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Echosounder for the investigation geological layers under the sea bottom.
Echosounder for the investigation geological layers under the sea bottom.
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机译:Echosounder用于调查海底下的地质层。
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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.
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