14 research outputs found
Evaluation of the Efficiency of High-Frequency Methods for Distance Determination in Mining Conditions
Π ΡΡΠ°ΡΡΠ΅ ΡΠ°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°ΡΡΡΡ ΠΌΠ΅ΡΠΎΠ΄Ρ ΠΎΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ ΡΠ°ΡΡΡΠΎΡΠ½ΠΈΡ Ρ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ ΡΠ»Π΅ΠΊΡΡΠΎΠΌΠ°Π³Π½ΠΈΡΠ½ΡΡ
Π²ΠΎΠ»Π½ Π‘βΠ΄ΠΈΠ°ΠΏΠ°Π·ΠΎΠ½Π° (4β8 ΠΠΡ) Π² ΡΡΠ»ΠΎΠ²ΠΈΡΡ
ΡΠ°Ρ
Ρ. ΠΡΠ΅Π΄ΡΡΠ°Π²Π»Π΅Π½ Π°Π½Π°Π»ΠΈΠ· ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ Π½Π°ΠΏΡΡΠΆΠ΅Π½Π½ΠΎΡΡΠΈ ΡΠ»Π΅ΠΊΡΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΏΠΎΠ»Ρ Π΄ΠΈΠΏΠΎΠ»ΡΠ½ΠΎΠΉ Π°Π½ΡΠ΅Π½Π½Ρ, ΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½Π½ΠΎΠΉ Π½Π° ΠΊΡΠ·ΠΎΠ² Π³ΡΡΠ·ΠΎΠ²ΠΎΠΉ ΠΌΠ°ΡΠΈΠ½Ρ, Π² Π³ΠΎΡΠ½ΡΡ
Π²ΡΡΠ°Π±ΠΎΡΠΊΠ°Ρ
Ρ ΠΏΠ΅ΡΠ΅ΠΌΠ΅Π½Π½ΡΠΌΠΈ ΡΠ²ΠΎΠΉΡΡΠ²Π°ΠΌΠΈ Π³ΠΎΡΠ½ΡΡ
ΠΏΠΎΡΠΎΠ΄. ΠΠ°Π½Π° Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠ° Π½Π΅Π³Π°ΡΠΈΠ²Π½ΡΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ², Π²Π»ΠΈΡΡΡΠΈΡ
Π½Π° ΡΠΎΡΠ½ΠΎΡΡΡ ΠΎΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ ΡΠ°ΡΡΡΠΎΡΠ½ΠΈΡ ΠΌΠ΅ΡΠΎΠ΄ΠΎΠΌ Time- Flight (ToF). Π’Π°ΠΊΠΆΠ΅ ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½Π° ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½Π°Ρ ΠΎΡΠ΅Π½ΠΊΠ° ΡΠ°ΡΡΡΠΎΡΠ½ΠΈΡ ΠΌΠ΅ΠΆΠ΄Ρ Π΄Π²ΡΠΌΡ UWB ΠΌΠΎΠ΄ΡΠ»ΡΠΌΠΈThe article discusses methods for determining the distance using electromagnetic waves Cβband (4β8 GHz) in mines. An analysis of the distribution of the electric field strength of a dipole antenna mounted on a truck body in mine workings with variable rock properties is presented. The characteristics of the negative factors affecting the accuracy of distance determination by the Time-
Flight (ToF) method are given. An experimental estimate of the distance between two UWB modules has also been mad
ΠΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ Π²Π·Π°ΠΈΠΌΠΎΠ΄Π΅ΠΉΡΡΠ²ΠΈΡ ΡΠ»Π΅ΠΊΡΡΠΎΠΌΠ°Π³Π½ΠΈΡΠ½ΡΡ ΠΈ Π°ΠΊΡΡΡΠΈΡΠ΅ΡΠΊΠΈΡ Π²ΠΎΠ»Π½ Π΄Π»Ρ ΠΏΠΎΠ΄Π²ΠΎΠ΄Π½ΠΎΠΉ ΡΠ°Π΄ΠΈΠΎΡΠ²ΡΠ·ΠΈ
The article describes the potentiality of submarine reception of radio signals emitted by shore radio
transmitter with a horizontal antenna in the wavelength range based on interaction radio and acoustic
waves in skin-layer.Π ΡΡΠ°ΡΡΠ΅ ΡΠ°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°Π΅ΡΡΡ Π²Π·Π°ΠΈΠΌΠΎΠ΄Π΅ΠΉΡΡΠ²ΠΈΠ΅ ΡΠ»Π΅ΠΊΡΡΠΎΠΌΠ°Π³Π½ΠΈΡΠ½ΡΡ
ΠΈ Π°ΠΊΡΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
Π²ΠΎΠ»Π½
Π² ΠΈΠΎΠ½ΠΎΠΏΡΠΎΠ²ΠΎΠ΄ΡΡΠΈΡ
ΡΡΠ΅Π΄Π°Ρ
, Π² ΡΠ°ΡΡΠ½ΠΎΡΡΠΈ, Π² ΠΌΠΎΡΡΠΊΠΎΠΉ Π²ΠΎΠ΄Π΅ Π΄Π»Ρ ΡΠ΅ΡΠ΅Π½ΠΈΡ ΠΏΡΠΈΠΊΠ»Π°Π΄Π½ΠΎΠΉ Π·Π°Π΄Π°ΡΠΈ
ΠΎΠ±Π΅ΡΠΏΠ΅ΡΠ΅Π½ΠΈΡ ΡΠ°Π΄ΠΈΠΎΠΏΡΠΈΠ΅ΠΌΠ° ΠΏΠΎΠ΄Π²ΠΎΠ΄Π½ΡΠΌΠΈ Π°ΠΏΠΏΠ°ΡΠ°ΡΠ°ΠΌΠΈ Π½Π° Π±ΠΎΠ»ΡΡΠΈΡ
Π³Π»ΡΠ±ΠΈΠ½Π°
Mathematical Models of the Motion of Submersible Apparat with Electromagnetic Expiation and Reception near the Sea Bottom
We give aqualitative assessment of the dispersion of the received electromagnetic interference due to
variations in the electrical conductivity of the medium and the distance to the soil when search vehicle
driving near these a water-soil boundary, we determine the best modes of motion and parameters of the
probing signal for different transmitter-receiver combinations
Investigation Natural Vibrations Rail Lashes for Organization of Emergency Acoustic Channel Communications in the Mines and Detection of Defects
Π Π°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°ΡΡΡΡ ΠΏΡΠΈΠΊΠ»Π°Π΄Π½ΡΠ΅ Π°ΡΠΏΠ΅ΠΊΡΡ ΠΏΡΠΈΠΌΠ΅Π½Π΅Π½ΠΈΡ ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΠΎΠ² ΡΠ°ΡΡΠΎΡΡ ΡΠΎΠ±ΡΡΠ²Π΅Π½Π½ΡΡ
ΠΌΠ΅Ρ
Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
(Π§Π‘Π) ΠΎΠ±ΡΠ΅ΠΊΡΠΎΠ². ΠΡΠΈΠ²Π΅Π΄Π΅Π½Ρ ΡΠ°ΡΡΠ΅ΡΠ½ΡΠ΅ ΠΈ ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΡΠ΅ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ
ΠΏΠΎ ΠΎΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ ΡΠ°ΡΡΠΎΡ ΡΠΎΠ±ΡΡΠ²Π΅Π½Π½ΡΡ
ΠΊΠΎΠ»Π΅Π±Π°Π½ΠΈΠΉ ΡΠ΅Π»ΡΡΠΎΠ² ΠΈ ΠΎΡΠ΅Π½ΠΊΠ° Π·Π°ΡΡΡ
Π°Π½ΠΈΡ ΠΊΠΎΠ»Π΅Π±Π°Π½ΠΈΠΉ Π½Π°
ΡΡΠΈΡ
ΡΠ°ΡΡΠΎΡΠ°Ρ
. ΠΡΡΠ»Π΅Π΄ΡΠ΅ΡΡΡ ΡΠ°Π΄ΠΈΠΎΠ»ΠΎΠΊΠ°ΡΠΈΠΎΠ½Π½ΡΠΉ (Π Π) ΠΌΠ΅ΡΠΎΠ΄, Π·Π°ΠΊΠ»ΡΡΠ°ΡΡΠΈΠΉΡΡ Π² ΠΏΠΎΠ»ΡΡΠ΅Π½ΠΈΠΈ
ΠΈΠ½ΡΠΎΡΠΌΠ°ΡΠΈΠΈ ΠΎ Π΄Π΅ΡΠ΅ΠΊΡΠ°Ρ
ΡΠ΅Π»ΡΡΠΎΠ²ΠΎΠ³ΠΎ ΡΡΠ°Π³ΠΌΠ΅Π½ΡΠ° ΠΏΡΡΡΠΌ ΡΠ΅Π³ΠΈΡΡΡΠ°ΡΠΈΠΈ ΠΊΠΎΠ»Π΅Π±Π°Π½ΠΈΠΉ Π§Π‘Π
ΠΌΠ΅ΠΆΠ΄ΡΡΠΏΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΏΡΠΎΠ»ΡΡΠ° ΡΠ΅Π»ΡΡΠ°This article discusses aspects of application parameters natural frequency objects. The calculated and
experimental results to determine the natural frequencies of the rails and the estimation of damping
vibrations at these frequencies. We investigate radar (RL) method is to obtain information about the
defects of the rail track by registering their own frequency mechanical vibrations between crosstie
rail spa
On the Observations of Seismic-Electric Effect and the Induced Polarization Potential on Minusinsk Gas Deposit Field in the Natural Noise Fields of the Earth
Π ΡΡΠ°ΡΡΠ΅ ΠΎΠΏΠΈΡΠ°Π½ΠΎ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠ΅ ΡΠ΅ΠΉΡΠΌΠΎΡΠ»Π΅ΠΊΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
(Π‘Π) ΡΠ²Π»Π΅Π½ΠΈΠΉ ΠΈ ΡΡΡΠ΅ΠΊΡΠ° Π²ΡΠ·Π²Π°Π½Π½ΠΎΠΉ ΠΏΠΎΠ»ΡΡΠΈΠ·Π°ΡΠΈΠΈ (ΠΠ) ΠΏΠΎ ΠΏΠ°ΡΡΠΈΠ²Π½ΠΎΠΌΡ ΠΌΠ΅ΡΠΎΠ΄Ρ, ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡΠ΅ΠΌΡ ΠΈΠ·Π²Π»Π΅ΠΊΠ°ΡΡ ΠΈΠ½ΡΠΎΡΠΌΠ°ΡΠΈΡ ΠΈΠ· Π΅ΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΡ
ΡΠ»Π΅ΠΊΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ ΡΠ΅ΠΉΡΠΌΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠΌΠΎΠ² ΠΠ΅ΠΌΠ»ΠΈ Π² Π΄ΠΈΠ°ΠΏΠ°Π·ΠΎΠ½Π΅ 1-20 ΠΡ. ΠΡΠΎ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠ΅ Π±ΡΠ»ΠΎ ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½ΠΎ Π² ΠΏΠ΅ΡΠΈΠΎΠ΄ 29-31 Π°Π²Π³ΡΡΡΠ° 2014 Π³. Π² ΡΠ°ΠΉΠΎΠ½Π΅ ΠΠΎΠ²ΠΎ-ΠΠΈΡ
Π°ΠΉΠ»ΠΎΠ²ΡΠΊΠΎΠΉ ΠΏΠ»ΠΎΡΠ°Π΄ΠΈ ΠΠΈΠ½ΡΡΠΈΠ½ΡΠΊΠΎΠ³ΠΎ Π³Π°Π·ΠΎΠΊΠΎΠ½Π΄Π΅Π½ΡΠ°ΡΠ½ΠΎΠ³ΠΎ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΡ (ΡΠ΅ΡΠΏΡΠ±Π»ΠΈΠΊΠ° Π₯Π°ΠΊΠ°ΡΠΈΡ). ΠΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π»ΡΡ ΠΏΡΠΈΠ±ΠΎΡ ΠΠΠΠΠΠ-Π1 (Π¨ΡΠΌ-6), ΡΠ°Π·ΡΠ°Π±ΠΎΡΠ°Π½Π½ΡΠΉ Π² Π‘ΠΈΠ±ΠΈΡΡΠΊΠΎΠΌ ΡΠ΅Π΄Π΅ΡΠ°Π»ΡΠ½ΠΎΠΌ ΡΠ½ΠΈΠ²Π΅ΡΡΠΈΡΠ΅ΡΠ΅. ΠΡΠΎΠ΄ΡΠΊΡΠΈΠ²Π½Π°Ρ Π·Π°Π»Π΅ΠΆΡ Π±ΡΠ»Π° ΠΎΡΠΌΠ΅ΡΠ΅Π½Π° ΠΏΠΎΠ²ΡΡΠ΅Π½ΠΈΠ΅ΠΌ Π·Π½Π°ΡΠ΅Π½ΠΈΡ ΠΊΠΎΡΡΡΠΈΡΠΈΠ΅Π½ΡΠ° Π²Π·Π°ΠΈΠΌΠ½ΠΎΠΉ ΠΊΠΎΡΡΠ΅Π»ΡΡΠΈΠΈ ΡΠ΅ΠΉΡΠΌΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ ΡΠ»Π΅ΠΊΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΏΠΎΠΌΠ΅Ρ
, Π° ΡΠ°ΠΊΠΆΠ΅ Π³ΡΠ°Π΄ΠΈΠ΅Π½ΡΠΎΠΌ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»Π° Π²ΡΠ·Π²Π°Π½Π½ΠΎΠΉ ΠΏΠΎΠ»ΡΡΠΈΠ·Π°ΡΠΈΠΈ, ΠΏΠΎΠ»ΡΡΠ°Π΅ΠΌΡΠΌ ΠΈΠ· ΡΠΈΠ³Π½Π°Π»ΠΎΠ², ΡΠ½ΠΈΠΌΠ°Π΅ΠΌΡΡ
Ρ Π΄Π²ΡΡ
ΡΠΌΠ΅ΠΆΠ½ΡΡ
ΡΠ»Π΅ΠΊΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
Π΄ΠΈΠΏΠΎΠ»Π΅ΠΉ. Π 2015 Π³. ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½Ρ ΠΏΠΎ Π‘Π Π±ΡΠ» ΠΏΠΎΠ²ΡΠΎΡΠ΅Π½ Π½Π° Π΄Π²ΡΡ
ΠΏΠ»ΠΎΡΠ°Π΄ΡΡ
ΡΡΠΎΠ³ΠΎ ΠΆΠ΅ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΡ, ΠΡΡΡΡΡΠ½ΡΠΊΠΎΠΉ ΠΈ ΠΠΎΠ²ΠΎ-ΠΠΈΡ
Π°ΠΉΠ»ΠΎΠ²ΡΠΊΠΎΠΉ ΠΏΠ»ΠΎΡΠ°Π΄ΠΈ. ΠΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½Ρ, ΠΏΠΎΠ΄ΡΠ²Π΅ΡΠ΄ΠΈΠ²ΡΠΈΠΉ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ 2014 Π³.The paper describe the exploration of seismic-electric phenomenon and the effect of the induced polarization by passive method, which is extracting information from natural the electrical and seismic noise of the Earth in the frequency range of 1-20 Hz. This research was performed in the period 29-31 August 2014 at the Novo-Mikhailovskaya area of Minusinsk condensate field (Rep. Khakassia). We have used the device developed at the Siberian Federal University VPEMPZ-M1 (Noise-6). Productive reservoir was detected by the cross-correlation coefficient of seismic and electrical noise. The potential gradient induced polarization was in 5-7 times higher than normal background. In 2015, the experiment was repeated in two areas of the same field, Bistriynskiy and Novo-Mikhailovskiy area, which confirmed the results of 201
Π€ΠΈΠ·ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΎΡΠ½ΠΎΠ²Ρ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΠ½Π΅ΡΠ³Π΅ΡΠΈΡΠ΅ΡΠΊΠΈ ΠΊΠ²Π°Π·ΠΈΠΎΠΏΡΠΈΠΌΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΈΠΌΠΏΡΠ»ΡΡΠ½ΠΎΠ³ΠΎ ΡΠ΅ΠΉΡΠΌΠΎΠ°ΠΊΡΡΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ Π²ΠΎΠ·Π΄Π΅ΠΉΡΡΠ²ΠΈΡ Π΄Π»Ρ Π³Π΅ΠΎΡΠΈΠ·ΠΈΡΠ΅ΡΠΊΠΈΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ Π² ΡΡΠ»ΠΎΠ²ΠΈΡΡ ΠΌΠ΅Π»ΠΊΠΎΠ²ΠΎΠ΄ΡΡ ΠΈ ΡΡΠ°Π½Π·ΠΈΡΠ½ΡΡ Π·ΠΎΠ½. Π§Π°ΡΡΡ 2. ΠΠΎΠ½ΡΡΡΡΠΊΡΠΈΡ Π²ΠΎΠ΄Π½ΠΎΠ³ΠΎ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ° ΠΈ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠΎΠ²
The article discusses theoretical aspects of seismic wave excitation of in the aquatic environ-
ment, addresses the problems of instrumental implementation of a fundamentally new source of seismic
vibrations that can work: in the water area, in tidal and coastal zones. The scientific substantiation of
the developed seismic source (SS) design is given.
The results of the seismic influence simulation of hydrodynamic resistance on the media, as well as the
formation of the βadded massβ are given. The results were obtained using the developed mathematical
model of the motion of the radiating surface. Based on the experimental work, a comparative analysis
of the energy efficiency of the developed seismic source model and the serial sample of the VEM-50
"Yenisei" water seismic source was made. Experimental results were obtained at the geophysical well of
the test and training areaΠ ΡΡΠ°ΡΡΠ΅ Π΄Π°Π΅ΡΡΡ Π½Π°ΡΡΠ½ΠΎΠ΅ ΠΎΠ±ΠΎΡΠ½ΠΎΠ²Π°Π½ΠΈΠ΅ ΡΠ°Π·ΡΠ°Π±ΠΎΡΠ°Π½Π½ΠΎΠΉ ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠΈ ΡΠ΅ΠΉΡΠΌΠΎΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ°
(Π‘Π). ΠΡΠ΅Π½ΠΈΠ²Π°Π΅ΡΡΡ ΡΡΡΠ΅ΠΊΡΠΈΠ²Π½ΠΎΡΡΡ Π΄Π²ΡΡ
ΠΏΠΎΠ»ΡΡΠ½ΠΎΠ³ΠΎ Π²ΠΎΠ·Π±ΡΠΆΠ΄Π΅Π½ΠΈΡ Π²ΠΎΠ΄Π½ΠΎΠΉ ΡΡΠ΅Π΄Ρ Π‘Π Π² ΡΡΠ°Π²Π½Π΅Π½ΠΈΠΈ Ρ ΠΈΠ·Π²Π΅ΡΡΠ½ΡΠΌΠΈ Π²ΠΎΠ΄Π½ΡΠΌΠΈ ΠΈΠΌΠΏΡΠ»ΡΡΠ½ΡΠΌΠΈ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ°ΠΌΠΈ ΡΠ΅ΡΠΈΠΈ Β«ΠΠ½ΠΈΡΠ΅ΠΉΒ». ΠΡΠΈΠ²ΠΎΠ΄ΡΡΡΡ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΡ Π²Π»ΠΈΡΠ½ΠΈΡ Π³ΠΈΠ΄ΡΠΎΠ΄ΠΈΠ½Π°ΠΌΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΡΠΎΠΏΡΠΎΡΠΈΠ²Π»Π΅Π½ΠΈΡ ΡΡΠ΅Π΄Ρ Π‘Π Π²ΠΎΠ·Π΄Π΅ΠΉΡΡΠ²ΠΈΡ, Π° ΡΠ°ΠΊΠΆΠ΅ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ
Β«ΠΏΡΠΈΡΠΎΠ΅Π΄ΠΈΠ½Π΅Π½Π½ΠΎΠΉ ΠΌΠ°ΡΡΡΒ». Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΏΠΎΠ»ΡΡΠ΅Π½Ρ Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ ΡΠ°Π·ΡΠ°Π±ΠΎΡΠ°Π½Π½ΠΎΠΉ ΠΌΠ°ΡΠ΅ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ
Π΄Π²ΠΈΠΆΠ΅Π½ΠΈΡ ΠΈΠ·Π»ΡΡΠ°ΡΡΠ΅ΠΉ ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠΈ. ΠΠ° ΠΎΡΠ½ΠΎΠ²Π΅ ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½Π½ΡΡ
ΠΎΠΏΡΡΠ½ΡΡ
ΡΠ°Π±ΠΎΡ ΡΠ΄Π΅Π»Π°Π½ ΡΡΠ°Π²Π½ΠΈΡΠ΅Π»ΡΠ½ΡΠΉ
Π°Π½Π°Π»ΠΈΠ· ΡΠ½Π΅ΡΠ³Π΅ΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΡΡΠ΅ΠΊΡΠΈΠ²Π½ΠΎΡΡΠΈ ΡΠ°Π±ΠΎΡΡ ΠΌΠ°ΠΊΠ΅ΡΠ° Π‘Π ΠΈ ΡΠ΅ΡΠΈΠΉΠ½ΠΎΠ³ΠΎ ΠΎΠ±ΡΠ°Π·ΡΠ° Π²ΠΎΠ΄Π½ΠΎΠ³ΠΎ Π‘Π ΠΠΠ-50
ΠΌΠΎΠ΄Π΅Π»ΡΠ½ΠΎΠ³ΠΎ ΡΡΠ΄Π° Β«ΠΠ½ΠΈΡΠ΅ΠΉΒ». ΠΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΡΠ΅ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΏΠΎΠ»ΡΡΠ΅Π½Ρ Π½Π° Π³Π΅ΠΎΡΠΈΠ·ΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΠΊΠ²Π°ΠΆΠΈΠ½Π΅
ΡΡΠ΅Π±Π½ΠΎ-ΠΈΡΠΏΡΡΠ°ΡΠ΅Π»ΡΠ½ΠΎΠ³ΠΎ ΠΏΠΎΠ»ΠΈΠ³ΠΎΠ½Π° Π‘ΠΈΠ±ΠΈΡΡΠΊΠΎΠ³ΠΎ ΡΠ΅Π΄Π΅ΡΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠ½ΠΈΠ²Π΅ΡΡΠΈΡΠ΅Ρ
Π€ΠΈΠ·ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΎΡΠ½ΠΎΠ²Ρ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΠ½Π΅ΡΠ³Π΅ΡΠΈΡΠ΅ΡΠΊΠΈ ΠΊΠ²Π°Π·ΠΈΠΎΠΏΡΠΈΠΌΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΈΠΌΠΏΡΠ»ΡΡΠ½ΠΎΠ³ΠΎ ΡΠ΅ΠΉΡΠΌΠΎΠ°ΠΊΡΡΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ Π²ΠΎΠ·Π΄Π΅ΠΉΡΡΠ²ΠΈΡ Π΄Π»Ρ Π³Π΅ΠΎΡΠΈΠ·ΠΈΡΠ΅ΡΠΊΠΈΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ Π² ΡΡΠ»ΠΎΠ²ΠΈΡΡ ΠΌΠ΅Π»ΠΊΠΎΠ²ΠΎΠ΄ΡΡ ΠΈ ΡΡΠ°Π½Π·ΠΈΡΠ½ΡΡ Π·ΠΎΠ½. Π§Π°ΡΡΡ 1. Π’Π΅ΠΎΡΠ΅ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΎΡΠ½ΠΎΠ²Ρ
Despite the development of alternative energy, hydrocarbon raw materials is one of the most important
energy resources in the world. The discovery of new deposits today is an urgent task. Long-term prospects
for the development of seismic exploration are associated with the development of the continental shelf,
in particular the Arctic. Also, a large raw material potential is expected from poorly studied territories
located on the Arctic coast of the Russian Federation, reef zones of the Persian Gulf states, and in the
transit and shallow waters (at a depth of up to 10 meters).
The article discusses the theoretical aspects of the excitation of seismic waves in the water, addresses
the problems of instrumental implementation of a new source of seismic vibrations that can work: in the
water area, in tidal and coastal zones, i.e. produce continuous seismic profiling from the water area to
the land. The scientific substantiation of the developed seismic source (SS) design is givenΠΠ΅ΡΠΌΠΎΡΡΡ Π½Π° ΡΠ°Π·Π²ΠΈΡΠΈΠ΅ Π°Π»ΡΡΠ΅ΡΠ½Π°ΡΠΈΠ²Π½ΠΎΠΉ ΡΠ½Π΅ΡΠ³Π΅ΡΠΈΠΊΠΈ, ΡΠ³Π»Π΅Π²ΠΎΠ΄ΠΎΡΠΎΠ΄Π½ΠΎΠ΅ ΡΡΡΡΠ΅ ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΎΠ΄Π½ΠΈΠΌ
ΠΈΠ· Π²Π°ΠΆΠ½Π΅ΠΉΡΠΈΡ
ΡΠ½Π΅ΡΠ³Π΅ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠ΅ΡΡΡΡΠΎΠ² Π²ΠΎ Π²ΡΠ΅ΠΌ ΠΌΠΈΡΠ΅. ΠΡΠΊΡΡΡΠΈΠ΅ Π½ΠΎΠ²ΡΡ
ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ ΠΏΠΎ-ΠΏΡΠ΅ΠΆΠ½Π΅ΠΌΡ Π°ΠΊΡΡΠ°Π»ΡΠ½Π°Ρ Π·Π°Π΄Π°ΡΠ°. Π‘ΡΠ΅Π΄Π½Π΅- ΠΈ Π΄ΠΎΠ»Π³ΠΎΡΡΠΎΡΠ½ΡΠ΅ ΠΏΠ΅ΡΡΠΏΠ΅ΠΊΡΠΈΠ²Ρ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΡΠ΅ΠΉΡΠΌΠΎΡΠ°Π·Π²Π΅Π΄ΠΊΠΈ
ΠΏΡΠΈΠ½ΡΡΠΎ ΡΠ²ΡΠ·ΡΠ²Π°ΡΡ Ρ ΠΎΡΠ²ΠΎΠ΅Π½ΠΈΠ΅ΠΌ ΠΊΠΎΠ½ΡΠΈΠ½Π΅Π½ΡΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠ΅Π»ΡΡΠ°, Π² ΡΠ°ΡΡΠ½ΠΎΡΡΠΈ Π°ΡΠΊΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ. Π’Π°ΠΊΠΆΠ΅
Π±ΠΎΠ»ΡΡΠΎΠΉ ΡΡΡΡΠ΅Π²ΠΎΠΉ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π» ΡΠ΅Π³ΠΎΠ΄Π½Ρ ΠΎΠΆΠΈΠ΄Π°Π΅ΡΡΡ ΠΎΡ ΠΌΠ°Π»ΠΎΠΈΠ·ΡΡΠ΅Π½Π½ΡΡ
ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΉ, ΡΠ°ΡΠΏΠΎΠ»ΠΎΠΆΠ΅Π½Π½ΡΡ
Π½Π° Π°ΡΠΊΡΠΈΡΠ΅ΡΠΊΠΎΠΌ ΠΏΠΎΠ±Π΅ΡΠ΅ΠΆΡΠ΅ Π Π€, ΡΠΈΡΠΎΠ²ΡΡ
Π·ΠΎΠ½Π°Ρ
Π³ΠΎΡΡΠ΄Π°ΡΡΡΠ² ΠΏΠ΅ΡΡΠΈΠ΄ΡΠΊΠΎΠ³ΠΎ Π·Π°Π»ΠΈΠ²Π°, Π° ΡΠ°ΠΊΠΆΠ΅ Π²
ΡΡΠ°Π½Π·ΠΈΡΠ½ΠΎΠΉ ΠΈ ΠΌΠ΅Π»ΠΊΠΎΠ²ΠΎΠ΄Π½ΠΎΠΉ Π·ΠΎΠ½Π΅ (Π½Π° Π³Π»ΡΠ±ΠΈΠ½Π΅ Π΄ΠΎ 10 ΠΌ).
Π ΡΡΠ°ΡΡΠ΅ ΠΈΡΡΠ»Π΅Π΄ΡΡΡΡΡ ΡΠ΅ΠΎΡΠ΅ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ Π°ΡΠΏΠ΅ΠΊΡΡ Π²ΠΎΠ·Π±ΡΠΆΠ΄Π΅Π½ΠΈΡ ΡΠ΅ΠΉΡΠΌΠΎΠ°ΠΊΡΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
(Π‘Π) Π²ΠΎΠ»Π½
Π² Π²ΠΎΠ΄Π½ΠΎΠΉ ΡΡΠ΅Π΄Π΅, ΡΠ°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°ΡΡΡΡ ΠΏΡΠΎΠ±Π»Π΅ΠΌΡ Π°ΠΏΠΏΠ°ΡΠ°ΡΡΡΠ½ΠΎΠΉ ΡΠ΅Π°Π»ΠΈΠ·Π°ΡΠΈΠΈ ΠΏΡΠΈΠ½ΡΠΈΠΏΠΈΠ°Π»ΡΠ½ΠΎ Π½ΠΎΠ²ΠΎΠ³ΠΎ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ° ΡΠ΅ΠΉΡΠΌΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΊΠΎΠ»Π΅Π±Π°Π½ΠΈΠΉ, ΡΠΏΠΎΡΠΎΠ±Π½ΠΎΠ³ΠΎ ΡΠ°Π±ΠΎΡΠ°ΡΡ Π½Π° Π°ΠΊΠ²Π°ΡΠΎΡΠΈΠΈ, Π² ΠΏΡΠΈΠ»ΠΈΠ²Π½ΠΎ-ΠΎΡΠ»ΠΈΠ²Π½ΠΎΠΉ ΠΈ Π±Π΅ΡΠ΅Π³ΠΎΠ²ΠΎΠΉ Π·ΠΎΠ½Π°Ρ
, Ρ.Π΅. ΠΏΡΠΎΠΈΠ·Π²ΠΎΠ΄ΠΈΡΡ Π½Π΅ΠΏΡΠ΅ΡΡΠ²Π½ΠΎΠ΅ ΡΠ΅ΠΉΡΠΌΠΈΡΠ΅ΡΠΊΠΎΠ΅ ΠΏΡΠΎΡΠΈΠ»ΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ Ρ Π°ΠΊΠ²Π°ΡΠΎΡΠΈΠΈ Π½Π° ΡΡΡ