29 research outputs found
ΠΠ»ΠΈΡΠ½ΠΈΠ΅ ΠΎΠΊΠ΅Π°Π½ΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΏΡΠΈΡΠΎΠΊΠ° ΡΠ΅ΠΏΠ»Π° Π² ΠΠ°ΡΠ΅Π½ΡΠ΅Π²ΠΎ ΠΌΠΎΡΠ΅ Π½Π° ΡΠ΅Π³ΠΈΠΎΠ½Π°Π»ΡΠ½ΡΠ΅ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ Π»Π΅Π΄ΠΎΠ²ΠΈΡΠΎΡΡΠΈ ΠΈ ΡΡΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΡΡΠΎΠΉΡΠΈΠ²ΠΎΡΡΠΈ Π°ΡΠΌΠΎΡΡΠ΅ΡΡ
The influence of the oceanic heat inflow into the Barents Sea on the sea ice concentration and atmospheric characteristics, including the atmospheric static stability during winter months, is investigated on the basis of the results of ensemble simulations with the regional climate model HIRHAM/NAOSIM for the Arctic. The static stability of the atmosphere is the important indicator of the spatial and temporal variability of polar mesocyclones in the Arctic region. The results of the HIRHAM/NAOSIM regional climate model ensemble simulations (RCM) for the period from 1979 to 2016 were used for the analysis. The initial and lateral boundary conditions for RCM in the atmosphere were set in accordance with the ERA-Interim reanalysis data. An analysis of 10Β ensemble simulations with identical boundary conditions and the same radiation forcing for the Arctic was performed. Various realizations of ensemble simulations with RCM were obtained by changing the initial conditions for integrating the oceanic block of the model. Different realizations of ensemble simulations with RCM are obtained by changing the initial conditions of the model oceanic block integration. The composites method was used for the analysis, i.e. the difference between the mean values for years with the maximum and minimum inflow of oceanic water into the Barents Sea. The statistical significance of the results (at a significance level of pΒ <Β 0.05) was estimated using Student's t-test. In general, the regional climate model reproduces the seasonal changes in the inflow of the oceanic water and heat into the Barents Sea reasonably well. There is a strong relationship between the changes in the oceanic water and ocean heat inflow, sea ice concentration, and surface air temperature in the Barents Sea. Herewith, the increase in the oceanic water inflow into the Barents Sea in winter leads to a decrease in static stability, which contributes to changes in regional cyclonic activity. The decrease of the static stability is most pronounced in the southern part of the Barents Sea and also to the west of Svalbard.ΠΠ° ΠΎΡΠ½ΠΎΠ²Π΅ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠΎΠ² Π°Π½ΡΠ°ΠΌΠ±Π»Π΅Π²ΡΡ
ΡΠ°ΡΡΡΡΠΎΠ² Ρ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ ΡΠ΅Π³ΠΈΠΎΠ½Π°Π»ΡΠ½ΠΎΠΉ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΠΌΠΎΠ΄Π΅Π»ΠΈ HIRHAM/NAOSIM Π΄Π»Ρ ΠΡΠΊΡΠΈΠΊΠΈ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΎ Π²Π»ΠΈΡΠ½ΠΈΠ΅ ΠΏΡΠΈΡΠΎΠΊΠ° ΠΎΠΊΠ΅Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
Π²ΠΎΠ΄ Π² ΠΠ°ΡΠ΅Π½ΡΠ΅Π²ΠΎ ΠΌΠΎΡΠ΅ Π½Π° ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΡ ΠΌΠΎΡΡΠΊΠΈΡ
Π»ΡΠ΄ΠΎΠ² ΠΈ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠΈ Π°ΡΠΌΠΎΡΡΠ΅ΡΡ Π² Π·ΠΈΠΌΠ½ΠΈΠ΅ ΠΌΠ΅ΡΡΡΡ. ΠΠΎΠΊΠ°Π·Π°Π½Π° ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΡΡΠ°Ρ ΡΠΎΠ»Ρ Π²Π°ΡΠΈΠ°ΡΠΈΠΉ ΠΏΡΠΈΡΠΎΠΊΠ° ΠΎΠΊΠ΅Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
Π²ΠΎΠ΄ Π² ΠΠ°ΡΠ΅Π½ΡΠ΅Π²ΠΎ ΠΌΠΎΡΠ΅ Π½Π° ΡΠ΅ΠΆΠΈΠΌ ΠΌΠΎΡΡΠΊΠΈΡ
Π»ΡΠ΄ΠΎΠ² ΠΈ ΠΏΡΠΈΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠ½ΠΎΠΉ ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡΡ Π²ΠΎΠ·Π΄ΡΡ
Π°, Π° ΡΠ°ΠΊΠΆΠ΅ ΡΡΠ°ΡΠΈΡΠ΅ΡΠΊΡΡ ΡΡΡΠΎΠΉΡΠΈΠ²ΠΎΡΡΡ Π°ΡΠΌΠΎΡΡΠ΅ΡΡ Π² Π·ΠΈΠΌΠ½ΠΈΠΉ ΠΏΠ΅ΡΠΈΠΎΠ΄
ΠΠ΅ΡΡΠΎ ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΡΡ ΠΏΡΠΎΠ΄ΡΠΊΡΠΎΠ² ΠΏΡΠΈΠΊΠΎΡΠΌΠ° Π² ΠΊΡΠΈΡΠΈΡΠ΅ΡΠΊΠΎΠΌ ΠΏΠ΅ΡΠΈΠΎΠ΄Π΅ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ Π·Π΄ΠΎΡΠΎΠ²ΡΡ ΡΠ΅Π±Π΅Π½ΠΊΠ°
The current development of medicine and the results of recent large-scale academic research in pediatrics provide the convincing conclusions that the formation of human health begins in the antenatal period of ontogenesis and continues throughout the infancy. The ideas and subsequent academic research on the influence of nutrition during the first thousand days of life on the programming of metabolism and the development of some chronic somatic diseases such as obesity, hypertension, coronary heart disease have become widespread. In addition, at the same period of life immune abnormalities with a predominance of one of the subpopulations, Th1 or Th2, can possibly form in children at risk of developing allergies when immune response is developing. The predominance of the Th2 cytokine profile (hyperproduction of interleukins 4, 5, 13, etc.) suggests the possibility of stable formation of the atopic status in a child afterwards. Consequently, the application of academic knowledge on the health status programming by nutrition during early ontogenesis is an important tool in preventive pediatric practice.Π Π°Π·Π²ΠΈΡΠΈΠ΅ ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΠΎΠΉ ΠΌΠ΅Π΄ΠΈΡΠΈΠ½Ρ, ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΏΠΎΡΠ»Π΅Π΄Π½ΠΈΡ
ΠΌΠ°ΡΡΡΠ°Π±Π½ΡΡ
Π½Π°ΡΡΠ½ΡΡ
ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ Π² ΠΏΠ΅Π΄ΠΈΠ°ΡΡΠΈΠΈ ΠΏΡΠΈΠ²ΠΎΠ΄ΡΡ ΠΊ ΡΠ±Π΅Π΄ΠΈΡΠ΅Π»ΡΠ½ΡΠΌ Π²ΡΠ²ΠΎΠ΄Π°ΠΌ, ΡΡΠΎ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ Π·Π΄ΠΎΡΠΎΠ²ΡΡ ΡΠ΅Π»ΠΎΠ²Π΅ΠΊΠ° Π½Π°ΡΠΈΠ½Π°Π΅ΡΡΡ Π² Π°Π½ΡΠ΅Π½Π°ΡΠ°Π»ΡΠ½ΠΎΠΌ ΠΏΠ΅ΡΠΈΠΎΠ΄Π΅ ΠΎΠ½ΡΠΎΠ³Π΅Π½Π΅Π·Π° ΠΈ ΠΏΡΠΎΠ΄ΠΎΠ»ΠΆΠ°Π΅ΡΡΡ Π½Π° ΠΏΡΠΎΡΡΠΆΠ΅Π½ΠΈΠΈ ΡΠ°Π½Π½Π΅Π³ΠΎ Π΄Π΅ΡΡΠΊΠΎΠ³ΠΎ Π²ΠΎΠ·ΡΠ°ΡΡΠ°. Π¨ΠΈΡΠΎΠΊΠΎΠ΅ ΡΠ°ΡΠΏΡΠΎΡΡΡΠ°Π½Π΅Π½ΠΈΠ΅ ΠΏΠΎΠ»ΡΡΠΈΠ»ΠΈ ΠΈΠ΄Π΅ΠΈ ΠΈ ΠΏΠΎΡΠ»Π΅Π΄ΠΎΠ²Π°Π²ΡΠΈΠ΅ Π·Π° Π½ΠΈΠΌΠΈ Π½Π°ΡΡΠ½ΡΠ΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ ΠΎ Π²Π»ΠΈΡΠ½ΠΈΠΈ ΠΏΠΈΡΠ°Π½ΠΈΡ ΠΏΠ΅ΡΠ²ΡΡ
ΡΡΡΡΡΠΈ Π΄Π½Π΅ΠΉ ΠΆΠΈΠ·Π½ΠΈ Π² ΠΏΡΠΎΠ³ΡΠ°ΠΌΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΠΈ ΠΌΠ΅ΡΠ°Π±ΠΎΠ»ΠΈΠ·ΠΌΠ° ΠΈ ΡΠ°Π·Π²ΠΈΡΠΈΠΈ Π½Π΅ΠΊΠΎΡΠΎΡΡΡ
Ρ
ΡΠΎΠ½ΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠΎΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
Π±ΠΎΠ»Π΅Π·Π½Π΅ΠΉ, ΡΠ°ΠΊΠΈΡ
ΠΊΠ°ΠΊ ΠΎΠΆΠΈΡΠ΅Π½ΠΈΠ΅, Π³ΠΈΠΏΠ΅ΡΡΠΎΠ½ΠΈΡΠ΅ΡΠΊΠ°Ρ Π±ΠΎΠ»Π΅Π·Π½Ρ, ΠΈΡΠ΅ΠΌΠΈΡΠ΅ΡΠΊΠ°Ρ Π±ΠΎΠ»Π΅Π·Π½Ρ ΡΠ΅ΡΠ΄ΡΠ°. ΠΠΌΠ΅ΡΡΠ΅ Ρ ΡΠ΅ΠΌ Π² ΡΡΠΎΡ ΠΆΠ΅ ΠΏΠ΅ΡΠΈΠΎΠ΄ ΠΆΠΈΠ·Π½ΠΈ Ρ Π΄Π΅ΡΠ΅ΠΉ Π³ΡΡΠΏΠΏ ΡΠΈΡΠΊΠ° ΠΏΠΎ ΡΠ°Π·Π²ΠΈΡΠΈΡ Π°Π»Π»Π΅ΡΠ³ΠΈΠΈ ΠΏΡΠΈ ΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΈΠΈ ΠΈΠΌΠΌΡΠ½Π½ΠΎΠ³ΠΎ ΠΎΡΠ²Π΅ΡΠ° Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎ ΠΏΡΠΎΠ³ΡΠ°ΠΌΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ ΠΈΠΌΠΌΡΠ½Π½ΡΡ
ΠΎΡΠΊΠ»ΠΎΠ½Π΅Π½ΠΈΠΉ Ρ ΠΏΡΠ΅ΠΎΠ±Π»Π°Π΄Π°Π½ΠΈΠ΅ΠΌ ΠΎΠ΄Π½ΠΎΠΉ ΠΈΠ· ΡΡΠ±ΠΏΠΎΠΏΡΠ»ΡΡΠΈΠΉ β Th1 ΠΈΠ»ΠΈ Th2. ΠΡΠ΅ΠΎΠ±Π»Π°Π΄Π°Π½ΠΈΠ΅ ΡΠΈΡΠΎΠΊΠΈΠ½ΠΎΠ²ΠΎΠ³ΠΎ ΠΏΡΠΎΡΠΈΠ»Ρ Th2 (Π³ΠΈΠΏΠ΅ΡΠΏΡΠΎΠ΄ΡΠΊΡΠΈΡ ΠΈΠ½ΡΠ΅ΡΠ»Π΅ΠΉΠΊΠΈΠ½ΠΎΠ² 4, 5, 13 ΠΈ Π΄Ρ.) ΠΏΡΠ΅Π΄ΠΏΠΎΠ»Π°Π³Π°Π΅Ρ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡΡ ΡΡΠΎΠΉΠΊΠΎΠ³ΠΎ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ Π°ΡΠΎΠΏΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΡΡΠ°ΡΡΡΠ° ΡΠ΅Π±Π΅Π½ΠΊΠ° Π² Π΄Π°Π»ΡΠ½Π΅ΠΉΡΠ΅ΠΌ. Π‘Π»Π΅Π΄ΠΎΠ²Π°ΡΠ΅Π»ΡΠ½ΠΎ, ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ Π½Π°ΡΡΠ½ΡΡ
Π·Π½Π°Π½ΠΈΠΉ ΠΎ ΠΏΡΠΎΠ³ΡΠ°ΠΌΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΠΈ ΡΠΎΡΡΠΎΡΠ½ΠΈΡ Π·Π΄ΠΎΡΠΎΠ²ΡΡ ΠΏΠΈΡΠ°Π½ΠΈΠ΅ΠΌ Π² ΠΏΡΠΎΡΠ΅ΡΡΠ΅ ΡΠ°Π½Π½Π΅Π³ΠΎ ΠΎΠ½ΡΠΎΠ³Π΅Π½Π΅Π·Π° ΡΠ²Π»ΡΠ΅ΡΡΡ Π²Π°ΠΆΠ½ΡΠΌ ΠΈΠ½ΡΡΡΡΠΌΠ΅Π½ΡΠΎΠΌ Π² ΠΏΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΠΏΡΠΎΡΠΈΠ»Π°ΠΊΡΠΈΡΠ΅ΡΠΊΠΎΠΉ ΠΏΠ΅Π΄ΠΈΠ°ΡΡΠΈΠΈ.ΠΠΠΠ€ΠΠΠΠ’ ΠΠΠ’ΠΠ ΠΠ‘ΠΠΠ’.Π. Π’ΡΡΡΠΈ, Π.Π. ΠΠΎΠΊΡΡΠ°Π²Π° ΡΠΎΡΡΡΠ΄Π½ΠΈΡΠ°ΡΡ Ρ ΠΠ Β«ΠΠ ΠΠΠ ΠΠ‘Π‘Β».Π.Π. ΠΠ΅Π»ΡΠ΅Π²Π° ΡΠΎΡΡΡΠ΄Π½ΠΈΡΠ°Π΅Ρ Ρ ΠΊΠΎΠΌΠΏΠ°Π½ΠΈΠ΅ΠΉ Β«ΠΡΠ°ΠΉΠ·Π΅Ρ ΠΠ½Π½ΠΎΠ²Π°ΡΠΈΠΈΒ».ΠΡΡΠ°Π»ΡΠ½ΡΠ΅ Π°Π²ΡΠΎΡΡ ΡΡΠ°ΡΡΠΈ ΠΏΠΎΠ΄ΡΠ²Π΅ΡΠ΄ΠΈΠ»ΠΈ ΠΎΡΡΡΡΡΡΠ²ΠΈΠ΅ ΠΊΠΎΠ½ΡΠ»ΠΈΠΊΡΠ° ΠΈΠ½ΡΠ΅ΡΠ΅ΡΠΎΠ²
The Application of Scanning Contact Potentiometry Method and Diffraction of Thermal Neutrons at Physico-Mechanical Tests of Materials
The results of physical and mechanical tests on the tensile strength of austenitic steel 12X18H10T, in the stress range from 100 MPa to the maximum value of 700 MPa, at which the sample was destroyed, are presented. Structural changes were registered synchronously by two methods: the method of scanning contact potentiometry and the method of diffraction of thermal neutrons. At loads above 650 MPa, the Ξ±-martensite phase was found in the austenite matrix, as well as the appearance of diffraction peaks characteristic of a cubic martensitic BCC lattice was observed in neutron spectra. On the potentiograms, this process corresponds to the appearance of local regions in which high values of electric potential gradients were observed. This is the case of discovery of the fatigue nucleus cracks in the tensile testing of steel ΠΠ847 by the method of scanning contact potentiometry
The influence of ocean heat transport in the Barents Sea on the regional sea ice and the atmospheric static stability
The influence of the oceanic heat inflow into the Barents Sea on the sea ice concentration and atmospheric characteristics, including the atmospheric static stability during winter months, is investigated on the basis of the results of ensemble simulations with the regional climate model HIRHAM/NAOSIM for the Arctic. The static stability of the atmosphere is the important indicator of the spatial and temporal variability of polar mesocyclones in the Arctic region. The results of the HIRHAM/NAOSIM regional climate model ensemble simulations (RCM) for the period from 1979 to 2016 were used for the analysis. The initial and lateral boundary conditions for RCM in the atmosphere were set in accordance with the ERA-Interim reanalysis data. An analysis of 10Β ensemble simulations with identical boundary conditions and the same radiation forcing for the Arctic was performed. Various realizations of ensemble simulations with RCM were obtained by changing the initial conditions for integrating the oceanic block of the model. Different realizations of ensemble simulations with RCM are obtained by changing the initial conditions of the model oceanic block integration. The composites method was used for the analysis, i.e. the difference between the mean values for years with the maximum and minimum inflow of oceanic water into the Barents Sea. The statistical significance of the results (at a significance level of pΒ <Β 0.05) was estimated using Student's t-test. In general, the regional climate model reproduces the seasonal changes in the inflow of the oceanic water and heat into the Barents Sea reasonably well. There is a strong relationship between the changes in the oceanic water and ocean heat inflow, sea ice concentration, and surface air temperature in the Barents Sea. Herewith, the increase in the oceanic water inflow into the Barents Sea in winter leads to a decrease in static stability, which contributes to changes in regional cyclonic activity. The decrease of the static stability is most pronounced in the southern part of the Barents Sea and also to the west of Svalbard
Detector for the FSD FourierDiffractometer Based on ZnS(Ag)/^{6}LiF Scintillation Screen and Wavelength Shifting Fibers Readout
At the IBR2 pulsed reactor (FLNP, JINR, Dubna), a specialized timeofflight instrument FourierStressDiffractometer (FSD) intended for the measurement of internal steresses in bulk samples by using highresolution neutron diffraction is under construction. One of the main components of the diffractometer is a newtype detector with combined electronic geometrical focusing uniting a large solid angle and a small geometry contribution to the instrumental resolution. The first two modules of the detector, based on scintillation screen ZnS(Ag)/^{6}LiF with wavelength shifting fibers readout have been developed and tested. The design of the detector and associated electronics are described. The method of time focusing surface approximation, using the screen flexibility is proposed. Characteristics of tested modules in comparison with a detector of previous generation are presented and advantages of new detector design for highresolution diffractometry are discussed