JPS6259273B2 - - Google Patents
Info
- Publication number
- JPS6259273B2 JPS6259273B2 JP54035303A JP3530379A JPS6259273B2 JP S6259273 B2 JPS6259273 B2 JP S6259273B2 JP 54035303 A JP54035303 A JP 54035303A JP 3530379 A JP3530379 A JP 3530379A JP S6259273 B2 JPS6259273 B2 JP S6259273B2
- Authority
- JP
- Japan
- Prior art keywords
- seabed
- output
- recording
- exploration
- circuit
- 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.)
- Expired
Links
Landscapes
- Geophysics And Detection Of Objects (AREA)
- Measurement Of Velocity Or Position Using Acoustic Or Ultrasonic Waves (AREA)
Description
【発明の詳細な説明】
本発明は海上を航行する船舶に塔載し音波を海
中に発射し海底及び海底下の地層境界面等からの
反射波を受信記録し海底下の地層構造を探査する
海底地層探査装置の改良に関するものである。[Detailed Description of the Invention] The present invention is mounted on a ship sailing on the sea, emits sound waves into the sea, receives and records reflected waves from the seabed and the stratum boundary surface under the seafloor, and explores the stratum structure under the seafloor. This relates to the improvement of submarine geological exploration equipment.
従来の海底地層探査装置は第1図に示すように
送信部31(音源1、送信回路2)、受信部32
(受波器3、プリアンプ4、ハンドパスフイルタ
5、記録増幅回路6、利得制御回路7、制御パル
ス発生回路8)及び記録部33(記録回路9、同
期パルス発生回路10)から構成される。 As shown in FIG. 1, a conventional submarine geological exploration device includes a transmitting section 31 (sound source 1, transmitting circuit 2) and a receiving section 32.
(wave receiver 3, preamplifier 4, handpass filter 5, recording amplifier circuit 6, gain control circuit 7, control pulse generation circuit 8) and recording section 33 (recording circuit 9, synchronization pulse generation circuit 10).
その動作は、制御パルス発生器8からの信号で
送信回路2が起動され、その出力で音源1が動作
し音波を海底に向けて発射する。海底や海底下の
地層境界面からの反射波は受波器3で電気信号に
変換された後、プリアンプ4、帯域波器5、及
び記録増幅回路6を介して記録回路9に入力され
る。尚、送信直後の残響を抑えるために制御パル
ス発生回路8からの信号で起動する利得制御回路
7の出力でプリアンプ4の利得を制御する。 In operation, the transmitting circuit 2 is activated by a signal from the control pulse generator 8, and the sound source 1 is activated by its output, which emits sound waves toward the ocean floor. Reflected waves from the ocean floor or the geological boundary surface beneath the ocean floor are converted into electrical signals by a wave receiver 3, and then input to a recording circuit 9 via a preamplifier 4, a bandpass converter 5, and a recording amplification circuit 6. Incidentally, in order to suppress reverberation immediately after transmission, the gain of the preamplifier 4 is controlled by the output of a gain control circuit 7 activated by a signal from a control pulse generation circuit 8.
上述のような従来の海底地層探査装置は単一周
波数による送受信を行なうため探査目的に応じて
機種を選定するか周波数の異なる音源に変更する
必要があつた。これは音波の伝搬特性等から高周
波数域の音源の場合は地層分解度の高い探査記録
が得られるが反面地層中の減衰が大きいため探査
深度が浅くなる。一方低周波数域の音源を使用す
れば減衰が小さく探査深度が深くなるが波長等の
関係で地層分解度が低下する。このため周波数の
異なる音源を用いて同一記録機に記録させても低
周波域の海底記録に高周波域の記録がおおわれて
分解度の高い記録は得られない。また周波数の異
なる複数の海底地層探査装置を用いる方法も行な
われているが地層探査装置の音源は一般に単一周
波数成分だけでなくかなり広い送信周波数範囲が
あり、しかも記録機が非同期のためそれぞれの反
射音波等が干渉しそれぞれの記録上に障害を与え
ることが多い。これらのことから分解度が高くし
かも探査深度の深い探査記録を得るためには同一
調査域を周波数の異なる装置で別個に探査する方
法も行なわれているがいずれの方法も探査記録の
画質の低下、作業量の増加また探査費用が高くな
る等の欠点があつた。 Conventional submarine geological exploration devices such as those described above transmit and receive signals using a single frequency, so it was necessary to select a model or change to a sound source with a different frequency depending on the exploration purpose. This is due to the propagation characteristics of sound waves, etc. If the sound source is in a high frequency range, exploration records with high stratum resolution can be obtained, but on the other hand, the attenuation in the strata is large, so the exploration depth becomes shallow. On the other hand, if a sound source in a low frequency range is used, the attenuation will be small and the exploration depth will be deeper, but the degree of stratum resolution will be lower due to the wavelength etc. For this reason, even if sound sources with different frequencies are used to record on the same recorder, records in the high-frequency range will overlap the submarine records in the low-frequency range, making it impossible to obtain highly resolved records. There are also methods using multiple submarine geological exploration devices with different frequencies, but the sound source of the geological exploration devices generally has not only a single frequency component but also a fairly wide transmission frequency range, and since the recorders are asynchronous, each Reflected sound waves and the like often interfere with each other and cause problems on each recording. For these reasons, in order to obtain exploration records with high resolution and deep exploration depth, methods have been used in which the same survey area is surveyed separately using devices with different frequencies, but both methods result in a decrease in the image quality of the exploration records. However, there were disadvantages such as an increase in the amount of work and an increase in exploration costs.
本発明は、海底地層探査装置において地層分解
度を高く保持し、かつ海底下深部までの探査を可
能とする探査装置を提供するものである。 The present invention provides a submarine geological exploration device that maintains a high degree of stratum resolution and enables exploration deep beneath the seabed.
即ち、本発明による装置は、周波数の異なる複
数の音波を海底に向けて発射する送波器と、海底
及び海底下地層からの反射信号を電気信号に変換
する受波器と、この受波器の出力を前記の異なる
周波数に対応する信号成分に弁別する複数の弁別
手段と、この弁別手段の出力を増幅する増幅器
と、前記弁別手段の少なくとも一つの出力から海
底からの反射信号成分を検出する検出手段と、こ
の検出手段の出力により前記増幅器の少なくとも
一つの増幅率を抑圧する手段と、前記増幅手段の
出力を重合して記録する記録手段とを備えて成る
ものである。 That is, the device according to the present invention includes a transmitter that emits a plurality of sound waves with different frequencies toward the seabed, a receiver that converts reflected signals from the seabed and the subsea floor layer into electrical signals, and this receiver. a plurality of discriminating means for discriminating the output of the above into signal components corresponding to the different frequencies, an amplifier for amplifying the output of the discriminating means, and detecting a signal component reflected from the seabed from the output of at least one of the discriminating means. The apparatus comprises a detecting means, a means for suppressing the amplification factor of at least one of the amplifiers using the output of the detecting means, and a recording means for superimposing and recording the outputs of the amplifying means.
次に本発明による海底地層探査装置の一実施例
を第2図を参照して説明する。 Next, an embodiment of the submarine geological exploration apparatus according to the present invention will be described with reference to FIG.
第2図は2つの周波数の音波を利用する場合を
示すものであり、複数の音源11a,11b、送
信回路12a,12bからなる送信部41では受
信部42の制御パルス発生回路20からの起動パ
ルスで同時に送信する。海底及び海底下の地層境
界面からの反射波は受波器13で受信し電気信号
に変換してハイパスフイルタ14、ローパスフイ
ルタ15で分離してそれぞれプリアンプ16a,
16bで増幅されバンドパスフイルタ18a,1
8bに供給される。プリアンプでは利得制御回路
17a,17bで送信直後の残響等を抑え又高周
波域プリアンプ16aとバンドパスフイルタ18
aの出力を海底検出パルス発生回路19に入れ海
底の検出を行ない海底パルスを発生しこの海底パ
ルスにより低周波域プリアンプ16bを利得制御
回路17bで利得制御を行なう。 FIG. 2 shows a case in which sound waves of two frequencies are used, and a transmitting section 41 consisting of a plurality of sound sources 11a, 11b and transmitting circuits 12a, 12b receives a starting pulse from a control pulse generating circuit 20 of a receiving section 42. and send at the same time. Reflected waves from the seabed and the geological interface under the seabed are received by a wave receiver 13, converted into electrical signals, separated by a high-pass filter 14 and a low-pass filter 15, and then sent to preamplifiers 16a and 15, respectively.
16b and bandpass filter 18a, 1
8b. In the preamplifier, gain control circuits 17a and 17b suppress reverberation immediately after transmission, and a high frequency preamplifier 16a and bandpass filter 18
The output of the signal a is input to a seabed detection pulse generation circuit 19 to detect the seabed and generate a seabed pulse, and the gain of the low frequency range preamplifier 16b is controlled by the gain control circuit 17b using this seabed pulse.
つまり低周波域プリアンプ16bでは送信直後
及び海底検出直後に利得を抑え利得制御回路17
bで設定された時定数で利得を回復させる。この
利得の抑圧回復時定数は任意に調整できるように
することにより高周波域プリアンプ16aの受信
信号が小さくなるとき低周波域プリアンプ16b
の利得を回復させることができる。それぞれのバ
ンドパスフイルタ18a,18bの出力は重合回
路21で重合され記録増幅回路22で記録レベル
まで増幅され記録部43の記録回路23に供給さ
れ記録紙上に海底下地層構造断面の模写図として
表示する。また同期パルス発生回路24では記録
部の記録機掃引に同期した基準パルスを発生す
る。 In other words, the low frequency preamplifier 16b suppresses the gain immediately after transmission and immediately after detecting the seabed, and the gain control circuit 17
The gain is restored with the time constant set in b. This gain suppression recovery time constant can be adjusted arbitrarily, so that when the received signal of the high frequency range preamplifier 16a becomes small, the low frequency range preamplifier 16b
gains can be restored. The outputs of the respective bandpass filters 18a and 18b are superimposed in a superimposing circuit 21, amplified to a recording level in a recording amplification circuit 22, and supplied to a recording circuit 23 of a recording section 43, where they are displayed on recording paper as a replica of the cross-section of the seabed substratum structure. do. Further, the synchronizing pulse generating circuit 24 generates a reference pulse synchronized with the recording machine sweep of the recording section.
以上の実施例による海底地層探査装置を使用す
ることによつて海底下地層探査において浅部の分
解度を高く保持したまま深部までの探査が可能と
なり探査能率の向上、探査記録画質の向上及び探
査費の経済性においてその効果は大である。 By using the submarine geological exploration device according to the above-described embodiments, it is possible to conduct deep exploration while maintaining high resolution in shallow areas during exploration of the submarine substratum, thereby improving exploration efficiency, improving the image quality of exploration records, and improving exploration. The effect is significant in terms of cost economy.
第1図は従来の海底地層探査装置の構成系統
図、第2図は本発明による海底地層探査装置の構
成系統図である。
11a,11b…音源(送波器)、12a,1
2b…送信回路、13…受波器、14…ハイパス
フイルタ、15…ローパスフイルタ、16a,1
6b…プリアンプ、17a,17b…利得制御回
路、18a,18b…バンドパスフイルタ、19
…海底検出パルス発生回路、20…制御パルス発
生回路、21…重合回路、22…記録増幅回路、
31,41…送信部、32,42…受信部、3
3,43…記録部。
FIG. 1 is a structural diagram of a conventional submarine geological exploration device, and FIG. 2 is a structural diagram of a submarine geological exploration device according to the present invention. 11a, 11b...sound source (transmitter), 12a, 1
2b... Transmission circuit, 13... Receiver, 14... High pass filter, 15... Low pass filter, 16a, 1
6b...Preamplifier, 17a, 17b...Gain control circuit, 18a, 18b...Band pass filter, 19
... seabed detection pulse generation circuit, 20 ... control pulse generation circuit, 21 ... superposition circuit, 22 ... recording amplification circuit,
31, 41... Transmitting section, 32, 42... Receiving section, 3
3,43...recording department.
Claims (1)
射する送波器と、海底及び海底下地層からの反射
信号を電気信号に変換する受波器と、この受波器
の出力を前記の異なる周波数に対応する信号成分
に弁別する複数の弁別手段と、この弁別手段の出
力を増幅する増幅器と、前記弁別手段の少なくと
も一つの出力から海底からの反射信号成分を検出
する検出手段と、この検出手段の出力により前記
増幅器の少なくとも一つの増幅率を抑圧する手段
と、前記増幅手段の出力を重合して記録する記録
手段とを備えて成ることを特徴とする海底地層探
査装置。 2 特許請求の範囲第1項記載の海底地層探査装
置において、前記検出手段の入力である前記弁別
手段の少なくとも一つの出力が最も高い周波数対
応の信号であることを特徴とする海底地層探査装
置。 3 特許請求の範囲第1項記載の海底地層探査装
置において、前記周波数の数が2個であることを
特徴とする海底地層探査装置。[Claims] 1. A transmitter that emits a plurality of sound waves with different frequencies toward the seabed, a receiver that converts reflected signals from the seabed and the subsea floor layer into electrical signals, and a receiver a plurality of discriminating means for discriminating the output into signal components corresponding to the different frequencies, an amplifier for amplifying the output of the discriminating means, and a detection for detecting a reflected signal component from the seabed from at least one output of the discriminating means. A submarine geological exploration device comprising: means for suppressing the amplification factor of at least one of the amplifiers by the output of the detecting means; and recording means for superimposing and recording the outputs of the amplifying means. . 2. The submarine geological exploration apparatus according to claim 1, wherein at least one output of the discriminating means, which is an input of the detection means, is a signal corresponding to the highest frequency. 3. The submarine geological exploration device according to claim 1, wherein the number of frequencies is two.
Priority Applications (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP3530379A JPS55126880A (en) | 1979-03-26 | 1979-03-26 | Submarine stratum probing unit |
Applications Claiming Priority (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP3530379A JPS55126880A (en) | 1979-03-26 | 1979-03-26 | Submarine stratum probing unit |
Publications (2)
| Publication Number | Publication Date |
|---|---|
| JPS55126880A JPS55126880A (en) | 1980-10-01 |
| JPS6259273B2 true JPS6259273B2 (en) | 1987-12-10 |
Family
ID=12438005
Family Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| JP3530379A Granted JPS55126880A (en) | 1979-03-26 | 1979-03-26 | Submarine stratum probing unit |
Country Status (1)
| Country | Link |
|---|---|
| JP (1) | JPS55126880A (en) |
Families Citing this family (1)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| JP5517429B2 (en) * | 2008-09-22 | 2014-06-11 | 株式会社日立製作所 | Sound imaging device |
Family Cites Families (1)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| IT1014987B (en) * | 1974-06-12 | 1977-04-30 | Snam Progetti | INTEGRATED PROCEDURE UREA AM MONIACA |
-
1979
- 1979-03-26 JP JP3530379A patent/JPS55126880A/en active Granted
Also Published As
| Publication number | Publication date |
|---|---|
| JPS55126880A (en) | 1980-10-01 |
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