共查询到19条相似文献,搜索用时 530 毫秒
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井间电阻率层析成像研究新进展 总被引:1,自引:3,他引:1
由于井间电阻率层析成像方法具有施工方便、成本低、对钻孔无破坏作用且穿透深度也较大等优点,因而得到越来越广泛的应用,在过去几年内对该方法研究的重点在于提高计算效率和改善成像质量,本文从井间电阻率层析成像的基本原理出发,对该方法近年的新进展进行了比较和综述,还介绍了概率层析成像算法的原理,认为今后几年内在此领域内的理论研究重点将是探索有效的反演方法和提高成像质量。 相似文献
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基于边界积分方程 ,提出了依据二极采样数据、但利用电位差的某种线性组合的“准三极”电阻率层析成像方法 .研究表明 ,该方法不仅较好地解决了对高阻异常体的成像问题 ,而且使低阻异常体的成像质量获得了明显改善和提高 ,因此增强了电阻率层析成像技术的实用性 . 相似文献
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基于边界积分方程,提出了依据二极采样数据、但利用电位差的某种线性组合的"准三极"电阻率层析成像方法.研究表明,该方法不仅较好地解决了对高阻异常体的成像问题,而且使低阻异常体的成像质量获得了明显改善和提高,因此增强了电阻率层析成像技术的实用性. 相似文献
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《地球物理学进展》2017,(1)
随着城市工程勘探及煤矿采矿区勘探要求的不断提高,二维地面及孔间电阻率成像无法确定电性异常沿垂直剖面方向延伸范围,三维地面电阻率成像面临着纵向分辨率小、空间覆盖不均匀等问题.本文提出井地井三维全通道电阻率成像方法,该方法计算时采用除去2个供电电极外其余全部接地电极所采集数据进行反演计算.在成像时首先采用有限差分方法求解3D静电场方程,并基于伴随矩阵方法计算非线性灵敏度矩阵,最后利用牛顿共轭梯度反演方法实现全通道电阻率层析成像.通过理论数据测试表明:全通道3D井地井联合观测方式能有效的对孔间电性结构三维成像,具有较好的纵横向分辨率,可以较好的解决实际工程地质问题及采空区在空间的分布形态难题. 相似文献
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电流线追踪电位电阻率层析成像方法初探 总被引:4,自引:3,他引:4
电阻率层析成像技术尽管已有了一些比较好的结果,但从国内外发表的文章可以看出,基本上采用的都是有限元方法,而电阻率层析成像的核心问题也就是雅可比矩阵的求取问题。有限元方法能够很好地实现该问题的求解,但需要的计算机内存及计算时间相当的大,为此我们类比地震学中走时射线追踪技术,开展了电流线追踪电位电阻率层析成像方法研究。 相似文献
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径向基神经网络(RBFNN)具有结构简单、学习速度快、不易陷入局部极小等优点,能够有效地提高电阻率层析成像反演的收敛速度和求解质量.本文针对电阻率层析成像反演的非线性特征,提出了一种基于汉南-奎因信息准则(HQC)的正交最小二乘法(OLS)学习算法(HQOLS).该算法通过计算HQC的最优值来自动选择RBFNN的网络结构,避免了传统OLS学习算法中阈值参数的设定,保证了网络的泛化性能.通过比较聚类法、梯度法、OLS和HQOLS等学习算法的反演性能,构建了基于RBFNN的电阻率层析成像反演模型.数值仿真和模型反演的结果表明,该方法实现简单,在准确性上优于BP反演,成像质量优于传统最小二乘法反演. 相似文献
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(金延龙,赵卫明)AnimprovementonthemethodofthepatternrecognitionICHAManditsapplication¥Wei-MingZHAOandYan-LongJIN(SeismologicalBureau... 相似文献
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The standard ray theory (RT) for inhomogeneous anisotropic media does not work properly or even fails when applied to S-wave
propagation in inhomogeneous weakly anisotropic media or in the vicinity of shear-wave singularities. In both cases, the two
shear waves propagate with similar phase velocities. The coupling ray theory was proposed to avoid this problem. In it, amplitudes
of the two S waves are computed by solving two coupled, frequency-dependent differential equations along a common S-wave ray.
In this paper, we test the recently developed approximation of coupling ray theory (CRT) based on the common S-wave rays obtained
by first-order ray tracing (FORT). As a reference, we use the Fourier pseudospectral method (FM), which does not suffer from
the limitations of the ray method and yields very accurate results. We study the behaviour of shear waves in weakly anisotropic
media as well as in the vicinity of intersection, kiss or conical singularities. By comparing CRT and RT results with results
of the FM, we demonstrate the clear superiority of CRT over RT in the mentioned regions as well as the dangers of using RT
there. 相似文献
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径向道变换(Radial Trace Transform)是将地震道集振幅值从偏移距一双程旅行时坐标系变换到视速度-双程旅行时坐标系,通过这种坐标系的变换,使相干噪声与有效信号在视速度和频率方面都有效分离.本文在介绍RT变换基本原理基础上,分析了RT变换中两种常用插值方法及其特点.并利用对模拟地震资料的处理,证明了RT域模拟-相减法较其带通滤波法在相干噪声压制与反射信号保持方面具有明显优势.最后,根据噪声特点,通过选择合理RT滤波参数,对实际地震资料进行处理试验,获得了较好的去噪效果,明显提高了资料信噪比,验证了研究方法的有效性. 相似文献
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The conventional nonstationary convolutional model assumes that the seismic signal is recorded at normal incidence. Raw shot gathers are far from this assumption because of the effects of offsets. Because of such problems, we propose a novel prestack nonstationary deconvolution approach. We introduce the radial trace (RT) transform to the nonstationary deconvolution, we estimate the nonstationary deconvolution factor with hyperbolic smoothing based on variable-step sampling (VSS) in the RT domain, and we obtain the high-resolution prestack nonstationary deconvolution data. The RT transform maps the shot record from the offset and traveltime coordinates to those of apparent velocity and traveltime. The ray paths of the traces in the RT better satisfy the assumptions of the convolutional model. The proposed method combines the advantages of stationary deconvolution and inverse Q filtering, without prior information for Q. The nonstationary deconvolution in the RT domain is more suitable than that in the space-time (XT) domain for prestack data because it is the generalized extension of normal incidence. Tests with synthetic and real data demonstrate that the proposed method is more effective in compensating for large-offset and deep data. 相似文献
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The linearly regressive Gamma Markov sequence is being increasingly used as a model for geophysical phenomena, one of the reasons being that it is possible to determine the distribution of (weighted or otherwise) cumulative sums of such a sequence. In this paper we show briefly how to simulate such a sequence and its seasonal extension; we also show how to estimate its parameters. It is shown that the estimates obtained by the method of moments do not have a high efficiency, whereas those obtained by a modified maximum likelihood method have an efficiency close to unity. 相似文献
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宇宙射线μ子检测技术具有穿透力强、对高Z材料敏感等特点,特别适合检测特殊核材料,是监控核材料走私的有效方式.图像重建问题是实现该技术的一个关键难点,MLS-EM算法是目前成像质量较好的算法,但其过长的运算时间制约了该算法在实际μ子检测系统中的应用.根据μ子检测系统的特点,本文提出了一种加速方法,在使用POCA重建图像作为迭代初值基础上进一步采用OS方法进行EM加速.模拟实验结果表明该方法能够有效地对MLS-EM重建算法进行加速,这对于宇宙射线μ子成像技术早日投入实际应用具有积极的意义. 相似文献