5 research outputs found
Stimulation of Seismic Waves by Puised Nonexplosive Source
Π Π°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°ΡΡΡΡ ΡΠΈΠ·ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΎΡΠ½ΠΎΠ²Ρ Π²ΠΎΠ·Π±ΡΠΆΠ΄Π΅Π½ΠΈΡ ΡΠ΅ΠΉΡΠΌΠΈΡΠ΅ΡΠΊΠΈΡ
Π²ΠΎΠ»Π½ Π² ΡΠ΅ΠΉΡΠΌΠΎΡΠ°Π·Π²Π΅Π΄ΠΊΠ΅ Ρ ΠΈΡΠΏΠΎΠ»Ρ-
Π·ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ ΠΈΠΌΠΏΡΠ»ΡΡΠ½ΡΡ
Π½Π΅Π²Π·ΡΡΠ²Π½ΡΡ
ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠΎΠ² Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ ΠΊΠΎΡΠΎΡΠΊΠΎΡ
ΠΎΠ΄ΠΎΠ²ΡΡ
ΡΠ»Π΅ΠΊΡΡΠΎΠΌΠ°Π³Π½ΠΈΡΠΎΠ².The physical foundations of seismic waves stimulation in seismic exploration with the help of puised
nonexplosive sources on the base of short-run electromagnets are examined
Stimulation of Seismic Waves by Puised Nonexplosive Source
Π Π°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°ΡΡΡΡ ΡΠΈΠ·ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΎΡΠ½ΠΎΠ²Ρ Π²ΠΎΠ·Π±ΡΠΆΠ΄Π΅Π½ΠΈΡ ΡΠ΅ΠΉΡΠΌΠΈΡΠ΅ΡΠΊΠΈΡ
Π²ΠΎΠ»Π½ Π² ΡΠ΅ΠΉΡΠΌΠΎΡΠ°Π·Π²Π΅Π΄ΠΊΠ΅ Ρ ΠΈΡΠΏΠΎΠ»Ρ-
Π·ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ ΠΈΠΌΠΏΡΠ»ΡΡΠ½ΡΡ
Π½Π΅Π²Π·ΡΡΠ²Π½ΡΡ
ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠΎΠ² Π½Π° ΠΎΡΠ½ΠΎΠ²Π΅ ΠΊΠΎΡΠΎΡΠΊΠΎΡ
ΠΎΠ΄ΠΎΠ²ΡΡ
ΡΠ»Π΅ΠΊΡΡΠΎΠΌΠ°Π³Π½ΠΈΡΠΎΠ².The physical foundations of seismic waves stimulation in seismic exploration with the help of puised
nonexplosive sources on the base of short-run electromagnets are examined
The Possibility of Creation of Rotary-Type Source of Seismic Transverse Waves with Electromagnetic Excitation
Use of transverse waves in exploration seismology provides some additional information needed to improve prediction of hydrocarbon deposits. Traditional sources of transverse waves have a number of disadvantages associated with bad reproducibility of influence, and the predominant excitation of longitudinal waves. In this work a variant of a rotary-type source of transverse waves with electromagnetic excitation which free from these disadvantages has been considered. Assessment of the required design parameters of this source and comparison the characteristics of the developed source in comparison with other similar devices are presented.ΠΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΏΠΎΠΏΠ΅ΡΠ΅ΡΠ½ΡΡ
Π²ΠΎΠ»Π½ Π² ΡΠ΅ΠΉΡΠΌΠΎΡΠ°Π·Π²Π΅Π΄ΠΊΠ΅ Π΄Π°Π΅Ρ ΡΡΠ΄ Π΄ΠΎΠΏΠΎΠ»Π½ΠΈΡΠ΅Π»ΡΠ½ΡΡ
ΡΠ²Π΅Π΄Π΅Π½ΠΈΠΉ, Π½Π΅ΠΎΠ±Ρ
ΠΎΠ΄ΠΈΠΌΡΡ
Π΄Π»Ρ ΠΏΠΎΠ²ΡΡΠ΅Π½ΠΈΡ ΠΊΠ°ΡΠ΅ΡΡΠ²Π° ΠΏΡΠΎΠ³Π½ΠΎΠ·ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ ΡΠ³Π»Π΅Π²ΠΎΠ΄ΠΎΡΠΎΠ΄ΠΎΠ². Π’ΡΠ°Π΄ΠΈΡΠΈΠΎΠ½Π½ΠΎ ΠΈΡΠΏΠΎΠ»ΡΠ·ΡΠ΅ΠΌΡΠ΅ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠΈ ΠΏΠΎΠΏΠ΅ΡΠ΅ΡΠ½ΡΡ
Π²ΠΎΠ»Π½ ΠΎΠ±Π»Π°Π΄Π°ΡΡ ΡΡΠ΄ΠΎΠΌ Π½Π΅Π΄ΠΎΡΡΠ°ΡΠΊΠΎΠ², ΡΠ²ΡΠ·Π°Π½Π½ΡΡ
ΠΊΠ°ΠΊ Ρ ΠΏΠ»ΠΎΡ
ΠΎΠΉ Π²ΠΎΡΠΏΡΠΎΠΈΠ·Π²ΠΎΠ΄ΠΈΠΌΠΎΡΡΡΡ Π²ΠΎΠ·Π΄Π΅ΠΉΡΡΠ²ΠΈΡ, ΡΠ°ΠΊ ΠΈ Ρ ΠΏΡΠ΅ΠΈΠΌΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΠΌ Π²ΠΎΠ·Π±ΡΠΆΠ΄Π΅Π½ΠΈΠ΅ΠΌ ΠΏΡΠΎΠ΄ΠΎΠ»ΡΠ½ΡΡ
Π²ΠΎΠ»Π½. Π ΡΡΠ°ΡΡΠ΅ ΡΠ°ΡΡΠΌΠΎΡΡΠ΅Π½ Π²Π°ΡΠΈΠ°Π½Ρ ΡΠΎΡΠΎΡΠ½ΠΎΠ³ΠΎ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ° ΠΏΠΎΠΏΠ΅ΡΠ΅ΡΠ½ΡΡ
Π²ΠΎΠ»Π½ Ρ ΡΠ»Π΅ΠΊΡΡΠΎΠΌΠ°Π³Π½ΠΈΡΠ½ΡΠΌ Π²ΠΎΠ·Π±ΡΠΆΠ΄Π΅Π½ΠΈΠ΅ΠΌ, ΡΠ²ΠΎΠ±ΠΎΠ΄Π½ΠΎΠ³ΠΎ ΠΎΡ ΡΠΊΠ°Π·Π°Π½Π½ΡΡ
Π½Π΅Π΄ΠΎΡΡΠ°ΡΠΊΠΎΠ². ΠΡΠΈΠ²Π΅Π΄Π΅Π½Ρ ΠΎΡΠ΅Π½ΠΊΠΈ Π½Π΅ΠΎΠ±Ρ
ΠΎΠ΄ΠΈΠΌΡΡ
ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠ²Π½ΡΡ
ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΠΎΠ² ΡΡΠΎΠ³ΠΎ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ° ΠΈ ΡΠΎΠΏΠΎΡΡΠ°Π²Π»Π΅Π½ΠΈΠ΅ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊ ΡΠ°Π·ΡΠ°Π±Π°ΡΡΠ²Π°Π΅ΠΌΠΎΠ³ΠΎ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ° ΠΏΠΎ ΡΡΠ°Π²Π½Π΅Π½ΠΈΡ Ρ Π΄ΡΡΠ³ΠΈΠΌΠΈ Π²ΠΈΠ΄Π°ΠΌΠΈ Π°Π½Π°Π»ΠΎΠ³ΠΈΡΠ½ΡΡ
ΡΡΡΡΠΎΠΉΡΡΠ²
The Possibility of Creation of Rotary-Type Source of Seismic Transverse Waves with Electromagnetic Excitation
Use of transverse waves in exploration seismology provides some additional information needed to improve prediction of hydrocarbon deposits. Traditional sources of transverse waves have a number of disadvantages associated with bad reproducibility of influence, and the predominant excitation of longitudinal waves. In this work a variant of a rotary-type source of transverse waves with electromagnetic excitation which free from these disadvantages has been considered. Assessment of the required design parameters of this source and comparison the characteristics of the developed source in comparison with other similar devices are presented.ΠΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΏΠΎΠΏΠ΅ΡΠ΅ΡΠ½ΡΡ
Π²ΠΎΠ»Π½ Π² ΡΠ΅ΠΉΡΠΌΠΎΡΠ°Π·Π²Π΅Π΄ΠΊΠ΅ Π΄Π°Π΅Ρ ΡΡΠ΄ Π΄ΠΎΠΏΠΎΠ»Π½ΠΈΡΠ΅Π»ΡΠ½ΡΡ
ΡΠ²Π΅Π΄Π΅Π½ΠΈΠΉ, Π½Π΅ΠΎΠ±Ρ
ΠΎΠ΄ΠΈΠΌΡΡ
Π΄Π»Ρ ΠΏΠΎΠ²ΡΡΠ΅Π½ΠΈΡ ΠΊΠ°ΡΠ΅ΡΡΠ²Π° ΠΏΡΠΎΠ³Π½ΠΎΠ·ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ ΡΠ³Π»Π΅Π²ΠΎΠ΄ΠΎΡΠΎΠ΄ΠΎΠ². Π’ΡΠ°Π΄ΠΈΡΠΈΠΎΠ½Π½ΠΎ ΠΈΡΠΏΠΎΠ»ΡΠ·ΡΠ΅ΠΌΡΠ΅ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠΈ ΠΏΠΎΠΏΠ΅ΡΠ΅ΡΠ½ΡΡ
Π²ΠΎΠ»Π½ ΠΎΠ±Π»Π°Π΄Π°ΡΡ ΡΡΠ΄ΠΎΠΌ Π½Π΅Π΄ΠΎΡΡΠ°ΡΠΊΠΎΠ², ΡΠ²ΡΠ·Π°Π½Π½ΡΡ
ΠΊΠ°ΠΊ Ρ ΠΏΠ»ΠΎΡ
ΠΎΠΉ Π²ΠΎΡΠΏΡΠΎΠΈΠ·Π²ΠΎΠ΄ΠΈΠΌΠΎΡΡΡΡ Π²ΠΎΠ·Π΄Π΅ΠΉΡΡΠ²ΠΈΡ, ΡΠ°ΠΊ ΠΈ Ρ ΠΏΡΠ΅ΠΈΠΌΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΠΌ Π²ΠΎΠ·Π±ΡΠΆΠ΄Π΅Π½ΠΈΠ΅ΠΌ ΠΏΡΠΎΠ΄ΠΎΠ»ΡΠ½ΡΡ
Π²ΠΎΠ»Π½. Π ΡΡΠ°ΡΡΠ΅ ΡΠ°ΡΡΠΌΠΎΡΡΠ΅Π½ Π²Π°ΡΠΈΠ°Π½Ρ ΡΠΎΡΠΎΡΠ½ΠΎΠ³ΠΎ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ° ΠΏΠΎΠΏΠ΅ΡΠ΅ΡΠ½ΡΡ
Π²ΠΎΠ»Π½ Ρ ΡΠ»Π΅ΠΊΡΡΠΎΠΌΠ°Π³Π½ΠΈΡΠ½ΡΠΌ Π²ΠΎΠ·Π±ΡΠΆΠ΄Π΅Π½ΠΈΠ΅ΠΌ, ΡΠ²ΠΎΠ±ΠΎΠ΄Π½ΠΎΠ³ΠΎ ΠΎΡ ΡΠΊΠ°Π·Π°Π½Π½ΡΡ
Π½Π΅Π΄ΠΎΡΡΠ°ΡΠΊΠΎΠ². ΠΡΠΈΠ²Π΅Π΄Π΅Π½Ρ ΠΎΡΠ΅Π½ΠΊΠΈ Π½Π΅ΠΎΠ±Ρ
ΠΎΠ΄ΠΈΠΌΡΡ
ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠ²Π½ΡΡ
ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΠΎΠ² ΡΡΠΎΠ³ΠΎ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ° ΠΈ ΡΠΎΠΏΠΎΡΡΠ°Π²Π»Π΅Π½ΠΈΠ΅ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊ ΡΠ°Π·ΡΠ°Π±Π°ΡΡΠ²Π°Π΅ΠΌΠΎΠ³ΠΎ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ° ΠΏΠΎ ΡΡΠ°Π²Π½Π΅Π½ΠΈΡ Ρ Π΄ΡΡΠ³ΠΈΠΌΠΈ Π²ΠΈΠ΄Π°ΠΌΠΈ Π°Π½Π°Π»ΠΎΠ³ΠΈΡΠ½ΡΡ
ΡΡΡΡΠΎΠΉΡΡΠ²