12 research outputs found
Memory effect of MnGe nanomagnets embedded inside a Mn-diluted Ge matrix
Crystalline Mn5Ge3 nanomagnets are formed inside a Mn-diluted Ge matrix using
Mn ion implantation. A temperature-dependent memory effect and slow magnetic
relaxation are observed below the superparamagnetic blocking temperature of
Mn5Ge3. Our findings corroborate that the observed spin-glass-like features are
caused by the size distribution of Mn5Ge3 nanomagnets, rather than by the
inter-particle interaction through the Mn-diluted Ge matrix.Comment: 10 pages, 4 figures,. submitted to Appl. Phys. Let
Ferromagnetic, structurally disordered ZnO implanted with Co ions
We present superparamagnetic clusters of structurally highly disordered
Co-Zn-O created by high fluence Co ion implantation into ZnO (0001) single
crystals at low temperatures. This secondary phase cannot be detected by common
x-ray diffraction but is observed by high-resolution transmission electron
microscopy. In contrast to many other secondary phases in a ZnO matrix it
induces low-field anomalous Hall effect and thus is a candidate for
magneto-electronics applications.Comment: 5 pages, 3 figure
Unsteady Coupled Heat Transfer in the Air and Surrounding Rock Mass for Mine Excavations with Distributed Heat Sources
This paper presents an unsteady coupled heat transfer model in mine air and surrounding rock mass in the presence of distributed heat sources. The case of distributed heat sources is typical when analyzing the temperature distribution in mine excavations equipped with conveyor systems. For this case, the asymptotic value of the air temperature at the end of the mine excavation is determined not only by the heat exchange between the air and surrounding rock mass but also by the thermal power of distributed heat sources and the total airflow. This conclusion is confirmed by the experimental data presented in the paper for a longwall in a potash mine. We formulate the mathematical model and calculate the distribution of air parameters along the length of an excavation, considering heat release from the conveyor and surrounding rock mass. The results show that a distributed heat release is necessary for correctly calculating the air temperature in working areas. The numerical simulations allow us to recommend a redistribution of air between the haulage and conveyor roadways in the presence of distributed heat sources
Analytical approach to estimation of water build-up effect in mine ventilation shafts
ΠΠΊΡΡΠ°Π»ΡΠ½ΠΎΡΡΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ ΠΎΠ±ΡΡΠ»ΠΎΠ²Π»Π΅Π½Π° Π½Π΅ΠΎΠ±Ρ
ΠΎΠ΄ΠΈΠΌΠΎΡΡΡΡ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΡ Π΄ΠΎΠΏΠΎΠ»Π½ΠΈΡΠ΅Π»ΡΠ½ΠΎΠΉ Π½Π°Π³ΡΡΠ·ΠΊΠΈ Π½Π° Π³Π»Π°Π²Π½ΡΠ΅ Π²Π΅Π½ΡΠΈΠ»ΡΡΠΎΡΠ½ΡΠ΅ ΡΡΡΠ°Π½ΠΎΠ²ΠΊΠΈ, ΡΠ²ΡΠ·Π°Π½Π½ΠΎΠΉ Ρ Π²ΠΎΠ·Π½ΠΈΠΊΠ½ΠΎΠ²Π΅Π½ΠΈΠ΅ΠΌ ΠΎΠ±ΡΠ°ΡΠ½ΠΎΠΉ ΡΡΠ³ΠΈ ΠΏΡΠΈ ΠΊΠ°ΠΏΠ΅ΠΆΠ΅ Π² Π²Π΅Π½ΡΠΈΠ»ΡΡΠΈΠΎΠ½Π½ΡΡ
ΡΡΠ²ΠΎΠ»Π°Ρ
ΡΠ°Ρ
Ρ ΠΈ ΡΡΠ΄Π½ΠΈΠΊΠΎΠ². ΠΠ°ΠΈΠ±ΠΎΠ»Π΅Π΅ ΠΎΡΡΡΠΎ ΠΏΡΠΎΠ±Π»Π΅ΠΌΠ° Π½ΠΎΡΠΌΠ°Π»ΠΈΠ·Π°ΡΠΈΠΈ ΡΠ°Π±ΠΎΡΡ Π²Π΅Π½ΡΠΈΠ»ΡΡΠΎΡΠ° Π²ΠΎΠ·Π½ΠΈΠΊΠ°Π΅Ρ Π² ΡΠ»ΡΡΠ°Π΅ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΠ³ΠΎ ΠΏΠ΅ΡΠ΅Ρ
ΠΎΠ΄Π° Π΅Π³ΠΎ Π² ΡΠ΅ΠΆΠΈΠΌ Π½Π΅ΡΡΡΠΎΠΉΡΠΈΠ²ΠΎΠΉ ΡΠ°Π±ΠΎΡΡ, ΡΡΠΎ ΡΠΎΠΏΡΡΠΆΠ΅Π½ΠΎ Ρ Π½Π΅ΠΎΠ±Ρ
ΠΎΠ΄ΠΈΠΌΠΎΡΡΡΡ Π½Π΅ ΡΠΎΠ»ΡΠΊΠΎ ΡΠ½Π΅ΡΠ³ΠΎΡΠ±Π΅ΡΠ΅ΠΆΠ΅Π½ΠΈΡ, Π½ΠΎ ΠΈ ΠΏΡΠ΅Π΄ΠΎΡΠ²ΡΠ°ΡΠ΅Π½ΠΈΡ Π΅Π³ΠΎ Π°Π²Π°ΡΠΈΠΉΠ½ΠΎΠ³ΠΎ ΠΎΡΡΠ°Π½ΠΎΠ²Π°. Π¦Π΅Π»Ρ: Π²ΡΡΡΠ½Π΅Π½ΠΈΠ΅ ΠΏΡΠΈΡΠΈΠ½ ΠΈ ΠΌΠ΅Ρ
Π°Π½ΠΈΠ·ΠΌΠ° Π²ΠΎΠ·Π½ΠΈΠΊΠ½ΠΎΠ²Π΅Π½ΠΈΡ ΡΡΡΠ΅ΠΊΡΠ° Β«Π²ΠΎΠ΄ΡΠ½ΠΎΠΉ ΠΏΡΠΎΠ±ΠΊΠΈΒ» Π² Π²Π΅Π½ΡΠΈΠ»ΡΡΠΈΠΎΠ½Π½ΡΡ
ΡΡΠ²ΠΎΠ»Π°Ρ
Ρ ΠΏΠΎΠ»ΡΡΠ΅Π½ΠΈΠ΅ΠΌ ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΡ
ΠΈ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΡ
ΠΎΡΠ΅Π½ΠΎΠΊ Π²Π΅Π»ΠΈΡΠΈΠ½Ρ ΠΎΠ±ΡΠ°ΡΠ½ΠΎΠΉ ΡΡΠ³ΠΈ Π² Π·Π°Π²ΠΈΡΠΈΠΌΠΎΡΡΠΈ ΠΎΡ ΡΠΊΠΎΡΠΎΡΡΠΈ Π΄Π²ΠΈΠΆΠ΅Π½ΠΈΡ Π²ΠΎΠ·Π΄ΡΡ
Π°, Π³Π»ΡΠ±ΠΈΠ½Ρ ΠΈ ΠΈΠ½ΡΠ΅Π½ΡΠΈΠ²Π½ΠΎΡΡΠΈ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ° Π²ΡΠ΄Π΅Π»Π΅Π½ΠΈΡ Π²Π»Π°Π³ΠΈ. ΠΠ±ΡΠ΅ΠΊΡΡ: Π²Π΅Π½ΡΠΈΠ»ΡΡΠΈΠΎΠ½Π½ΡΠ΅ ΡΡΠ²ΠΎΠ»Ρ ΡΠ°Ρ
Ρ. ΠΠ΅ΡΠΎΠ΄Ρ: Π°Π½Π°Π»ΠΈΡΠΈΡΠ΅ΡΠΊΠΎΠ΅ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ ΠΏΡΠΎΡΠ΅ΡΡΠΎΠ² ΠΊΠΎΠ½Π΄Π΅Π½ΡΠ°ΡΠΈΠΈ Π²Π»Π°Π³ΠΈ ΠΈ Π΄Π²ΠΈΠΆΠ΅Π½ΠΈΡ ΠΊΠ°ΠΏΠ΅Π»Ρ Π² Π²ΠΎΡΡ
ΠΎΠ΄ΡΡΠ΅ΠΌ Π²ΠΎΠ·Π΄ΡΡΠ½ΠΎΠΌ ΠΏΠΎΡΠΎΠΊΠ΅; ΡΡΠ°Π²Π½ΠΈΡΠ΅Π»ΡΠ½ΡΠΉ Π°Π½Π°Π»ΠΈΠ· ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΡΡ
ΠΈ ΠΌΠΎΠ΄Π΅Π»ΡΠ½ΡΡ
Π΄Π°Π½Π½ΡΡ
. Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ. ΠΡΠΎΠ²Π΅Π΄ΡΠ½ Π°Π½Π°Π»ΠΈΠ· ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΡΡ
Π΄Π°Π½Π½ΡΡ
ΠΏΠΎ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ ΠΈ Π΄Π²ΠΈΠΆΠ΅Π½ΠΈΡ ΠΊΠ°ΠΏΠ΅Π»ΡΠ½ΠΎΠΉ Π²Π»Π°Π³ΠΈ Π² Π²Π΅Π½ΡΠΈΠ»ΡΡΠΈΠΎΠ½Π½ΡΡ
ΡΡΠ²ΠΎΠ»Π°Ρ
ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
ΡΡΠ΄Π½ΠΈΠΊΠΎΠ². ΠΡΠΌΠ΅ΡΠ΅Π½ΠΎ, ΡΡΠΎ ΡΡΡΠ΅ΠΊΡ Π²ΠΎΠ΄ΡΠ½ΠΎΠΉ ΠΏΡΠΎΠ±ΠΊΠΈ Π½Π°Π±Π»ΡΠ΄Π°Π΅ΡΡΡ Π² ΠΎΠ³ΡΠ°Π½ΠΈΡΠ΅Π½Π½ΠΎΠΌ Π΄ΠΈΠ°ΠΏΠ°Π·ΠΎΠ½Π΅ ΡΠΊΠΎΡΠΎΡΡΠ΅ΠΉ Π΄Π²ΠΈΠΆΠ΅Π½ΠΈΡ Π²ΠΎΠ·Π΄ΡΡ
Π° ΠΎΡ 7 Π΄ΠΎ 12 ΠΌ/Ρ, Π½ΠΎ Π² Π½Π΅ΠΊΠΎΡΠΎΡΡΡ
ΡΠ»ΡΡΠ°ΡΡ
ΡΡΡΠ΅ΠΊΡ ΠΎΡΡΡΡΡΡΠ²ΡΠ΅Ρ, Π΄Π°ΠΆΠ΅ Π½Π΅ΡΠΌΠΎΡΡΡ Π½Π° Π½Π°Π»ΠΈΡΠΈΠ΅ Π³ΡΡΡΠΎΠ³ΠΎ ΡΡΠΌΠ°Π½Π° ΠΈ ΠΎΠ±ΠΈΠ»ΡΠ½ΠΎΠΉ ΠΊΠΎΠ½Π΄Π΅Π½ΡΠ°ΡΠΈΠΈ Π²Π»Π°Π³ΠΈ Π½Π° ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠΈ ΠΊΡΠ΅ΠΏΠΈ ΠΈ Π°ΡΠΌΠΈΡΠΎΠ²ΠΊΠΈ ΡΡΠ²ΠΎΠ»Π°. Π Π°ΡΡΠΌΠΎΡΡΠ΅Π½Ρ ΡΡΠΈ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΡΡ
ΡΡΠ΅Π½Π°ΡΠΈΡ Π²ΠΎΠ·Π½ΠΈΠΊΠ½ΠΎΠ²Π΅Π½ΠΈΡ ΡΡΡΠ΅ΠΊΡΠ°: Π½Π°ΠΊΠΎΠΏΠ»Π΅Π½ΠΈΠ΅ Π±ΠΎΠ»ΡΡΠΎΠ³ΠΎ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π° Π·Π°Π²ΠΈΡΠ°ΡΡΠΈΡ
Π² Π²ΠΎΠ·Π΄ΡΡ
Π΅ ΠΊΠ°ΠΏΠ΅Π»Ρ ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΠ½Π½ΠΎΠ³ΠΎ ΡΠ°Π·ΠΌΠ΅ΡΠ°; ΠΏΠ°Π΄Π΅Π½ΠΈΠ΅ ΠΊΠ°ΠΏΠ΅Π»Ρ ΠΊΡΡΠΏΠ½ΡΡ
ΡΠ°Π·ΠΌΠ΅ΡΠΎΠ² ΠΏΠΎ Π²ΡΠ΅ΠΉ Π³Π»ΡΠ±ΠΈΠ½Π΅ ΡΡΠ²ΠΎΠ»Π° Ρ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠΎΠΌ Π²ΡΠ΄Π΅Π»Π΅Π½ΠΈΡ Π²Π»Π°Π³ΠΈ Π² Π΅Π³ΠΎ Π²Π΅ΡΡ
Π½Π΅ΠΉ ΡΠ°ΡΡΠΈ ΠΈ ΡΠ°Π·Π½ΠΎΠ½Π°ΠΏΡΠ°Π²Π»Π΅Π½Π½ΠΎΠ΅ Π΄Π²ΠΈΠΆΠ΅Π½ΠΈΠ΅ ΠΊΠ°ΠΏΠ΅Π»Ρ Π² Π·Π°Π²ΠΈΡΠΈΠΌΠΎΡΡΠΈ ΠΎΡ ΠΈΡ
ΡΠ°Π·ΠΌΠ΅ΡΠ° Ρ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠΎΠΌ Π²Π»Π°Π³ΠΎΠ²ΡΠ΄Π΅Π»Π΅Π½ΠΈΡ, ΡΠ°ΡΠΏΠΎΠ»ΠΎΠΆΠ΅Π½Π½ΡΠΌ Π½Π° ΠΏΡΠΎΠΈΠ·Π²ΠΎΠ»ΡΠ½ΠΎΠΉ Π³Π»ΡΠ±ΠΈΠ½Π΅. Π£ΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΎ, ΡΡΠΎ ΠΏΠ΅ΡΠ²ΡΠ΅ Π΄Π²Π΅ ΠΌΠΎΠ΄Π΅Π»ΠΈ Π½Π΅ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡΡ ΠΏΠΎΠ»ΡΡΠΈΡΡ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΡ ΠΎΡΠ΅Π½ΠΊΡ Π²Π΅Π»ΠΈΡΠΈΠ½Ρ ΡΡΡΠ΅ΠΊΡΠ° Π²Π²ΠΈΠ΄Ρ Π½Π΅ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΠ½Π½ΠΎΡΡΠΈ ΡΡΠ°ΠΊΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΡΠΎΡΡΠ°Π²Π° ΠΊΠ°ΠΏΠ΅Π»Ρ, ΠΊΡΠΈΡΠΈΡΠ΅ΡΠΊΠΈΠΉ ΡΠ°Π·ΠΌΠ΅Ρ Π·Π°Π²ΠΈΡΠ°Π½ΠΈΡ ΠΊΠΎΡΠΎΡΡΡ
ΡΠ²Π΅Π»ΠΈΡΠΈΠ²Π°Π΅Ρ ΠΎΠ±ΡΠ°ΡΠ½ΡΡ ΡΡΠ³Ρ Π΄ΠΎ Π±Π΅ΡΠΊΠΎΠ½Π΅ΡΠ½ΠΎΡΡΠΈ. ΠΡΠΎΡ Π½Π΅Π΄ΠΎΡΡΠ°ΡΠΎΠΊ ΡΡΡΡΠ°Π½ΡΠ½ Π² ΡΡΠ΅ΡΡΠ΅ΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ Π²Π²Π΅Π΄Π΅Π½ΠΈΠ΅ΠΌ ΡΡΠ½ΠΊΡΠΈΠΈ ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ ΠΊΠ°ΠΏΠ΅Π»Ρ ΠΏΠΎ ΡΠ°Π·ΠΌΠ΅ΡΠ°ΠΌ, ΡΡΠΎ Π΄Π°Π»ΠΎ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡΡ ΠΏΠΎΠ»ΡΡΠΈΡΡ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΠ΅ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ. ΠΠΎΠΊΠ°Π·Π°Π½ΠΎ, ΡΡΠΎ Π²ΡΠ΄Π΅Π»Π΅Π½ΠΈΠ΅ Π²Π»Π°Π³ΠΈ ΠΈΠ· Π²ΠΎΠ·Π΄ΡΡ
Π° Π½Π΅ ΠΌΠΎΠΆΠ΅Ρ ΡΠ²Π»ΡΡΡΡΡ ΠΏΡΠΈΡΠΈΠ½ΠΎΠΉ Π²ΠΎΠ·Π½ΠΈΠΊΠ½ΠΎΠ²Π΅Π½ΠΈΡ ΡΡΡΠ΅ΠΊΡΠ° Β«Π²ΠΎΠ΄ΡΠ½ΠΎΠΉ ΠΏΡΠΎΠ±ΠΊΠΈΒ», Π° ΠΏΡΠΈΡΠΈΠ½ΠΎΠΉ ΡΠ²Π»ΡΡΡΡΡ Π²ΠΎΠ΄ΠΎΠΏΡΠΈΡΠΎΠΊΠΈ Π² ΡΡΠ²ΠΎΠ» Ρ ΠΈΠ½ΡΠ΅Π½ΡΠΈΠ²Π½ΠΎΡΡΡΡ, Π½Π° ΠΏΠΎΡΡΠ΄ΠΎΠΊ ΠΏΡΠ΅Π²ΡΡΠ°ΡΡΠ΅ΠΉ ΠΊΠΎΠ½Π΄Π΅Π½ΡΠ°ΡΠΈΡ. ΠΠΎ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠ°ΠΌ ΡΠΈΡΠ»Π΅Π½Π½ΠΎΠ³ΠΎ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΏΠΎΠΊΠ°Π·Π°Π½ΠΎ, ΡΡΠΎ ΠΌΠ°ΠΊΡΠΈΠΌΠ°Π»ΡΠ½Π°Ρ ΠΎΠ±ΡΠ°ΡΠ½Π°Ρ ΡΡΠ³Π° Π²ΠΎΠ·Π½ΠΈΠΊΠ°Π΅Ρ ΠΏΡΠΈ ΠΏΡΠΎΠ½ΠΈΠΊΠ½ΠΎΠ²Π΅Π½ΠΈΠΈ Π² ΡΡΠ²ΠΎΠ» ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠ½ΡΡ
Π³ΡΡΠ½ΡΠΎΠ²ΡΡ
Π²ΠΎΠ΄.The relevance of the study is caused by the need to reduce the additional aerodynamic load on the main fans associated with the occurrence of pressure drop caused by water build-up effect in mine ventilation shafts. This negative effect can lead to significant increase in the air resistance of the mine and to subsequent unstable operation mode of main fan. Avoiding this effect is important not only for energy save mine ventilation, but also for preventing emergency stop of the main fan. Purpose: finding out the causes and mechanism of the water build-up effect with obtaining qualitative and quantitative estimates of the pressure drop value depending on the air velocity, shaft depth and intensity of the groundwater inflows. Objects: ventilation shafts. Methods: analytical modeling of moisture condensation and droplet movement in an ascending air flow in ventilation shaft; comparative analysis of experimental and model data. Results. The authors have analyzed the experimental data on formation and movement of droplet moisture in the ventilation shafts of various mines. It is noted that the water build-up effect is observed in the range of air velocities from 7 to 12 m/s, but in some cases the effect is absent even despite the presence of thick fog and abundant condensation of moisture on the surface of the shaft lining and other equipment. Three possible scenarios of the effect are considered: accumulation of a large number of drops of a certain size hanging in the air; drops of large size fall along the entire depth of the shaft with a source of moisture release in its upper part and multidirectional movement of drops depending on their size with a source of moisture release located at arbitrary depth. It is established that the first two models do not allow us to obtain a quantitative estimate of the water build-up effect value due to the uncertainty of the fractional composition of drops, the critical size of which increases the pressure drop to infinity. This drawback was eliminated in the third model by introducing the droplet size distribution function, which made it possible to obtain quantitative results. It is proved that the release of moisture from the air cannot be the cause of the water build-up effect, and the cause is the ground water flows into the shaft with intensity of an order of magnitude higher than moisture condensation. Based on the results of numerical modeling, it is shown that the maximum pressure drop occurs when surface groundwater enters the shaft
Methods for microclimate normalization in deep long blind drifts
ΠΠΊΡΡΠ°Π»ΡΠ½ΠΎΡΡΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ ΠΎΠ±ΡΡΠ»ΠΎΠ²Π»Π΅Π½Π° Π½Π΅ΠΎΠ±Ρ
ΠΎΠ΄ΠΈΠΌΠΎΡΡΡΡ ΡΡΠ΄Π½ΠΈΠΊΠΎΠ² ΡΠ΅ΡΠ°ΡΡ Π½ΠΎΠ²ΡΠ΅ ΠΏΡΠΎΠ±Π»Π΅ΠΌΡ Π½ΠΎΡΠΌΠ°Π»ΠΈΠ·Π°ΡΠΈΠΈ ΠΌΠΈΠΊΡΠΎΠΊΠ»ΠΈΠΌΠ°ΡΠ°, Π²ΠΎΠ·Π½ΠΈΠΊΠ°ΡΡΠΈΠ΅ ΠΏΡΠΈ ΠΏΡΠΎΡ
ΠΎΠ΄ΠΊΠ΅ Π²ΡΠ΅ Π±ΠΎΠ»Π΅Π΅ Π³Π»ΡΠ±ΠΎΠΊΠΈΡ
ΠΈ Π½Π°Π³ΡΠ΅ΡΡΡ
ΠΏΠΎΡΠΎΠ΄Π½ΡΡ
ΠΌΠ°ΡΡΠΈΠ²ΠΎΠ² ΠΏΡΠΎΡΡΠΆΠ΅Π½Π½ΡΠΌΠΈ ΡΡΠΏΠΈΠΊΠΎΠ²ΡΠΌΠΈ Π²ΡΡΠ°Π±ΠΎΡΠΊΠ°ΠΌΠΈ. Π¦Π΅Π»Ρ: ΠΎΠΏΡΠ΅Π΄Π΅Π»ΠΈΡΡ ΡΡΡΠ΅ΠΊΡΠΈΠ²Π½ΠΎΡΡΡ ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
ΡΠΏΠΎΡΠΎΠ±ΠΎΠ² Π½ΠΎΡΠΌΠ°Π»ΠΈΠ·Π°ΡΠΈΠΈ ΠΌΠΈΠΊΡΠΎΠΊΠ»ΠΈΠΌΠ°ΡΠ° Π² Π·Π°Π±ΠΎΠ΅ ΡΠ°Π·Π²Π΅Π΄ΠΎΡΠ½ΠΎΠΉ Π²ΡΡΠ°Π±ΠΎΡΠΊΠΈ-2 ΠΠΠ Β«ΠΠΠ "ΠΠΎΡΠΈΠ»ΡΡΠΊΠΈΠΉ Π½ΠΈΠΊΠ΅Π»Ρ"Β». ΠΠ±ΡΠ΅ΠΊΡΡ: Π³Π΅ΠΎΠ»ΠΎΠ³ΠΎΡΠ°Π·Π²Π΅Π΄ΠΎΡΠ½Π°Ρ Π²ΡΡΠ°Π±ΠΎΡΠΊΠ°-2 ΠΠΠ Β«ΠΠΠ "ΠΠΎΡΠΈΠ»ΡΡΠΊΠΈΠΉ Π½ΠΈΠΊΠ΅Π»Ρ"Β». ΠΠ΅ΡΠΎΠ΄Ρ: ΡΠΈΡΠ»Π΅Π½Π½ΠΎΠ΅ ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ ΡΠ΅ΠΏΠ»ΠΎΠΌΠ°ΡΡΠΎΠΏΠ΅ΡΠ΅Π½ΠΎΡΠ° Π² Π°ΡΠΌΠΎΡΡΠ΅ΡΠ΅ Π³ΠΎΡΠ½ΠΎΠΉ Π²ΡΡΠ°Π±ΠΎΡΠΊΠΈ, ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½ΠΈΠ΅ ΡΡΠ°Π²Π½ΠΈΡΠ΅Π»ΡΠ½ΠΎΠ³ΠΎ Π°Π½Π°Π»ΠΈΠ·Π° ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠΎΠ² ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΡ. Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ. Π Π°ΡΡΠΌΠΎΡΡΠ΅Π½Ρ ΡΠΏΠΎΡΠΎΠ±Ρ Π½ΠΎΡΠΌΠ°Π»ΠΈΠ·Π°ΡΠΈΠΈ ΠΌΠΈΠΊΡΠΎΠΊΠ»ΠΈΠΌΠ°ΡΠ° Π² Π³Π»ΡΠ±ΠΎΠΊΠΈΡ
ΠΏΡΠΎΡΡΠΆΠ΅Π½Π½ΡΡ
ΡΡΠΏΠΈΠΊΠΎΠ²ΡΡ
Π²ΡΡΠ°Π±ΠΎΡΠΊΠ°Ρ
, ΠΈΡ
ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ, ΠΏΡΠ΅ΠΈΠΌΡΡΠ΅ΡΡΠ²Π° ΠΈ Π½Π΅Π΄ΠΎΡΡΠ°ΡΠΊΠΈ. ΠΡΠ΅Π΄ΡΡΠ°Π²Π»Π΅Π½Π° ΠΌΠ°ΡΠ΅ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠ°Ρ ΠΌΠΎΠ΄Π΅Π»Ρ ΡΠ΅ΠΏΠ»ΠΎΠΌΠ°ΡΡΠΎΠΏΠ΅ΡΠ΅Π½ΠΎΡΠ° Π² Π°ΡΠΌΠΎΡΡΠ΅ΡΠ΅ Π³ΠΎΡΠ½ΠΎΠΉ Π²ΡΡΠ°Π±ΠΎΡΠΊΠΈ Ρ Π²Π΅Π½ΡΠΈΠ»ΡΡΠΈΠΎΠ½Π½ΡΠΌ ΡΡΡΠ±ΠΎΠΏΡΠΎΠ²ΠΎΠ΄ΠΎΠΌ, ΡΡΠΈΡΡΠ²Π°ΡΡΠ°Ρ ΠΊΠΎΠ½Π²Π΅ΠΊΡΠΈΠ²Π½ΡΠΉ ΠΈ Π»ΡΡΠΈΡΡΡΠΉ ΡΠ΅ΠΏΠ»ΠΎΠΎΠ±ΠΌΠ΅Π½. ΠΡΠ΅Π΄ΡΡΠ°Π²Π»Π΅Π½Ρ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΡΠ°ΡΡΠ΅ΡΠ° ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
ΡΠΏΠΎΡΠΎΠ±ΠΎΠ² ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΡ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ Π²ΠΎΠ·Π΄ΡΡ
Π°, ΠΏΠΎΠ΄Π°Π²Π°Π΅ΠΌΠΎΠ³ΠΎ Π² Π·Π°Π±ΠΎΠΉ Π³Π΅ΠΎΠ»ΠΎΠ³ΠΎΡΠ°Π·Π²Π΅Π΄ΠΎΡΠ½ΠΎΠΉ Π²ΡΡΠ°Π±ΠΎΡΠΊΠΈ, ΡΡΡΠΎΡΡΠ΅ΠΉΡΡ Π½Π° ΠΌΠ΅Π΄Π½ΠΎ-Π½ΠΈΠΊΠ΅Π»Π΅Π²ΠΎΠΌ ΡΡΠ΄Π½ΠΈΠΊΠ΅ ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠΈ ΠΠΠ Β«ΠΠΠ "ΠΠΎΡΠΈΠ»ΡΡΠΊΠΈΠΉ Π½ΠΈΠΊΠ΅Π»Ρ"Β». ΠΡΠΎΠ²Π΅Π΄Π΅Π½ ΡΡΠ°Π²Π½ΠΈΡΠ΅Π»ΡΠ½ΡΠΉ Π°Π½Π°Π»ΠΈΠ· ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
Π³ΠΎΡΠ½ΠΎΡΠ΅Ρ
Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈ ΡΠ΅ΠΏΠ»ΠΎΡΠ΅Ρ
Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΌΠ΅ΡΠΎΠΏΡΠΈΡΡΠΈΠΉ ΠΏΠΎ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΡ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ Π²ΠΎΠ·Π΄ΡΡ
Π° Π² Π·Π°Π±ΠΎΠ΅ Π²ΡΡΠ°Π±ΠΎΡΠΊΠΈ Π΄ΠΎ Π·Π½Π°ΡΠ΅Π½ΠΈΠΉ, Π΄ΠΎΠΏΡΡΡΠΈΠΌΡΡ
ΡΠΎΠ³Π»Π°ΡΠ½ΠΎ ΠΡΠ°Π²ΠΈΠ»Π°ΠΌ Π±Π΅Π·ΠΎΠΏΠ°ΡΠ½ΠΎΡΡΠΈ. ΠΡΡΠ²Π»Π΅Π½ΠΎ, ΡΡΠΎ ΡΠ²Π΅Π»ΠΈΡΠ΅Π½ΠΈΠ΅ ΠΎΠ±ΡΠ΅ΠΌΠ° ΠΏΠΎΠ΄Π°ΡΠΈ Π²ΠΎΠ·Π΄ΡΡ
Π° Π½Π΅ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΠ΅Ρ Π·Π½Π°ΡΠΈΡΠ΅Π»ΡΠ½ΠΎ ΡΠ½ΠΈΠ·ΠΈΡΡ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ Π² Π·Π°Π±ΠΎΠ΅. ΠΡΠΈΠΌΠ΅Π½Π΅Π½ΠΈΠ΅ ΡΠ΅ΠΏΠ»ΠΎΠΈΠ·ΠΎΠ»ΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠ³ΠΎ Π²Π΅Π½ΡΠΈΠ»ΡΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΡΡΡΠ±ΠΎΠΏΡΠΎΠ²ΠΎΠ΄Π° ΡΡΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎ ΡΠ½ΠΈΠΆΠ°Π΅Ρ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ ΠΏΠΎΠ΄Π°Π²Π°Π΅ΠΌΠΎΠ³ΠΎ Π² Π·Π°Π±ΠΎΠΉ Π²ΠΎΠ·Π΄ΡΡ
Π°, Π½ΠΎ Π΅Ρ Π·Π½Π°ΡΠ΅Π½ΠΈΠ΅ ΠΏΠΎ-ΠΏΡΠ΅ΠΆΠ½Π΅ΠΌΡ ΠΎΡΡΠ°Π΅ΡΡΡ Π²ΡΡΠ΅ Π΄ΠΎΠΏΡΡΡΠΈΠΌΡΡ
Π·Π½Π°ΡΠ΅Π½ΠΈΠΉ. ΠΠΎΠΊΠ°Π·Π°Π½ΠΎ, ΡΡΠΎ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΊΠ°ΠΌΠ΅ΡΡ ΠΎΡΠΎΡΠ΅Π½ΠΈΡ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΠ΅Ρ ΠΎΠ±Π΅ΡΠΏΠ΅ΡΠΈΡΡ Π΄ΠΎΠΏΡΡΡΠΈΠΌΡΡ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ Π²ΠΎΠ·Π΄ΡΡ
Π° Π² Π·ΠΈΠΌΠ½ΠΈΠΉ ΠΏΠ΅ΡΠΈΠΎΠ΄, Π½ΠΎ Π½Π΅ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΠ΅Ρ ΠΎΠ±Π΅ΡΠΏΠ΅ΡΠΈΡΡ Π΅Ρ Π² Π»Π΅ΡΠ½ΠΈΠΉ ΠΏΠ΅ΡΠΈΠΎΠ΄. ΠΠ°ΠΈΠ±ΠΎΠ»Π΅Π΅ ΡΠ½ΠΈΠ²Π΅ΡΡΠ°Π»ΡΠ½ΡΠΌ, ΡΡΡΠ΅ΠΊΡΠΈΠ²Π½ΡΠΌ, Π½ΠΎ Π΄ΠΎΡΠΎΠ³ΠΎΡΡΠΎΡΡΠΈΠΌ ΡΠΏΠΎΡΠΎΠ±ΠΎΠΌ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΡ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ Π²ΠΎΠ·Π΄ΡΡ
Π° ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΏΡΠΈΠΌΠ΅Π½Π΅Π½ΠΈΠ΅ ΠΏΠΎΠ΄Π·Π΅ΠΌΠ½ΡΡ
ΡΠΈΡΡΠ΅ΠΌ ΠΊΠΎΠ½Π΄ΠΈΡΠΈΠΎΠ½ΠΈΡΠΎΠ²Π°Π½ΠΈΡ Π²ΠΎΠ·Π΄ΡΡ
Π° Π½Π° Π±Π°Π·Π΅ ΠΏΠ°ΡΠΎΠΊΠΎΠΌΠΏΡΠ΅ΡΡΠΈΠΎΠ½Π½ΡΡ
ΠΌΠ°ΡΠΈΠ½.The relevance of the research is provided by the complexity of microclimate normalization in long blind drifts which are driven deeply through geothermally heated rocks. The aim of the research is the evaluation of usability of different ways for microclimate normalization in the working section of the exploration drift-2 in the mine of PJSC Β«MMC "Norilsk Nickel"Β». Objects: the exploration mine exploration drift-2 of PJSC Β«MMC "Norilsk Nickel"Β». Methods: the numerical simulation of heat and mass transfer in the atmosphere of the long exploration drift, the comparative analysis of simulation results. Results. The paper reviews ways, comparing their features, advantages, and disadvantages, for microclimate normalization in deep blind drifts. The presented mathematical model describes the heat and mass transfer in the working section of the blind drift with ventilation through the air duct. The model considers convective and radiant heat transfers. The results of the numerical simulation are given for different air-cooling methods which are applicable in the case of the deep copper-nickel mine of PJSC Β«MMC "Norilsk Nickel"Β». Drawing on this, different mining and thermal engineering operations for normalization of air temperatures in the working section regarding safety requirements are compared. It is defined that increasing the intake air flowrate could not decrease the air temperature near the face. The use of thermally insulated duct significantly decreases the air temperature in the working section but does not reduce it to the permitted value. It is shown, that the air irrigation could normalize temperatures in winter and not during the summer months. Underground air conditioning is the most universal and effective way for this purpose but highly expensive