JPS6327785A - Apparatus for displaying topography of sea bottom - Google Patents

Apparatus for displaying topography of sea bottom

Info

Publication number
JPS6327785A
JPS6327785A JP17139986A JP17139986A JPS6327785A JP S6327785 A JPS6327785 A JP S6327785A JP 17139986 A JP17139986 A JP 17139986A JP 17139986 A JP17139986 A JP 17139986A JP S6327785 A JPS6327785 A JP S6327785A
Authority
JP
Japan
Prior art keywords
output
circuit
correlation
reflected wave
standard
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Pending
Application number
JP17139986A
Other languages
Japanese (ja)
Inventor
Mikio Mitamura
三田村 幹雄
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
NEC Corp
Original Assignee
NEC Corp
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by NEC Corp filed Critical NEC Corp
Priority to JP17139986A priority Critical patent/JPS6327785A/en
Publication of JPS6327785A publication Critical patent/JPS6327785A/en
Pending legal-status Critical Current

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  • Measurement Of Velocity Or Position Using Acoustic Or Ultrasonic Waves (AREA)

Abstract

PURPOSE:To accurately measure the distance up to the sea bottom, by a method wherein a sonic wave is emitted to output a standard reflected wave corresponding to the estimated depth of water down to the sea bottom and the actual depth of water is operationally processed on the max. correlation between the standard reflected wave and receiving output. CONSTITUTION:The receiving signal 22 of a receiving circuit 12 is sent to a mutual correlation processing circuit 14 and the output signal 23a of a standard reflected wave form generating circuit 13 is compared with the receiving signal 22 to perform correlation processing. The standard reflected wave form generating circuit 13 generates a standard reflected wave becoming a standard on the basis of the output 23b of a depth-of-water value operation output circuit 16. A max. correlation detection circuit 15 detects the max. correlation between the receiving signal 22 and the output signal 23a on the basis of the output of the mutual correlation processing circuit 14 and detects the time difference of both signals based on the max. correlation. The depth-of-water value operation output circuit 16 converts the time difference to a distance corresponding to the output of the max. correlation detection circuit 15 to operate the depth-of- water value down to the sea bottom.

Description

【発明の詳細な説明】 (産業上の利用分野) 本発明は音響測深儀KI!AL、特許こ複数の音響ビー
ムを用いることにより、船舶の直下のみならず直下付近
の海底をも斜ビームを用いて同時に測探して海底地形を
表示する海底地形表示装置に関する。
[Detailed Description of the Invention] (Industrial Application Field) The present invention is based on the acoustic sounding instrument KI! AL, Patent This invention relates to a submarine topography display device that uses multiple acoustic beams to simultaneously measure and search not only the seabed immediately below a ship but also the vicinity directly below it using an oblique beam to display the topography of the seafloor.

(従来の技術) 従来、この種の海底地形表示装置は、垂直面内で広い指
向性を有するクロスファンビームを形成するラインアレ
ー送受波器を備え、複数の音響ビームによって同時に多
点の測深を行ない、測深値に対応した等条線図を表示器
に表示出力するものが一般的となっていた。
(Prior Art) Conventionally, this type of submarine topography display device is equipped with a line array transducer that forms a cross-fan beam with wide directivity in the vertical plane, and can simultaneously measure depth at multiple points using multiple acoustic beams. It has become common practice to carry out measurements and display a contour map corresponding to the sounding values on a display.

特に、測深値は、該当ビームの受信信号の対応する海底
地点近傍からの反射信号を時間的に選択し、ある閾値を
設定してその立上シを求めることにより、即ち、反射信
号の信号レベルが閾値を上回った時点までに要する所要
時間を距離に換算して測深値を求めていた。
In particular, the sounding value can be determined by temporally selecting the reflected signal near the seabed point corresponding to the received signal of the beam, and determining its rise by setting a certain threshold, that is, the signal level of the reflected signal. The sounding value was calculated by converting the time required until the time when the depth exceeded the threshold value into distance.

(発明が解決しようとする問題点) 上述した従来の測深値を得る手法では、斜音響ビームに
よシ測探した場合の受信波形は鉛直方向からの音響ビー
ムの角度、海底に対する入射角度の差異による海底面の
音響的な後方散乱強度、伝搬経路差による減衰量、海底
に於ける音響照射面積、音響ビームパターンによシ歪を
含んだものとなシ、この歪を含んだ受信信号から立上シ
をとらえて水深を測定したのでは大きな誤差が避けられ
ないという欠点がある。
(Problems to be Solved by the Invention) In the conventional method of obtaining sounding values described above, the received waveform when measuring with an oblique acoustic beam is based on the difference between the angle of the acoustic beam from the vertical direction and the angle of incidence on the seabed. The acoustic backscattering intensity of the seabed surface due to the noise, the amount of attenuation due to the propagation path difference, the acoustic irradiation area on the seabed, and the acoustic beam pattern include distortion. Measuring water depth by looking at the top has the disadvantage that large errors are unavoidable.

本発明は、上記問題点に鑑みてなされたもので、正確に
海底までの距離を測定して海底の地形を表示する海底地
形表示装置を提供することを目的とするう (問題点を解決するための手段う 前述の問題点を解決し上記目的を達成するために本発明
が提供する海底地形表示装置は、送信装置から発射した
音波の海底等による反射波を受信装置で受信し、該受信
装置の受信出力に基づいて前記海底の地形を表示器に表
示する海底地形表示装置であって、前記音波を発射した
海底までの予測水深に応じて標準反射波形出力する標準
反射波発生回路と、該標準反射波と前記受信出力との最
大相関に基づいて実際の水深をa耳処理する演算処理手
段とを設けたことを特徴とする。
The present invention has been made in view of the above-mentioned problems, and an object of the present invention is to provide a submarine topography display device that accurately measures the distance to the seabed and displays the topography of the seafloor. Means for Solving the above-mentioned problems and achieving the above object, the present invention provides a submarine topography display device in which a receiving device receives reflected waves of sound waves emitted from a transmitting device on the seabed, etc. A submarine topography display device that displays the topography of the seabed on a display based on the received output of the device, and a standard reflected wave generation circuit that outputs a standard reflected waveform according to a predicted water depth to the seabed from which the sound wave was emitted; The present invention is characterized in that it includes arithmetic processing means for processing the actual water depth based on the maximum correlation between the standard reflected wave and the received output.

(実施例) 本発明の実施例を図面を参照して説明する。(Example) Embodiments of the present invention will be described with reference to the drawings.

第1図は本発明の一実施例を示すブロック図である。1
8は制御器であり、制御器18からの送信トリガ19a
によって送信回路6を作動させ、送信回路6によシ発生
した送信電気信号は所望する測深方向へ送信指向性形成
回路7により整相され、送信電力増幅回路8により増幅
されたのち、ラインアレー送波器9により電気信号から
音響信号に変換され、変換した音響信号を海中へ送信す
る。所望する海底からの反射音響信号は、ラインアレー
受波器10によシ受波し、受波した音響信号は電気信号
21に変換され、受信指向性形成回路11により測深方
向へ整相され、受信回路12で受信される。受信回路1
2の受信信号22は相互相関処理回路14に送出される
。この相互相関処理回路14は、制御器18の制御信号
19iに応じて作動し、標準反射波形発生回路13の出
力信号23aと受信信号22とを比較して相関処理をす
る。この標準反射波形発生回路13は、後で説明する水
深値演算出力回路16の出力23bに基づいて基準とな
る標準反射波を発生する。15は相互相関処理回路14
の出力に基づいて受信信号22と出力信号23aの最大
相関を検出し、最大相関に基づく双方の信号の時間差、
即ち遅延量を検出する最大相関検出回路である。16は
水深値演算出力回路であυ、制御器18の制御信号19
fに基づいて作動し、最大相関検出回路15の出力、即
ち受信信号22と出力信号23aの時間差に応じて、該
時間差を距離に換算して海底までの水深値を演算する。
FIG. 1 is a block diagram showing one embodiment of the present invention. 1
8 is a controller, and a transmission trigger 19a from the controller 18
The transmitter circuit 6 is activated, and the transmitter electrical signal generated by the transmitter circuit 6 is phased by the transmitter directivity forming circuit 7 in the desired sounding direction, amplified by the transmitter power amplifier circuit 8, and then transmitted to the line array. The electrical signal is converted into an acoustic signal by the transducer 9, and the converted acoustic signal is transmitted to the sea. The desired reflected acoustic signal from the seabed is received by the line array receiver 10, the received acoustic signal is converted into an electrical signal 21, and the receiving directivity forming circuit 11 phase-phases it in the sounding direction. It is received by the receiving circuit 12. Receiving circuit 1
The second received signal 22 is sent to the cross-correlation processing circuit 14. This cross-correlation processing circuit 14 operates in response to a control signal 19i from the controller 18, and performs correlation processing by comparing the output signal 23a of the standard reflected waveform generation circuit 13 and the received signal 22. This standard reflected waveform generation circuit 13 generates a standard reflected wave as a reference based on the output 23b of the water depth value calculation output circuit 16, which will be explained later. 15 is a cross-correlation processing circuit 14
Detect the maximum correlation between the received signal 22 and the output signal 23a based on the output of , and calculate the time difference between the two signals based on the maximum correlation,
That is, it is a maximum correlation detection circuit that detects the amount of delay. 16 is a water depth value calculation output circuit υ, and a control signal 19 of the controller 18
f, and according to the output of the maximum correlation detection circuit 15, that is, the time difference between the received signal 22 and the output signal 23a, the time difference is converted into a distance and the water depth value to the seabed is calculated.

17は表示器であり、水深値演算出力回路16の信号2
0に基づいて海底の地形を表示する。19b、19c、
19d。
17 is a display device, and the signal 2 of the water depth value calculation output circuit 16
Displays the topography of the ocean floor based on 0. 19b, 19c,
19d.

19eは各回路部の同期をとるだめの制御信号である。19e is a control signal for synchronizing each circuit section.

第2図は信号処理回路40における信号波形図である。FIG. 2 is a signal waveform diagram in the signal processing circuit 40.

第2図を参照して水深の演算処理を説明スル。斜音響ビ
ームによる海底からの反射波の受信信号波形1は海底傾
糾等の影響によシ伸張した波形となっているが、該当す
る水深値は受波レベルの最大値近傍の時間に対応してい
る。
The water depth calculation process will be explained with reference to FIG. The received signal waveform 1 of the wave reflected from the seabed by the oblique acoustic beam is an elongated waveform due to the influence of seafloor tilting, etc., but the corresponding water depth value corresponds to the time near the maximum value of the received wave level. ing.

一方、標準反射波形2は、前回測深値よりあらかじめ予
測される水深値に基づいた理論上の波形であって既知の
ものである。
On the other hand, the standard reflection waveform 2 is a known theoretical waveform based on a water depth value predicted in advance from the previous sounding value.

受信信号波形1と標準反射波形2との時間領域に於ける
相互相関をとると、相互相関曲線は符号3で示す如くな
シ、最大相関点5と標準反射波形2の最大値との間には
遅延時間Tだけ差を生じる。
When we take the cross-correlation in the time domain between the received signal waveform 1 and the standard reflected waveform 2, the cross-correlation curve is as shown by code 3, and there is a curve between the maximum correlation point 5 and the maximum value of the standard reflected waveform 2. produces a difference by delay time T.

従って、予測水深値に対する音響伝搬時間に比べて実際
の伝搬経路の伝搬時間は遅延時間Tだけ差があることに
なシ、この時間差Tを伝搬距離に換算して該当水深値を
得る。
Therefore, compared to the acoustic propagation time for the predicted water depth value, the propagation time of the actual propagation path differs by the delay time T, and this time difference T is converted into a propagation distance to obtain the corresponding water depth value.

(発明の効果) 以上説明したように、本発明は、予想標準受信信号と実
際の受信信号の相互相関をとることにより予想値との差
異を求め、それによって真の測深値を求めることができ
、斜音響ビームの特徴であるピークの不明瞭な受信信号
に対しても測深誤差を低減できる効果がある7、
(Effects of the Invention) As explained above, the present invention calculates the difference between the expected standard received signal and the actual received signal by calculating the cross-correlation between the expected standard received signal and the actual received signal, thereby making it possible to determine the true sounding value. , it is effective in reducing sounding errors even for received signals with unclear peaks, which is a characteristic of oblique acoustic beams7.

【図面の簡単な説明】[Brief explanation of drawings]

第1図は本発明の一実施例を示したブロック図、第2図
は第1図の要部の信号波形図である。 1・・・受信信号波形、2・・・標準反射波形、3・・
・相互相関曲線、5・・・最大相関点、6・・・送信回
路、7・・・送信指向性形成回路、8・・・送信電力増
幅回路、9・・・ラインアレー送波器、10・・・ライ
ンアレー受波器、11・・・受信指向性形成回路、12
・・・受信回路、13・・・標準反射波形発生回路、1
4・−・相互相関処理回路、15・・・最大相関検出回
路、16・・・水深値演算出力回路、17・・・表示器
、18・・・制御器、19a〜19i・・・制御信号、
20・・・水深値出力、21・・・未整相入力信号、2
2・・・受信信号、23a・・・標準反射波形出力、2
3b・・・初期値又は直前測深値。 代理人  弁理士  本 庄 伸 介 ? 第2図
FIG. 1 is a block diagram showing an embodiment of the present invention, and FIG. 2 is a signal waveform diagram of the main part of FIG. 1. 1... Received signal waveform, 2... Standard reflected waveform, 3...
- Cross-correlation curve, 5... Maximum correlation point, 6... Transmission circuit, 7... Transmission directivity forming circuit, 8... Transmission power amplification circuit, 9... Line array transmitter, 10 ... Line array receiver, 11 ... Reception directivity forming circuit, 12
...Reception circuit, 13...Standard reflected waveform generation circuit, 1
4... Cross correlation processing circuit, 15... Maximum correlation detection circuit, 16... Water depth value calculation output circuit, 17... Display, 18... Controller, 19a to 19i... Control signal ,
20...Water depth value output, 21...Unphased input signal, 2
2... Received signal, 23a... Standard reflected waveform output, 2
3b...Initial value or last sounding value. Agent: Patent attorney Shinsuke Honjo? Figure 2

Claims (1)

【特許請求の範囲】 送信装置から発射した音波の海底等による反射波を受信
装置で受信し、該受信装置の受信出力に基づいて前記海
底の地形を表示器に表示する海底地形表示装置において
、 前記音波を発射した海底までの予測水深に応じて標準反
射波を出力する標準反射波発生回路と、該標準反射波発
生回路の標準反射波と前記受信装置の受信出力との最大
相関に基づいて実際の水深を演算処理する演算処理手段
とを設けたことを特徴とする海底地形表示装置。
[Scope of Claims] A seafloor topography display device that receives reflected waves of sound waves emitted from a transmitter and reflected from the seabed, etc. by a receiver, and displays the topography of the seafloor on a display based on the received output of the receiver, Based on a standard reflected wave generation circuit that outputs a standard reflected wave according to the predicted water depth to the seabed from which the sound wave was emitted, and the maximum correlation between the standard reflected wave of the standard reflected wave generation circuit and the received output of the receiving device. What is claimed is: 1. A submarine topography display device comprising: arithmetic processing means for calculating actual water depth.
JP17139986A 1986-07-21 1986-07-21 Apparatus for displaying topography of sea bottom Pending JPS6327785A (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
JP17139986A JPS6327785A (en) 1986-07-21 1986-07-21 Apparatus for displaying topography of sea bottom

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
JP17139986A JPS6327785A (en) 1986-07-21 1986-07-21 Apparatus for displaying topography of sea bottom

Publications (1)

Publication Number Publication Date
JPS6327785A true JPS6327785A (en) 1988-02-05

Family

ID=15922433

Family Applications (1)

Application Number Title Priority Date Filing Date
JP17139986A Pending JPS6327785A (en) 1986-07-21 1986-07-21 Apparatus for displaying topography of sea bottom

Country Status (1)

Country Link
JP (1) JPS6327785A (en)

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