180 research outputs found
Π€Π΅Π½ΠΎΠΌΠ΅Π½ ΠΠ΅ΡΡΠΎΠ²ΡΠΊΠΎΠ³ΠΎ (ΠΊ 75-Π»Π΅ΡΠ½Π΅ΠΌΡ ΡΠ±ΠΈΠ»Π΅Ρ)
Brief scientific biography of a well-known scientist, a leader in the field of experimental study of crystallization processes with usage the holographic method for quantitative analysis of temperature-convective inhomogeneities in the Β«growth-criticalstoneΒ» system, a specialist in crystallographic-mineralogical study of diamonds and their accessory minerals, a successful researcher of modern mineral formation at Kamchatka volcanoes, one of the founders of the Β«literally from scratchΒ» enterprise for the production of industrial diamonds.ΠΡΠ°ΡΠΊΠ°Ρ Π½Π°ΡΡΠ½Π°Ρ Π±ΠΈΠΎΠ³ΡΠ°ΡΠΈΡ ΠΈΠ·Π²Π΅ΡΡΠ½ΠΎΠ³ΠΎ ΡΡΠ΅Π½ΠΎΠ³ΠΎ β Π»ΠΈΠ΄Π΅ΡΠ° Π² ΠΎΠ±Π»Π°ΡΡΠΈ ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΈΠ·ΡΡΠ΅Π½ΠΈΡ ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΊΡΠΈΡΡΠ°Π»Π»ΠΈΠ·Π°ΡΠΈΠΈ Ρ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ Π³ΠΎΠ»ΠΎΠ³ΡΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΌΠ΅ΡΠΎΠ΄Π° Π΄Π»Ρ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎΠ³ΠΎ Π°Π½Π°Π»ΠΈΠ·Π° ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΠ½ΠΎ-ΠΊΠΎΠ½Π²Π΅ΠΊΡΠΈΠ²Π½ΡΡ
Π½Π΅ΠΎΠ΄Π½ΠΎΡΠΎΠ΄Π½ΠΎΡΡΠ΅ΠΉ Π² ΡΠΈΡΡΠ΅ΠΌΠ΅ Β«ΠΊΡΠΈΡΡΠ°Π»Π»βΡΡΠ΅Π΄Π°Β», ΡΠΏΠ΅ΡΠΈΠ°Π»ΠΈΡΡΠ° ΠΏΠΎ ΠΊΡΠΈΡΡΠ°Π»Π»ΠΎΠ³ΡΠ°ΡΠΎΠΌΠΈΠ½Π΅ΡΠ°Π»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΎΠΌΡ ΠΈΠ·ΡΡΠ΅Π½ΠΈΡ Π°Π»ΠΌΠ°Π·ΠΎΠ² ΠΈ ΠΈΡ
ΠΌΠΈΠ½Π΅ΡΠ°Π»ΠΎΠ²-ΡΠΏΡΡΠ½ΠΈΠΊΠΎΠ², ΡΡΠΏΠ΅ΡΠ½ΠΎΠ³ΠΎ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°ΡΠ΅Π»Ρ ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΠΎΠ³ΠΎ ΠΌΠΈΠ½Π΅ΡΠ°Π»ΠΎΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ Π½Π° ΠΊΠ°ΠΌΡΠ°ΡΡΠΊΠΈΡ
Π²ΡΠ»ΠΊΠ°Π½Π°Ρ
, ΠΎΠ΄Π½ΠΎΠ³ΠΎ ΠΈΠ· ΡΠΎΠ·Π΄Π°ΡΠ΅Π»Π΅ΠΉ Β«Π±ΡΠΊΠ²Π°Π»ΡΠ½ΠΎ Π½Π° ΠΏΡΡΡΠΎΠΌ ΠΌΠ΅ΡΡΠ΅Β» Π²ΡΡΠΎΠΊΠΎΡΠ΅Ρ
Π½ΠΎΠ»ΠΎΠ³ΠΈΡΠ½ΠΎΠ³ΠΎ ΠΏΡΠ΅Π΄ΠΏΡΠΈΡΡΠΈΡ ΠΏΠΎ ΠΏΡΠΎΠΈΠ·Π²ΠΎΠ΄ΡΡΠ²Ρ ΡΠ΅Ρ
Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
Π°Π»ΠΌΠ°Π·ΠΎΠ²
Π£Π½ΠΈΠ²Π΅ΡΡΠ°Π»ΡΠ½ΡΠΉ Π³ΠΈΡΠΎΠΈΠ½ΠΊΠ»ΠΈΠ½ΠΎΠΌΠ΅ΡΡ Π½Π° Π±Π°Π·Π΅ Π΅Π΄ΠΈΠ½ΡΡΠ²Π΅Π½Π½ΠΎΠ³ΠΎ ΠΎΠ΄Π½ΠΎΠΎΡΠ½ΠΎΠ³ΠΎ Π΄Π°ΡΡΠΈΠΊΠ° ΡΠ³Π»ΠΎΠ²ΠΎΠΉ ΡΠΊΠΎΡΠΎΡΡΠΈ
Introduction. Currently, the versatility and reliability of gyroscopic inclinometers (GI), more than accuracy, determine their configuration and design. Imperative conditions for versatility include a diameter of 42β¦44.5 mm and a combination of point and continuous survey modes. Reliability is primarily determined by the robustness of the main elements. The fundamental parameter is adaptability to the trajectory, in other words, equal accuracy in the operating range of zenith angles, which determines the choice of orientation of the angular velocity sensors (ARS) with incomplete (< 3) number of their axis. Presently, biaxial dynamically tuned gyroscopes (DNG) are widely used due to their dimension and accuracy criteria; however, their elastic suspension gradually degrades as a result of frequent sidetracking operations (from previously drilled ones) accompanied by high-intensity impacts.Aim. To develop an inexpensive versatile GI that maintains a balance between shock resistance and accuracy (com[1]parable to fiber-optic ARS) based on a single-axis vibrating ring gyroscope (VRG) with an induction-type resonator made using MEMS technology.Materials and methods. The method of multi-position compassing with a single uniaxial ARS was implemented by transition from simultaneous biaxial measurements to uniaxial measurements in five successive positions of the frame (through 90Β°) along the toolface angle. Experimental data on the drifts of the selected VRG allow statistical methods to be used to construct an Allan-variance plot to confirm that the proposed method does not increase the total compassing time compared to the basic one. The continuous mode of such a GI, studied by solving differential equations, requires holding the input axis of the ARS near the apsidal plane using the same rotating frame.Results. The obtained ratios confirm that the performance characteristics of a GI with a uniaxial ARS approximately correspond to the conventional biaxial scheme. These conclusions were also confirmed by the mathematical modeling of a survey of a typical oil and gas well.Conclusion. The described GI containing a single ARS with indirect stabilization of the input axis is the result of a consistent development of the approach to the use of incomplete informationΠΠ²Π΅Π΄Π΅Π½ΠΈΠ΅. Π‘Π΅Π³ΠΎΠ΄Π½Ρ ΡΠ½ΠΈΠ²Π΅ΡΡΠ°Π»ΡΠ½ΠΎΡΡΡ ΠΈ Π½Π°Π΄Π΅ΠΆΠ½ΠΎΡΡΡ Π³ΠΈΡΠΎΡΠΊΠΎΠΏΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈΠ½ΠΊΠ»ΠΈΠ½ΠΎΠΌΠ΅ΡΡΠΎΠ² (ΠΠ) Π±ΠΎΠ»Π΅Π΅, ΡΠ΅ΠΌ ΡΠΎΡΠ½ΠΎΡΡΡ, ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΡΡ ΠΈΡ
ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠ°ΡΠΈΡ ΠΈ ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠ²Π½ΡΠΉ ΠΎΠ±Π»ΠΈΠΊ. ΠΠΌΠΏΠ΅ΡΠ°ΡΠΈΠ²Π½ΡΠ΅ ΡΡΠ»ΠΎΠ²ΠΈΡ ΡΠ½ΠΈΠ²Π΅ΡΡΠ°Π»ΡΠ½ΠΎΡΡΠΈ: Π΄ΠΈΠ°ΠΌΠ΅ΡΡ 42...44.5 ΠΌΠΌ ΠΈ ΡΠΎΠ²ΠΌΠ΅ΡΠ΅Π½ΠΈΠ΅ ΡΡΠ½ΠΊΡΠΈΠΉ ΡΡΠ΅ΠΌΠΊΠΈ ΡΠΎΡΠ΅ΡΠ½ΠΎΠΉ ΠΈ Π½Π΅ΠΏΡΠ΅ΡΡΠ²Π½ΠΎΠΉ; Π° Π±Π΅Π·ΠΎΡΠΊΠ°Π·Π½ΠΎΡΡΡ ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΠ΅ΡΡΡ, ΠΏΡΠ΅ΠΆΠ΄Π΅ Π²ΡΠ΅Π³ΠΎ, ΡΠΎΠ±Π°ΡΡΠ½ΠΎΡΡΡΡ ΠΎΡΠ½ΠΎΠ²Π½ΡΡ
ΡΠ»Π΅ΠΌΠ΅Π½ΡΠΎΠ². ΠΡΠΈΠ½ΡΠΈΠΏΠΈΠ°Π»ΡΠ½Π° "Π°Π΄Π°ΠΏΡΠΈΠ²Π½ΠΎΡΡΡ" ΠΊ ΡΡΠ°Π΅ΠΊΡΠΎΡΠΈΠΈ β "ΡΠ°Π²Π½ΠΎΡΠΎΡΠ½ΠΎΡΡΡ" Π² ΡΠ°Π±ΠΎΡΠ΅ΠΌ Π΄ΠΈΠ°ΠΏΠ°Π·ΠΎΠ½Π΅ Π·Π΅Π½ΠΈΡΠ½ΡΡ
ΡΠ³Π»ΠΎΠ², ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΡΡΠ΅ΠΌ Π²ΡΠ±ΠΎΡ ΠΎΡΠΈΠ΅Π½ΡΠ°ΡΠΈΠΈ Π΄Π°ΡΡΠΈΠΊΠΎΠ² ΡΠ³Π»ΠΎΠ²ΠΎΠΉ ΡΠΊΠΎΡΠΎΡΡΠΈ (ΠΠ£Π‘) ΠΏΡΠΈ ΠΈΡ
Π½Π΅ΠΏΠΎΠ»Π½ΠΎΠΌ (< 3) ΡΠΈΡΠ»Π΅. ΠΠΎ ΡΠΎΠ²ΠΎΠΊΡΠΏΠ½ΠΎΡΡΠΈ ΠΊΡΠΈΡΠ΅ΡΠΈΠ΅Π² Π³Π°Π±Π°ΡΠΈΡΠΎΠ² ΠΈ ΡΠΎΡΠ½ΠΎΡΡΠΈ ΡΠ΅Π³ΠΎΠ΄Π½Ρ ΠΏΡΠ΅ΠΈΠΌΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎ ΠΏΡΠΈΠΌΠ΅Π½ΡΡΡΡΡ Π΄Π²ΡΡ
ΠΎΡΠ½ΡΠ΅ Π΄ΠΈΠ½Π°ΠΌΠΈΡΠ΅ΡΠΊΠΈ Π½Π°ΡΡΡΠ°ΠΈΠ²Π°Π΅ΠΌΡΠ΅ Π³ΠΈΡΠΎΡΠΊΠΎΠΏΡ, Π½ΠΎ ΠΈΡ
ΡΠΏΡΡΠ³ΠΈΠΉ ΠΏΠΎΠ΄Π²Π΅Ρ ΠΏΡΠΈ ΡΠ°ΡΡΡΡ
ΠΎΠΏΠ΅ΡΠ°ΡΠΈΡΡ
"Π·Π°ΡΠ΅Π·ΠΊΠΈ Π±ΠΎΠΊΠΎΠ²ΡΡ
ΡΡΠ²ΠΎΠ»ΠΎΠ²" (ΠΈΠ· ΡΠ°Π½Π΅Π΅ ΠΏΡΠΎΠ±ΡΡΠ΅Π½Π½ΡΡ
), ΡΠΎΠΏΡΠΎΠ²ΠΎΠΆΠ΄Π°Π΅ΠΌΡΡ
ΡΠ΄Π°ΡΠ°ΠΌΠΈ Π±ΠΎΠ»ΡΡΠΎΠΉ ΠΈΠ½ΡΠ΅Π½ΡΠΈΠ²Π½ΠΎΡΡΠΈ, ΠΏΠΎΡΡΠ΅ΠΏΠ΅Π½Π½ΠΎ Π΄Π΅Π³ΡΠ°Π΄ΠΈΡΡΠ΅Ρ.Π¦Π΅Π»Ρ ΡΠ°Π±ΠΎΡΡ. Π‘ΠΎΠ·Π΄Π°ΡΡ Π½Π΅Π΄ΠΎΡΠΎΠ³ΠΎΠΉ ΡΠ½ΠΈΠ²Π΅ΡΡΠ°Π»ΡΠ½ΡΠΉ ΠΠ, ΡΠΎΡ
ΡΠ°Π½ΡΡΡΠΈΠΉ ΠΊΠΎΠΌΠΏΡΠΎΠΌΠΈΡΡ ΡΠ΄Π°ΡΠΎΡΡΠΎΠΉΠΊΠΎΡΡΠΈ ΠΈ ΡΠΎΡΠ½ΠΎΡΡΠΈ (ΡΠΎΠΏΠΎΡΡΠ°Π²ΠΈΠΌΠΎΠΉ Ρ Π²ΠΎΠ»ΠΎΠΊΠΎΠ½Π½ΠΎ-ΠΎΠΏΡΠΈΡΠ΅ΡΠΊΠΈΠΌΠΈ ΠΠ£Π‘), Π½Π° Π±Π°Π·Π΅ ΠΎΠ΄Π½ΠΎΠΎΡΠ½ΠΎΠ³ΠΎ ΠΊΠΎΠ»ΡΡΠ΅Π²ΠΎΠ³ΠΎ Π²ΠΈΠ±ΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ Π³ΠΈΡΠΎΡΠΊΠΎΠΏΠ° (ΠΠΠ) Ρ ΡΠ΅Π·ΠΎΠ½Π°ΡΠΎΡΠΎΠΌ ΠΈΠ½Π΄ΡΠΊΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΡΠΈΠΏΠ°, Π²ΡΠΏΠΎΠ»Π½Π΅Π½Π½ΡΠΌ ΠΏΠΎ MEMS-ΡΠ΅Ρ
Π½ΠΎΠ»ΠΎΠ³ΠΈΠΈ.ΠΠ°ΡΠ΅ΡΠΈΠ°Π»Ρ ΠΈ ΠΌΠ΅ΡΠΎΠ΄Ρ. ΠΠ΅ΡΠΎΠ΄ ΠΌΠ½ΠΎΠ³ΠΎΠΏΠΎΠ·ΠΈΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΠΊΠΎΠΌΠΏΠ°ΡΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΏΡΠΈ Π΅Π΄ΠΈΠ½ΡΡΠ²Π΅Π½Π½ΠΎΠΌ ΠΎΠ΄Π½ΠΎΠΎΡΠ½ΠΎΠΌ ΠΠ£Π‘ ΡΠ΅Π°Π»ΠΈΠ·ΡΠ΅ΡΡΡ ΠΏΠ΅ΡΠ΅Ρ
ΠΎΠ΄ΠΎΠΌ ΠΎΡ ΠΎΠ΄Π½ΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΡΡ
Π΄Π²ΡΡ
ΠΎΡΠ½ΡΡ
ΠΈΠ·ΠΌΠ΅ΡΠ΅Π½ΠΈΠΉ ΠΊ ΠΎΠ΄Π½ΠΎΠΎΡΠ½ΡΠΌ β Π² ΠΏΡΡΠΈ ΠΏΠΎΡΠ»Π΅Π΄ΠΎΠ²Π°ΡΠ΅Π»ΡΠ½ΡΡ
(ΡΠ΅ΡΠ΅Π· 90Β°) ΠΏΠΎΠ»ΠΎΠΆΠ΅Π½ΠΈΡΡ
ΡΠ°ΠΌΠΊΠΈ ΠΏΠΎ ΡΠ³Π»Ρ ΠΎΡΠΊΠ»ΠΎΠ½ΠΈΡΠ΅Π»Ρ. ΠΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΡΠ΅ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»Ρ ΠΎ Π΄ΡΠ΅ΠΉΡΠ°Ρ
Π²ΡΠ±ΡΠ°Π½Π½ΠΎΠ³ΠΎ ΠΠΠ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡ ΡΡΠ°ΡΠΈΡΡΠΈΡΠ΅ΡΠΊΠΈΠΌΠΈ ΠΌΠ΅ΡΠΎΠ΄Π°ΠΌΠΈ ΠΏΠΎΡΡΡΠΎΠΈΡΡ Π²Π°ΡΠΈΠ°ΡΠΈΡ ΠΠ»Π»Π°Π½Π°, ΠΊΠΎΡΠΎΡΠ°Ρ ΠΏΠΎΠ΄ΡΠ²Π΅ΡΠΆΠ΄Π°Π΅Ρ, ΡΡΠΎ ΠΏΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½Π½Π°Ρ ΠΌΠ΅ΡΠΎΠ΄ΠΈΠΊΠ° ΠΏΠΎ ΡΡΠ°Π²Π½Π΅Π½ΠΈΡ Ρ Π±Π°Π·ΠΎΠ²ΠΎΠΉ Π½Π΅ ΡΠ²Π΅Π»ΠΈΡΠΈΠ²Π°Π΅Ρ ΠΎΠ±ΡΠ΅Π³ΠΎ Π²ΡΠ΅ΠΌΠ΅Π½ΠΈ ΠΊΠΎΠΌΠΏΠ°ΡΠΈΡΠΎΠ²Π°Π½ΠΈΡ. ΠΠ΅ΠΏΡΠ΅ΡΡΠ²Π½ΡΠΉ ΡΠ΅ΠΆΠΈΠΌ ΡΠ°ΠΊΠΎΠ³ΠΎ ΠΠ, ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Π½ΡΠΉ ΠΌΠ΅ΡΠΎΠ΄Π°ΠΌΠΈ ΡΠ΅ΡΠ΅Π½ΠΈΡ Π΄ΠΈΡΡΠ΅ΡΠ΅Π½ΡΠΈΠ°Π»ΡΠ½ΡΡ
ΡΡΠ°Π²Π½Π΅Π½ΠΈΠΉ, ΡΡΠ΅Π±ΡΠ΅Ρ ΡΠ΄Π΅ΡΠΆΠ°Π½ΠΈΡ Π²Ρ
ΠΎΠ΄Π½ΠΎΠΉ ΠΎΡΠΈ ΠΠ£Π‘ ΠΎΠΊΠΎΠ»ΠΎ Π°ΠΏΡΠΈΠ΄Π°Π»ΡΠ½ΠΎΠΉ ΠΏΠ»ΠΎΡΠΊΠΎΡΡΠΈ Ρ ΠΏΠΎΠΌΠΎΡΡΡ ΡΠΎΠΉ ΠΆΠ΅ ΠΏΠΎΠ²ΠΎΡΠΎΡΠ½ΠΎΠΉ ΡΠ°ΠΌΠΊΠΈ.Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ. ΠΠΎΠ»ΡΡΠ΅Π½Π½ΡΠ΅ ΡΠΎΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΡ ΠΏΠΎΠ΄ΡΠ²Π΅ΡΠΆΠ΄Π°ΡΡ: ΡΠ°ΠΊΡΠΈΠΊΠΎ-ΡΠ΅Ρ
Π½ΠΈΡΠ΅ΡΠΊΠΈΠ΅ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠΈ ΠΠ Ρ ΠΎΠ΄Π½ΠΎΠΎΡΠ½ΡΠΌ ΠΠ£Π‘ ΠΏΡΠΈΠΌΠ΅ΡΠ½ΠΎ ΡΠΎΠΎΡΠ²Π΅ΡΡΡΠ²ΡΡΡ ΡΡΠ°Π΄ΠΈΡΠΈΠΎΠ½Π½ΠΎΠΉ Π΄Π²ΡΡ
ΠΎΡΠ½ΠΎΠΉ ΡΡ
Π΅ΠΌΠ΅. Π ΡΠ΅ΠΌ ΠΆΠ΅ Π²ΡΠ²ΠΎΠ΄Π°ΠΌ ΠΏΡΠΈΠ²ΠΎΠ΄ΡΡ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΌΠ°ΡΠ΅ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΡΠ΅ΠΌΠΊΠΈ ΡΠΈΠΏΠΎΠ²ΠΎΠ³ΠΎ Π½Π΅ΡΡΠ΅Π³Π°Π·ΠΎΠ²ΠΎΠ³ΠΎ ΡΡΠ²ΠΎΠ»Π°.ΠΠ°ΠΊΠ»ΡΡΠ΅Π½ΠΈΠ΅. ΠΠΏΠΈΡΠ°Π½ΡΠΉ ΠΠ, ΡΠΎΠ΄Π΅ΡΠΆΠ°ΡΠΈΠΉ Π΅Π΄ΠΈΠ½ΡΡΠ²Π΅Π½Π½ΡΠΉ ΠΠ£Π‘ Ρ ΠΊΠΎΡΠ²Π΅Π½Π½ΠΎΠΉ ΡΡΠ°Π±ΠΈΠ»ΠΈΠ·Π°ΡΠΈΠ΅ΠΉ Π²Ρ
ΠΎΠ΄Π½ΠΎΠΉ ΠΎΡΠΈ, β ΠΈΡΠΎΠ³ ΠΏΠΎΡΠ»Π΅Π΄ΠΎΠ²Π°ΡΠ΅Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΠΏΠΎΠ΄Ρ
ΠΎΠ΄Π° ΠΊ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΡ Π½Π΅ΠΏΠΎΠ»Π½ΠΎΠΉ ΠΈΠ½ΡΠΎΡΠΌΠ°ΡΠΈ
ΠΡΠ΅ΡΡΡΡΠΊΠΈΠ΅ Π°Π»ΠΌΠ°Π·Ρ: ΠΊΠΎΠ½ΡΡΠΈΡΡΡΠΈΡ, ΠΏΠΎΠ²Π΅ΡΡ Π½ΠΎΡΡΠ½ΠΎ-ΠΏΠ»ΡΠ½ΠΎΡΠ½ΡΠ΅ ΠΌΠΈΠΊΡΠΎΠΌΠΈΠ½Π΅ΡΠ°Π»ΠΈΠ·Π°ΡΠΈΠΈ, Π³Π΅Π½Π΅Π·ΠΈΡ
Diamonds from the Ichetyu deposit of disputable genesis have been studied using X-ray diffraction analysis, scanning electron microscopy, cathode-, photo- and X-ray luminescence; spectroscopy of Raman scattering and IR absorption, LA-ICP-MS, isotope mass spectrometry. The crystal morphology of diamonds has been analyzed, the parameters of the forms of their mantle dissolution, the degree and nature of plastic and impact deformations have been determined. Features of the internal structure, luminescent-spectroscopic properties were revealed. The bulk concentration of structural nitrogen, the degree of aggregation of point nitrogen defects, and the temperature of mantle annealing are estimated. The composition of microelements and carbon isotopy were determined. The mineral-phase composition of films on the surface of diamonds has been studied. A conclusion was made about the tuffizite-fluidisite genetic type of the Ichetyu depositΠΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Ρ Π°Π»ΠΌΠ°Π·Ρ ΠΈΠ· ΠΡΠ΅ΡΡΡΡΠΊΠΎΠ³ΠΎ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΡ ΡΠΏΠΎΡΠ½ΠΎΠ³ΠΎ Π³Π΅Π½Π΅Π·ΠΈΡΠ° Ρ ΠΏΡΠΈΠΌΠ΅Π½Π΅Π½ΠΈΠ΅ΠΌ ΠΌΠ΅ΡΠΎΠ΄ΠΎΠ² ΡΠ΅Π½ΡΠ³Π΅Π½ΠΎΡΡΡΡΠΊΡΡΡΠ½ΠΎΠ³ΠΎ Π°Π½Π°Π»ΠΈΠ·Π°, ΡΠΊΠ°Π½ΠΈΡΡΡΡΠ΅ΠΉ ΡΠ»Π΅ΠΊΡΡΠΎΠ½Π½ΠΎΠΉ ΠΌΠΈΠΊΡΠΎΡΠΊΠΎΠΏΠΈΠΈ, ΠΊΠ°ΡΠΎΠ΄ΠΎ-, ΡΠΎΡΠΎ- ΠΈ ΡΠ΅Π½ΡΠ³Π΅Π½ΠΎΠ»ΡΠΌΠΈΠ½Π΅ΡΡΠ΅Π½ΡΠΈΠΈ; ΡΠΏΠ΅ΠΊΡΡΠΎΡΠΊΠΎΠΏΠΈΠΈ ΠΊΠΎΠΌΠ±ΠΈΠ½Π°ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΡΠ°ΡΡΠ΅ΡΠ½ΠΈΡ ΠΈ ΠΠ-ΠΏΠΎΠ³Π»ΠΎΡΠ΅Π½ΠΈΡ, ΠΠ-ΠΠ‘Π-ΠΠ‘, ΠΈΠ·ΠΎΡΠΎΠΏΠ½ΠΎΠΉ ΠΌΠ°ΡΡΡΠΏΠ΅ΠΊΡΡΠΎΠΌΠ΅ΡΡΠΈΠΈ. ΠΡΠΎΠ°Π½Π°Π»ΠΈΠ·ΠΈΡΠΎΠ²Π°Π½Π° ΠΊΡΠΈΡΡΠ°Π»Π»ΠΎΠΌΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΡ Π°Π»ΠΌΠ°Π·ΠΎΠ², ΠΎΠΏΡΠ΅Π΄Π΅Π»Π΅Π½Ρ ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΡ ΡΠΎΡΠΌ ΠΈΡ
ΠΌΠ°Π½ΡΠΈΠΉΠ½ΠΎΠ³ΠΎ ΡΠ°ΡΡΠ²ΠΎΡΠ΅Π½ΠΈΡ, ΡΡΠ΅ΠΏΠ΅Π½Ρ ΠΈ Ρ
Π°ΡΠ°ΠΊΡΠ΅Ρ ΠΏΠ»Π°ΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ ΡΠ΄Π°ΡΠ½ΡΡ
Π΄Π΅ΡΠΎΡΠΌΠ°ΡΠΈΠΉ. ΠΡΡΠ²Π»Π΅Π½Ρ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ Π²Π½ΡΡΡΠ΅Π½Π½Π΅Π³ΠΎ ΡΡΡΠΎΠ΅Π½ΠΈΡ, Π»ΡΠΌΠΈΠ½Π΅ΡΡΠ΅Π½ΡΠ½ΠΎ-ΡΠΏΠ΅ΠΊΡΡΠΎΡΠΊΠΎΠΏΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΡΠ²ΠΎΠΉΡΡΠ²Π°. ΠΡΠ΅Π½Π΅Π½Ρ Π²Π°Π»ΠΎΠ²Π°Ρ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΡ ΡΡΡΡΠΊΡΡΡΠ½ΠΎΠ³ΠΎ Π°Π·ΠΎΡΠ°, ΡΡΠ΅ΠΏΠ΅Π½Ρ Π°Π³ΡΠ΅Π³Π°ΡΠΈΠΈ ΡΠΎΡΠ΅ΡΠ½ΡΡ
Π°Π·ΠΎΡΠ½ΡΡ
Π΄Π΅ΡΠ΅ΠΊΡΠΎΠ², ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΠ° ΠΌΠ°Π½ΡΠΈΠΉΠ½ΠΎΠ³ΠΎ ΠΎΡΠΆΠΈΠ³Π°. ΠΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ ΡΠΎΡΡΠ°Π² ΠΌΠΈΠΊΡΠΎΡΠ»Π΅ΠΌΠ΅Π½ΡΠΎΠ² ΠΈ ΠΈΠ·ΠΎΡΠΎΠΏΠΈΡ ΡΠ³Π»Π΅ΡΠΎΠ΄Π°. ΠΠ·ΡΡΠ΅Π½ ΠΌΠΈΠ½Π΅ΡΠ°Π»ΡΠ½ΠΎ-ΡΠ°Π·ΠΎΠ²ΡΠΉ ΡΠΎΡΡΠ°Π² ΠΏΠ»ΡΠ½ΠΎΠΊ Π½Π° ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠΈ Π°Π»ΠΌΠ°Π·ΠΎΠ². Π‘Π΄Π΅Π»Π°Π½ Π²ΡΠ²ΠΎΠ΄ ΠΎ ΡΡΡΡΠΈΠ·ΠΈΡΠΎ-ΡΠ»ΡΠΈΠ΄ΠΈΠ·Π°ΡΠ½ΠΎΠΌ Π³Π΅Π½Π΅ΡΠΈΡΠ΅ΡΠΊΠΎΠΌ ΡΠΈΠΏΠ΅ ΠΡΠ΅ΡΡΡΡΠΊΠΎΠ³ΠΎ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈ
ΠΠΎΡΠ΅Π½Π½ΠΎΠ΅ Π·ΠΎΠ»ΠΎΡΠΎΠΏΡΠΎΡΠ²Π»Π΅Π½ΠΈΠ΅ Π½Π° Β«Π’Π΅ΡΡΠΈΡΠΎΡΠΈΠΈΒ» ΠΠ»Π΅Π³Π° ΠΡΠ²Π°Π΅Π²Π° (ΡΠ΅Π²Π΅Ρ Π§ΡΠΊΠΎΡΡΠΊΠΎΠ³ΠΎ Π½Π°Π³ΠΎΡΡΡ)
A sample of a gold-bearing quartz vein from the Upper-Ichuveem ore occurrence, discovered in the Triassic terrigenous complex in the north of the Chukotka Upland, the Oleg Kuvaev's βTerritoryβ, had been comprehensively studied. The gross gold grade was estimated at 3β4 g / t. The vein includes quartz, native gold, sulfide-gold-silver solid solutions, alumoseladonite, aluminium-sulfate-phosphates Fe-Pb-Mg-Ca compound, apatite, pyrite, iron-titanium oxides, litharge, native phases composed of Fe (Ni), Ag-Pb-Bi, Fe-Al-PS-As, multicomponent ocher of hypergene origin. Native gold ranges from medium to fine. The vein contains particles of non-crystalline organic matter, which is close in composition of organic groups to polysaccharides. It is possible that the carbon particles found in the gold-quartz vein are of an abiogenic nature and can be compared with abiogenic condensed organelles in the products of modern volcanism. The data obtained make it possible to attribute the Upper Ichuveem gold ore occurrence to a low-sulfide gold-quartz formation, but with additional signs of gold-silver and polymetallic formations, which can be regarded as a favorable prerequisite for prospecting and exploration in Oleg Kuvaev's Β«TerritoryΒ» not only of gold-placer deposits, but also of lode gold deposits.ΠΠΎΠΌΠΏΠ»Π΅ΠΊΡΠ½ΠΎ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ ΠΎΠ±ΡΠ°Π·Π΅Ρ Π·ΠΎΠ»ΠΎΡΠΎΠ½ΠΎΡΠ½ΠΎΠΉ ΠΊΠ²Π°ΡΡΠ΅Π²ΠΎΠΉ ΠΆΠΈΠ»Ρ Ρ ΠΠ΅ΡΡ
Π½Π΅-ΠΡΡΠ²Π΅Π΅ΠΌΡΠΊΠΎΠ³ΠΎ ΡΡΠ΄ΠΎΠΏΡΠΎΡΠ²Π»Π΅Π½ΠΈΡ, Π²ΡΡΠ²Π»Π΅Π½Π½ΠΎΠ³ΠΎ Π² ΡΡΠΈΠ°ΡΠΎΠ²ΠΎΠΌ ΡΠ΅ΡΡΠΈΠ³Π΅Π½Π½ΠΎΠΌ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠ΅ Π½Π° ΡΠ΅Π²Π΅ΡΠ΅ Π§ΡΠΊΠΎΡΡΠΊΠΎΠ³ΠΎ Π½Π°Π³ΠΎΡΡΡ β Β«Π’Π΅ΡΡΠΈΡΠΎΡΠΈΠΈΒ» ΠΠ»Π΅Π³Π° ΠΡΠ²Π°Π΅Π²Π°. ΠΠ°Π»ΠΎΠ²ΠΎΠ΅ ΡΠΎΠ΄Π΅ΡΠΆΠ°Π½ΠΈΠ΅ Π·ΠΎΠ»ΠΎΡΠ° ΠΎΡΠ΅Π½ΠΈΠ²Π°Π΅ΡΡΡ Π² 3β4 Π³/Ρ. Π ΡΠΎΡΡΠ°Π² ΠΆΠΈΠ»Ρ Π²Ρ
ΠΎΠ΄ΡΡ ΠΊΠ²Π°ΡΡ, ΡΠ°ΠΌΠΎΡΠΎΠ΄Π½ΠΎΠ΅ Π·ΠΎΠ»ΠΎΡΠΎ, ΡΡΠ»ΡΡΠΈΠ΄Π½ΠΎ-Π·ΠΎΠ»ΠΎΡΠΎ-ΡΠ΅ΡΠ΅Π±ΡΡΠ½ΡΠ΅ ΡΠ²Π΅ΡΠ΄ΡΠ΅ ΡΠ°ΡΡΠ²ΠΎΡΡ, Π°Π»ΡΠΌΠΎΡΠ΅Π»Π°Π΄ΠΎΠ½ΠΈΡ, Π°Π»ΡΠΌΠΎ-ΡΡΠ»ΡΡΠ°ΡΠΎ-ΡΠΎΡΡΠ°ΡΡ Fe-Pb-Mg-Ca ΡΠΎΡΡΠ°Π²Π°, Π°ΠΏΠ°ΡΠΈΡ, ΠΏΠΈΡΠΈΡ, ΠΆΠ΅Π»Π΅Π·ΠΎ-ΡΠΈΡΠ°Π½ΠΎΠ²ΡΠ΅ ΠΎΠΊΡΠΈΠ΄Ρ, Π³Π»ΡΡ, ΡΠ°ΠΌΠΎΡΠΎΠ΄Π½ΡΠ΅ ΡΠ°Π·Ρ ΡΠΎΡΡΠ°Π²Π° Fe (Ni), Ag-Pb-Bi, Fe-Al-P-S-As, ΠΏΠΎΠ»ΠΈΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½ΡΠ½ΡΠ΅ ΠΎΡ
ΡΡ Π³ΠΈΠΏΠ΅ΡΠ³Π΅Π½Π½ΠΎΠ³ΠΎ ΠΏΡΠΎΠΈΡΡ
ΠΎΠΆΠ΄Π΅Π½ΠΈΡ. Π‘Π°ΠΌΠΎΡΠΎΠ΄Π½ΠΎΠ΅ Π·ΠΎΠ»ΠΎΡΠΎ ΠΊΠΎΠ»Π΅Π±Π»Π΅ΡΡΡ ΠΎΡ ΡΡΠ΅Π΄Π½Π΅- Π΄ΠΎ Π²ΡΡΠΎΠΊΠΎΠΏΡΠΎΠ±Π½ΠΎΠ³ΠΎ. Π ΡΠΎΡΡΠ°Π²Π΅ ΠΆΠΈΠ»Ρ ΠΎΠ±Π½Π°ΡΡΠΆΠ΅Π½Ρ ΡΠ°ΡΡΠΈΡΡ Π½Π΅ΠΊΡΠΈΡΡΠ°Π»Π»ΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ Π²Π΅ΡΠ΅ΡΡΠ²Π°, Π±Π»ΠΈΠ·ΠΊΠΎΠ³ΠΎ ΠΏΠΎ ΡΠΎΡΡΠ°Π²Ρ ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
Π³ΡΡΠΏΠΏ ΠΊ ΠΏΠΎΠ»ΠΈΡΠ°Ρ
Π°ΡΠΈΠ΄Π°ΠΌ. ΠΠ΅ ΠΈΡΠΊΠ»ΡΡΠ΅Π½ΠΎ, ΡΡΠΎ Π²ΡΡΠ²Π»Π΅Π½Π½ΡΠ΅ Π² Π·ΠΎΠ»ΠΎΡΠΎΠΊΠ²Π°ΡΡΠ΅Π²ΠΎΠΉ ΠΆΠΈΠ»Π΅ ΡΠ³Π»Π΅ΡΠΎΠ΄Π½ΡΠ΅ ΡΠ°ΡΡΠΈΡΡ ΠΈΠΌΠ΅ΡΡ Π°Π±ΠΈΠΎΠ³Π΅Π½Π½ΡΡ ΠΏΡΠΈΡΠΎΠ΄Ρ ΠΈ ΠΌΠΎΠ³ΡΡ Π±ΡΡΡ ΡΠΎΠΏΠΎΡΡΠ°Π²Π»Π΅Π½Ρ Ρ Π°Π±ΠΈΠΎΠ³Π΅Π½Π½ΡΠΌΠΈ ΠΊΠΎΠ½Π΄Π΅Π½ΡΠΈΡΠΎΠ²Π°Π½Π½ΡΠΌΠΈ ΠΎΡΠ³Π°Π½ΠΎΠΈΠ΄Π°ΠΌΠΈ Π² ΠΏΡΠΎΠ΄ΡΠΊΡΠ°Ρ
ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΠΎΠ³ΠΎ Π²ΡΠ»ΠΊΠ°Π½ΠΈΠ·ΠΌΠ°. ΠΠΎΠ»ΡΡΠ΅Π½Π½ΡΠ΅ Π΄Π°Π½Π½ΡΠ΅ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡ ΠΎΡΠ½Π΅ΡΡΠΈ ΠΠ΅ΡΡ
Π½Π΅-ΠΡΡΠ²Π΅Π΅ΠΌΡΠΊΠΎΠ΅ Π·ΠΎΠ»ΠΎΡΠΎΡΡΠ΄Π½ΠΎΠ΅ ΠΏΡΠΎΡΠ²Π»Π΅Π½ΠΈΠ΅ ΠΊ ΠΌΠ°Π»ΠΎΡΡΠ»ΡΡΠΈΠ΄Π½ΠΎΠΉ Π·ΠΎΠ»ΠΎΡΠΎΠΊΠ²Π°ΡΡΠ΅Π²ΠΎΠΉ ΡΠΎΡΠΌΠ°ΡΠΈΠΈ, Π½ΠΎ Ρ Π΄ΠΎΠΏΠΎΠ»Π½ΠΈΡΠ΅Π»ΡΠ½ΡΠΌΠΈ ΠΏΡΠΈΠ·Π½Π°ΠΊΠ°ΠΌΠΈ Π·ΠΎΠ»ΠΎΡΠΎΡΠ΅ΡΠ΅Π±ΡΡΠ½ΠΎΠΉ ΠΈ ΠΏΠΎΠ»ΠΈΠΌΠ΅ΡΠ°Π»Π»ΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠΎΡΠΌΠ°ΡΠΈΠΉ, ΡΡΠΎ ΠΌΠΎΠΆΠ½ΠΎ ΡΠ°ΡΡΠ΅Π½ΠΈΠ²Π°ΡΡ ΠΊΠ°ΠΊ Π±Π»Π°Π³ΠΎΠΏΡΠΈΡΡΠ½ΡΡ ΠΏΡΠ΅Π΄ΠΏΠΎΡΡΠ»ΠΊΡ Π΄Π»Ρ ΠΏΠΎΠΈΡΠΊΠΎΠ² ΠΈ ΡΠ°Π·Π²Π΅Π΄ΠΎΠΊ Π½Π° Β«Π’Π΅ΡΡΠΈΡΠΎΡΠΈΠΈΒ» ΠΠ»Π΅Π³Π° ΠΡΠ²Π°Π΅Π²Π° Π½Π΅ ΡΠΎΠ»ΡΠΊΠΎ Π·ΠΎΠ»ΠΎΡΠΎ-ΡΠΎΡΡΡΠΏΠ½ΡΡ
, Π½ΠΎ ΠΈ Π·ΠΎΠ»ΠΎΡΠΎ-ΠΊΠΎΡΠ΅Π½Π½ΡΡ
ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ
ΠΠΎΡΡΠ½ΡΠ΅ ΠΎΡΡΠ°Π½ΠΊΠΈ ΠΈΠ· ΠΌΠΎΠ³ΠΈΠ»ΡΠ½ΠΈΠΊΠΎΠ² ΠΠ΅ΡΠΌΠΈ ΠΡΡΠ΅Π³ΠΎΠ΄ΡΠΊΠΎΠΉ (XIβXIV Π²Π².): ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΌΡΠ»ΡΡΠΈΠ΄ΠΈΡΡΠΈΠΏΠ»ΠΈΠ½Π°ΡΠ½ΡΡ Π½Π°ΡΡΠ½ΡΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ ΠΈ ΡΠΊΠΎΠ»ΠΎΠ³ΠΎ-ΠΈΡΡΠΎΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΡΠ΅ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠΈ
Using a wide range of modern mineralogical and physicochemical methods, a representative collection of human bones from seven burial grounds of the Vychegda Permians of the 11thβ14th centuries was studied. The microstructureof bones, their chemical and normative-mineral composition, the content of microelements, the nanoporosity of the organo-mineral composite, the composition and properties of bioanatite and bone collagen were analyzed. Fundamental differences in the properties of raw and so-called calcified bones are determined. Based on isotope data on bioapatite and collagen of raw bones, the climatic conditions for the existence of the Vychegda Permians and their diets were reconstructed.Π‘ ΠΏΡΠΈΠΌΠ΅Π½Π΅Π½ΠΈΠ΅ΠΌ ΡΠΈΡΠΎΠΊΠΎΠ³ΠΎ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠ° ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΡΡ
ΠΌΠΈΠ½Π΅ΡΠ°Π»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
, ΡΠΈΠ·ΠΈΠΊΠΎ-Ρ
ΠΈΠΌΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ ΠΈΠ·ΠΎΡΠΎΠΏΠ½ΡΡ
ΠΌΠ΅ΡΠΎΠ΄ΠΎΠ² ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Π° ΠΏΡΠ΅Π΄ΡΡΠ°Π²ΠΈΡΠ΅Π»ΡΠ½Π°Ρ ΠΊΠΎΠ»Π»Π΅ΠΊΡΠΈΡ ΡΠ΅Π»ΠΎΠ²Π΅ΡΠ΅ΡΠΊΠΈΡ
ΠΊΠΎΡΡΠ΅ΠΉ ΠΈΠ· ΡΠ΅ΠΌΠΈ ΠΌΠΎΠ³ΠΈΠ»ΡΠ½ΠΈΠΊΠΎΠ² Π²ΡΡΠ΅Π³ΠΎΠ΄ΡΠΊΠΈΡ
ΠΏΠ΅ΡΠΌΡΠ½ XIβXIV Π²Π². ΠΡΠΎΠ°Π½Π°Π»ΠΈΠ·ΠΈΡΠΎΠ²Π°Π½Ρ ΠΌΠΈΠΊΡΠΎΡΡΡΠΎΠ΅Π½ΠΈΠ΅ ΠΊΠΎΡΡΠ΅ΠΉ, ΠΈΡ
Ρ
ΠΈΠΌΠΈΡΠ΅ΡΠΊΠΈΠΉ ΠΈ Π½ΠΎΡΠΌΠ°ΡΠΈΠ²Π½ΠΎ-ΠΌΠΈΠ½Π΅ΡΠ°Π»ΡΠ½ΡΠΉ ΡΠΎΡΡΠ°Π², ΡΠΎΠ΄Π΅ΡΠΆΠ°Π½ΠΈΠ΅ ΠΌΠΈΠΊΡΠΎΡΠ»Π΅ΠΌΠ΅Π½ΡΠΎΠ², Π½Π°Π½ΠΎΠΏΠΎΡΠΈΡΡΠΎΡΡΡ ΠΎΡΠ³Π°Π½ΠΎ-ΠΌΠΈΠ½Π΅ΡΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΊΠΎΠΌΠΏΠΎΠ·ΠΈΡΠ°, ΡΠΎΡΡΠ°Π² ΠΈ ΡΠ²ΠΎΠΉΡΡΠ²Π° Π±ΠΈΠΎΠ°ΠΏΠ°ΡΠΈΡΠ° ΠΈ ΠΊΠΎΡΡΠ½ΠΎΠ³ΠΎ ΠΊΠΎΠ»Π»Π°Π³Π΅Π½Π°. ΠΠΏΡΠ΅Π΄Π΅Π»Π΅Π½Ρ ΠΏΡΠΈΠ½ΡΠΈΠΏΠΈΠ°Π»ΡΠ½ΡΠ΅ ΡΠ°Π·Π»ΠΈΡΠΈΡ Π² ΡΠ²ΠΎΠΉΡΡΠ²Π°Ρ
ΡΡΡΡΡ
ΠΈ ΡΠ°ΠΊ Π½Π°Π·ΡΠ²Π°Π΅ΠΌΡΡ
ΠΊΠ°Π»ΡΡΠΈΠ½ΠΈΡΠΎΠ²Π°Π½Π½ΡΡ
ΠΊΠΎΡΡΠ΅ΠΉ. ΠΠ° ΠΎΡΠ½ΠΎΠ²Π°Π½ΠΈΠΈ ΠΈΠ·ΠΎΡΠΎΠΏΠ½ΡΡ
Π΄Π°Π½Π½ΡΡ
ΠΏΠΎ Π±ΠΈΠΎΠ°ΠΏΠ°ΡΠΈΡΡ ΠΈ ΠΊΠΎΠ»Π»Π°Π³Π΅Π½Ρ ΡΡΡΡΡ
ΠΊΠΎΡΡΠ΅ΠΉ ΡΠ΅ΠΊΠΎΠ½ΡΡΡΡΠΈΡΠΎΠ²Π°Π½Ρ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΡΡΠ»ΠΎΠ²ΠΈΡ ΡΡΡΠ΅ΡΡΠ²ΠΎΠ²Π°Π½ΠΈΡ Π²ΡΡΠ΅Π³ΠΎΠ΄ΡΠΊΠΈΡ
ΠΏΠ΅ΡΠΌΡΠ½ ΠΈ ΡΠ°ΡΠΈΠΎΠ½Ρ ΠΈΡ
ΠΏΠΈΡΠ°Π½ΠΈ
Simulations of events for the LUX-ZEPLIN (LZ) dark matter experiment
The LUX-ZEPLIN dark matter search aims to achieve a sensitivity to the WIMP-nucleon spin-independent cross-section down to (1β2)Γ10β12 pb at a WIMP mass of 40 GeV/c2. This paper describes the simulations framework that, along with radioactivity measurements, was used to support this projection, and also to provide mock data for validating reconstruction and analysis software. Of particular note are the event generators, which allow us to model the background radiation, and the detector response physics used in the production of raw signals, which can be converted into digitized waveforms similar to data from the operational detector. Inclusion of the detector response allows us to process simulated data using the same analysis routines as developed to process the experimental data
Recommended from our members
Projected sensitivity of the LUX-ZEPLIN experiment to the 0Ξ½Ξ²Ξ² decay of Xe 136
The LUX-ZEPLIN (LZ) experiment will enable a neutrinoless double Ξ² decay search in parallel to the main science goal of discovering dark matter particle interactions. We report the expected LZ sensitivity to Xe136 neutrinoless double Ξ² decay, taking advantage of the significant (>600 kg) Xe136 mass contained within the active volume of LZ without isotopic enrichment. After 1000 live-days, the median exclusion sensitivity to the half-life of Xe136 is projected to be 1.06Γ1026 years (90% confidence level), similar to existing constraints. We also report the expected sensitivity of a possible subsequent dedicated exposure using 90% enrichment with Xe136 at 1.06Γ1027 years
Recommended from our members
Projected WIMP sensitivity of the LUX-ZEPLIN dark matter experiment
LUX-ZEPLIN (LZ) is a next-generation dark matter direct detection experiment that will operate 4850 feet underground at the Sanford Underground Research Facility (SURF) in Lead, South Dakota, USA. Using a two-phase xenon detector with an active mass of 7 tonnes, LZ will search primarily for low-energy interactions with weakly interacting massive particles (WIMPs), which are hypothesized to make up the dark matter in our galactic halo. In this paper, the projected WIMP sensitivity of LZ is presented based on the latest background estimates and simulations of the detector. For a 1000 live day run using a 5.6-tonne fiducial mass, LZ is projected to exclude at 90% confidence level spin-independent WIMP-nucleon cross sections above 1.4Γ10-48 cm2 for a 40 GeV/c2 mass WIMP. Additionally, a 5Ο discovery potential is projected, reaching cross sections below the exclusion limits of recent experiments. For spin-dependent WIMP-neutron(-proton) scattering, a sensitivity of 2.3Γ10-43 cm2 (7.1Γ10-42 cm2) for a 40 GeV/c2 mass WIMP is expected. With underground installation well underway, LZ is on track for commissioning at SURF in 2020
Π’ΡΡΡΠΈΠ·ΠΈΡΠΎΠ²ΡΠ΅ Π°Π»ΠΌΠ°Π·Ρ Π½Π° ΠΠ½ΠΈΡΠ΅ΠΉΡΠΊΠΎΠΌ ΠΊΡΡΠΆΠ΅
First complete mineralogical and geochemical studies were conducted for diamonds and tuffisites-like source rocks identified at the Eniseyskiy Ridge. Studied diamonds are characterized by green color, cubo-octahedral morphology, moderate nitrogen content, and unaggregated nitrogen structural defects. The xenomineral film on the surface of diamond consist of a variety of native metal, carbide, sulfide and sulfate, halosulfide and oxide phases. The main micro-impurities are presented by Ni, Fe, Mn. The individual crystals as well as the diamonds in whole vary significantly in the isotopic composition of carbon. The results confirm the widespread dissemination of the diamonds on the Siberian Platform and their polygenesis.ΠΠΏΠ΅ΡΠ²ΡΠ΅ ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½Ρ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠ½ΡΠ΅ ΠΌΠΈΠ½Π΅ΡΠ°Π»ΠΎΠ³ΠΎ-Π³Π΅ΠΎΡ
ΠΈΠΌΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ Π°Π»ΠΌΠ°Π·ΠΎΠ² ΠΈ ΡΡΡΡΠΈΠ·ΠΈΡΠΎΠΏΠΎΠ΄ΠΎΠ±Π½ΡΡ
Π°Π»ΠΌΠ°Π·ΠΎΠ½ΠΎΡΠ½ΡΡ
ΠΏΠΎΡΠΎΠ΄, Π²ΡΡΠ²Π»Π΅Π½Π½ΡΡ
Π½Π° ΠΠ½ΠΈΡΠ΅ΠΉΡΠΊΠΎΠΌ ΠΊΡΡΠΆΠ΅. ΠΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½Π½ΡΠ΅ Π°Π»ΠΌΠ°Π·Ρ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΠ·ΡΡΡΡΡ Π·Π΅Π»Π΅Π½ΡΠΌ ΡΠ²Π΅ΡΠΎΠΌ, ΠΊΡΠ±ΠΎΠΊΡΠ°ΡΠ΄ΡΠΈΡΠ΅ΡΠΊΠΈΠΌ Π³Π°Π±ΠΈΡΡΡΠΎΠΌ, ΡΠΌΠ΅ΡΠ΅Π½Π½ΠΎΠΉ Π°Π·ΠΎΡΠ½ΠΎΡΡΡΡ, Π½Π΅Π°Π³ΡΠ΅Π³ΠΈΡΠΎΠ²Π°Π½Π½ΡΠΌ ΡΠΎΡΡΠΎΡΠ½ΠΈΠ΅ΠΌ Π°Π·ΠΎΡΠ½ΡΡ
ΡΡΡΡΠΊΡΡΡΠ½ΡΡ
Π΄Π΅ΡΠ΅ΠΊΡΠΎΠ². ΠΠ° ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠΈ Π°Π»ΠΌΠ°Π·ΠΎΠ² ΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½Ρ ΠΊΡΠ΅Π½ΠΎΠΌΠΈΠ½Π΅ΡΠ°Π»ΡΠ½ΡΠ΅ ΠΏΠ»Π΅Π½ΠΊΠΈ, Π² ΡΠΎΡΡΠ°Π² ΠΊΠΎΡΠΎΡΡΡ
Π²Ρ
ΠΎΠ΄ΡΡ ΡΠ°Π·Π½ΠΎΠΎΠ±ΡΠ°Π·Π½ΡΠ΅ ΡΠ°ΠΌΠΎΡΠΎΠ΄Π½ΠΎ-ΠΌΠ΅ΡΠ°Π»Π»ΠΈΡΠ΅ΡΠΊΠΈΠ΅, ΠΊΠ°ΡΠ±ΠΈΠ΄Π½ΡΠ΅, ΡΡΠ»ΡΡΠΈΠ΄Π½ΡΠ΅ ΠΈ Π³Π°Π»ΠΎΠ³Π΅Π½ΡΡΠ»ΡΡΠΈΠ΄Π½ΡΠ΅, ΡΡΠ»ΡΡΠ°ΡΠ½ΡΠ΅ ΠΈ ΠΎΠΊΡΠΈΠ΄Π½ΡΠ΅ ΡΠ°Π·Ρ. Π ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅ ΠΎΡΠ½ΠΎΠ²Π½ΡΡ
ΠΌΠΈΠΊΡΠΎΡΠ»Π΅ΠΌΠ΅Π½ΡΠΎΠ²-ΠΏΡΠΈΠΌΠ΅ΡΠ΅ΠΉ Π²ΡΡΡΡΠΏΠ°ΡΡ Ni, FΠ΅, Mn. ΠΠ΅ΡΡΠΌΠ° Π½Π΅ΠΎΠ΄Π½ΠΎΡΠΎΠ΄Π½Ρ ΠΏΠΎ ΠΈΠ·ΠΎΡΠΎΠΏΠ½ΠΎΠΌΡ ΡΠΎΡΡΠ°Π²Ρ ΡΠ³Π»Π΅ΡΠΎΠ΄Π° ΠΊΠ°ΠΊ Π°Π»ΠΌΠ°Π·Ρ-ΠΈΠ½Π΄ΠΈΠ²ΠΈΠ΄Ρ, ΡΠ°ΠΊ ΠΈ Π°Π»ΠΌΠ°Π·Ρ ΠΈΠ·ΡΡΠ΅Π½Π½ΠΎΠΉ ΠΏΠΎΠΏΡΠ»ΡΡΠΈΠΈ Π² ΡΠ΅Π»ΠΎΠΌ. ΠΠΎΠ»ΡΡΠ΅Π½Π½ΡΠ΅ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΏΠΎΠ΄ΡΠ²Π΅ΡΠΆΠ΄Π°ΡΡ Π²ΡΠ²ΠΎΠ΄Ρ ΠΎ ΠΏΠΎΠ²ΡΠ΅ΠΌΠ΅ΡΡΠ½ΠΎΠΉ Π·Π°ΡΠ°ΠΆΠ΅Π½Π½ΠΎΡΡΠΈ Π‘ΠΈΠ±ΠΈΡΡΠΊΠΎΠΉ ΠΏΠ»Π°ΡΡΠΎΡΠΌΡ Π°Π»ΠΌΠ°Π·Π°ΠΌΠΈ ΠΈ ΠΈΡ
ΠΏΠΎΠ»ΠΈΠ³Π΅Π½Π½ΠΎΡΡΠΈ
Π‘ΠΎΠ²ΠΌΠ΅ΡΡΠ½ΡΠ΅ ΠΏΠΎΡΠ΅Π²Ρ ΠΊΡΠΊΡΡΡΠ·Ρ ΠΈ ΡΠΎΠΈ Π² ΡΡΠ»ΠΎΠ²ΠΈΡΡ Π»Π΅ΡΠΎΡΡΠ΅ΠΏΠΈ ΠΠ°ΠΏΠ°Π΄Π½ΠΎΠΉ Π‘ΠΈΠ±ΠΈΡΠΈ
The paper presents the results of studies on the cultivation of maise in joint crops with soybean in the forest-steppe zone of Western Siberia in 2003-2005. The authors studied plant height and dynamics of green mass yield of maise and soybean. As a result of recording plant height, the authors observed that corn hybrid Ob 150 CB by 25-30 cm and corn hybrid Krasnodar 382 MB by 35-47 cm were higher in single-seeded crops by harvest than in joint crops, indicating the negative impact of soybeans on corn. The maise hybrid Krasnodarskiy 382 MB reacted more strongly to the depress- ing effect of soybean than the hybrid Obskiy 150 SV in terms of plant height. This comparison was especially noticeable when it was cultivated in joint crops with the early-ripening soybean variety SibNIIK-315. In the early stages of development, the height of soybean plants in single-species and different variants of common crops did not practically differ. However, starting from the phase of fruit formation, the authors observed a decrease in the height of soybean plants in the row with maise and its increase in the intercropping. By harvesting, the difference between the height of soybean plants of the variety October 70 in the row and across the row was on average 11-24 cm. At the same time, the soybean plants of the variety October 70 were lower in the row with maise and higher in the row spacing than in the single-seeded crop. The height of the plants proves not only the principle of competitiveness but also the effect of the high range of tiering, which forces the legume component to reach for the light. In a mixture with the late-ripening maise hybrid Krasnodarskiy 382 MB, the early-ripening soybean variety contributed to a more significant decrease in the green mass yield of maise than the late-ripening soybean variety October 70. Harvesting, conducted on 2-6 September, showed that joint crops of maise, regardless of early maturity, provided a green matter yield of 23.7-40.1 t/ha. This yield was 49% and 14% lower than in the single-species crops of early maturing hybrid maise Ob 150 CB and 2-3 times lower than the mid-season hybrid Krasnodar 382 MV. The nature of the interspecific relationships indicates a more significant negative impact of early maturing soybean variety SibNIIK-315 on the productivity of maise and especially the medium-maturing hybrid Krasnodarskiy 382 MV, where the differences with the single-species sowing showed the most significant value β 51 %.ΠΡΠ΅Π΄ΡΡΠ°Π²Π»Π΅Π½Ρ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ ΠΏΠΎ Π²ΠΎΠ·Π΄Π΅Π»ΡΠ²Π°Π½ΠΈΡ ΠΊΡΠΊΡΡΡΠ·Ρ Π² ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΡΡ
ΠΏΠΎΡΠ΅Π²Π°Ρ
Ρ ΡΠΎΠ΅ΠΉ Π² ΡΡΠ»ΠΎΠ²ΠΈΡΡ
Π»Π΅ΡΠΎΡΡΠ΅ΠΏΠ½ΠΎΠΉ Π·ΠΎΠ½Ρ ΠΠ°ΠΏΠ°Π΄Π½ΠΎΠΉ Π‘ΠΈΠ±ΠΈΡΠΈ Π² 2003β2005 Π³Π³. ΠΠ·ΡΡΠ΅Π½Ρ Π²ΡΡΠΎΡΠ° ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ ΠΈ Π΄ΠΈΠ½Π°ΠΌΠΈΠΊΠ° ΡΡΠΎΠΆΠ°ΠΉΠ½ΠΎΡΡΠΈ Π·Π΅Π»Π΅Π½ΠΎΠΉ ΠΌΠ°ΡΡΡ ΠΊΡΠΊΡΡΡΠ·Ρ ΠΈ ΡΠΎΠΈ. Π ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠ΅ ΡΡΠ΅ΡΠ° Π²ΡΡΠΎΡΡ ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ Π³ΠΈΠ±ΡΠΈΠ΄ ΠΊΡΠΊΡΡΡΠ·Ρ ΠΠ±ΡΠΊΠΈΠΉ 150 Π‘Π ΠΊ ΡΠ±ΠΎΡΠΊΠ΅ Π² ΠΎΠ΄Π½ΠΎΠ²ΠΈΠ΄ΠΎΠ²ΡΡ
ΠΏΠΎΡΠ΅Π²Π°Ρ
Π±ΡΠ» Π½Π° 25β30 ΡΠΌ, Π° Π³ΠΈΠ±ΡΠΈΠ΄ ΠΊΡΠΊΡΡΡΠ·Ρ ΠΡΠ°ΡΠ½ΠΎΠ΄Π°ΡΡΠΊΠΈΠΉ 382 ΠΠ Π½Π° 35β47 ΡΠΌ Π²ΡΡΠ΅, ΡΠ΅ΠΌ Π² ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΡΡ
, ΡΡΠΎ ΡΠΊΠ°Π·ΡΠ²Π°Π΅Ρ Π½Π° Π½Π΅Π³Π°ΡΠΈΠ²Π½ΠΎΠ΅ Π²ΠΎΠ·Π΄Π΅ΠΉΡΡΠ²ΠΈΠ΅ ΡΠΎΠΈ Π½Π° ΠΊΡΠΊΡΡΡΠ·Ρ. ΠΠΈΠ±ΡΠΈΠ΄ ΠΊΡΠΊΡΡΡΠ·Ρ ΠΡΠ°ΡΠ½ΠΎΠ΄Π°ΡΡΠΊΠΈΠΉ 382 ΠΠ ΠΏΠΎ Π²ΡΡΠΎΡΠ΅ ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ ΡΠΈΠ»ΡΠ½Π΅Π΅ ΡΠ΅Π°Π³ΠΈΡΠΎΠ²Π°Π» Π½Π° ΡΠ³Π½Π΅ΡΠ°ΡΡΠ΅Π΅ Π²Π»ΠΈΡΠ½ΠΈΠ΅ ΡΠΎΠΈ, ΡΠ΅ΠΌ Π³ΠΈΠ±ΡΠΈΠ΄ ΠΠ±ΡΠΊΠΈΠΉ 150 Π‘Π, ΡΡΠΎ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎ Π·Π°ΠΌΠ΅ΡΠ½ΠΎ ΠΏΡΠΈ Π΅Π³ΠΎ Π²ΠΎΠ·Π΄Π΅Π»ΡΠ²Π°Π½ΠΈΠΈ Π² ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΡΡ
ΠΏΠΎΡΠ΅Π²Π°Ρ
ΡΠΎ ΡΠΊΠΎΡΠΎΡΠΏΠ΅Π»ΡΠΌ ΡΠΎΡΡΠΎΠΌ ΡΠΎΠΈ Π‘ΠΈΠ±ΠΠΠΠ-315. ΠΠ° ΡΠ°Π½Π½ΠΈΡ
ΡΡΠ°ΠΏΠ°Ρ
ΡΠ°Π·Π²ΠΈΡΠΈΡ Π²ΡΡΠΎΡΠ° ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ ΡΠΎΠΈ Π² ΠΎΠ΄Π½ΠΎΠ²ΠΈΠ΄ΠΎΠ²ΡΡ
ΠΈ Π² ΡΠ°Π·Π½ΡΡ
Π²Π°ΡΠΈΠ°Π½ΡΠ°Ρ
ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΡΡ
ΠΏΠΎΡΠ΅Π²ΠΎΠ² ΠΏΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠΈ Π½Π΅ ΡΠ°Π·Π»ΠΈΡΠ°Π»Π°ΡΡ, ΠΎΠ΄Π½Π°ΠΊΠΎ Π½Π°ΡΠΈΠ½Π°Ρ Ρ ΡΠ°Π·Ρ ΠΏΠ»ΠΎΠ΄ΠΎΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ ΠΎΡΠΌΠ΅ΡΠ°Π΅ΡΡΡ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΠ΅ ΠΏΡΠΈΡΠΎΡΡΠ° Π²ΡΡΠΎΡΡ ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ ΡΠΎΠΈ Π² ΡΡΠ΄ΠΊΠ΅ Ρ ΠΊΡΠΊΡΡΡΠ·ΠΎΠΉ ΠΈ Π΅Π΅ ΡΠ²Π΅Π»ΠΈΡΠ΅Π½ΠΈΠ΅ Π² ΡΠ΅ΡΠ΅Π·ΡΡΠ΄Π½ΠΎΠΌ ΠΏΠΎΡΠ΅Π²Π΅. Π ΡΠ±ΠΎΡΠΊΠ΅ ΡΠ°Π·Π½ΠΈΡΠ° ΠΌΠ΅ΠΆΠ΄Ρ Π²ΡΡΠΎΡΠΎΠΉ ΡΠ°ΡΡΠ΅Π½ΠΈΠΉ ΡΠΎΠΈ ΡΠΎΡΡΠ° ΠΠΊΡΡΠ±ΡΡ 70 Π² ΡΡΠ΄ΠΊΠ΅ ΠΈ ΡΠ΅ΡΠ΅Π·ΡΡΠ΄Π½ΠΎΠΌ ΠΏΠΎΡΠ΅Π²Π΅ ΡΠΎΡΡΠ°Π²ΠΈΠ»Π° Π² ΡΡΠ΅Π΄Π½Π΅ΠΌ 11β24 ΡΠΌ. ΠΡΠΈ ΡΡΠΎΠΌ ΡΠ°ΡΡΠ΅Π½ΠΈΡ ΡΠΎΠΈ ΡΠΎΡΡΠ° ΠΠΊΡΡΠ±ΡΡ 70 Π² ΡΡΠ΄ΠΊΠ΅ Ρ ΠΊΡΠΊΡΡΡΠ·ΠΎΠΉ Π±ΡΠ»ΠΈ Π½ΠΈΠΆΠ΅, Π° Π² ΡΠ΅ΡΠ΅Π·ΡΡΠ΄Π½ΠΎΠΌ ΠΏΠΎΡΠ΅Π²Π΅ β Π²ΡΡΠ΅, ΡΠ΅ΠΌ Π² ΠΎΠ΄Π½ΠΎΠ²ΠΈΠ΄ΠΎΠ²ΠΎΠΌ ΠΏΠΎΡΠ΅Π²Π΅, Π΄ΠΎΠΊΠ°Π·ΡΠ²Π°Ρ Π½Π΅ ΡΡΠΎΠ»ΡΠΊΠΎ ΠΏΡΠΈΠ½ΡΠΈΠΏ ΠΊΠΎΠ½ΠΊΡΡΠ΅Π½ΡΠ½ΠΎΡΡΠΈ, ΡΠΊΠΎΠ»ΡΠΊΠΎ Π΄Π΅ΠΉΡΡΠ²ΠΈΠ΅ Π²ΡΡΠΎΠΊΠΎΠ³ΠΎ Π΄ΠΈΠ°ΠΏΠ°Π·ΠΎΠ½Π° ΡΡΡΡΠ½ΠΎΡΡΠΈ, ΠΊΠΎΡΠΎΡΠΎΠ΅ Π²ΡΠ½ΡΠΆΠ΄Π°Π΅Ρ Π±ΠΎΠ±ΠΎΠ²ΡΠΉ ΠΊΠΎΠΌΠΏΠΎΠ½Π΅Π½Ρ ΡΡΠ½ΡΡΡΡΡ ΠΊ ΡΠ²Π΅ΡΡ. Π ΡΠΌΠ΅ΡΠΈ Ρ ΠΏΠΎΠ·Π΄Π½Π΅ΡΠΏΠ΅Π»ΡΠΌ Π³ΠΈΠ±ΡΠΈΠ΄ΠΎΠΌ ΠΊΡΠΊΡΡΡΠ·Ρ ΠΡΠ°ΡΠ½ΠΎΠ΄Π°ΡΡΠΊΠΈΠΉ 382 ΠΠ ΡΠ°Π½Π½Π΅ΡΠΏΠ΅Π»ΡΠΉ ΡΠΎΡΡ ΡΠΎΠΈ ΡΠΏΠΎΡΠΎΠ±ΡΡΠ²ΠΎΠ²Π°Π» Π±ΠΎΠ»ΡΡΠ΅ΠΌΡ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΡ ΡΡΠΎΠΆΠ°ΠΉΠ½ΠΎΡΡΠΈ Π·Π΅Π»Π΅Π½ΠΎΠΉ ΠΌΠ°ΡΡΡ ΠΊΡΠΊΡΡΡΠ·Ρ, ΡΠ΅ΠΌ ΠΏΠΎΠ·Π΄Π½Π΅ΡΠΏΠ΅Π»ΡΠΉ ΡΠΎΡΡ ΡΠΎΠΈ ΠΠΊΡΡΠ±ΡΡΒ 70. Π£Π±ΠΎΡΠΊΠ° ΡΡΠΎΠΆΠ°Ρ, ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½Π½Π°Ρ 2β6 ΡΠ΅Π½ΡΡΠ±ΡΡ, ΠΏΠΎΠΊΠ°Π·Π°Π»Π°, ΡΡΠΎ ΡΠΎΠ²ΠΌΠ΅ΡΡΠ½ΡΠ΅ ΠΏΠΎΡΠ΅Π²Ρ ΠΊΡΠΊΡΡΡΠ·Ρ, Π½Π΅Π·Π°Π²ΠΈΡΠΈΠΌΠΎ ΠΎΡ ΡΠΊΠΎΡΠΎΡΠΏΠ΅Π»ΠΎΡΡΠΈ, ΠΎΠ±Π΅ΡΠΏΠ΅ΡΠΈΠ»ΠΈ ΡΡΠΎΠΆΠ°ΠΉΠ½ΠΎΡΡΡ Π·Π΅Π»Π΅Π½ΠΎΠΉ ΠΌΠ°ΡΡΡ 23,7β40,1 Ρ/Π³Π°, ΡΡΠΎ Π½ΠΈΠΆΠ΅ Π½Π° 49 ΠΈ 14 %, ΡΠ΅ΠΌ Π² ΠΎΠ΄Π½ΠΎΠ²ΠΈΠ΄ΠΎΠ²ΡΡ
ΠΏΠΎΡΠ΅Π²Π°Ρ
ΡΠ°Π½Π½Π΅ΡΠΏΠ΅Π»ΠΎΠ³ΠΎ Π³ΠΈΠ±ΡΠΈΠ΄Π° ΠΊΡΠΊΡΡΡΠ·Ρ ΠΠ±ΡΠΊΠΈΠΉ 150 Π‘Π ΠΈ Π² 2β3 ΡΠ°Π·Π° β ΡΡΠ΅Π΄Π½Π΅ΡΠΏΠ΅Π»ΠΎΠ³ΠΎ Π³ΠΈΠ±ΡΠΈΠ΄Π° ΠΡΠ°ΡΠ½ΠΎΠ΄Π°ΡΡΠΊΠΈΠΉ 382 ΠΠ. Π₯Π°ΡΠ°ΠΊΡΠ΅Ρ ΠΌΠ΅ΠΆΠ²ΠΈΠ΄ΠΎΠ²ΡΡ
Π²Π·Π°ΠΈΠΌΠΎΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΠΉ ΡΠ²ΠΈΠ΄Π΅ΡΠ΅Π»ΡΡΡΠ²ΡΠ΅Ρ ΠΎ Π±ΠΎΠ»ΡΡΠ΅ΠΌ Π½Π΅Π³Π°ΡΠΈΠ²Π½ΠΎΠΌ Π²Π»ΠΈΡΠ½ΠΈΠΈ ΡΠΎΠΈ ΡΠ°Π½Π½Π΅ΡΠΏΠ΅Π»ΠΎΠ³ΠΎ ΡΠΎΡΡΠ° Π‘ΠΈΠ±ΠΠΠΠ-315 Π½Π° ΠΏΡΠΎΠ΄ΡΠΊΡΠΈΠ²Π½ΠΎΡΡΡ ΠΊΡΠΊΡΡΡΠ·Ρ ΠΈ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎ ΡΡΠ΅Π΄Π½Π΅ΡΠΏΠ΅Π»ΠΎΠ³ΠΎ Π³ΠΈΠ±ΡΠΈΠ΄Π° ΠΡΠ°ΡΠ½ΠΎΠ΄Π°ΡΡΠΊΠΈΠΉ 382 ΠΠ, Π³Π΄Π΅ ΡΠ°Π·Π»ΠΈΡΠΈΡ Ρ ΠΎΠ΄Π½ΠΎΠ²ΠΈΠ΄ΠΎΠ²ΡΠΌ ΠΏΠΎΡΠ΅Π²ΠΎΠΌ ΠΏΠΎΠΊΠ°Π·Π°Π»ΠΈ ΡΠ°ΠΌΡΡ Π·Π½Π°ΡΠΈΡΠ΅Π»ΡΠ½ΡΡ Π²Π΅Π»ΠΈΡΠΈΠ½Ρ β 51 %
- β¦