• A new scheme to define all time apparent resistivity is introduced.

    介绍了一种新的全区视电阻率计算方法。

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  • Ore distributed shape was deduced by the apparent resistivity section.

    利用视电阻率切片图来推演矿体展布形态。

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  • Prom these values the apparent resistivity on the ground surface can be calculated.

    由这些值可计算地表的视电阻率。

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  • Usually, side-wall core taker uses apparent resistivity curve for locating formation.

    井壁取心通常是采用跟踪视电阻率曲线定位。

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  • Parameters of apparent resistivity, impedance phase, and anomaly phase can be acquired.

    可提供视电阻率、阻抗相位、异常相位等地电学参数。

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  • Aimed at central loop array, a method calculating the all-time apparent resistivity is proposed, .

    给出了一种方便快捷的瞬变电磁全区视电阻率数值计算方法逆样条插值法。

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  • The differential curve of apparent resistivity has a higher resolution than apparent resistivity itself.

    视电阻率差分曲线具有比视电阻率曲线更高的分辨率。

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  • The present paper introduces the working method of the transborehole synchronous apparent resistivity survey.

    本文介绍了跨孔同步视电阻串测量工作方法。

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  • In addition, this paper gives an example of quantitative analysis of the annual variation of apparent resistivity.

    本文还举了一个定量分析视电阻率年变化的例子。

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  • The apparent resistivity in the version profiles of TEM sounding were figured and the shapes of ore bodies was outlined.

    并作出TEM测深视电阻率反演断面图,勾绘出矿体的空间形态。

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  • At present, the far-zone apparent resistivity definition is usually used in the frequency domain electromagnetic methods.

    目前在频率域电磁法中常常采用远区视电阻率定义。

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  • The method is used for processing the apparent resistivity of magnetotelluric measured depth, and better result is achieved.

    使用该方法对大地电磁测深视电阻率进行了处理,应用效果良好。

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  • Sied-hole reference for estimating the gradient anomaly of apparent resistivity is put forward on the basis of literature 3.

    本文在文献3的基础上,提出了一种计算视电阻率梯度异常的旁井参照法。

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  • In TM mode, the distortion of phase is less than apparent resistivity, so the weight of phase in inversion can be increased.

    对于TM模式,相位受三维畸变影响较小,视电阻率较大,所以二维反演中可适当加大相位的权;

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  • The engineering in this paper case commences designing to apply apparent resistivity in detection of karst cracks developed.

    本文所述工程实例开始设计应用视电阻率测深来探测工程区的岩溶裂隙发育情况。

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  • Pole-pole electrical potential can be transformed to apparent resistivity of any electrode arrangement by linear combination.

    通过线性组合,单极—单极电位可以转换到各种装置的视电阻率。

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  • Practice proved the combined apparent resistivity and induced polarization method to find underground water was very successful.

    实践证明,利用视电阻率法和激发极化法相结合的方法找寻地下水是非常成功的。

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  • The apparent resistivity mapping of the helicopter frequency domain em system in magnetic area has been a problem of long controversy.

    直升机频率域电磁系统在磁性地区的视电阻率填图,长期存在争议。

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  • The theoretic formula of apparent resistivity in horizontal, uniform bedded medium can be transformed into a convolution filtering expression.

    水平均匀层状介质的视电阻率理论计算公式,可以转换成一种褶积滤波形式。

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  • The location of the crack can be found by the change of the apparent resistivity, based on four-probe electrical resistivity measuring technique.

    基于四探针电阻率测量技术,依据试验测得的混凝土表观电阻率变化确定裂缝位置。

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  • The curves of apparent resistivity obtained from Magnetotelluric Sounding are greatly distorted by the lateral inhomogeneity of surficial structures.

    大地电磁测深结果受表层构造横向不均匀性的影响,其视电阻率曲线会发生畸变。

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  • A numerical method for calculating the exact all-time apparent resistivity for time domain transient electromagnetic method is proposed in this paper.

    给出了一种时间域瞬变电磁法视电阻率的数值计算方法,利用该方法可以容易地求出中心方式的全程视电阻率。

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  • The joint-inversion method of three kinds of one-component apparent resistivity-phase is studied. Morever, the practical applied results are expounded.

    研究了电偶源频率电磁测深中三种单分量视电阻率—相位联合反演的实施方法,并论述了其实际应用效果。

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  • To effectively make use of resistivity information, apparent resistivity and its difference curve are used respectively in engineering and compared them.

    将视电阻率曲线与视电阻率一阶差分曲线应用于岩土工程施工中。

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  • The results of filtering and then inversion for the surveyed data show that it is feasible and useful to carried out filtering on apparent resistivity data.

    本文对高密度电阻率法野外实测资料进行了滤波处理,并且通过实际反演计算结果,认为对视电阻率进行滤波是可行的。

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  • In this paper, full-space late-time and all-time apparent resistivity formula was derived based on homogeneous full-space response equation of central loop.

    从全空间中心回线源响应公式出发,推导了全空间晚期和全区视电阻率公式;

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  • In MT, apparent resistivity and phase have been used as interpretative parameter for a long time. However, apparent resistivity and phase have some limitations.

    大地电磁测深研究中,长期以来使用视电阻率和相位作为解释参数,但视电阻率和相位均存在一定的局限性。

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  • Combined with practical work, the application of composite profile method and apparent resistivity sounding method in primary de-sign of building project is introduced.

    结合工程实例,介绍了联合剖面法、视电阻率测深法在土建项目初步设计中的应用,解释了其应用中的异常特征与推断,为项目初步设计提供工程水文地质依据。

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  • Solving the equation system, we can obtain the electric potential value on nodes. According to these value, the apparent resistivity on ground surface can be calculated.

    解方程组,得各节点的电位值,由此可计算地表的视电阻率。

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  • Solving the equation system, we can obtain the electric potential value on nodes. According to these value, the apparent resistivity on ground surface can be calculated.

    解方程组,得各节点的电位值,由此可计算地表的视电阻率。

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