JP3511026B2 - Calibration method of relative permittivity of electromagnetic wave probe and electromagnetic wave probe - Google Patents
Calibration method of relative permittivity of electromagnetic wave probe and electromagnetic wave probeInfo
- Publication number
- JP3511026B2 JP3511026B2 JP2002534869A JP2002534869A JP3511026B2 JP 3511026 B2 JP3511026 B2 JP 3511026B2 JP 2002534869 A JP2002534869 A JP 2002534869A JP 2002534869 A JP2002534869 A JP 2002534869A JP 3511026 B2 JP3511026 B2 JP 3511026B2
- Authority
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- Prior art keywords
- signal
- relative permittivity
- electromagnetic wave
- period
- analysis
- Prior art date
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Classifications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V3/00—Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation
- G01V3/15—Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation specially adapted for use during transport, e.g. by a person, vehicle or boat
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01S—RADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
- G01S13/00—Systems using the reflection or reradiation of radio waves, e.g. radar systems; Analogous systems using reflection or reradiation of waves whose nature or wavelength is irrelevant or unspecified
- G01S13/88—Radar or analogous systems specially adapted for specific applications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01S—RADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
- G01S7/00—Details of systems according to groups G01S13/00, G01S15/00, G01S17/00
- G01S7/02—Details of systems according to groups G01S13/00, G01S15/00, G01S17/00 of systems according to group G01S13/00
- G01S7/04—Display arrangements
- G01S7/06—Cathode-ray tube displays or other two dimensional or three-dimensional displays
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01S—RADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
- G01S7/00—Details of systems according to groups G01S13/00, G01S15/00, G01S17/00
- G01S7/02—Details of systems according to groups G01S13/00, G01S15/00, G01S17/00 of systems according to group G01S13/00
- G01S7/04—Display arrangements
- G01S7/06—Cathode-ray tube displays or other two dimensional or three-dimensional displays
- G01S7/062—Cathode-ray tube displays or other two dimensional or three-dimensional displays in which different colours are used
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01S—RADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
- G01S7/00—Details of systems according to groups G01S13/00, G01S15/00, G01S17/00
- G01S7/02—Details of systems according to groups G01S13/00, G01S15/00, G01S17/00 of systems according to group G01S13/00
- G01S7/04—Display arrangements
- G01S7/06—Cathode-ray tube displays or other two dimensional or three-dimensional displays
- G01S7/10—Providing two-dimensional [2D] co-ordinated display of distance and direction
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01S—RADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
- G01S13/00—Systems using the reflection or reradiation of radio waves, e.g. radar systems; Analogous systems using reflection or reradiation of waves whose nature or wavelength is irrelevant or unspecified
- G01S13/88—Radar or analogous systems specially adapted for specific applications
- G01S13/885—Radar or analogous systems specially adapted for specific applications for ground probing
Landscapes
- Engineering & Computer Science (AREA)
- Remote Sensing (AREA)
- Physics & Mathematics (AREA)
- Radar, Positioning & Navigation (AREA)
- General Physics & Mathematics (AREA)
- Computer Networks & Wireless Communication (AREA)
- Life Sciences & Earth Sciences (AREA)
- Electromagnetism (AREA)
- Environmental & Geological Engineering (AREA)
- Geology (AREA)
- General Life Sciences & Earth Sciences (AREA)
- Geophysics (AREA)
- Geophysics And Detection Of Objects (AREA)
- Radar Systems Or Details Thereof (AREA)
Description
【発明の詳細な説明】
技術分野
本発明は電磁波探査機の比誘電率校正方法および電磁
波探査機に係り、更に詳しくは、探査現場で正確にしか
も容易に比誘電率の校正を行い得る新規な技術に関す
る。Description: TECHNICAL FIELD The present invention relates to a method for calibrating the relative permittivity of an electromagnetic wave probe and an electromagnetic probe, and more particularly, to a novel method for accurately and easily calibrating the relative permittivity at an inspection site. Regarding technology.
背景技術
従来より、アンテナから電磁波を輻射し、物体からの
反射波を受信解析して探査を行う電磁波探査機が開発さ
れ、埋設管や地雷などの埋設物探査を目的として用いら
れている。BACKGROUND ART Conventionally, an electromagnetic wave probe for radiating an electromagnetic wave from an antenna and receiving and analyzing a reflected wave from an object to perform an exploration has been developed and used for the purpose of exploring a buried object such as a buried pipe or a land mine.
このような電磁波探査機は、アンテナから所定周期毎
に高周波の電磁波を輻射し、その反射波を受信解析して
物体までの距離を求めると共に、電磁波の通過した物体
の物性を判別するもので、探査対象を非破壊測定するも
のである。Such an electromagnetic wave probe radiates a high frequency electromagnetic wave from the antenna at a predetermined cycle, determines the distance to the object by receiving and analyzing the reflected wave, and determines the physical properties of the object through which the electromagnetic wave passes. Non-destructive measurement of exploration target.
一般に、探査機では探査結果を種々のモードで表示さ
せることができる。例えば、図11に示すように、ある
探査位置における一つの受信信号を、横軸を時間軸、縦
軸を振幅軸とした画面に受信波形として表示させること
ができる。或いは、探査対象の水平方向に所定間隔の複
数の探査位置におけるそれぞれの受信信号を記憶保持し
ておき、これら複数の受信信号に所定の信号処理を施す
ことにより、縦軸を深度、横軸を探査位置(走査回数)
とする探査対象の2次元の断面画像(若しくは、パルス
エコー像)を生成し、この断面画像を図12に示すよう
に表示することができる。なお、上記信号処理には、パ
ルス圧縮処理(pulse compression process)や、合成開
口処理(synthetic aperture process)などを例示でき
る。Generally, the spacecraft can display the spacecraft search results in various modes. For example, as shown in FIG. 11, one received signal at a certain search position can be displayed as a received waveform on a screen with the horizontal axis representing the time axis and the vertical axis representing the amplitude axis. Alternatively, by storing and holding the respective received signals at a plurality of search positions at predetermined intervals in the horizontal direction of the search target, and subjecting the plurality of received signals to predetermined signal processing, the vertical axis represents the depth and the horizontal axis represents the horizontal axis. Search position (number of scans)
It is possible to generate a two-dimensional cross-sectional image (or pulse echo image) of the search target, and display the cross-sectional image as shown in FIG. The signal processing may be a pulse compression process or a synthetic aperture process.
探査に際しては、気温や湿度等の各種の条件によって
高周波回路の特性が変化するため、事前に受信波形に基
づいて手動や自動で探査機の校正や設定などを行ってお
くことが、精密な探査を行うために不可欠である。During exploration, the characteristics of the high-frequency circuit change depending on various conditions such as temperature and humidity.Therefore, it is necessary to calibrate or set the probe manually or automatically based on the received waveform beforehand. Is essential to do.
ところで、受信信号に基づいて図11や図12に示す
画像表示を行う場合、受信信号の起点を明確にする必要
がある。仮に、図11に示す受信信号の起点が変動する
と地表面の反射波Pや埋設物による反射波P1が時間軸
方向へ変動し、これに起因して、図12の断面画像上で
深度軸方向へdの変動が発生する。このため、複雑な断
面画像となるうえ埋設物の正確な深度や物性判別ができ
ない。By the way, when the image display shown in FIGS. 11 and 12 is performed based on the received signal, it is necessary to clarify the starting point of the received signal. If the starting point of the received signal shown in FIG. 11 fluctuates, the reflected wave P on the ground surface and the reflected wave P1 due to the buried object fluctuate in the time axis direction, and due to this, in the depth axis direction on the cross-sectional image of FIG. The fluctuation of d occurs. For this reason, the sectional image becomes complicated, and the depth and physical properties of the buried object cannot be accurately determined.
そこで、従来の探査機は図11に示す受信信号におけ
る表面波Pの特定点(例えば、振幅の第1ピーク点)P0
を受信起点として捕捉し、捕捉した受信起点P0に基づ
いて自動的にトラッキング処理を行う自動トラッキング
機能を有したものが多い。Therefore, the conventional probe uses a specific point (for example, the first peak point of amplitude) P 0 of the surface wave P in the received signal shown in FIG.
Many have an automatic tracking function of capturing as a reception start point and automatically performing tracking processing based on the captured reception start point P 0 .
また、近時の探査機の傾向として、地雷探査、埋設物
探査あるいは壁面探査など探査目的に応じて特化された
専用機が多く、前記した自動トラッキング機能などを装
備して測定に際しての面倒な調整や校正などを極力除い
たものが多い。In addition, as a trend of recent spacecraft, there are many specialized machines specialized for the purpose of landmine survey, buried object survey, wall surface survey, etc. There are many things that exclude adjustment and calibration as much as possible.
ところが、従来の探査機では、アンテナから輻射され
る電磁波が非常に広帯域であって、多数の高調波や低周
波が含まれるため、受信信号にも同様に広帯域の周波数
成分が多数含有され、該受信信号は複雑な波形を呈して
いた。このため、表面波Pの第1ピーク点P0を的確に
捕らえることができずに誤った点を捕捉するような不具
合が生じ、安定した探査を行うための自動トラッキング
機能が逆に不安定要素を生み出す要因となっていた。However, in the conventional probe, since the electromagnetic wave radiated from the antenna has a very wide band and contains many harmonics and low frequencies, the received signal also contains many frequency components in the wide band, The received signal had a complicated waveform. For this reason, the first peak point P 0 of the surface wave P cannot be accurately captured, causing a problem of capturing an incorrect point, and the automatic tracking function for performing stable search is an unstable element. Was a factor that produced.
また、自動トラッキング回路が周囲の温度変動や回路
部材のばらつきなどで変動し、これがトラッキングゾー
ンの変動の要因となり、同一仕様の製品であるにも拘わ
らず測定結果にばらつきが発生し信頼性に問題を生じて
いた。In addition, the automatic tracking circuit fluctuates due to ambient temperature fluctuations and fluctuations in circuit members, which causes fluctuations in the tracking zone, resulting in fluctuations in measurement results even though the products have the same specifications. Was occurring.
更に、広帯域の送信電磁波が媒質中のあらゆる点で様
々な位相点において反射し、この多数の反射波の合成波
により受信波が形成されるが、広帯域であるが故に、受
信波形の周期と、媒質の比誘電率や比抵抗とに相関性を
持たせることができず、地表面上の特定の測定点で観測
される単一の受信波形のみを解析することによっては、
媒質の比誘電率を測定することができないものであっ
た。Furthermore, a wideband transmitted electromagnetic wave is reflected at various phase points at all points in the medium, and a received wave is formed by a composite wave of a large number of reflected waves, but since it is a wideband, the period of the received waveform and It is not possible to correlate with the relative permittivity or resistivity of the medium, and by analyzing only a single received waveform observed at a specific measurement point on the ground surface,
It was impossible to measure the relative permittivity of the medium.
本願発明者は、送信波の帯域を非常に狭く(例えば、
中心周波数1GHzの場合で帯域20MHz程度)する
とともにパルス状に輻射し、かかる狭帯域の電磁波の反
射波を受信アンテナで検知し、この検知信号を新規な検
波回路によって検波することにより、受信波形の周期と
媒質の比誘電率との間に所定の相関関係が生じることを
見出した。即ち、パルス状の狭帯域電磁波は、媒質中を
伝搬する過程で、媒質の比誘電率に応じた伝搬速度と減
衰率とを有する。さらに、媒質中のあらゆる点で反射波
が発生し、該多数の反射波の合成により受信波が形成さ
れる。ここで、媒質の深度方向の単位距離毎に反射波が
発生すると仮定すると、各反射波は媒質の比誘電率に応
じた速度で媒質中を伝搬するから、地上の受信アンテナ
で受信される各反射波には、媒質の比誘電率に応じて所
定の位相のずれが生じる。かかる多数の反射波の合成か
らなる受信波形には、探査対象の各深度毎の平均比誘電
率に対応する信号成分が含まれる。例えば、この受信波
形の各位相毎の周期が、探査対象の深度毎の平均誘電率
に応じて変化するものとなったり、受信波の各位相のノ
イズ成分が、探査対象中の深度毎の平均誘電率に対応す
るものとなる。したがって、これらの信号成分に基づい
て、探査対象中の深度毎の誘電率変化を観測できる。The present inventor has found that the band of the transmitted wave is very narrow (for example,
When the center frequency is 1 GHz, the band is about 20 MHz) and the radiation is performed in a pulse shape. The reflected wave of the electromagnetic wave in the narrow band is detected by the reception antenna, and the detection signal is detected by a new detection circuit to detect the reception waveform. It has been found that a predetermined correlation occurs between the period and the relative permittivity of the medium. That is, the pulsed narrow-band electromagnetic wave has a propagation velocity and an attenuation rate according to the relative permittivity of the medium in the process of propagating in the medium. Further, a reflected wave is generated at every point in the medium, and a received wave is formed by combining the large number of reflected waves. Here, assuming that a reflected wave is generated for each unit distance in the depth direction of the medium, each reflected wave propagates in the medium at a speed according to the relative permittivity of the medium, so that each received wave is received by a receiving antenna on the ground. A predetermined phase shift occurs in the reflected wave according to the relative permittivity of the medium. The received waveform formed by combining a large number of reflected waves contains a signal component corresponding to the average relative permittivity for each depth of the search target. For example, the cycle of each phase of the received waveform changes according to the average dielectric constant for each depth of the search target, or the noise component of each phase of the received wave is the average for each depth of the search target. It corresponds to the dielectric constant. Therefore, based on these signal components, it is possible to observe the change in the dielectric constant for each depth in the exploration target.
しかし、誘電率変化が観測できたとしても、その変化
の基準が存在しなければ受信波形から探査対象の深度毎
の比誘電率を求めることができない。However, even if the change in permittivity can be observed, the relative permittivity for each depth of the object to be searched cannot be obtained from the received waveform unless there is a reference for the change.
本発明は、このような事情に鑑みて提案されるもの
で、探査対象の深度毎の誘電率を受信波形中に観測し得
る電磁波探査機において、探査に先だって比誘電率の校
正を容易に行うことのできる電磁波探査機の比誘電率校
正方法を提供することを目的としている。また同時に提
案される本発明は、この比誘電率校正方法を効果的に実
施することのできる電磁波探査機を提供することを目的
としている。The present invention is proposed in view of such circumstances, and in an electromagnetic wave probe capable of observing the permittivity for each depth of the probe in the received waveform, the relative permittivity can be easily calibrated prior to the probe. An object of the present invention is to provide a method for calibrating the relative permittivity of an electromagnetic wave probe that can be used. Another object of the present invention proposed at the same time is to provide an electromagnetic wave probe capable of effectively implementing this relative permittivity calibration method.
発明の開示
前記目的を達成するために提案される本発明の比誘電
率校正方法は、電磁波を輻射する送信アンテナと、輻射
された電磁波の反射波を受信する受信アンテナと、該受
信アンテナの検知信号に基づいて受信信号を生成する受
信ユニットと、前記受信信号を処理して解析用信号を出
力する信号処理部とを備え、該信号処理部は、周波数変
換によって受信信号を信号周期の異なる解析用信号に変
換する周期調整部を有し、該周期調整部は周波数変換定
数の設定手段を有する電磁波探査機において、送信アン
テナから電磁波を対空輻射したときの前記解析用信号の
周期を、基準比誘電率に応じて予め定められた基準時間
と一致させるように前記設定手段を調節するものであ
る。なお、上記本発明は、探査対象中の深度毎の平均比
誘電率と、解析用信号波形の各位相毎の平均周期とが、
所定の相関関係を有する電磁波探査機に好適に適用する
ことができ、より好ましくは、解析用信号波形の各位相
毎の平均周期が、探査対象中の深度毎の平均比誘電率の
平方根にほぼ比例する関係となる解析用信号波形を生成
する信号処理回路を備える電磁波探査機に用いるのが良
い。また、上記本発明は、送信アンテナや送信回路の最
適化により狭帯域のパルス状電磁波を輻射するものに好
適に採用できる。なお、上基本発明において、受信ユニ
ットは高周波回路によって主構成することができ、受信
ユニットの主たる機能は、反射波の検波を行うものとす
ることができ、この受信ユニットの出力信号である受信
信号は、KHz帯〜十数MHz帯とするのが良い。ま
た、受信ユニットと信号処理部(信号処理回路)とは、
別の基板上に回路構成されていてもよく、同一基板上に
一体的に回路構成されていてもよい。DISCLOSURE OF THE INVENTION The relative permittivity calibration method of the present invention proposed to achieve the above-mentioned object is a transmitting antenna that radiates an electromagnetic wave, a receiving antenna that receives a reflected wave of the radiated electromagnetic wave, and detection of the receiving antenna. A reception unit that generates a reception signal based on a signal, and a signal processing unit that processes the reception signal and outputs an analysis signal, the signal processing unit analyzes the reception signal by a frequency conversion with different signal periods. In the electromagnetic wave exploration device having a frequency conversion constant setting unit, the period of the analysis signal when electromagnetic waves are radiated from the transmitting antenna to the reference ratio. The setting means is adjusted so as to match a predetermined reference time according to the dielectric constant. In the present invention, the average relative permittivity for each depth in the exploration target, and the average period for each phase of the analysis signal waveform,
It can be suitably applied to an electromagnetic wave probe having a predetermined correlation, and more preferably, the average period for each phase of the analysis signal waveform is approximately the square root of the average relative dielectric constant for each depth in the probe target. It is preferably used in an electromagnetic wave probe equipped with a signal processing circuit that generates a proportional signal waveform for analysis. Further, the present invention can be suitably applied to a device that radiates a narrow band pulsed electromagnetic wave by optimizing a transmission antenna or a transmission circuit. In the above basic invention, the receiving unit can be mainly composed of a high-frequency circuit, and the main function of the receiving unit can be to detect the reflected wave, and the received signal which is the output signal of this receiving unit. Is preferably in the KHz band to a dozen MHz band. In addition, the receiving unit and the signal processing unit (signal processing circuit),
The circuit may be configured on another substrate, or may be integrally configured on the same substrate.
上記本発明における周波数変換とは、解析用信号と時
間軸との対応を変化させることにより等価的に周波数を
変化させる処理を総称するもので、解析用信号自体を時
間軸方向へ変化させる処理や時間軸の単位時間を変化さ
せる処理などを全て包含する。例えば、解析用信号がア
ナログ信号の場合、ダブルバランスドミキサ(Double B
alanced Mixer)などの周波数変換回路によって解析用
信号を周波数変換することができる。また、解析用信号
が、受信信号をA−D変換してなるデジタルデータの集
合で表される場合には、実際のサンプリングタイミング
とは異なるタイミングでサンプリングされたものとして
上記デジタルデータ群を取り扱うことによって(言い換
えれば、各サンプリングデータ間の単位時間を変化させ
ることによって)、解析用信号が周波数変換されること
となる。上記周波数変換定数の設定手段は、適宜の構成
を採ることができ、例えば周期調整手段が上記のような
周波数変換回路により構成される場合は上記設定手段は
回路内に設けられた可変抵抗器や可変コンデンサなどの
回路構成素子により構成でき、また、周期調整手段が所
定のプログラムに基づいて動作するマイクロコンピュー
タにより構成される場合は上記設定手段は、書き換え可
能なメモリ、該メモリ内のデータを書き換えるプログラ
ム、並びに、データ入力のためのスイッチ等の入力手段
により構成できる。The frequency conversion in the present invention is a general term for the process of equivalently changing the frequency by changing the correspondence between the analysis signal and the time axis, and the process of changing the analysis signal itself in the time axis direction. It includes all processes for changing the unit time on the time axis. For example, if the analysis signal is an analog signal, a double balanced mixer (Double B
The signal for analysis can be frequency-converted by a frequency conversion circuit such as a balanced mixer. Further, when the analysis signal is represented by a set of digital data obtained by A / D converting the reception signal, the digital data group is treated as being sampled at a timing different from the actual sampling timing. (In other words, by changing the unit time between each sampling data), the analysis signal is frequency-converted. The frequency conversion constant setting means may have an appropriate configuration. For example, when the period adjusting means is constituted by the frequency conversion circuit as described above, the setting means is a variable resistor or a variable resistor provided in the circuit. When the period adjusting means is constituted by a microcomputer that operates based on a predetermined program, the setting means is a rewritable memory and rewrites data in the memory. The program and the input means such as a switch for inputting data can be used.
探査機における比誘電率の校正とは、当該比誘電率を
有する媒体における受信信号の信号周期と時間軸との対
応を取ることである。The calibration of the relative permittivity in the probe is to make the signal period of the received signal in the medium having the relative permittivity correspond to the time axis.
ここで、媒体の比誘電率をεr 、空気中の電磁波の伝
搬速度をC0とすると、電磁波の伝搬距離(深度)Dと
時間tとの間には、一般的に次式の関係が成立する。Here, assuming that the relative permittivity of the medium is ε r and the propagation velocity of the electromagnetic wave in the air is C 0 , the propagation distance (depth) D of the electromagnetic wave and the time t are generally related by the following equation. To establish.
則ち、伝搬時間を求めることにより伝搬距離(深度)
が求まる。 That is, the propagation distance (depth) can be calculated by finding the propagation time.
Is required.
ところで、受信信号に基づく解析用信号を、横軸を時
間軸、縦軸を振幅軸とした受信波形として画面表示させ
た場合、比誘電率の校正が行われない状態では、解析用
信号の各位相毎の周期と画面上における時間軸との間に
相関関係があっても、基準が存在しないため、例えば、
表面反射波と埋設物体における反射波とを含むような解
析用信号を画面表示させた場合、波形形状は判別できる
ものの、表面反射波と物体反射波との間の時間に基づい
て、埋設物体までの距離(深度)を求めることができな
い。また、基準となる比誘電率における受信信号の周期
が定まらないため、異なる周期の受信信号に対して比誘
電率を特定できず、物性解析ができない。則ち、信号処
理のための基準となる時間が定まらないため、解析用信
号の周期と信号処理部における時間軸との対応が取れな
い。By the way, when the analysis signal based on the received signal is displayed on the screen as a received waveform with the horizontal axis as the time axis and the vertical axis as the amplitude axis, the relative position of the analysis signal is Even if there is a correlation between the cycle for each phase and the time axis on the screen, there is no standard, so, for example,
When an analysis signal containing the surface reflected wave and the reflected wave from the embedded object is displayed on the screen, the waveform shape can be discriminated, but even the embedded object can be detected based on the time between the surface reflected wave and the object reflected wave. The distance (depth) cannot be obtained. Further, since the period of the received signal at the reference relative permittivity is not determined, the relative permittivity cannot be specified for the received signals of different periods, and the physical property cannot be analyzed. That is, since the reference time for signal processing is not determined, the period of the analysis signal cannot be associated with the time axis in the signal processing unit.
そこで、所定の比誘電率を有する媒体を通過した反射
波に基づく解析用信号について、その周期と時間軸との
対応を校正することにより、画面に表示された解析用信
号波形の任意点間の伝搬時間を時間軸から得ることがで
きる。これにより、信号処理部における解析用信号の周
期と時間軸との対応が取れ、校正された時間軸に基づい
た信号処理を行うことが可能となる。Therefore, for an analysis signal based on a reflected wave that has passed through a medium having a predetermined relative permittivity, by calibrating the correspondence between the period and the time axis, the analysis signal waveform between arbitrary points displayed on the screen is displayed. The propagation time can be obtained from the time axis. As a result, the period of the analysis signal in the signal processing unit and the time axis can be associated with each other, and the signal processing based on the calibrated time axis can be performed.
前記本発明の校正方法によれば、電磁波を対空輻射し
たときの解析用信号の周期(表面反射波の周期)を基準
時間と一致させるように周期調整部の設定手段を調整設
定するものであり、これによって、基準比誘電率の媒体
で校正された状態を等価的に作り出している。According to the calibration method of the present invention, the setting unit of the cycle adjusting unit is adjusted and set so that the cycle of the analysis signal (the cycle of the surface reflected wave) when the electromagnetic wave is radiated to the air coincides with the reference time. By this, the state calibrated with the medium of the reference relative dielectric constant is equivalently created.
この校正方法によれば、校正のための特別な装置や手
続きを必要とせず、対空輻射を行った場合の解析用信号
を表示させて周期調整を行うだけで校正操作を行うこと
ができ、探査現場において正確且つ容易に校正を行うこ
とができる。According to this calibration method, no special device or procedure for calibration is required, and the calibration operation can be performed simply by displaying the analysis signal when performing anti-radiation and adjusting the period. Accurate and easy calibration can be performed on site.
また、この校正方法によれば、探査機の内部回路の温
度変動などに起因して解析用信号の周期に変動が生じて
も、変動状態における解析用信号の周期を基準時間に一
致させるように校正が行われる。これにより、温度など
が急激に変動しない限り、解析用信号における比誘電率
に応じた周期同士の変動誤差が相殺されて誤差の少ない
測定を行うことができる。また、対空輻射の解析用信号
を用いて校正を行うので、送信アンテナに対する誘電体
の影響を極力除くことができ、一層正確な校正が可能と
なる。Further, according to this calibration method, even if the cycle of the analysis signal fluctuates due to the temperature fluctuation of the internal circuit of the probe, etc., the cycle of the analysis signal in the fluctuation state is made to match the reference time. Calibration is done. As a result, as long as the temperature or the like does not change abruptly, the fluctuation error between the cycles corresponding to the relative permittivity in the analysis signal is canceled out, and the measurement with a small error can be performed. Further, since the calibration is performed using the analysis signal of the radiation to the air, the influence of the dielectric substance on the transmitting antenna can be eliminated as much as possible, and the calibration can be performed more accurately.
解析用信号の周期を基準時間と一致させる場合、表面
反射波を用いて周期を一致させるのが良い。ここに対空
輻射時の表面反射波とは、送信アンテナから輻射された
電磁波による最初の反射に基づくもので、例えば、アン
テナ基板などの反射を含むものである。When making the period of the analysis signal coincide with the reference time, it is preferable to make the period coincide with the surface reflected wave. Here, the surface reflected wave at the time of radiation to the air is based on the first reflection by the electromagnetic wave radiated from the transmitting antenna, and includes, for example, the reflection of the antenna substrate or the like.
前記本発明において信号処理部が、媒体の比誘電率に
応じて周期の異なる受信信号に基づいて、周期と比誘電
率との間に所定の関係を有する解析用信号を生成出力す
る構成とすることができる。In the present invention, the signal processing unit is configured to generate and output an analysis signal having a predetermined relationship between the period and the relative permittivity, based on a received signal having a different period according to the relative permittivity of the medium. be able to.
比誘電率の異なる媒体を通過する電磁波は通過媒体に
応じて伝搬速度の変動を生じ、これに伴って受信信号に
は媒体の比誘電率に応じた周波数変動(周期変動)が生
じる。An electromagnetic wave passing through a medium having a different relative permittivity causes a change in propagation velocity depending on the passing medium, and accordingly, a received signal undergoes a frequency change (period change) according to the relative permittivity of the medium.
そこで、例えば、受信信号の周期と比誘電率の平方根
との間に線型性を持つように信号処理部で処理を施した
解析用信号を出力させることができる。Therefore, for example, it is possible to output an analysis signal that has been processed by the signal processing unit so as to have linearity between the period of the received signal and the square root of the relative dielectric constant.
これにより、解析用信号の周期と比誘電率との相関関
係が明確になり、解析用信号に基づいて各深度毎の平均
比誘電率を算出するとともに、算出された平均比誘電率
に基づいた深度解析を容易に行えるようになる。This clarifies the correlation between the period of the analysis signal and the relative permittivity, calculates the average relative permittivity for each depth based on the analysis signal, and based on the calculated average relative permittivity. Depth analysis can be performed easily.
同時に提案される本発明は、前記本発明の比誘電率校
正方法における基準時間の導出方法であって、送信アン
テナから所定の比誘電率および校正距離を有する基準誘
電体に向けて電磁波を輻射し、解析用信号に含まれる基
準誘電体表面および校正距離における反射波間の時間を
電磁波が基準誘電体内において校正距離を伝搬する時間
に一致させるように前記設定手段を調節し、この後、送
信アンテナから対空輻射を行ったときの前記解析用信号
の周期を基準時間として定めるものである。The present invention proposed at the same time is a method for deriving a reference time in the relative permittivity calibration method of the present invention, in which electromagnetic waves are radiated from a transmitting antenna toward a reference dielectric having a predetermined relative permittivity and a calibration distance. Adjusting the setting means so that the time between the reflected waves at the reference dielectric surface and the calibration distance contained in the analysis signal coincides with the time when the electromagnetic wave propagates the calibration distance in the reference dielectric, and then from the transmitting antenna The period of the analysis signal when radiation to the air is performed is determined as a reference time.
ここに、電磁波が基準誘電体内において校正距離を伝
搬する時間とは、基準誘電体の表面と校正距離との間を
電磁波が往復する時間を指す。Here, the time that the electromagnetic wave propagates in the calibration distance within the reference dielectric means the time that the electromagnetic wave travels back and forth between the surface of the reference dielectric and the calibration distance.
この基準時間の導出方法によれば、基準誘電体によっ
て校正を行い、この校正された状態で対空輻射を行った
場合の反射波の周期を、校正のための基準時間として利
用するものである。According to the method of deriving the reference time, the period of the reflected wave when the calibration is performed by the reference dielectric and the anti-air radiation is performed in the calibrated state is used as the reference time for the calibration.
前記した本発明の校正方法は、このようにして得られ
た基準時間を用いるもので、基準誘電率で校正された状
態において、対空輻射時における解析用信号の周期を校
正のための基準時間として利用した点に本発明の優れた
着想を認めることができる。The above-described calibration method of the present invention uses the reference time thus obtained, and in the state calibrated with the reference dielectric constant, the period of the analysis signal at the time of radiation to the air is used as the reference time for the calibration. The excellent idea of the present invention can be recognized in the point of utilization.
同時に提案される本発明は、電磁波を輻射する送信ア
ンテナと、輻射された電磁波の反射波を受信する受信ア
ンテナと、該受信アンテナの検知信号に基づいて受信信
号を生成する受信ユニットと、該受信信号を処理して解
析用信号を出力する信号処理部と、基準比誘電率値を含
む計測条件データを記憶する記憶手段と、演算手段とを
備え、信号処理部は周波数変換によって受信信号を信号
周期の異なる解析用信号に変換する周期調整部を有し、
該周期調整部は周波数変換定数の設定手段を有する電磁
波探査機である。かかる本発明の電磁波探査機におい
て、前記設定手段は、送信アンテナから電磁波を対空輻
射したときの前記解析用信号の周期を、基準比誘電率に
応じて予め定められた基準時間と一致させるように調節
可能に構成することができる。さらに、前記信号処理部
は、探査における受信信号を比誘電率に応じて校正され
た解析用信号として生成し、演算手段は記憶手段に記憶
された計測条件データに基づいて解析用信号に所定の演
算を施した解析データを生成する構成とすることができ
る。The present invention proposed at the same time, a transmitting antenna that radiates an electromagnetic wave, a receiving antenna that receives a reflected wave of the radiated electromagnetic wave, a receiving unit that generates a received signal based on a detection signal of the receiving antenna, and the receiving unit. The signal processing unit includes a signal processing unit that processes a signal and outputs a signal for analysis, a storage unit that stores measurement condition data including a reference relative permittivity value, and a calculation unit. The signal processing unit outputs a received signal by frequency conversion. Includes a cycle adjustment unit that converts into an analysis signal with a different cycle,
The period adjusting unit is an electromagnetic wave probe having a means for setting a frequency conversion constant. In the electromagnetic wave probe of the present invention, the setting means, the period of the analysis signal when electromagnetic waves are radiated from the transmitting antenna to the air, so as to match the reference time predetermined according to the reference relative permittivity. It can be configured to be adjustable. Further, the signal processing unit generates a reception signal in the exploration as an analysis signal calibrated according to the relative permittivity, and the arithmetic unit determines a predetermined analysis signal based on the measurement condition data stored in the storage unit. It can be configured to generate analysis data that has been subjected to calculation.
この電磁波探査機において前記した比誘電率の校正方
法を用いることができる。The above-described method of calibrating the relative permittivity can be used in this electromagnetic wave probe.
信号処理部の所定の回路定数の最適化を図ることなど
によって比誘電率の校正を行うことにより、当該比誘電
率における解析用信号と時間軸との対応が校正され、校
正後は、信号処理部は受信信号に対して設定手段の設定
に応じた周期調整処理を施した解析用信号を生成出力す
る。この解析用信号の周期は、地中などの媒体の有する
比誘電率と一定の関係を有するものとなる。By calibrating the relative permittivity by, for example, optimizing the predetermined circuit constants of the signal processing unit, the correspondence between the analysis signal at the relative permittivity and the time axis is calibrated. The unit generates and outputs an analysis signal obtained by performing a cycle adjustment process on the received signal according to the setting of the setting unit. The period of this analysis signal has a fixed relationship with the relative permittivity of a medium such as underground.
生成された解析用信号は演算手段に送られ、記憶手段
に記憶された計測条件データに基づいて必要な演算が施
されて探査結果の表示などに必要な解析データが生成さ
れる。計測条件データとしては、基準比誘電率値や探査
結果の表示モードに対応して解析用信号に加えるべき演
算処理プログラムなどのデータが含まれる。The generated analysis signal is sent to the calculation means, and necessary calculation is performed based on the measurement condition data stored in the storage means to generate analysis data necessary for displaying the search result. The measurement condition data includes data such as an arithmetic processing program to be added to the analysis signal corresponding to the reference relative permittivity value and the search result display mode.
また、前記信号処理部が、上記比誘電率の校正方法を
行う電磁波探査機と同様に、周期と比誘電率との間に所
定の関係を有する解析用信号を生成出力する構成とする
ことも可能である。Further, the signal processing unit may be configured to generate and output an analysis signal having a predetermined relationship between the period and the relative permittivity, similarly to the electromagnetic wave probe that performs the relative permittivity calibration method. It is possible.
図面の簡単な説明
図1は、本発明の実施例に係る電磁波探査機の要部構
成を示すブロック図である。BRIEF DESCRIPTION OF THE DRAWINGS FIG. 1 is a block diagram showing a main configuration of an electromagnetic wave probe according to an embodiment of the present invention.
図2は、比誘電率が低い媒体における受信信号のサン
プリング状態を示す説明図である。FIG. 2 is an explanatory diagram showing a sampling state of a received signal in a medium having a low relative dielectric constant.
図3は、比誘電率が高い媒体における受信信号のサン
プリング状態を示す説明図である。FIG. 3 is an explanatory diagram showing a sampling state of a received signal in a medium having a high relative dielectric constant.
図4は、図1に示す探査機の表示器を用いて、本発明
の比誘電率の校正を行う手順を示す説明図である。FIG. 4 is an explanatory diagram showing a procedure for calibrating the relative permittivity of the present invention using the indicator of the probe shown in FIG.
図5は、基準誘電体(乾燥まさ土)を示す正面図であ
る。FIG. 5 is a front view showing a reference dielectric (dry Masa soil).
図6は、基準誘電体における解析用信号に基づいて校
正距離を一致させる手順を示す説明図である。FIG. 6 is an explanatory diagram showing a procedure for matching the calibration distances based on the analysis signal in the reference dielectric.
図7は、対空輻射時における解析用信号の表面反射波
の周期を基準時間に一致させる手順を示す説明図であ
る。FIG. 7 is an explanatory diagram showing a procedure for making the period of the surface reflected wave of the analysis signal at the time of radiation to the air coincide with the reference time.
図8は、表面波処理を行うことによって、図6に示す
校正距離を一致させる手順を示す説明図である。FIG. 8 is an explanatory diagram showing a procedure for matching the calibration distances shown in FIG. 6 by performing surface wave processing.
図9は、基準誘電体(エポキシ樹脂)を示す正面図で
ある。FIG. 9 is a front view showing a reference dielectric (epoxy resin).
図10は、基準誘電体における解析用信号に基づいて
校正距離を一致させる手順を示す説明図である。FIG. 10 is an explanatory diagram showing a procedure for matching the calibration distances based on the analysis signal in the reference dielectric.
図11は、従来の、解析用信号におけるトラッキング
ゾーンの説明図である。FIG. 11 is an explanatory diagram of a conventional tracking zone in an analysis signal.
図12は、トラッキングゾーンの変動によって断面画
像に生じる変動を示す説明図である。FIG. 12 is an explanatory diagram showing a change that occurs in a cross-sectional image due to a change in the tracking zone.
発明を実施するための最良の形態
本発明において、周期調整部で周波数変換によって受
信信号の周期を変化させる方法としては種々のものが挙
げられる。BEST MODE FOR CARRYING OUT THE INVENTION In the present invention, there are various methods for changing the cycle of a received signal by frequency conversion in the cycle adjusting section.
例えば、受信信号を固定した状態で、受信信号に対応
させる時間軸を周期調整部の設定手段により調整する。
これにより、受信信号と時間軸との対応を校正し、結果
的に受信信号に対して周波数変換の施された解析用信号
を生成することができる。For example, with the received signal fixed, the time axis corresponding to the received signal is adjusted by the setting means of the cycle adjustment unit.
As a result, the correspondence between the received signal and the time axis can be calibrated, and as a result, the analysis signal in which the received signal is frequency-converted can be generated.
一方、時間軸を固定した状態で、設定手段の設定に応
じて周期調整部により受信信号自体に周波数変換(周期
変換)を施すこともでき、これにより、受信信号と時間
軸との対応を校正した解析用信号を生成することができ
る。On the other hand, with the time axis fixed, it is also possible to perform frequency conversion (period conversion) on the received signal itself by the cycle adjustment unit according to the setting of the setting means, and thereby the correspondence between the received signal and the time axis can be calibrated. The analyzed signal can be generated.
受信信号自体に周波数変換(周期変換)を施す方法と
しても種々のものが挙げられる。There are various methods for performing frequency conversion (period conversion) on the received signal itself.
例えば、受信信号に対してヘテロダイン処理を施すこ
とにより周波数を変化させた解析用信号を得ることがで
きる。For example, it is possible to obtain an analysis signal in which the frequency is changed by subjecting the received signal to heterodyne processing.
また、アナログ・デジタル変換によって受信信号を一
旦デジタル受信データに変換し、変換された受信データ
にデジタル処理を施すことによって周波数を変化させた
解析用信号とすることも可能である。Further, it is also possible to convert the received signal into digital received data once by analog-digital conversion, and subject the converted received data to digital processing to obtain an analysis signal in which the frequency is changed.
ここで、本発明において、送信アンテナから輻射され
る送信信号、並びに、受信アンテナの検知信号は、数百
MHz〜略1GHzのマイクロ波帯に属するものとする
のが好ましいが、これによれば、受信アンテナの検知信
号自体に直接信号処理を施すことが困難である。Here, in the present invention, it is preferable that the transmission signal radiated from the transmission antenna and the detection signal of the reception antenna belong to a microwave band of several hundred MHz to approximately 1 GHz. It is difficult to directly perform signal processing on the detection signal itself of the receiving antenna.
そこで、例えば、所定周期毎に繰り返し受信される受
信アンテナ検知信号のサンプリングポイントを徐々にず
らしながら所定回数だけサンプリングを繰り返して受信
信号を生成する一連の処理を、受信ユニットで繰り返し
て行うように構成することもできる。Therefore, for example, the receiving unit repeatedly performs a series of processes for generating a reception signal by repeating sampling a predetermined number of times while gradually shifting the sampling point of the reception antenna detection signal that is repeatedly received at predetermined intervals. You can also do it.
則ち、繰り返し受信される受信アンテナ検知信号の振
幅をサンプリングしながらピーク値ホールド或いは平均
値ホールドなどを行い、これらのピーク値或いは平均値
を包絡値検波することにより元の受信アンテナ検知信号
に対して周波数を低減させた信号処理に適した受信信号
を受信ユニットで生成することが可能である。そして、
生成された受信信号に対して信号処理部において校正の
ための周期調整を行うことができる。In other words, the peak value hold or average value hold is performed while sampling the amplitude of the receiving antenna detection signal that is repeatedly received, and the original receiving antenna detection signal is detected by envelope detection of these peak values or average values. It is possible to generate a reception signal suitable for signal processing in which the frequency is reduced by the receiving unit. And
The signal processing unit can perform period adjustment for calibration on the generated reception signal.
なお、サンプリングのための三角波信号(鋸歯状波)
を含むパルス状の制御信号をパルスコントローラより出
力し、この制御信号により受信信号のサンプリングを行
うことができる。さらに上記制御信号における三角波信
号の立ち上がり時間を、検知信号の電位変化量(ΔV)
に連動して変動させることにより、媒質の比誘電率が大
きく受信信号の周期が大きい場合には比較的長い時間幅
(観測窓)で受信波形を観測することができ、媒質の比
誘電率が小さく受信信号の周期が小さい場合には比較的
短い時間幅(観測窓)で受信波形を観測できる。その
他、送信波や受信波の周波数近傍で周波数特性が比較的
大きく変動するダイオード(例えば、ショットキーバリ
アダイオード)によるダイオードブリッジを用い、該ダ
イオードの応答特性と周波数特性との相関作用により、
各サンプリングポイントを変動させ得る受信回路を構成
することによっても、検知信号のΔVの変化を敏感に検
知しつつ受信信号のサンプリングを行い、媒質の比誘電
率が大きく受信信号の周期が大きい場合には比較的長い
時間幅(観測窓)で受信波形を観測することができ、媒
質の比誘電率が小さく受信信号の周期が小さい場合には
比較的短い時間幅(観測窓)で受信波形を観測できる。A triangular wave signal (sawtooth wave) for sampling
It is possible to output a pulse-shaped control signal including a pulse controller from the pulse controller and sample the received signal by this control signal. Further, the rise time of the triangular wave signal in the control signal is determined by the potential change amount (ΔV) of the detection signal.
When the relative permittivity of the medium is large and the period of the received signal is large, the received waveform can be observed in a relatively long time width (observation window) by varying the relative permittivity of the medium. When the cycle of the received signal is small, the received waveform can be observed in a relatively short time width (observation window). In addition, by using a diode bridge with a diode (for example, a Schottky barrier diode) whose frequency characteristic relatively varies greatly in the vicinity of the frequency of the transmitted wave or the received wave, and by the correlation between the response characteristic of the diode and the frequency characteristic,
By configuring a reception circuit that can change each sampling point, the reception signal is sampled while sensitively detecting the change in ΔV of the detection signal, and when the relative permittivity of the medium is large and the cycle of the reception signal is large. Can observe the received waveform in a relatively long time width (observation window), and can observe the received waveform in a relatively short time width (observation window) when the relative permittivity of the medium is small and the period of the received signal is small. it can.
ところで、前記したように所定比誘電率によって校正
を行った場合、異なる比誘電率を有する媒体を通過した
解析用信号については、比誘電率に応じた異なる周期を
呈する。By the way, when the calibration is performed with the predetermined relative permittivity as described above, the analysis signal passing through the medium having the different relative permittivity has a different cycle according to the relative permittivity.
そこで、予め測定によって解析用信号の周期と実時間
との関係を示す補正データテーブルを作成しておくこと
により、周期に応じた補正周期を換算することで解析用
信号から時間(深度)を求めることができる。また、信
号処理部に補正データテーブルを保有することにより、
受信信号の周期と実時間とが所定の関係を有するように
信号処理を施した解析用信号を生成出力することも可能
である。Therefore, a time (depth) is obtained from the analysis signal by converting the correction cycle according to the cycle by creating a correction data table indicating the relationship between the cycle of the analysis signal and the real time by measurement in advance. be able to. In addition, by holding the correction data table in the signal processing unit,
It is also possible to generate and output an analysis signal that has undergone signal processing so that the cycle of the received signal and the real time have a predetermined relationship.
次に、本発明の比誘電率校正方法における基準時間の
導出方法を具体的に説明する。尚、説明中、電磁波が基
準誘電体内において校正距離を伝搬する時間とは、基準
誘電体の表面と校正距離との間を電磁波が往復する時間
を指す。Next, a method of deriving the reference time in the relative permittivity calibration method of the present invention will be specifically described. In the description, the time taken for the electromagnetic wave to propagate within the reference dielectric within the calibration distance refers to the time required for the electromagnetic wave to travel back and forth between the surface of the reference dielectric and the calibration distance.
基準の比誘電率εr を有する基準誘電体において校正
距離Dだけ電磁波が往復伝搬するのに要する時間tは次
式で示される。但し、大気中の電磁波の伝搬速度をC0
とする。The time t required for the electromagnetic wave to travel back and forth by the calibration distance D in the reference dielectric having the reference relative permittivity ε r is expressed by the following equation. However, the propagation velocity of electromagnetic waves in the atmosphere is C 0
And
そこで、基準誘電体に電磁波を輻射したときの反射波
において、基準誘電体表面における反射波と校正距離に
おける反射波との間の時間を校正距離Dに要する伝搬時
間tと一致させるように設定手段を調整する。これによ
り、信号処理部における解析用信号と時間軸との対応が
校正される。この校正状態において、対空輻射を行い反
射波の周期を求めることにより基準時間が定まる。 Therefore, in the reflected wave when the electromagnetic wave is radiated to the reference dielectric, the setting means is set so that the time between the reflected wave on the surface of the reference dielectric and the reflected wave at the calibration distance matches the propagation time t required for the calibration distance D. Adjust. As a result, the correspondence between the analysis signal and the time axis in the signal processing unit is calibrated. In this calibration state, the reference time is determined by performing radiation to the air and determining the period of the reflected wave.
このようにして基準時間が求められた後は、対空輻射
を行った場合の周期をこの基準時間と一致させるだけ
で、等価的に基準比誘電率で校正された状態を再現する
ことができる。After the reference time is obtained in this way, it is possible to reproduce the state equivalently calibrated with the reference relative permittivity simply by matching the period when the anti-air radiation is performed with the reference time.
基準時間の導出は、電磁波探査機のユーザー側で行う
ことも可能であるが大掛かりな基準誘電体を必要とす
る。そこで、基準時間の導出は基本的に探査機を提供す
る製造者側で行うものとし、探査機に交換して取り付け
ることのできる各アンテナ毎に基準時間を求めてユーザ
ー側に明示しておけば、ユーザー側で正確、且つ、容易
に比誘電率の校正を行うことができる。The derivation of the reference time can be performed by the user of the electromagnetic wave probe, but a large-scale reference dielectric is required. Therefore, it is assumed that the manufacturer of the spacecraft will basically derive the reference time, and if the reference time is obtained for each antenna that can be replaced and installed in the spacecraft, the reference time can be specified to the user side. The user can accurately and easily calibrate the relative permittivity.
前記基準誘電体としては、比誘電率εr =12、校正
距離50cmの「乾燥まさ土」などが安価で実用的であ
るが、他の比誘電率を有する媒体を基準誘電体として用
いても良い。なお、まさ土とは、風化花崗岩からなる礫
質土である。As the reference dielectric, “dry Masato” having a relative permittivity ε r = 12 and a calibration distance of 50 cm is inexpensive and practical, but a medium having another relative permittivity may be used as the reference dielectric. good. Note that the Masa soil is gravelly soil made of weathered granite.
ところで、「乾燥まさ土」を基準誘電体として用いる
場合、まさ土内部の湿度が影響して比誘電率が変動する
虞がある。そこで、湿度の影響を受けにくく比誘電率の
安定したエポキシ系樹脂材(比誘電率=3.5〜4.
5)やメラミン系樹脂材(比誘電率=6.5〜7)など
の基準誘電体を用いて「乾燥まさ土」の比誘電率の管理
を行うことが必要となる。By the way, when "dry Masato" is used as the reference dielectric, the relative permittivity may change due to the humidity inside the Masato. Therefore, an epoxy resin material (relative dielectric constant = 3.5 to 4.
It is necessary to control the relative permittivity of “dry Masato” using a reference dielectric such as 5) or a melamine resin material (relative permittivity = 6.5 to 7).
例えば、所定の校正距離を有するエポキシ樹脂を基準
誘電体として用いて「乾燥まさ土」の比誘電率の管理を
行う場合、まず、エポキシ樹脂において校正距離(校正
時間)を一致させるように校正を行う。この校正手順
は、前記した「乾燥まさ土」における校正と同様であ
る。For example, when managing the relative permittivity of “dry Masato” using an epoxy resin with a predetermined calibration distance as a reference dielectric, first calibrate the epoxy resin so that the calibration distance (calibration time) is the same. To do. This calibration procedure is the same as the calibration in the above-mentioned “dry Masato”.
次いで、「乾燥まさ土」において校正距離(校正時
間)を測定する。この測定値が所定の誤差範囲内である
ことを確認することにより、「乾燥まさ土」の比誘電率
の管理を行うことが可能である。Then, the calibration distance (calibration time) is measured in “dry Masato”. By confirming that the measured value is within the predetermined error range, it is possible to manage the relative permittivity of "dry Masato".
前記した基準誘電体として、例えば、比誘電率が12
の「乾燥まさ土」を用いて50cmの校正距離を持つ構
造とする場合、木材などで成した箱の内部に乾燥まさ土
を充填し、箱の上面にアクリル板などを設けて「まさ
土」の状態を見易くした構造とすることができ、この構
造において目的の校正距離を呈するように形成すること
ができる。As the above-mentioned reference dielectric, for example, the relative dielectric constant is 12
If you want to make a structure with a calibration distance of 50 cm using the "dry Masato", fill the inside of the box made of wood with dry Masato, and install an acrylic plate etc. on the top of the box to make "Masato" It is possible to provide a structure that makes it easier to see the state of, and to form a target calibration distance in this structure.
また、比誘電率の異なる媒体を適宜組み合わせて等価
的に所定の比誘電率および校正距離を有する基準誘電体
を形成することも可能である。It is also possible to equivalently form a reference dielectric having a predetermined relative dielectric constant and a calibration distance by appropriately combining media having different relative dielectric constants.
次に、媒体の比誘電率に応じて周期の異なる受信信号
に対して、周期と比誘電率との間に所定の関係を有する
解析用信号を信号処理部で生成出力する構成について説
明する。Next, a configuration will be described in which the signal processing unit generates and outputs an analysis signal having a predetermined relationship between the period and the relative permittivity for a received signal having a different period depending on the relative permittivity of the medium.
媒体を通過する電磁波の周期Tは、媒体の比誘電率ε
r 、大気中の電磁波の伝搬速度C0、および、電磁波の
周波数fを用いて次式で示される。The period T of the electromagnetic wave passing through the medium is the relative permittivity ε of the medium.
It is expressed by the following equation using r , the propagation velocity C 0 of the electromagnetic wave in the atmosphere, and the frequency f of the electromagnetic wave.
従って、例えば、比誘電率εr=12の媒体における
周期は比誘電率εr=45の媒体における周期の略1/
2倍であり、受信信号には媒体の比誘電率に応じた周波
数変動(周期変動)が生じる。 Therefore, for example, the period in the medium having the relative permittivity ε r = 12 is approximately 1 / the period of the medium having the relative permittivity ε r = 45.
This is twice the frequency, and the received signal undergoes frequency fluctuation (periodic fluctuation) according to the relative permittivity of the medium.
そこで、比誘電率εr0=12における解析用信号の周
期をT0、比誘電率εr=45における解析用信号の周期
をTとすると、例えば、
の関係が成立するように、受信信号に対して信号処理を
施した解析用信号を信号処理部で生成することができ
る。則ち、解析用信号と比誘電率の平方根との間に線型
性を持たせた解析用信号を生成することが可能である。Therefore, assuming that the period of the analysis signal when the relative permittivity ε r0 = 12 is T 0 and the period of the analysis signal when the relative permittivity ε r = 45 is T, for example, It is possible to generate an analysis signal, which is obtained by subjecting the received signal to signal processing, by the signal processing unit so that the relationship is established. That is, it is possible to generate an analysis signal having linearity between the analysis signal and the square root of the relative permittivity.
この処理により、解析用信号の周期と比誘電率との対
応が明確になり、特に、断面画像として表示させる場合
の信号処理が極めて容易になる。By this processing, the correspondence between the period of the analysis signal and the relative permittivity becomes clear, and in particular, the signal processing when displaying as a cross-sectional image becomes extremely easy.
次に、図面を参照して本発明による電磁波探査機の実
施例を説明する。Next, an embodiment of the electromagnetic wave probe according to the present invention will be described with reference to the drawings.
電磁波探査機1は、図1に示すように、アンテナユニ
ットAT、信号処理部10、演算手段11、記憶手段1
2および表示部13を備えている。As shown in FIG. 1, the electromagnetic wave probe 1 includes an antenna unit AT, a signal processing unit 10, a calculation unit 11, and a storage unit 1.
2 and the display unit 13.
アンテナユニットATは、所定の周期毎に電磁波を輻
射する送信アンテナTと、輻射された電磁波の反射波を
受信する受信アンテナRとを隣接させて一体的に内蔵し
ている。The antenna unit AT has a transmitting antenna T that radiates an electromagnetic wave at a predetermined cycle and a receiving antenna R that receives a reflected wave of the radiated electromagnetic wave adjacent to each other and integrated therein.
信号処理部10は、送信アンテナTへインパルスやバ
イアス電圧を供給する送信ユニット10bと、受信アン
テナRで捕らえた検知信号に対して必要な前置処理を行
う受信ユニット10cと、受信ユニット10cから伝送
される受信信号に対して周波数変換による周期調整を施
した解析用信号を生成する周期調整部10dと、当該周
期調整部10dの周波数変換定数を可変設定する設定手
段10eとを備えている。尚、信号処理部10の各構成
部は信号処理回路10aと接続されており、必要な制御
信号などを受けて動作を行う。The signal processing unit 10 includes a transmission unit 10b that supplies an impulse or a bias voltage to the transmission antenna T, a reception unit 10c that performs necessary preprocessing on the detection signal captured by the reception antenna R, and a transmission from the reception unit 10c. The received signal is provided with a period adjusting unit 10d that generates an analysis signal in which a period adjustment is performed by frequency conversion, and a setting unit 10e that variably sets a frequency conversion constant of the period adjusting unit 10d. It should be noted that each component of the signal processing unit 10 is connected to the signal processing circuit 10a, and receives a necessary control signal or the like to operate.
演算手段11はデジタル処理を行うもので、アナログ・
デジタル変換部を有し、信号処理部10から伝送される
アナログの解析用信号をデジタルデータに変換する機能
を備えている。そして、周期調整部10dから伝送され
る解析用信号に対して、記憶手段12に記憶されている
計測条件データに基づく演算処理を施した解析データを
生成する。The calculation means 11 performs digital processing, and
It has a digital conversion unit and has a function of converting an analog analysis signal transmitted from the signal processing unit 10 into digital data. Then, the analysis signal transmitted from the cycle adjustment unit 10d is subjected to arithmetic processing based on the measurement condition data stored in the storage unit 12 to generate analysis data.
例えば、探査機1で設定された表示モードに応じて、
解析用信号に対して対応した演算処理を施した解析デー
タを生成し、生成された解析データに基づいて探査結果
の表示を行わせる。For example, according to the display mode set by the probe 1,
The analysis data is generated by performing the corresponding arithmetic processing on the analysis signal, and the search result is displayed based on the generated analysis data.
また、表示部13は演算手段11から伝送される演算
処理の施された解析データを受けて表示制御を行う表示
コントローラ13aと、表示コントローラ13aから出
力される表示信号に基づいて表示を行う表示器13b
と、表示器13bの表示位置調整などを行う表示調整部
13cとを備えている。Further, the display unit 13 receives the analysis data that has been subjected to the arithmetic processing transmitted from the arithmetic means 11 and performs display control, and a display device that performs display based on the display signal output from the display controller 13a. 13b
And a display adjustment unit 13c for adjusting the display position of the display 13b.
周期調整部10dは、受信ユニット10cから伝送さ
れるアナログの受信信号を受けて、設定手段10eの設
定に応じて受信信号の周期を変化させることにより時間
軸との対応を変化させる動作を行う。The cycle adjusting unit 10d receives the analog reception signal transmitted from the receiving unit 10c, and changes the cycle of the reception signal according to the setting of the setting unit 10e to change the correspondence with the time axis.
本実施例では、これらの調整処理をアナログ処理を主
体として行っている。In this embodiment, these adjustment processes are mainly performed by analog processes.
則ち、周期調整部10dから出力される解析用信号を
演算手段11を介して表示部13で表示させ、設定手段
10eの半固定抵抗器(不図示)を調整することにより
解析用信号の時間軸方向への掃引速度を変化させて周期
調整、則ち、比誘電率の校正を行っている。In other words, the analysis signal output from the period adjusting unit 10d is displayed on the display unit 13 via the calculating unit 11, and the semi-fixed resistor (not shown) of the setting unit 10e is adjusted to adjust the analysis signal time. The period is adjusted by changing the sweep speed in the axial direction, that is, the relative permittivity is calibrated.
本実施例の探査機1では、比誘電率が略3〜50の媒
体における探査を中心としており、比誘電率の平方根と
受信信号の周期との間に線型性を有した解析用信号を必
要とする。また、受信信号の周波数が略500MHz〜
1.5GHzであるため、受信信号に直接信号処理を施
すのが困難である。The probe 1 of this embodiment is centered on a probe in a medium having a relative permittivity of about 3 to 50, and requires an analysis signal having linearity between the square root of the relative permittivity and the period of the received signal. And The frequency of the received signal is approximately 500 MHz
Since it is 1.5 GHz, it is difficult to directly perform signal processing on the received signal.
このため、本実施例では、周期調整部10dの処理に
先立って、受信信号の周波数を低減させ、且つ、通過媒
体の比誘電率に応じた周期を有する解析用信号を得るた
めの前置処理を受信ユニット10cで行っている。Therefore, in this embodiment, prior to the process of the period adjusting unit 10d, the preprocessing for reducing the frequency of the received signal and obtaining the analysis signal having the period according to the relative permittivity of the passing medium. Is performed by the receiving unit 10c.
受信ユニット10cの動作を図2および図3を参照し
て説明する。The operation of the receiving unit 10c will be described with reference to FIGS.
対空輻射による反射波を受信して、受信信号を所定の
時間軸と振幅軸で受信波形として表示すると、図2に示
すような減衰波形となる。一方、比誘電率εr の媒体に
おける反射波を受信した場合、電磁波の伝搬速度が大気
中に比べて低下するので、図2と同一時間軸を用いる
と、図3に示すように減衰までの所要時間が長い受信信
号となる。When a reflected wave due to radiation to the air is received and the received signal is displayed as a received waveform on a predetermined time axis and amplitude axis, an attenuated waveform as shown in FIG. 2 is obtained. On the other hand, when a reflected wave from a medium having a relative permittivity ε r is received, the propagation speed of the electromagnetic wave is lower than that in the atmosphere. Therefore, if the same time axis as in FIG. The received signal has a long required time.
そこで、受信ユニット10cでは、ショットキーバリ
アダイオード(以下、SBDと記載)の周波数特性およ
びオン特性の非線形部分を積極的に組み合わせて利用す
ることにより、媒体の比誘電率と周期との間に所定の関
係を持つ解析用信号を前置出力させている。Therefore, in the receiving unit 10c, the non-linear portion of the frequency characteristic and the ON characteristic of the Schottky barrier diode (hereinafter, referred to as SBD) is positively combined to be used, so that the relative permittivity of the medium and the period can be predetermined. An analysis signal having the relationship of is output in front.
則ち、SBDの特性によって受信信号の時間tに対す
る出力レベルVの傾斜(ΔV/Δt)に応じた時間間隔
毎に受信信号のサンプリングを行いつつピーク置ホール
ド或いは平均置ホールドを行い、所定回数の受信信号を
受信し終えた時点で周波数の低減された解析用信号を生
成させる一連の処理を繰り返す動作を行なわせている。That is, depending on the characteristics of the SBD, the received signal is sampled at each time interval according to the slope (ΔV / Δt) of the output level V with respect to the time t of the received signal, and the peak position hold or the average position hold is performed and the predetermined number of At the time when the reception signal is completely received, the operation for repeating the series of processes for generating the analysis signal with the reduced frequency is performed.
この構成の探査機1で地層の探査テストを行ったとこ
ろ、媒体の比誘電率と前置生成した解析用信号の周期と
の間に、比誘電率の平方根に略比例した線型性が得られ
ることが分かった。When an exploration test of the stratum is conducted with the spacecraft 1 having this configuration, linearity approximately proportional to the square root of the relative permittivity is obtained between the relative permittivity of the medium and the period of the analysis signal generated in advance. I found out.
則ち、受信信号の周期が短い場合は生成される周波数
の低減された解析用信号の周期も短く、逆に、受信信号
の周期が長い場合は生成される解析用信号の周期も長く
なるように前置処理を施すことが可能となる。In other words, if the period of the received signal is short, the period of the analysis signal with a reduced frequency generated is also short, and conversely, if the period of the received signal is long, the period of the generated analysis signal is also long. It is possible to apply pretreatment to the.
また、図2,3に示すように、SBDの特性を用いて
受信信号の周期に応じてサンプリングの時間間隔(t
1,t2)を変化させることにより、比誘電率の大きい
媒体における受信信号においても、減衰信号の途中でサ
ンプリングが終了するような不都合が生じず、しかも、
周波数が低減された解析用信号が得られた。Further, as shown in FIGS. 2 and 3, the sampling time interval (t
By changing (1, t2), there is no inconvenience that sampling ends in the middle of the attenuation signal even in a reception signal in a medium having a large relative dielectric constant, and
An analysis signal with a reduced frequency was obtained.
尚、本実施例では、信号処理部10の信号処理回路1
0aから伝送される制御信号を受信ユニット10cで受
けてアナログ処理によって受信信号を生成しているが、
デジタル処理によって受信信号を生成することも可能で
ある。In the present embodiment, the signal processing circuit 1 of the signal processing unit 10
The receiving unit 10c receives the control signal transmitted from 0a and generates the receiving signal by analog processing.
It is also possible to generate the received signal by digital processing.
次に、探査機1において比誘電率の校正を行う方法を
述べる。Next, a method of calibrating the relative permittivity in the probe 1 will be described.
まず送信アンテナTから電磁波を対空輻射し、受信ア
ンテナRで受信され信号処理部10で生成された解析用
信号を図4に示すように表示器13bに表示させる。First, electromagnetic waves are radiated from the transmitting antenna T to the air, and the analysis signal received by the receiving antenna R and generated by the signal processing unit 10 is displayed on the display 13b as shown in FIG.
この解析用信号における表面反射波Wo の周期を、基
準比誘電率に応じて予め定められた基準時間tと一致さ
せるように設定手段10eを調節する。これにより、基
準比誘電率における解析用信号の周期と時間軸との対応
が取られて比誘電率の校正が完了する。The setting means 10e is adjusted so that the cycle of the surface reflected wave Wo in the analysis signal matches the reference time t that is predetermined according to the reference relative permittivity. As a result, the period of the analysis signal at the reference relative permittivity and the time axis are associated with each other, and the calibration of the relative permittivity is completed.
比誘電率の校正を行った後に、解析用信号Wの表面反
射波W0の振幅の第1ピーク点P0を時間軸の始点(左
端)に一致させるように表示調整部13cを調整設定す
る。これにより、解析用信号Wの起点を送信アンテナT
から輻射される電磁波と略一致させて探査解析における
解析用信号の起点を明確にしている。After the relative permittivity is calibrated, the display adjustment unit 13c is adjusted and set so that the first peak point P 0 of the amplitude of the surface reflected wave W 0 of the analysis signal W coincides with the start point (left end) of the time axis. . As a result, the starting point of the analysis signal W is set to the transmission antenna T.
The origin of the analysis signal in the exploration analysis is clarified by making it approximately coincident with the electromagnetic wave radiated from.
以上の校正および調整によって、探査機1の比誘電率
の校正が行われ探査準備が整う。By the above calibration and adjustment, the relative permittivity of the probe 1 is calibrated and the probe preparation is completed.
このようにして比誘電率の校正が行われると、以降
は、受信アンテナRで受信された受信信号に対して、設
定手段10eの設定に応じて周期調整部10dで周波数
変換が施された解析用信号が生成され、生成された解析
用信号に演算手段11で演算処理を施した解析用信号を
用いて探査解析処理が行われる。After the relative permittivity is calibrated in this way, the received signal received by the receiving antenna R is then subjected to frequency conversion by the period adjusting unit 10d according to the setting of the setting unit 10e. A search signal is generated, and an exploration analysis process is performed using the analysis signal obtained by performing a calculation process on the generated analysis signal by the calculation unit 11.
言い換えれば、比誘電率εr=12の媒体における反
射波を受信した場合には、表示器13bで表示される解
析用信号の周期と時間軸との対応が取れ、信号処理部1
0の信号処理における時間の基準が明確になる。In other words, when the reflected wave in the medium having the relative permittivity ε r = 12 is received, the period of the analysis signal displayed on the display 13b and the time axis are associated with each other, and the signal processing unit 1
The time standard in the signal processing of 0 becomes clear.
尚、本発明の比誘電率の校正は極めて容易であるの
で、例えば、探査作業を所定時間行う毎に校正を行え
ば、一層正確な探査を行うことができる。Since the relative permittivity of the present invention is extremely easy to calibrate, for example, if the calibration is performed every predetermined time, a more accurate survey can be performed.
更に、前記したように信号処理部10の受信ユニット
10cでは、基準誘電率における解析用信号の周期を基
準として、比誘電率の異なる媒体における受信信号に対
しては比誘電率の平方根に略比例した周期の解析用信号
を生成する。Further, as described above, in the receiving unit 10c of the signal processing unit 10, the period of the analysis signal at the reference dielectric constant is used as a reference, and the reception signal in the medium having a different dielectric constant is approximately proportional to the square root of the dielectric constant. An analysis signal having a specified period is generated.
演算手段11では、記憶手段12に記憶された計測条
件データに応じて、探査結果を表示させるために必要な
処理を解析用信号に施して解析データを生成して表示部
13に送出する。In the calculation means 11, according to the measurement condition data stored in the storage means 12, processing necessary for displaying the search result is applied to the analysis signal to generate analysis data and sent to the display unit 13.
これにより、解析データに基づいて探査結果の判定に
必要な種々の表示を行うことができ、埋設物の推定が容
易になる。As a result, various displays necessary for determining the exploration result can be displayed based on the analysis data, and the buried object can be easily estimated.
尚、本実施例では、受信ユニット10cにおいて、比
誘電率の平方根に略比例した周期の解析用信号を生成し
ているが、受信ユニット10cで周波数を低減させた解
析用信号を生成し、演算手段11において比誘電率の平
方根に略比例した周期を有する解析データを生成させる
ことも可能である。In the present embodiment, the receiving unit 10c generates an analysis signal having a period substantially proportional to the square root of the relative permittivity. However, the receiving unit 10c generates an analysis signal with a reduced frequency, and the calculation is performed. It is also possible for the means 11 to generate analysis data having a period approximately proportional to the square root of the relative permittivity.
このように、本発明の比誘電率校正方法によれば、特
別な装置を用いることなく対空輻射時における解析用信
号の周期を基準時間と一致させるだけで容易に行うこと
が可能であり、正確な探査を行うことができる。As described above, according to the relative permittivity calibration method of the present invention, it is possible to easily perform it by simply matching the period of the analysis signal at the time of radiation to the air with the reference time without using a special device. It is possible to conduct various explorations.
また、比誘電率と深度との対応が明確なので断面画像
から探査状態の推定が容易になり、探査の作業性が向上
する。Moreover, since the correspondence between the relative permittivity and the depth is clear, it is easy to estimate the exploration state from the cross-sectional image, and the exploration workability is improved.
また、輻射周波数の異なるアンテナユニットATに交
換して探査を行う場合でも、製造者側から予め提示され
た基準時間によって直ちに比誘電率の校正を行うことが
可能である。Further, even when the antenna unit AT having a different radiation frequency is exchanged for the search, it is possible to immediately calibrate the relative permittivity according to the reference time presented in advance by the manufacturer.
次に、前記した比誘電率の校正の基礎となる基準時間
の導出方法を、図5を参照して説明する。尚、基準比誘
電率において電磁波が校正距離を伝搬するのに要する時
間(校正距離の往復伝搬時間)tは、予め算出されてい
るものとする。Next, a method of deriving the reference time, which is the basis of the above-described relative permittivity calibration, will be described with reference to FIG. Note that the time required for the electromagnetic wave to propagate through the calibration distance at the reference relative permittivity (round-trip propagation time of the calibration distance) t is calculated in advance.
図5に示すように、比誘電率εr=12、校正距離d
=50cmの「乾燥まさ土」で成る基準誘電体20に探
査機1のアンテナATを当接して電磁波を輻射し、その
受信信号を解析用信号として表示器13bに表示させ
る。As shown in FIG. 5, the relative permittivity ε r = 12 and the calibration distance d
The antenna AT of the probe 1 is brought into contact with the reference dielectric body 20 of "dry Masato" of 50 cm to radiate an electromagnetic wave, and the received signal is displayed on the display 13b as an analysis signal.
図6は、その解析用信号Wを示すもので、表面反射波
W0と校正距離d(50cm)における反射波W1とが
含まれている。FIG. 6 shows the analysis signal W, which includes the surface reflected wave W 0 and the reflected wave W1 at the calibration distance d (50 cm).
この表面反射波W0と反射波W1との間の時間t0が校
正距離の伝搬時間tと一致するように周期調整部10d
の設定手段10eを調整する。これにより、比誘電率ε
r=12における比誘電率の校正、則ち、解析用信号W
の周期と時間軸との校正が完了する。The period adjusting unit 10d is configured so that the time t 0 between the surface reflected wave W 0 and the reflected wave W1 coincides with the propagation time t of the calibration distance.
The setting means 10e is adjusted. As a result, the relative permittivity ε
Calibration of relative permittivity at r = 12, that is, analysis signal W
Calibration of the cycle and time axis is completed.
このようにして比誘電率が校正された状態で対空輻射
を行い、図7に示すように解析用信号の表面反射波の周
期tを時間軸から読み取ることにより基準時間tを求め
ることができる。In this way, radiation to air is performed with the relative permittivity calibrated, and the reference time t can be obtained by reading the period t of the surface reflected wave of the analysis signal from the time axis as shown in FIG.
尚、図6において、反射波W1の起点が不明瞭な場合
には、信号処理回路10aにおいて解析用信号Wの間の
差信号成分を抽出する表面波処理(探査機1の有する表
面波処理モード)を施すことによって容易に起点を把握
できる。In FIG. 6, when the starting point of the reflected wave W1 is unclear, the signal processing circuit 10a extracts the difference signal component between the analysis signals W by the surface wave processing (the surface wave processing mode of the probe 1). ), The starting point can be easily grasped.
則ち、図8に示すように、表面波処理の施された差信
号成分を解析用信号W’として表示させ、基準誘電体2
0の校正距離dの位置(基準誘電体20の下面)に金属
板などを当接離遠させる。このときの解析用信号W’を
観測することにより反射波W1’が変動要素として表示
されるので起点を容易に把握することができる。従っ
て、表面反射波W0の起点と反射波W1’の起点との間
の時間をt0に調整することにより、容易に校正を行う
ことができる。That is, as shown in FIG. 8, the difference signal component subjected to the surface wave processing is displayed as the analysis signal W ′, and the reference dielectric 2
A metal plate or the like is brought into contact with or separated from the position of the calibration distance d of 0 (the lower surface of the reference dielectric 20). By observing the analysis signal W ′ at this time, the reflected wave W1 ′ is displayed as a variable element, so that the starting point can be easily grasped. Therefore, the calibration can be easily performed by adjusting the time between the origin of the surface reflected wave W 0 and the origin of the reflected wave W1 ′ to t 0 .
前記したように、比誘電率の校正の基礎となる基準時
間を「乾燥まさ土」などを用いた安価な基準誘電体20
によって容易に導出することができる。As described above, the reference time which is the basis for the calibration of the relative permittivity is set at a low cost by using “dry Masato” or the like.
Can be easily derived by.
基準誘電体20は探査機1の製造者側で備えればユー
ザー側で特に備える必要はなく、取扱説明書などにより
基準時間を明示するだけでユーザー側で確実な校正を行
うことができる。If the manufacturer of the probe 1 needs to provide the reference dielectric 20, the user does not need to provide the reference dielectric 20, and the user can surely calibrate the reference dielectric 20 simply by indicating the reference time in the instruction manual.
次に、「乾燥まさ土」を用いた基準誘電体20の比誘
電率の管理方法について説明する。Next, a method of managing the relative permittivity of the reference dielectric 20 using “dry Masato” will be described.
図9に示すように、比誘電率εr =4.0、校正距離
d1=20cmのエポキシ樹脂で成る基準誘電体21に
探査機1のアンテナATを当接して電磁波を輻射し、そ
の受信信号を解析用信号として表示器13bに表示させ
る。As shown in FIG. 9, the antenna AT of the probe 1 is brought into contact with the reference dielectric 21 made of an epoxy resin having a relative permittivity ε r = 4.0 and a calibration distance d1 = 20 cm to radiate an electromagnetic wave, and a reception signal thereof is received. Is displayed on the display 13b as a signal for analysis.
図10は、その解析用信号Wを示すもので、表面反射
波W0と校正距離(50cm)における反射波W1とが
含まれている。FIG. 10 shows the analysis signal W, which includes the surface reflected wave W 0 and the reflected wave W1 at the calibration distance (50 cm).
この表面反射波W0と反射波W1との間の時間t0を校
正距離の伝搬時間tと一致させるように周期調整部10
dの設定手段10eを調整する。これにより、比誘電率
εr=4.0における比誘電率の校正、則ち、解析用信
号Wの周期と時間軸とが校正される。The period adjusting unit 10 adjusts the time t 0 between the surface reflected wave W 0 and the reflected wave W 1 to match the propagation time t of the calibration distance.
The d setting means 10e is adjusted. This calibrates the relative permittivity when the relative permittivity ε r = 4.0, that is, the period of the analysis signal W and the time axis.
比誘電率εr=4.0に校正された状態で、前記した
図5に示すように、比誘電率εr=12、校正距離d=
50cmの「乾燥まさ土」で成る基準誘電体20に探査
機1のアンテナATを当接して電磁波を輻射し、その受
信信号を解析用信号として表示器13bに表示させる。With the relative permittivity ε r = 4.0 calibrated, as shown in FIG. 5, the relative permittivity ε r = 12 and the calibration distance d =
The antenna AT of the explorer 1 is brought into contact with the reference dielectric 20 of 50 cm of "dry Masato" to radiate an electromagnetic wave, and the received signal is displayed on the display 13b as an analysis signal.
解析用信号Wには、前記図6に示すように表面反射波
W0と校正距離(50cm)における反射波W1とが含ま
れている。As shown in FIG. 6, the analysis signal W includes the surface reflected wave W 0 and the reflected wave W1 at the calibration distance (50 cm).
この表面反射波W0と反射波W1との間の時間t0を時
間軸から読み取り、比誘電率εr=12における校正距
離の伝搬時間tとの誤差を求め、誤差が所定範囲以内で
あれば基準誘電体20の比誘電率が維持されているもの
とする。The time t 0 between the surface reflected wave W 0 and the reflected wave W1 is read from the time axis, the error with the propagation time t of the calibration distance at the relative permittivity ε r = 12 is calculated, and the error is within a predetermined range. For example, it is assumed that the relative dielectric constant of the reference dielectric 20 is maintained.
しかし、誤差が所定値を超える場合には、基準誘電体
20のまさ土を乾燥させるなどして誤差範囲内に収まる
ように調整する。However, if the error exceeds a predetermined value, the soil of the reference dielectric 20 is dried to adjust the error to be within the error range.
尚、解析用信号に含まれる表面反射波W0と反射波W
1との間の時間を時間軸から読み取る場合には、表示調
整部13cを調整して時間を読み取り易い位置に解析用
信号を移動させれば良い。The surface reflected wave W 0 and the reflected wave W included in the analysis signal
When the time between 1 and 1 is read from the time axis, the display adjustment unit 13c may be adjusted to move the analysis signal to a position where it is easy to read the time.
尚、前記図1では、信号処理部10および演算手段1
1を別の構成として示しているが、演算手段11を信号
処理部10の信号処理回路10aと共通のCPUを用い
た構成とすることも可能である。In FIG. 1, the signal processing unit 10 and the computing means 1 are shown.
Although 1 is shown as another configuration, it is also possible to employ a configuration in which the arithmetic means 11 uses a CPU that is common to the signal processing circuit 10a of the signal processing unit 10.
また、周期調整部10dや設定手段10eの処理をデ
ジタル化することも可能である。It is also possible to digitize the processing of the cycle adjusting unit 10d and the setting means 10e.
次に、上記電磁波探査機の応用例として、媒質中(地
中)の深度毎の平均比誘電率を測定する方法を説明す
る。Next, as an application example of the electromagnetic wave probe, a method of measuring an average relative dielectric constant for each depth in a medium (underground) will be described.
この比誘電率の測定方法は、次の(a)〜(d)のス
テップを有することができる。This method of measuring the relative dielectric constant can include the following steps (a) to (d).
(a)電磁波の伝搬する波形の全てのピーク位置(正側
ピークと負側ピーク)を検知するステップ。(A) A step of detecting all peak positions (positive side peak and negative side peak) of a waveform propagating an electromagnetic wave.
(b)上記各ピーク位置の伝搬速度を、正側ピークと零
クロス点、負側ピークと零クロス点として、各区間の時
間幅を順次時間測定し、伝搬周期の変化、即ち、誘電率
変化を、次式
比誘電率 = (測定周期時間/基準周期時間)2 × 基準校正比誘電率
から求めるステップ(なお、この比誘電率は区間毎の平
均値)。(B) With the propagation velocity at each peak position as the positive peak and the zero cross point, and the negative peak and the zero cross point, the time width of each section is sequentially measured to change the propagation period, that is, the dielectric constant. Is calculated from the following formula: relative permittivity = (measurement period time / reference period time) 2 × reference calibration relative permittivity (where, this relative permittivity is an average value for each section).
(c)各区間の伝搬周期の検証を、他区間を信号成分を
零にして周波数スペクトル解析し、その正規化を最大ス
ペクトルの二乗和(直流成分を除く)により計算し卓越
周波数を求めて、Δf=Δεrの相関を確認するステッ
プ。(C) In the verification of the propagation period of each section, the frequency spectrum is analyzed by setting the signal component to zero in other sections, and its normalization is calculated by the sum of squares of the maximum spectrum (excluding the DC component) to obtain the dominant frequency, Confirming the correlation of Δf = Δε r .
(d)各区間毎に求めた比誘電率をカラーバー分類して
地層の深さ方向の誘電率分布図として表示装置に画面表
示するステップ。(D) A step of displaying the relative permittivity obtained for each section by color bar classification and displaying it on the display device as a permittivity distribution map in the depth direction of the formation.
上記相関の確認は、具体的には、210分解のフーリエ
解析なら512点離散周期が得られる為、基準周期によ
り得られる測定可能周期(5msec最大で0.5msec
基準周期なら10離散周期相当になるので誘電率比率の
離散周期ずれを検定する)とのずれを検定し、誘電率と
の線形的な相関を評価する。To confirm the above-mentioned correlation, since a 512-point discrete period can be obtained by a Fourier analysis of 2 10 decomposition, the measurable period obtained by the reference period (5 msec, 0.5 msec at maximum)
Since the reference period corresponds to 10 discrete periods, the discrepancy between the permittivity ratio and the discrete period is verified), and the linear correlation with the permittivity is evaluated.
このようにして求めた誘電率(比誘電率)をカラーバ
ー分類して地層の深さ方向の誘電率分布図・深度図とし
て表示することにより、熟練した探査員でなくとも容易
に地中の状態や誘電率や地層などを判別できるものとな
る。さらに、上記カラーバーにカーソルを設け、分析し
た区間距離をサーチすれば、区間の平均誘電率や、トー
タル深度等を同時観測することができ、電磁波探査を飛
躍的に簡単化するとともに高機能化を図ることができ
る。By displaying the permittivity (relative permittivity) thus obtained by color bar classification and displaying it as a permittivity distribution map / depth map in the depth direction of the stratum, it is easy for an experienced explorer to understand The state, permittivity, stratum, etc. can be identified. Furthermore, if a cursor is placed on the color bar and the analyzed section distance is searched, the average permittivity of the section, the total depth, etc. can be observed simultaneously, dramatically simplifying electromagnetic wave exploration and increasing functionality. Can be achieved.
以上説明したように、本発明の比誘電率校正方法によ
れば、特別な装置を必要とせず、対空輻射によって得ら
れた受信信号に基づく解析用信号の周期を基準時間に一
致させるだけで所定の比誘電率における校正を直ちに行
うことができ、探査現場における作業性が向上すると共
に精密な探査を行うことが可能となる。As described above, according to the relative permittivity calibration method of the present invention, a special device is not required, and the period of the analysis signal based on the received signal obtained by the radiation to the air is set to be equal to the reference time. The relative dielectric constant can be immediately calibrated, the workability at the exploration site is improved, and the precise exploration can be performed.
また、同時に提案される本発明の基準時間の導出方法
によれば、基準誘電体を用いて容易に求めることが可能
となる。Further, according to the method of deriving the reference time of the present invention that is proposed at the same time, it is possible to easily obtain the reference time by using the reference dielectric.
また、同時に提案される本発明の電磁波探査機によれ
ば、本発明の比誘電率校正方法を効果的に実施すること
が可能となる。Further, according to the electromagnetic wave probe of the present invention that is proposed at the same time, the relative permittivity calibration method of the present invention can be effectively implemented.
───────────────────────────────────────────────────── フロントページの続き (58)調査した分野(Int.Cl.7,DB名) G01V 3/12 G01S 7/03 G01S 13/88 ─────────────────────────────────────────────────── ─── Continuation of front page (58) Fields surveyed (Int.Cl. 7 , DB name) G01V 3/12 G01S 7/03 G01S 13/88
Claims (6)
れた電磁波の反射波を受信する受信アンテナと、該受信
アンテナの検知信号に基づいて受信信号を生成する受信
ユニットと、前記受信信号を処理して解析用信号を出力
する信号処理部とを備え、該信号処理部は、周波数変換
によって前記受信信号を信号周期の異なる前記解析用信
号に変換する周期調整手段を有し、該周期調整手段は周
波数変換定数の設定手段を有する電磁波探査機におい
て、 送信アンテナから電磁波を対空輻射したときの前記解析
用信号の周期が、基準比誘電率に応じて予め定められた
基準時間と一致するように、前記設定手段を調節するこ
とを特徴とする電磁波探査機の比誘電率校正方法。1. A transmission antenna that radiates an electromagnetic wave, a reception antenna that receives a reflected wave of the radiated electromagnetic wave, a reception unit that generates a reception signal based on a detection signal of the reception antenna, and the reception signal is processed. And a signal processing unit for outputting an analysis signal, the signal processing unit having a period adjusting unit for converting the received signal into the analyzing signal having a different signal period by frequency conversion, and the period adjusting unit. Is an electromagnetic wave probe having a means for setting a frequency conversion constant, so that the period of the analysis signal when electromagnetic waves are radiated from the transmitting antenna to the air matches the reference time predetermined according to the reference relative permittivity. A method for calibrating the relative permittivity of an electromagnetic wave probe, comprising adjusting the setting means.
校正方法において、 前記信号処理部が、媒体の比誘電率に応じて異なる周期
を呈する受信信号に基づいて、周期と比誘電率との間に
所定の関係を有する解析用信号を生成出力することを特
徴とする電磁波探査機の比誘電率校正方法。2. The method for calibrating the relative permittivity of an electromagnetic wave probe according to claim 1, wherein the signal processing unit determines the period and the relative permittivity based on a received signal having a different period according to the relative permittivity of the medium. A method for calibrating a relative permittivity of an electromagnetic wave probe, comprising generating and outputting an analysis signal having a predetermined relationship with a coefficient.
校正方法において、 前記基準時間は、前記送信アンテナから所定の比誘電率
および校正距離を有する基準誘電体に向けて電磁波を輻
射し、前記解析用信号に含まれる基準誘電体表面および
校正距離における反射波間の時間を電磁波が当該基準誘
電体内において校正距離を伝搬する時間に一致させるよ
うに前記設定手段を調節した後、前記送信アンテナから
対空輻射を行ったときの前記解析用信号の周期であるこ
とを特徴とする電磁波探査機の比誘電率校正方法。3. The method for calibrating the relative permittivity of an electromagnetic wave probe according to claim 1, wherein the reference time radiates an electromagnetic wave from the transmitting antenna toward a reference dielectric having a predetermined relative permittivity and a calibration distance. Then, after adjusting the setting means so that the time between reflected waves at the reference dielectric surface and the calibration distance included in the analysis signal coincides with the time during which the electromagnetic wave propagates the calibration distance in the reference dielectric, the transmission is performed. A method for calibrating the relative permittivity of an electromagnetic wave probe, which is the period of the analysis signal when radiation from the antenna to the air is performed.
れた電磁波の反射波を受信する受信アンテナと、該受信
アンテナの検知信号に基づいて受信信号を生成する受信
ユニットと、前記受信信号を処理して解析用信号を出力
する信号処理部と、基準比誘電率値を含む計測条件デー
タを記憶する記憶手段と、演算手段とを備え、 前記信号処理部は周波数変換によって受信信号を信号周
期の異なる解析用信号に変換する周期調整部を有し、該
周期調整部は周波数変換定数の設定手段を有し、 前記設定手段は、送信アンテナから電磁波を対空輻射し
たときの前記解析用信号の周期を、基準比誘電率に応じ
て予め定められた基準時間と一致させるように調節可能
に構成されていることを特徴とする電磁波探査機。4. A transmission antenna that radiates an electromagnetic wave, a reception antenna that receives a reflected wave of the radiated electromagnetic wave, a reception unit that generates a reception signal based on a detection signal of the reception antenna, and the reception signal is processed. And a signal processing unit for outputting a signal for analysis, a storage unit for storing measurement condition data including a reference relative permittivity value, and a calculation unit, wherein the signal processing unit frequency-converts the received signal into a signal cycle of There is a period adjusting unit for converting into a different analysis signal, the period adjusting unit has a frequency conversion constant setting means, the setting means, the period of the analysis signal when electromagnetic waves are radiated from the transmitting antenna to the air Is configured to be adjustable so as to match a predetermined reference time according to the reference relative permittivity.
じて校正された解析用信号として生成し、 前記演算手段は記憶手段に記憶された計測条件データに
基づいて前記解析用信号に所定の演算を施した解析デー
タを生成することを特徴とする電磁波探査機。5. The electromagnetic wave probe according to claim 4, wherein the signal processing unit generates a received signal in the probe as an analysis signal calibrated according to a relative permittivity, and the arithmetic unit is stored in a storage unit. An electromagnetic wave exploring device, which generates analysis data by performing a predetermined calculation on the analysis signal based on the measured condition data.
を呈する受信信号に対して、周期と比誘電率との間に所
定の関係を有する解析用信号を生成出力することを特徴
とする電磁波探査機。6. The electromagnetic wave probing machine according to claim 4, wherein the signal processing unit sets a predetermined value between the period and the relative permittivity for a received signal having a different period according to the relative permittivity of the medium. An electromagnetic wave explorer characterized by generating and outputting an analysis signal having the relationship of
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| JP2000312145 | 2000-10-12 | ||
| JP2000-312145 | 2000-10-12 | ||
| PCT/JP2001/007328 WO2002031537A1 (en) | 2000-10-12 | 2001-08-27 | Method for calibrating relative permittivity of electromagnetic detector and electromagnetic detector |
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| JPWO2002031537A1 JPWO2002031537A1 (en) | 2004-02-19 |
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| JP2018068850A (en) * | 2016-11-02 | 2018-05-10 | 国際化工株式会社 | Manufacturing method of resin dish |
| WO2021214917A1 (en) * | 2020-04-22 | 2021-10-28 | 日本電信電話株式会社 | Object permittivity measurement device and object thickness measurement device |
| JP2022110737A (en) * | 2021-01-19 | 2022-07-29 | ソニーグループ株式会社 | Measurement device and measurement method |
| JP7590483B2 (en) * | 2023-03-20 | 2024-11-26 | 三菱電機ソフトウエア株式会社 | Information processing device, information processing program, and information processing method |
| JP7634036B2 (en) * | 2023-03-20 | 2025-02-20 | 三菱電機ソフトウエア株式会社 | Information processing device, information processing program, and information processing method |
| WO2024195198A1 (en) * | 2023-03-20 | 2024-09-26 | 三菱電機ソフトウエア株式会社 | Information processing device, information processing program, and information processing method |
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| JP2000147111A (en) | 1998-11-05 | 2000-05-26 | Meisei Electric Co Ltd | Device and method for detecting object buried in ground |
| JP2000221266A (en) | 1998-11-24 | 2000-08-11 | Osaka Gas Co Ltd | Three-dimensional voxel data display method and device |
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| JP2557682B2 (en) * | 1988-05-06 | 1996-11-27 | 株式会社光電製作所 | Underground exploration device with a dielectric constant measurement function in the soil |
| JP3407988B2 (en) * | 1994-09-16 | 2003-05-19 | 三井造船株式会社 | Underground exploration equipment |
-
2001
- 2001-08-27 AU AU2001293352A patent/AU2001293352A1/en not_active Abandoned
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| JP2000147111A (en) | 1998-11-05 | 2000-05-26 | Meisei Electric Co Ltd | Device and method for detecting object buried in ground |
| JP2000221266A (en) | 1998-11-24 | 2000-08-11 | Osaka Gas Co Ltd | Three-dimensional voxel data display method and device |
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