Geophysical research, acoustics and hydroacoustics

  • Large thermostratified experimental tank (20 m long, 4 m wide, and 2 m deep) is designed for scale modeling of the wave processes in the upper ocean and the ocean – atmosphere surface layer. It implements a unique method for temperature stratification of the water layer to retrieve a typical profile of the deep-water dependence of the water temperature in the real ocean at about 1:100 ratio. The tank is equipped with a high-speed direct-flow wind-wave channel for modeling a wide range of wind speeds (up to hurricane conditions).
Large thermostratified tank
  • Ring-shaped wind-wave stratified tank (20 m long and having a 0.3 × 0.6 m hydrochannel) is designed for modeling the dynamics of wind waves and their interaction with internal waves and surface-active substance films, as well as for testing the methods of remote (radar and optical) sensing of the sea surface.
  • Hydroacoustic tank (4.5 × 3.5 × 3 m) is designed for modeling the propagation and nonlinear interaction of acoustic waves in inhomogeneous media and for calibration of measuring equipment.
Scale acoustic modeling facility (“Bezvodnoye” test area of the IAP RAS)
  • Automated ship complex is designed for recording the spatio-temporal parameters of water surface waves in real time by radar and optical methods.
  • A set of equipment for a study of atmospheric electricity, including thunderstorm activity, is intended for measuring the electric-field and conduction-current variation under fine weather conditions and in thunderstorms, monitoring of thunderstorm activity, and control of the radio emission of thunderstorm clouds in a wide range of frequencies with high temporal resolution.
  • Marine autonomous measuring complex is designed for studying the characteristics of noise emission and acoustic imaging of extended sources (antenna aperture 200 m, installation depth up to 300 m, and dynamic range up to 120 dB).
  • Passive ground-based radiometric complex for remote sensing of the thermal structure of the stratosphere and monitoring of the Earth's ozone layer at altitudes of 15 to 70 km.
  • Acoustic unechoic chamber (having an operating volume of 100 m3 and a noise level of 26 dB) for scale modeling and checkout of radiation systems and structures, approval of acoustic measurement methods, and testing of sound-receiving devices.
  • Scale acoustic modeling facility for approval and commissioning of measuring devices, checkout, and examination of acoustic models of vibroactive structures.
  • A set of tools for vibroacoustic control is designed for field studies of noise emission and vibration fields of various sources.
  • Low-frequency hydroacoustic emitters of different frequency ranges (from tens of Hertz to several kilohertz) with high radiation power and efficiency (model specimens).
  • Hydroacoustic cabel antennas (connecting up to 64 digital hydrophones) are designed for field measurements and model studies in hydroacoustics.
  • Receiving and emitting hydroacoustic complex is designed for low-frequency acoustic monitoring of shallow-sea basins and sea-bottom sounding.
  • Mobile receiving and emitting seismoacoustic complex is designed for diagnostics of the state of surface terrestrial rocks and seismic engineering by the methods of high-resolution coherent seismo-acoustics (operating range 20 to 1000 Hz).
  • Computer cluster (64 cores, 512 Gb RAM) for the numerical simulation of acoustic and vibration characteristics of elastic structures by the finite-element method.