FIELD: hydroacoustics.
SUBSTANCE: invention relates to the field of hydroacoustics and can be used in the development of means of searching for objects located in the upper layer of the seabed, and invisible for such sonar means as side-scanning sonar. According to the disclosed solution, a pulsed acoustic signal is emitted from the carrier of the sonar equipment into the aqueous medium, an acoustic signal reflected from the bottom soil is received by the receiving system, time t of acoustic signal propagation from the emitter to the reflecting object and from the reflecting object to the receiving system is measured. Carrier of the sonar equipment with the hydroacoustic emitter is moved above the bottom at a distance from the bottom Z1, which is related to depth Z2 of the intended location of the object in the bottom soil by the ratio Z1=Z2/ρ12 (ρ12=ρ1/ρ2, ρ1, ρ2 – density of water and soil, respectively). In this case, a vertically oriented radiator directed in a vertical plane is used as an emitter, vertical size of which L1 is related to the expected maximum distance to the object R located in the bottom soil by ratio L12=λR (λ is the wavelength). A horizontally oriented antenna directed in a horizontal plane is used as a receiving system, horizontal dimension of which L2 is related to spatial resolution δR in the direction of movement of the carrier of the sonar equipment by the ratio L2=1.2 λR/δR. An acoustic signal is emitted in the traverse direction and the distance from the radiator to the object located in the thickness of the bottom soil is calculated using a predetermined propagation speed of a non-uniform boundary type wave (Brewster wave).
EFFECT: increase in the range of detection of objects located in the thickness of the bottom soil, the reflecting capacity (target force) of which is low, and reducing the "dead zone" of control associated with the masking effect of signals reflected directly from the water-sea bottom interface.
1 cl, 2 dwg
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Authors
Dates
2024-03-12—Published
2023-11-08—Filed