首页> 外国专利> UNDERGROUND RELATIVE DIELECTRIC CONSTANT MEASURING METHOD AND GEOLOGICAL FEATURES MEASURING METHOD AND POSITION MEASURING METHOD

UNDERGROUND RELATIVE DIELECTRIC CONSTANT MEASURING METHOD AND GEOLOGICAL FEATURES MEASURING METHOD AND POSITION MEASURING METHOD

机译:地下相对介电常数测量方法,地质特征测量方法和位置测量方法

摘要

PURPOSE: To measure underground relative dielectric constant with high precision and measure a distance up to a reflected object and geological features with high precision in the same way. ;CONSTITUTION: Electromagnetic waves having a certain frequency f0 are transmitted into the ground from a transmission antenna 3, and surface reflected waves synthesized by the transmitted waves are received by a reception antenna 4 to distinguish frequency f from the attenuation cycle of a first cycle. By checking this frequency f with frequency.relative dielectric constant characteristics data which indicates correlation with relative dielectric constant, corresponding relative dielectric constant is obtained. A voltage peak point of mutual correlation function of a waveform of the received signal and natural attenuation waveform in the case where there is no reflection due to an obstacle is obtained, and the position of the reflected object is calculated based on time T of the peak point and propagation velocity μ of electromagnetic waves obtained from the relative dielectric constant which is measured previously. Furthermore, an attenuation rate is obtained from the natural attenuation waveform in the case where there is no reflection due to the obstacle to calculate specific resistance or conductivity from the attenuation rate, and corresponding type of geological features is extracted from data base by using this value and relative dielectric constant which is measured previously as parameters.;COPYRIGHT: (C)1996,JPO
机译:目的:以高精度测量地下相对介电常数,并以相同的方式高精度测量到反射物体的距离和地质特征。组成:具有一定频率f0的电磁波从发射天线3发射到地面,由发射波合成的表面反射波被接收天线4接收,以将频率f与第一周期的衰减周期区分开。通过用表示相对介电常数的相关性的频率相对介电常数特性数据来检查该频率f,可以获得对应的相对介电常数。获得在没有由于障碍物引起的反射的情况下接收信号的波形和自然衰减波形的互相关函数的电压峰值点,并且基于峰值的时间T来计算反射物体的位置。由先前测量的相对介电常数获得的电磁波的点和传播速度μ。此外,在由于障碍物而没有反射的情况下,从自然衰减波形中获得衰减率,从而根据该衰减率计算比电阻或电导率,并使用该值从数据库中提取相应的地质特征类型。相对介电常数,先前已将其作为参数进行测量。;版权:(C)1996,日本特许厅

著录项

  • 公开/公告号JPH08122279A

    专利类型

  • 公开/公告日1996-05-17

    原文格式PDF

  • 申请/专利权人 TOBISHIMA CORP;KOSU:KK;

    申请/专利号JP19940281518

  • 申请日1994-10-21

  • 分类号G01N22/00;E21D9/06;G01S13/88;G01V3/12;

  • 国家 JP

  • 入库时间 2022-08-22 04:02:18

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