532 research outputs found
Analysis of priority sectors of the economy in the policy of import substitution
In this paper, the authors considered the priority sectors of the economy in the policy of import substitution. Analyses were carried outthe work of foreign and domestic scientistproposed the author's interpretation of the import substitution policy, presentedthe scheme of work of the industry of import substitution in the Russian Federatio
Π‘ΡΡΡΠΊΡΡΡΠ½ΡΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ ΡΠΊΠ»ΠΎΠ³ΠΈΡΡΠΎΠ΄Π΅ΡΠΆΠ°ΡΠΈΡ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠΎΠ² ΡΠ΅Π²Π΅ΡΠ° Π£ΡΠ°Π»Π° ΠΏΠΎ Π³ΡΠ°Π²ΠΈΠΌΠ°Π³Π½ΠΈΡΠ½ΡΠΌ Π΄Π°Π½Π½ΡΠΌ
The paper presents the results of integrated petrophysical and geophysical studies of Marunkeu and Nerkayu complexes in the north of the Urals. Qualitative interpretation of magnetic and gravitational fields is performed. It is shown that a wide range of changes in the magnetic properties of rocks of eclogite-containing complexes is not always connected with the magnetic field strength. On the contrary, contrasting density distribution in the studied complexes is recorded in the local anomalies of increased intensity in a gravitational field and is the main source of information on the deep structure of Nerkayu and Marunkeu complexes. In this article, big attention is paid to the analysis of local anomalies that have a significant impact on the nature of the anomalous gravitational field. Dedicated local anomalies of the upper and middle crust represent areas of high-density (more mafic) rocks of Nerkayu and Marunkeu complexes. The results of the qualitative interpretation of the gravity field, the similarity for the deep characteristics of eclogite complexes in local anomalies, and their connection with mapped surface objects allow suggesting a unified deep nature of Nerkayu and Marunkeu complexes.ΠΠ·Π»ΠΎΠΆΠ΅Π½Ρ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠ½ΡΡ
ΠΏΠ΅ΡΡΠΎΡΠΈΠ·ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ Π³Π΅ΠΎΡΠΈΠ·ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ ΠΌΠ°ΡΡΠ½ΠΊΠ΅ΡΡΠΊΠΎΠ³ΠΎ ΠΈ Π½Π΅ΡΠΊΠ°ΡΡΠΊΠΎΠ³ΠΎ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠΎΠ² ΡΠ΅Π²Π΅ΡΠ° Π£ΡΠ°Π»Π°. ΠΡΠΏΠΎΠ»Π½Π΅Π½Π° ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅Π½Π½Π°Ρ ΠΈΠ½ΡΠ΅ΡΠΏΡΠ΅ΡΠ°ΡΠΈΡ ΠΌΠ°Π³Π½ΠΈΡΠ½ΠΎΠ³ΠΎ ΠΈ Π³ΡΠ°Π²ΠΈΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΠΏΠΎΠ»Π΅ΠΉ. ΠΠΎΠΊΠ°Π·Π°Π½ΠΎ, ΡΡΠΎ ΡΠΈΡΠΎΠΊΠΈΠΉ Π΄ΠΈΠ°ΠΏΠ°Π·ΠΎΠ½ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ ΠΌΠ°Π³Π½ΠΈΡΠ½ΡΡ
ΡΠ²ΠΎΠΉΡΡΠ² ΠΏΠΎΡΠΎΠ΄ ΡΠΊΠ»ΠΎΠ³ΠΈΡΡΠΎΠ΄Π΅ΡΠΆΠ°ΡΠΈΡ
ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠΎΠ² Π½Π΅ Π²ΡΠ΅Π³Π΄Π° ΡΠ²ΡΠ·Π°Π½ Ρ Π½Π°ΠΏΡΡΠΆΠ΅Π½Π½ΠΎΡΡΡΡ ΠΌΠ°Π³Π½ΠΈΡΠ½ΠΎΠ³ΠΎ ΠΏΠΎΠ»Ρ. ΠΠ°ΠΏΡΠΎΡΠΈΠ², ΠΊΠΎΠ½ΡΡΠ°ΡΡΠ½ΠΎΠ΅ ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΠ΅ ΠΏΠ»ΠΎΡΠ½ΠΎΡΡΠΈ Π² ΠΈΠ·ΡΡΠ°Π΅ΠΌΡΡ
ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠ°Ρ
ΡΠΈΠΊΡΠΈΡΡΠ΅ΡΡΡ Π² Π»ΠΎΠΊΠ°Π»ΡΠ½ΡΡ
Π°Π½ΠΎΠΌΠ°Π»ΠΈΡΡ
ΠΏΠΎΠ²ΡΡΠ΅Π½Π½ΠΎΠΉ ΠΈΠ½ΡΠ΅Π½ΡΠΈΠ²Π½ΠΎΡΡΠΈ Π² Π³ΡΠ°Π²ΠΈΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠΌ ΠΏΠΎΠ»Π΅ ΠΈ ΡΠ²Π»ΡΠ΅ΡΡΡ Π³Π»Π°Π²Π½ΡΠΌ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠΎΠΌ ΠΈΠ½ΡΠΎΡΠΌΠ°ΡΠΈΠΈ ΠΎ Π³Π»ΡΠ±ΠΈΠ½Π½ΠΎΠΌ ΡΡΡΠΎΠ΅Π½ΠΈΠΈ Π½Π΅ΡΠΊΠ°ΡΡΠΊΠΎΠ³ΠΎ ΠΈ ΠΌΠ°ΡΡΠ½ΠΊΠ΅ΡΡΠΊΠΎΠ³ΠΎ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠΎΠ². Π ΡΡΠ°ΡΡΠ΅ Π±ΠΎΠ»ΡΡΠΎΠ΅ Π²Π½ΠΈΠΌΠ°Π½ΠΈΠ΅ ΡΠ΄Π΅Π»ΡΠ΅ΡΡΡ Π°Π½Π°Π»ΠΈΠ·Ρ Π»ΠΎΠΊΠ°Π»ΡΠ½ΡΡ
Π°Π½ΠΎΠΌΠ°Π»ΠΈΠΉ, ΠΎΠΊΠ°Π·ΡΠ²Π°ΡΡΠΈΡ
ΡΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎΠ΅ Π²Π»ΠΈΡΠ½ΠΈΠ΅ Π½Π° Ρ
Π°ΡΠ°ΠΊΡΠ΅Ρ Π°Π½ΠΎΠΌΠ°Π»ΡΠ½ΠΎΠ³ΠΎ Π³ΡΠ°Π²ΠΈΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΠΏΠΎΠ»Ρ. ΠΡΠ΄Π΅Π»Π΅Π½Π½ΡΠΌ Π»ΠΎΠΊΠ°Π»ΡΠ½ΡΠΌ Π°Π½ΠΎΠΌΠ°Π»ΠΈΡΠΌ Π²Π΅ΡΡ
Π½Π΅ΠΉ ΠΈ ΡΡΠ΅Π΄Π½Π΅ΠΉ Π·Π΅ΠΌΠ½ΠΎΠΉ ΠΊΠΎΡΡ ΡΠΎΠΎΡΠ²Π΅ΡΡΡΠ²ΡΡΡ ΡΡΠ°ΡΡΠΊΠΈ Π²ΡΡΠΎΠΊΠΎΠΏΠ»ΠΎΡΠ½ΡΡ
(Π±ΠΎΠ»Π΅Π΅ ΠΎΡΠ½ΠΎΠ²Π½ΡΡ
) ΠΏΠΎΡΠΎΠ΄ Π½Π΅ΡΠΊΠ°ΡΡΠΊΠΎΠ³ΠΎ ΠΈ ΠΌΠ°ΡΡΠ½ΠΊΠ΅ΡΡΠΊΠΎΠ³ΠΎ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠΎΠ². Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎΠΉ ΠΈΠ½ΡΠ΅ΡΠΏΡΠ΅ΡΠ°ΡΠΈΠΈ Π³ΡΠ°Π²ΠΈΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΠΏΠΎΠ»Ρ, ΡΡ
ΠΎΠ΄ΡΡΠ²ΠΎ Π² ΡΠ°ΡΡΠΈΡΡΠΎΠ²ΠΊΠ΅ Π³Π»ΡΠ±ΠΈΠ½Π½ΡΡ
Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊ ΡΠΊΠ»ΠΎΠ³ΠΈΡΡΠΎΠ΄Π΅ΡΠΆΠ°ΡΠΈΡ
ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠΎΠ² ΠΏΠΎ Π»ΠΎΠΊΠ°Π»ΡΠ½ΡΠΌ Π°Π½ΠΎΠΌΠ°Π»ΠΈΡΠΌ ΠΈ ΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΈΠ΅ ΡΠ²ΡΠ·ΠΈ ΠΈΡ
Ρ ΠΊΠ°ΡΡΠΈΡΡΠ΅ΠΌΡΠΌΠΈ Ρ ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠΈ ΠΎΠ±ΡΠ΅ΠΊΡΠ°ΠΌΠΈ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡ ΠΏΡΠ΅Π΄ΠΏΠΎΠ»ΠΎΠΆΠΈΡΡ Π΅Π΄ΠΈΠ½ΡΡ Π³Π»ΡΠ±ΠΈΠ½Π½ΡΡ ΠΏΡΠΈΡΠΎΠ΄Ρ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ Π½Π΅ΡΠΊΠ°ΡΡΠΊΠΎΠ³ΠΎ ΠΈ ΠΌΠ°ΡΡΠ½ΠΊΠ΅ΡΡΠΊΠΎΠ³ΠΎ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡΠΎΠ² ΡΠ΅Π²Π΅ΡΠ° Π£ΡΠ°Π»Π°
Arc Magmas from Slab to Eruption: The Case of Kliuchevskoy Volcano
Arc magmas are generated by a number of mantle and
crustal processes. Our multidisciplinary, long-term research is
aimed at deciphering these processes for a single arc volcano,
Kliuchevskoy volcano in Kamchatka. Some key results of the
study follow:
1) Modeling of trace element and H2O contents in melt
inclusions suggests that the primary magmas originate via
hydrous flux-melting of the mantle wedge at temperatures
close to the dry peridotite solidus. The role of decompression
melting is minor or absent at Kliuchevskoy and other arc
volcanoes built on relatively thick crust.
2) Geochemistry of high-Mg olivine suggests that primary
Kliuchevskoy magmas have substantial contribution from
olivine-free pyroxenite (up to 30 %), which could be formed
by reaction of slab melts (or supercritical fluids) with mantle
wedge peridotite.
3) Parental Kliuchevskoy melts start to crystallize as deep
as the Moho boundary, and the erupted magmas reflect multistage
and complex processes of crystallization, magma mixing
and crustal assimilation. None of the Kliuchevskoy rocks
analyzed thus far represent true primary melt compositions.
4) The Kliuchevskoy Holocene eruptive history is not
steady-state in terms of eruption rate and geochemistry. There
are two millenial cycles with major and trace element and OSr-
Nd-Pb and U-series isotope compositions of the magmas
changing gradually from more to less affected by crustal (?)
assimilation. The onset of the cycles correlates with periods of
enhanced volcanic activity in Kamchatka, suggesting that the
extent of magma-crust interaction is inversely related to
magma production rate and thus magma flux from the mantle
Critical phenomena in 1D Ising model with arbitrary spin
The aim of this work was to study critical phenomena taking place in 1D Ising model with different exchange interactions signs and arbitrary spin values in a magnetic field. Exact analytical formulas for frustration fields, zero temperature magnetization and entropy at these fields are obtained. The general behavior of pair spin correlation function with the accounting of only interactions between nearest neighbors is examined. Β© 2018 The Authors, published by EDP Sciences.The reflorted study was carried out within the state assignment of FASO of Russia (theme Β«QuantumΒ» n. 01201463332) and was funded by RFBR according to the research flroject n. 16-32-00032
The importance of professional skills competitions for the training of specialists of industrial
The training of highly qualified specialists in working professions is the main problem at present. The system of competitions of professional skill and its importance for the training of highly skilled workers is shown and analyzed. The experience of the Russian State Pedagogical University in solving the existing problem is given on the example of the competence Β«Welding technologiesΒ»ΠΠΎΠ΄Π³ΠΎΡΠΎΠ²ΠΊΠ° Π²ΡΡΠΎΠΊΠΎΠΊΠ²Π°Π»ΠΈΡΠΈΡΠΈΡΠΎΠ²Π°Π½Π½ΡΡ
ΡΠΏΠ΅ΡΠΈΠ°Π»ΠΈΡΡΠΎΠ² ΠΏΠΎ ΡΠ°Π±ΠΎΡΠΈΠΌ ΠΏΡΠΎΡΠ΅ΡΡΠΈΡΠΌ β ΠΎΡΠ½ΠΎΠ²Π½Π°Ρ ΠΏΡΠΎΠ±Π»Π΅ΠΌΠ° Π² Π½Π°ΡΡΠΎΡΡΠ΅Π΅ Π²ΡΠ΅ΠΌΡ. ΠΠΎΠΊΠ°Π·Π°Π½Π° ΠΈ ΠΏΡΠΎΠ°Π½Π°Π»ΠΈΠ·ΠΈΡΠΎΠ²Π°Π½Π° ΡΠΈΡΡΠ΅ΠΌΠ° ΠΊΠΎΠ½ΠΊΡΡΡΠΎΠ² ΠΏΡΠΎΡΠ΅ΡΡΠΈΠΎΠ½Π°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΌΠ°ΡΡΠ΅ΡΡΡΠ²Π° ΠΈ Π΅Π΅ Π·Π½Π°ΡΠ΅Π½ΠΈΠ΅ Π΄Π»Ρ ΠΏΠΎΠ΄Π³ΠΎΡΠΎΠ²ΠΊΠΈ Π²ΡΡΠΎΠΊΠΎΠΊΠ²Π°Π»ΠΈΡΠΈΡΠΈΡΠΎΠ²Π°Π½Π½ΡΡ
ΡΠ°Π±ΠΎΡΠΈΡ
. ΠΡΠΈΠ²Π΅Π΄Π΅Π½ ΠΎΠΏΡΡ Π ΠΠΠΠ£ Π² ΡΠ΅ΡΠ΅Π½ΠΈΠΈ ΡΡΡΠ΅ΡΡΠ²ΡΡΡΠ΅ΠΉ ΠΏΡΠΎΠ±Π»Π΅ΠΌΡ Π½Π° ΠΏΡΠΈΠΌΠ΅ΡΠ΅ ΠΊΠΎΠΌΠΏΠ΅ΡΠ΅Π½ΡΠΈΠΈ Β«Π‘Π²Π°ΡΠΎΡΠ½ΡΠ΅ ΡΠ΅Ρ
Π½ΠΎΠ»ΠΎΠ³ΠΈΠΈ
On the Transversal Vibrations of an Axially Moving Continuum With a Time-Varying Velocity: Transient From String to Beam Behavior,β
ABSTRACT In this paper an initial-boundary value problem for a linear equation describing an axially moving stretched beam will be considered. The velocity of the beam is assumed to be timevarying. since the order of magnitude of the bending stiffness terms depends on the vibrations modes and the frequencies involved a that combination of two simplified models (a string equation and a beam with string effect equation) will be used to describe the transversal vibrations of the system accurately. Based on the calculations of the natural frequencies the regions of applicability of these models will be determined. A two time-scales perturbation method will be used to construct formal asymptotic approximations of the solutions. It will be shown that the linear axially moving "string to beam" model already has complicated dynamical behavior. NOMENCLATURE U(X, T ) the displacement of the string in vertical direction, V (T ) the time-varying belt speed, c the wave speed, X the coordinate in horizontal direction, E the modulus of elasticity, I the moment of inertia with the respect to the X (horizontal) axis, Ο the mass density of the belt, A the area of the cross section of the belt, T the time, and ΟL the distance between the pulleys. INTRODUCTION Axially moving systems are present in a vast class of engineering problems which arise in industrial, civil, aerospatial, mechanical, electronic, medical, and automotive applications. Serpentine belts, aerial cables, tram and train ways, oil pipelines, magnetic tapes, power transmission belts, band saw blades, chair lifts in skiing resorts, and even models of human DNA are examples of real objects where axial transport of mass can be associated with transverse vibrations. Investigating transverse vibrations of a belt system is a challenging subject which has been studied for many years by many researches and still is of interest today (see references for a recent overview). In the classical analysis of axially moving continua the vibrations are usually classified into two types, i.e. whether it is of a string-like type or of a beam-like type, depending on the bending stiffness of the belt. If the bending stiffness can be neglected then the system is classified as string (wave)-like, otherwise it is classified as beam-like. The transverse vibrations of a belt system (with time-varying velocity V (t)) can be modelled mathematically as
INFORMATION ABOUT THE QUALITY OF FUR PRODUCTS
there has been less illegal business, but it has not completely disappeared, as well as the pros and cons of introducing this labeling system for its participants.Π Π΄Π°Π½Π½ΠΎΠΉ ΡΡΠ°ΡΡΠ΅ ΡΠ°ΡΠΊΡΡΠ²Π°Π΅ΡΡΡ ΠΏΠΎΠ½ΡΡΠΈΠ΅ ΠΌΠ°ΡΠΊΠΈΡΠΎΠ²ΠΊΠΈ ΠΌΠ΅Ρ
ΠΎΠ²ΡΡ
ΠΈΠ·Π΄Π΅Π»ΠΈΠΉ. Π Π°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°ΡΡΡΡ Π²ΠΈΠ΄Ρ Π½Π°Π½Π΅ΡΠ΅Π½ΠΈΡ ΠΌΠ°ΡΠΊΠΈΡΠΎΠ²ΠΊΠΈ Π½Π° ΠΌΠ΅Ρ
ΠΎΠ²ΡΠ΅ ΠΈΠ·Π΄Π΅Π»ΠΈΡ. ΠΠ΅Π»Π°Π΅ΡΡΡ Π²ΡΠ²ΠΎΠ΄, ΡΡΠΎ Ρ ΠΏΠΎΡΠ²Π»Π΅Π½ΠΈΠ΅ΠΌ ΠΎΠ±ΡΠ·Π°ΡΠ΅Π»ΡΠ½ΠΎΠΉ ΠΌΠ°ΡΠΊΠΈΡΠΎΠ²ΠΊΠΈ ΠΌΠ΅Ρ
ΠΎΠ²ΡΡ
ΠΈΠ·Π΄Π΅Π»ΠΈΠΉ ΡΡΠ°Π»ΠΎ ΠΌΠ΅Π½ΡΡΠ΅ Π½Π΅Π»Π΅Π³Π°Π»ΡΠ½ΠΎΠ³ΠΎ Π±ΠΈΠ·Π½Π΅ΡΠ°, Π½ΠΎ ΠΎΠΊΠΎΠ½ΡΠ°ΡΠ΅Π»ΡΠ½ΠΎ ΠΎΠ½ Π½Π΅ ΠΈΡΡΠ΅Π·, Π° ΡΠ°ΠΊΠΆΠ΅ ΠΎ ΠΏΠ»ΡΡΠ°Ρ
ΠΈ ΠΌΠΈΠ½ΡΡ Π²Π²Π΅Π΄Π΅Π½ΠΈΡ Π΄Π°Π½Π½ΠΎΠΉ ΡΠΈΡΡΠ΅ΠΌΡ ΠΌΠ°ΡΠΊΠΈΡΠΎΠ²ΠΊΠΈ Π΄Π»Ρ Π΅Ρ ΡΡΠ°ΡΡΠ½ΠΈΠΊΠΎΠ²
ΠΠΏΡΡ ΠΏΠ°Π»ΠΈΠ½ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ Π² Π½Π΅ΡΡΡΠ½ΠΎΠΉ Π³Π΅ΠΎΠ»ΠΎΠ³ΠΈΠΈ
The authors present the directions for palynological research: detailed (zonal) palynostratigraphy for clarifying the age and correlation of reservoirs; palynological facial analysis for reconstruct the position of the ancient coastline; determination of the degree of catagenesis of organic matter using the palynomorphs color index for assessing the oil and gas generation potential of terrigenous sediments of the Perm region.ΠΠ²ΡΠΎΡΡ ΠΏΡΠ΅Π΄ΡΡΠ°Π²ΠΈΠ»ΠΈ Π½Π°ΠΏΡΠ°Π²Π»Π΅Π½ΠΈΡ ΠΏΠ°Π»ΠΈΠ½ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ: Π΄Π΅ΡΠ°Π»ΡΠ½Π°Ρ (Π·ΠΎΠ½Π°Π»ΡΠ½Π°Ρ) ΠΏΠ°Π»ΠΈΠ½ΠΎΡΡΡΠ°ΡΠΈΠ³ΡΠ°ΡΠΈΡ Π΄Π»Ρ ΡΡΠΎΡΠ½Π΅Π½ΠΈΡ Π²ΠΎΠ·ΡΠ°ΡΡΠ° ΠΈ ΠΊΠΎΡΡΠ΅Π»ΡΡΠΈΠΈ ΠΏΡΠΎΠ΄ΡΠΊΡΠΈΠ²Π½ΡΡ
ΠΏΠ»Π°ΡΡΠΎΠ²; ΠΏΠ°Π»ΠΈΠ½ΠΎΡΠ°ΡΠΈΠ°Π»ΡΠ½ΡΠΉ Π°Π½Π°Π»ΠΈΠ· Π΄Π»Ρ ΡΠ΅ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠΈ ΠΏΠΎΠ»ΠΎΠΆΠ΅Π½ΠΈΡ Π΄ΡΠ΅Π²Π½Π΅ΠΉ Π±Π΅ΡΠ΅Π³ΠΎΠ²ΠΎΠΉ Π»ΠΈΠ½ΠΈΠΈ; ΠΎΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΠ΅ ΡΡΠ΅ΠΏΠ΅Π½ΠΈ ΠΊΠ°ΡΠ°Π³Π΅Π½Π΅Π·Π° ΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ Π²Π΅ΡΠ΅ΡΡΠ²Π° ΠΏΠΎ ΡΠ²Π΅ΡΠΎΠ²ΠΎΠΌΡ ΠΈΠ½Π΄Π΅ΠΊΡΡ ΠΏΠ°Π»ΠΈΠ½ΠΎΠΌΠΎΡΡ Π΄Π»Ρ ΠΎΡΠ΅Π½ΠΊΠΈ Π½Π΅ΡΡΠ΅Π³Π°Π·ΠΎΠ³Π΅Π½Π΅ΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»Π° ΡΠ΅ΡΡΠΈΠ³Π΅Π½Π½ΡΡ
ΠΎΡΠ»ΠΎΠΆΠ΅Π½ΠΈΠΉ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ ΠΠ΅ΡΠΌΡΠΊΠΎΠ³ΠΎ ΠΊΡΠ°Ρ
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