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Echosounder for the investigation geological layers under the sea bottom.

机译:Echosounder用于调查海底下的地质层。

摘要

1,109,443. Geophysical exploration. SMITHS INDUSTRIES Ltd. 25 May, 1965 [29 May, 1964], No. 22377/64. Heading H4D. In an ultrasonic pulse-echo sounding system for examining strata below the sea-bed, a control circuit responsive to the sea-bed echo generates a control waveform for varying the gain of an amplifier connected between the receiving transducer and a chart recorder in such a manner that the gain has a low value when the sea-bed echo is received and subsequently rises progressively to a higher value, thereby suppressing the sea-bed echo reverberation in the recording and compensating for the rapid attenuation of acoustic energy in the strata. In the embodiment of Fig. 1 (Provisional) the sea-bed echo is selected by a fixedgain amplifier 15 and triggers a generator 16 to produce the control waveform for varying the gain of the receiving amplifier 13. A suppression pulse is also applied to generator 16 from a transmission pulse generator 10 to prevent generator 16 responding to the signal produced by direct passage of the transmitted pulse to the receiving transducer. The control waveform produces a sharp drop in gain upon receipt of the sea-bed echo, followed by a progressive recovery to the level determined by a sensitivity control signal which is also applied (not shown) to amplifier 13. The sensitivity control signal may provide conventional swept gain to compensate for the decreasing strength of echo signals with distance. In the embodiment of Fig. 2 (not shown), generator 16 is replaced by a waveform generator (17) and a suppression gating circuit (18) whose outputs are such that the gain of amplifier 13 is normally held at a low value, rises progressively during a gated recording interval commencing with the arrival of the sea-bed echo, then returns to the low value. To suppress the sea-bed re-echo, a generator (22) produces a suppression waveform for amplifier 13 after a delay (measured from the instant of transmission of an acoustic pulse) which is selected by circuits (19) and (20) according to the interval between the transmission of the acoustic pulse and the reception of the first sea-bed echo. An additional, adjustable, delay is provided to take into account the fact that the transmitting and receiving transducers (or combined transmitting-receiving transducer) are (or is) below the surface of the water and the sea-bed re-echo time is therefore not exactly twice the sea-bed first-echo time. The amplitude and rate of decay of the sea-bed re-echo suppression waveform are adjustable. In either embodiment, the rate and magnitude of the variation of the gain of amplifier 13 are adjustable, and a delay device may be connected between the receiving transducer and the gain control circuits to introduce a delay such that one sea-bed first-echo signal generates the control waveform for the passage of the next sea-bed first-echo signal through receiver amplifier 13.
机译:1,109,443。地球物理勘探。 SMITHS INDUSTRIES Ltd.,1965年5月25日[1964年5月29日],编号22377/64。标题H4D。在用于检查海床下面的地层的超声脉冲回波探测系统中,响应于海床回波的控制电路产生控制波形,该控制波形用于改变在这种情况下连接在接收换能器和图表记录器之间的放大器的增益。这种方式是当接收到海床回波时增益具有较低的值,然后逐渐上升到较高的值,从而抑制了记录中的海床回波混响并补偿了层中声能的快速衰减。在图1(临时)的实施例中,海底回波由固定增益放大器15选择,并触发发生器16以产生用于改变接收放大器13的增益的控制波形。还向发生器施加抑制脉冲。发射脉冲发生器10产生的信号如图16所示,以防止发生器16响应由发射脉冲直接传递到接收换能器而产生的信号。在接收到海床回波后,控制波形使增益急剧下降,然后逐渐恢复到由灵敏度控制信号确定的电平,该灵敏度控制信号也被施加(未示出)到放大器13。灵敏度控制信号可以提供传统的扫频增益可以补偿回声信号随距离而降低的强度。在图2的实施例中(未示出),发生器16由波形发生器(17)和抑制门电路(18)代替,其输出使得放大器13的增益通常保持在低值,抑制门电路(18)上升。随着海床回波的到来,在选通的记录间隔内逐渐减小,然后返回到较低的值。为了抑制海底回波,发生器(22)在由电路(19)和(20)选择的延迟(从声脉冲的传输的瞬间测量)之后产生用于放大器13的抑制波形。到声脉冲的发射与第一海底回波的接收之间的间隔。考虑到发射和接收换能器(或组合的发射-接收换能器)在水面以下(或位于水面以下)的事实,因此提供了一个额外的可调延迟,因此海床的回波时间为不是海床第一次回波时间的两倍。海床回波抑制波形的幅度和衰减率是可调的。在任一实施例中,放大器13的增益变化的速率和幅度是可调节的,并且延迟装置可以连接在接收换能器和增益控制电路之间,以引入延迟,使得一个海床第一回波信号产生用于下一个海床第一回波信号通过接收放大器13的控制波形。

著录项

  • 公开/公告号DE1498018B2

    专利类型

  • 公开/公告日1971-08-05

    原文格式PDF

  • 申请/专利权人

    申请/专利号DE1965S097373

  • 发明设计人

    申请日1965-05-29

  • 分类号G01V1/38;

  • 国家 DE

  • 入库时间 2022-08-23 09:53:40

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