Borehole Surrounded by Porous Formation 下载免费PDF全文
Seismoelectric fieM excited by purely torsional loading applied directly to the borehole wall is considered. A brief formulation and some computed waveforms show the advantage of using shear-horizontal (SH) transverseelectric (TE) seismoelectric waves logging to measure shear velocity in a fluid-saturated porous formation. By assuming that the acoustic field is not influenced by its induced electromagnetic field due to seismoeleetric effect, the coupling governing equations for electromagnetic field are reduced to Maxwell equations with a propagation current source. It is shown that this simplification is valid and the borehole seismoelectric conversion efficient is mainly dependent on the electrokinetic coupling coefficient. The receivers to detect the conversion electromagnetic field and to obtain shear velocity can be set in the borehole fluid in the SH-TE seismoelectric wave log. 相似文献
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研究浅层土壤中声波耦合的地震波的传播特性, 用于声波探雷技术的机理分析. 根据浅层土壤具有孔隙度和可压缩性的特点, 利用非饱和三相孔隙介质中的地震波模型, 研究了土壤孔隙度、含水饱和度等参数对地震波传播特性的影响. 计算结果显示: 在给定的参数条件下, 地震波的传播速度和衰减系数均随频率的增加而增加; 纵波的传播速度随孔隙度的增加而减小, 横波的传播速度随孔隙度的增加而增加; 地震波的传播特性随含水饱和度的增加变化比较复杂. 通过对计算结果与已发表实验结果的比较分析, 讨论了解析方法的可行性, 为声-地震耦合机理及其在声波探雷研究中的应用提供了一定的理论基础.
关键词:
声-地震耦合
地震波
孔隙度
声波探雷 相似文献
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The conversion of energy between seismic and electromagnetic wave fields has been described by Pride’s coupled equations in porous media. In this paper, the seismoelectric field excited by the explosive point source located at the outside of the borehole is studied. The scattering fields inside and outside a borehole are analyzed and deduced under the boundary conditions at the interface between fluid and porous media. The influences of the distance of the point source, multipole components of the eccentric explosive source, and the receiving position along the axis of vertical borehole, on the converted waves inside the borehole are all investigated. When the distance from the acoustic source to the axis of a borehole is far enough, the longitudinal and coseismic longitudinal wave packets dominate the acoustic and electric field, respectively. The three components of both electric field and magnetic field can be detected, and the radial electric field is mainly excited and converted by the dipole component. Owing to the existence of borehole, the electric fields and magnetic fields in the borehole are azimuthal. The distance from the point where the maximum amplitude of the axial components of electric field is recorded, to the origin of coordinate indicates the horizontal distance from the explosive source to the axis of vertical borehole. 相似文献
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Shear-horizontal transverse-electric seismoelectric waves in cylindrical double layer porous media 下载免费PDF全文
The shear-horizontal(SH) waves excited by the shear source in a borehole are easy to analyze due to the simple waveform. The borehole-side structures make the formation properties discontinuous. We consider a cylindrical double layer structure and study the borehole shear-horizontal and transverse-electric(SH-TE) seismoelectric waves. We first derive the expressions of the basic field quantities, and simulate the acoustic field and electric field using the real axis integral method. Compared with the wave fields of an infinitely homogeneous porous medium outside the borehole, the cylindrical layered structure makes the multi-mode cylindrical Love waves and their accompanying electric fields excited.Next, in order to study the interface response law of the inducing electric fields, we use the secant integral method to calculate the interface converted electromagnetic waves and analyze the causes of each component. It is found that an interface response occurs each time the SH wave impinges the interface in the layered porous medium. The results show that the SH-TE mode has a potential application for borehole-side interface detection in geophysical logs. 相似文献
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The scattering of electromagnetic waves in fractal media is studied. The fractal dimension is naturally involved in the formulation of two physical problems studied in this paper. The general theory of multiple scattering of electromagnetic wave in fractal media is developed by modifying Twersky's theory. Statistical quantities, such as the average field and average intensity of the multiple scattered wave, are studied for a wave propagating in a fractal medium. The scattering cross section of the medium is deduced. The backscattering of electromagnetic waves is also studied. The results showing the range of dependence of the backscattered signals are in agreement with numerical simulations by Rastogi and Scheucher (1990). It also suggests a method of measuring the fractal dimension of the fractal embedded media using radar sounding. The theory developed in this paper can also be used for problems related to multiple scattering of other kinds of waves, such as acoustic waves, elastic waves etc, in fractal media. 相似文献
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Acoustic and electromagnetic fields are coupled in a fluid saturated porous medium due to seismoelectric effect. Seismoelectric
well logging method has been proposed to detect deep target formation utilizing such effect. Because of uncoupling of SH waves
with P-SV waves, a simple and forthright way to get shear waves information is possible, especially for soft or slow formation
whose shear wave velocity is lower than the velocity of borehole fluid. We consider the wave fields excited by a vertical
magnetic dipole (VMD) source. Two methods are used to simulate, one is the coupled method based on Pride model and the other
is the uncoupled method. For two methods, the frequency wavenumber domain representations of the acoustic field and associated
seismoelectric field are formulated. The full waveforms of acoustic waves and electromagnetic wave induced SH waves excited
by VMD source in the time domain propagation in borehole are simulated and analyzed. 相似文献
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Acousto-electric well logging by eccentric source and extraction of shear wave 总被引:1,自引:0,他引:1 下载免费PDF全文
The nonaxisymmetric acousto-electric field excited by
an eccentric acoustic source in the borehole based on Pride seismoelectric
theory is considered. It is shown that the acoustic field inside the borehole,
converted electric and magnetic fields and coupled fields outside the borehole
are composed of an infinitude of multipole fields with different orders.
The numerical results show that
both the electromagnetic waves and the seismoelectric field in the borehole,
and the three components of both electric field and magnetic field
can be detected. Measurements on the borehole axis will be of
advantage to determining shear velocity information. The components
of the symmetric and nonsymmetric acoustic and electromagnetic fields
can be strengthened or weakened by adding or subtracting the two full
waveforms logged in some azimuths. It may be a new method of directly
measuring the shear wave velocity by using the borehole
seismoelectric effect. 相似文献
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《Waves in Random and Complex Media》2013,23(1):97-103
Abstract The scattering of electromagnetic waves in fractal media is studied. The fractal dimension is naturally involved in the formulation of two physical problems studied in this paper. The general theory of multiple scattering of electromagnetic wave in fractal media is developed by modifying Twersky's theory. Statistical quantities, such as the average field and average intensity of the multiple scattered wave, are studied for a wave propagating in a fractal medium. The scattering cross section of the medium is deduced. The backscattering of electromagnetic waves is also studied. The results showing the range of dependence of the backscattered signals are in agreement with numerical simulations by Rastogi and Scheucher (1990). It also suggests a method of measuring the fractal dimension of the fractal embedded media using radar sounding. The theory developed in this paper can also be used for problems related to multiple scattering of other kinds of waves, such as acoustic waves, elastic waves etc, in fractal media. 相似文献