327 research outputs found

    Adsorption-desorption kinetics in nanoscopically confined oligomer films under shear

    Get PDF
    The method of molecular dynamics computer simulations is employed to study oligomer melts confined in ultra-thin films and subjected to shear. The focus is on the self-diffusion of oligomers near attractive surfaces and on their desorption, together with the effects of increasing energy of adsorption and shear. It is found that the mobility of the oligomers near an attractive surface is strongly decreased. Moreover, although shearing the system forces the chains to stretch parallel to the surfaces and thus increase the energy of adsorption per chain, flow also promotes desorption. The study of chain desorption kinetics reveals the molecular processes responsible for the enhancement of desorption under shear. They involve sequences of conformations starting with a desorbed tail and proceeding in a very fast, correlated, segment-by-segment manner to the desorption of the oligomers from the surfaces.

    Quantum equivalence of sigma models related by non Abelian Duality Transformations

    Get PDF
    Coupling constant renormalization is investigated in 2 dimensional sigma models related by non Abelian duality transformations. In this respect it is shown that in the one loop order of perturbation theory the duals of a one parameter family of models, interpolating between the SU(2) principal model and the O(3) sigma model, exhibit the same behaviour as the original models. For the O(3) model also the two loop equivalence is investigated, and is found to be broken just like in the already known example of the principal model.Comment: As a result of the collaboration of new authors the previously overlooked gauge contribution is inserted into eq.(43) changing not so much the formulae as part of the conclusion: for the models considered non Abelian duality is OK in one loo

    БостояниС ΠΈΡ…Ρ‚ΠΈΠΎ-, ΠΌΠ΅Π·ΠΎ- ΠΈ ΠΌΠ°ΠΊΡ€ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π½Ρ‹Ρ… комплСксов Ρƒ ΠšΡ€Ρ‹ΠΌΡΠΊΠΎΠ³ΠΎ полуострова (Π§Ρ‘Ρ€Π½ΠΎΠ΅ ΠΌΠΎΡ€Π΅) Π² связи с особСнностями гидрологичСского Ρ€Π΅ΠΆΠΈΠΌΠ° Π² октябрС 2016 Π³.

    Get PDF
    ΠšΠ»ΠΈΠΌΠ°Ρ‚ΠΈΡ‡Π΅ΡΠΊΠΈΠ΅ измСнСния Π² гидрологичСском Ρ€Π΅ΠΆΠΈΠΌΠ΅ Π§Ρ‘Ρ€Π½ΠΎΠ³ΠΎ моря, ΠΎΡ‚ΠΌΠ΅Ρ‡Π°Π΅ΠΌΡ‹Π΅ с 1990-Ρ… Π³Π³., ΠΎΡ‚Ρ€Π°Π·ΠΈΠ»ΠΈΡΡŒ Π½Π° состоянии эпипСлагичСских комплСксов морских ΠΎΡ€Π³Π°Π½ΠΈΠ·ΠΌΠΎΠ², ΠΏΡ€Π΅ΠΆΠ΄Π΅ всСго Π½Π° сСзонной измСнчивости ΠΈΡ… биологичСских Ρ†ΠΈΠΊΠ»ΠΎΠ². Π­Ρ‚ΠΎ ΠΎΠΊΠ°Π·Π°Π»ΠΎ сущСствСнноС влияниС Π½Π° Ρ„Π΅Π½ΠΎΠ»ΠΎΠ³ΠΈΡŽ нСрСста ΠΏΡ€ΠΈΡ€ΠΎΠ΄Π½Ρ‹Ρ… популяций Ρ€Ρ‹Π±, Π²ΠΈΠ΄ΠΎΠ²ΠΎΠ΅ Ρ€Π°Π·Π½ΠΎΠΎΠ±Ρ€Π°Π·ΠΈΠ΅ ΠΈ пространствСнноС распрСдСлСниС ΠΈΡ…Ρ‚ΠΈΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π°, Π° Ρ‚Π°ΠΊΠΆΠ΅ Π½Π° ΡƒΡΡ‚ΠΎΡΠ²ΡˆΠΈΠ΅ΡΡ трофичСскиС Π²Π·Π°ΠΈΠΌΠΎΠΎΡ‚Π½ΠΎΡˆΠ΅Π½ΠΈΡ Π² ΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π½ΠΎΠΌ сообщСствС. Π’ ΠΊΠΎΠ½Π΅Ρ‡Π½ΠΎΠΌ ΠΈΡ‚ΠΎΠ³Π΅ Ρ…Π°Ρ€Π°ΠΊΡ‚Π΅Ρ€ взаимодСйствия ΠΌΠ΅ΠΆΠ΄Ρƒ Ρ€Π°Π·Π»ΠΈΡ‡Π½Ρ‹ΠΌΠΈ звСньями трофичСской Ρ†Π΅ΠΏΠΈ Π² эпипСлагичСских комплСксах, ΠΈΡ… сСзонная ΠΈ мСТгодовая ΠΈΠ·ΠΌΠ΅Π½Ρ‡ΠΈΠ²ΠΎΡΡ‚ΡŒ Π²Π»ΠΈΡΡŽΡ‚ Π½Π° ΡΡ„Ρ„Π΅ΠΊΡ‚ΠΈΠ²Π½ΠΎΡΡ‚ΡŒ нСрСста Ρ€Ρ‹Π±, ΠΏΡ€Π΅ΠΆΠ΄Π΅ всСго массовых промысловых Π²ΠΈΠ΄ΠΎΠ², ΠΈ Π² Π·Π½Π°Ρ‡ΠΈΡ‚Π΅Π»ΡŒΠ½ΠΎΠΉ стСпСни ΠΎΠΏΡ€Π΅Π΄Π΅Π»ΡΡŽΡ‚ успСх пополнСния ΠΈΡ… Π±ΡƒΠ΄ΡƒΡ‰ΠΈΡ… ΠΏΠΎΠΊΠΎΠ»Π΅Π½ΠΈΠΉ. Π‘ Ρ†Π΅Π»ΡŒΡŽ изучСния Π²ΠΈΠ΄ΠΎΠ²ΠΎΠ³ΠΎ состава, числСнности ΠΈ пространствСнного распрСдСлСния ΠΈΡ…Ρ‚ΠΈΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π° Π² октябрС 2016 Π³. (89-ΠΉ рСйс НИБ Β«ΠŸΡ€ΠΎΡ„Π΅ΡΡΠΎΡ€ Водяницкий», 30 сСнтября β€” 19 октября) Π±Ρ‹Π»ΠΈ ΠΏΡ€ΠΎΠ²Π΅Π΄Π΅Π½Ρ‹ исслСдования Π² ΡˆΠ΅Π»ΡŒΡ„ΠΎΠ²Ρ‹Ρ… ΠΈ ΠΎΡ‚ΠΊΡ€Ρ‹Ρ‚Ρ‹Ρ… Π²ΠΎΠ΄Π°Ρ… Π§Ρ‘Ρ€Π½ΠΎΠ³ΠΎ моря Ρƒ ΠšΡ€Ρ‹ΠΌΡΠΊΠΎΠ³ΠΎ полуострова, ΠΏΡ€ΠΎΠ°Π½Π°Π»ΠΈΠ·ΠΈΡ€ΠΎΠ²Π°Π½Ρ‹ Π½Π΅ Ρ‚ΠΎΠ»ΡŒΠΊΠΎ ΠΈΠΊΡ€Π° ΠΈ Π»ΠΈΡ‡ΠΈΠ½ΠΊΠΈ Ρ€Ρ‹Π±, Π½ΠΎ ΠΈ биомасса ΠΌΠ΅Π·ΠΎ- ΠΈ ΠΌΠ°ΠΊΡ€ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π°. ΠŸΡ€ΠΎΠ±Ρ‹ ΠΈΡ…Ρ‚ΠΈΠΎ- ΠΈ ΠΌΠ°ΠΊΡ€ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π° ΠΎΡ‚Π±ΠΈΡ€Π°Π»ΠΈ ΡΠ΅Ρ‚ΡŒΡŽ Π‘ΠΎΠ³ΠΎΡ€ΠΎΠ²Π° β€” Расса (ΠΏΠ»ΠΎΡ‰Π°Π΄ΡŒ Π²Ρ…ΠΎΠ΄Π½ΠΎΠ³ΠΎ отвСрстия β€” 0,5 ΠΌΒ²; ячСя β€” 300 ΠΌΠΊΠΌ) ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΎΠΌ Ρ‚ΠΎΡ‚Π°Π»ΡŒΠ½Ρ‹Ρ… Π²Π΅Ρ€Ρ‚ΠΈΠΊΠ°Π»ΡŒΠ½Ρ‹Ρ… Π»ΠΎΠ²ΠΎΠ² ΠΎΡ‚ Π΄Π½Π° Π΄ΠΎ повСрхности моря Π² области ΡˆΠ΅Π»ΡŒΡ„Π° ΠΈ ΠΎΡ‚ Π½ΠΈΠΆΠ½Π΅ΠΉ Π³Ρ€Π°Π½ΠΈΡ†Ρ‹ кислородной Π·ΠΎΠ½Ρ‹ Π΄ΠΎ повСрхности моря Π² Π³Π»ΡƒΠ±ΠΎΠΊΠΎΠ²ΠΎΠ΄Π½ΠΎΠΉ части. Π˜Ρ…Ρ‚ΠΈΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½ фиксировали 4%-Π½Ρ‹ΠΌ раствором Ρ„ΠΎΡ€ΠΌΠ°Π»ΠΈΠ½Π° ΠΈ Π°Π½Π°Π»ΠΈΠ·ΠΈΡ€ΠΎΠ²Π°Π»ΠΈ ΠΏΠΎΠ·ΠΆΠ΅ ΠΏΠΎΠ΄ микроскопом, опрСдСляя таксономичСский состав ΠΎΡ€Π³Π°Π½ΠΈΠ·ΠΌΠΎΠ² ΠΈ ΠΏΠΎ возмоТности β€” Π½Π°Π»ΠΈΡ‡ΠΈΠ΅ ΠΈ состав ΠΏΠΈΡ‰ΠΈ Π² ΠΊΠΈΡˆΠ΅Ρ‡Π½ΠΈΠΊΠ°Ρ… Π»ΠΈΡ‡ΠΈΠ½ΠΎΠΊ Ρ€Ρ‹Π±. ΠŸΡ€ΠΎΠ°Π½Π°Π»ΠΈΠ·ΠΈΡ€ΠΎΠ²Π°Π½Ρ‹ Π΄Π°Π½Π½Ρ‹Π΅ ΠΎ Π²ΠΈΠ΄ΠΎΠ²ΠΎΠΌ составС ΠΈ пространствСнном распрСдСлСнии ΠΈΡ…Ρ‚ΠΈΠΎ-, ΠΌΠ΅Π·ΠΎ- ΠΈ ΠΌΠ°ΠΊΡ€ΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π°, Π° Ρ‚Π°ΠΊΠΆΠ΅ ΠΎ ΠΏΠΈΡ‚Π°Π½ΠΈΠΈ Π»ΠΈΡ‡ΠΈΠ½ΠΎΠΊ Ρ€Ρ‹Π± Π§Ρ‘Ρ€Π½ΠΎΠ³ΠΎ моря Ρƒ ΠšΡ€Ρ‹ΠΌΡΠΊΠΎΠ³ΠΎ полуострова Π² октябрС 2016 Π³. ΠŸΠ΅Ρ€ΠΈΠΎΠ΄ ΡΡŠΡ‘ΠΌΠΊΠΈ соотвСтствовал Π½Π°Ρ‡Π°Π»ΡŒΠ½ΠΎΠΉ Ρ„Π°Π·Π΅ осСннСго гидрологичСского сСзона. Π˜Ρ…Ρ‚ΠΈΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½ Π±Ρ‹Π» прСдставлСн ΠΈΠΊΡ€ΠΎΠΉ ΠΈ Π»ΠΈΡ‡ΠΈΠ½ΠΊΠ°ΠΌΠΈ 9 Π²ΠΈΠ΄ΠΎΠ² Ρ‚Π΅ΠΏΠ»ΠΎΠ²ΠΎΠ΄Π½Ρ‹Ρ… ΠΈ 6 Π²ΠΈΠ΄ΠΎΠ² ΡƒΠΌΠ΅Ρ€Π΅Π½Π½ΠΎΠ²ΠΎΠ΄Π½Ρ‹Ρ… Ρ€Ρ‹Π±. БрСдняя Ρ‡ΠΈΡΠ»Π΅Π½Π½ΠΎΡΡ‚ΡŒ ΠΈΠΊΡ€Ρ‹ Ρ€Ρ‹Π± составляла 2,92, Π° Π»ΠΈΡ‡ΠΈΠ½ΠΎΠΊ β€” 3,56 экз.Β·ΠΌβˆ’2. Низкая доля (30 %) ΠΌΡ‘Ρ€Ρ‚Π²ΠΎΠΉ ΠΈΠΊΡ€Ρ‹ Ρ‚Π΅ΠΏΠ»ΠΎΠ²ΠΎΠ΄Π½ΠΎΠΉ хамсы Engraulis encrasicolus, Π° Ρ‚Π°ΠΊΠΆΠ΅ Π½Π°Π»ΠΈΡ‡ΠΈΠ΅ Π΅Ρ‘ Ρ€Π°Π·Π½ΠΎΡ€Π°Π·ΠΌΠ΅Ρ€Π½Ρ‹Ρ… Π»ΠΈΡ‡ΠΈΠ½ΠΎΠΊ Π² ΠΌΠΎΡ€Π΅ ΡΠ²ΠΈΠ΄Π΅Ρ‚Π΅Π»ΡŒΡΡ‚Π²ΠΎΠ²Π°Π»ΠΈ ΠΎ ΠΏΡ€ΠΎΠ΄ΠΎΠ»ΠΆΠ΅Π½ΠΈΠΈ Ρ€Π΅Π·ΡƒΠ»ΡŒΡ‚Π°Ρ‚ΠΈΠ²Π½ΠΎΠ³ΠΎ нСрСста. Биомасса Π·ΠΎΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π° возрастала Π² Π½Π°ΠΏΡ€Π°Π²Π»Π΅Π½ΠΈΠΈ ΠΎΡ‚ ΡˆΠ΅Π»ΡŒΡ„Π° ΠΊ Π³Π»ΡƒΠ±ΠΎΠΊΠΎΠ²ΠΎΠ΄Π½Ρ‹ΠΌ Ρ€Π°ΠΉΠΎΠ½Π°ΠΌ. ΠœΠ΅Π»ΠΊΠΎΡ€Π°Π·ΠΌΠ΅Ρ€Π½Ρ‹Π΅ Ρ„Ρ€Π°ΠΊΡ†ΠΈΠΈ ΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π½Ρ‹Ρ… ΠΎΡ€Π³Π°Π½ΠΈΠ·ΠΌΠΎΠ² ΠΏΡ€Π΅ΠΎΠ±Π»Π°Π΄Π°Π»ΠΈ Π½Π° ΡˆΠ΅Π»ΡŒΡ„Π΅, обСспСчивая здСсь Π»ΡƒΡ‡ΡˆΠΈΠ΅ ΠΊΠΎΡ€ΠΌΠΎΠ²Ρ‹Π΅ условия для выТивания Π»ΠΈΡ‡ΠΈΠ½ΠΎΠΊ Ρ€Ρ‹Π±. НСсмотря Π½Π° Π·Π½Π°Ρ‡ΠΈΡ‚Π΅Π»ΡŒΠ½ΡƒΡŽ биомассу ΠΆΠ΅Π»Π΅Ρ‚Π΅Π»Ρ‹Ρ…-ΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΡ„Π°Π³ΠΎΠ² Π² октябрС 2016 Π³., ΠΈΡ… влияниС Π½Π° ΠΈΡ…Ρ‚ΠΈΠΎΠΏΠ»Π°Π½ΠΊΡ‚ΠΎΠ½Π½Ρ‹Π΅ комплСксы Π§Ρ‘Ρ€Π½ΠΎΠ³ΠΎ моря, ΠΏΠΎ-Π²ΠΈΠ΄ΠΈΠΌΠΎΠΌΡƒ, ΠΎΡΡ‚Π°Π²Π°Π»ΠΎΡΡŒ нСсущСствСнным

    Structural and transport properties of GaAs/delta<Mn>/GaAs/InxGa1-xAs/GaAs quantum wells

    Full text link
    We report results of investigations of structural and transport properties of GaAs/Ga(1-x)In(x)As/GaAs quantum wells (QWs) having a 0.5-1.8 ML thick Mn layer, separated from the QW by a 3 nm thick spacer. The structure has hole mobility of about 2000 cm2/(V*s) being by several orders of magnitude higher than in known ferromagnetic two-dimensional structures. The analysis of the electro-physical properties of these systems is based on detailed study of their structure by means of high-resolution X-ray diffractometry and glancing-incidence reflection, which allow us to restore the depth profiles of structural characteristics of the QWs and thin Mn containing layers. These investigations show absence of Mn atoms inside the QWs. The quality of the structures was also characterized by photoluminescence spectra from the QWs. Transport properties reveal features inherent to ferromagnetic systems: a specific maximum in the temperature dependence of the resistance and the anomalous Hall effect (AHE) observed in samples with both "metallic" and activated types of conductivity up to ~100 K. AHE is most pronounced in the temperature range where the resistance maximum is observed, and decreases with decreasing temperature. The results are discussed in terms of interaction of 2D-holes and magnetic Mn ions in presence of large-scale potential fluctuations related to random distribution of Mn atoms. The AHE values are compared with calculations taking into account its "intrinsic" mechanism in ferromagnetic systems.Comment: 15 pages, 9 figure

    Normal families of functions and groups of pseudoconformal diffeomorphisms of quaternion and octonion variables

    Full text link
    This paper is devoted to the specific class of pseudoconformal mappings of quaternion and octonion variables. Normal families of functions are defined and investigated. Four criteria of a family being normal are proven. Then groups of pseudoconformal diffeomorphisms of quaternion and octonion manifolds are investigated. It is proven, that they are finite dimensional Lie groups for compact manifolds. Their examples are given. Many charactersitic features are found in comparison with commutative geometry over R\bf R or C\bf C.Comment: 55 pages, 53 reference

    New limits on the resonant absorption of solar axions obtained with a 169^{169}Tm-containing cryogenic detector

    Full text link
    A search for resonant absorption of solar axions by 169^{169}Tm nuclei was carried out. A newly developed approach involving low-background cryogenic bolometer based on Tm3_3Al5_5O12_{12} crystal was used that allowed for significant improvement of sensitivity in comparison with previous 169^{169}Tm based experiments. The measurements performed with 8.188.18 g crystal during 6.66.6 days exposure yielded the following limits on axion couplings: ∣gAΞ³(gAN0+gAN3)≀1.44Γ—10βˆ’14|g_{A\gamma} (g_{AN}^0 + g_{AN}^3) \leq 1.44 \times 10^{-14} GeVβˆ’1^{-1} and ∣gAe(gAN0+gAN3)≀2.81Γ—10βˆ’16|g_{Ae} (g_{AN}^0 + g_{AN}^3) \leq 2.81 \times 10^{-16}.Comment: 7 pages, 5 figure

    Comparing electron precipitation fluxes calculated from pitch angle diffusion coefficients to LEO satellite observations

    Get PDF
    Particle precipitation is a loss mechanism from the Radiation Belts whereby particles trapped by the Earth’s magnetic field are scattered into the loss cone due to wave‐particle interactions. Energetic electron precipitation creates ozone destroying chemicals which can affect the temperatures of the polar regions, therefore it is crucial to accurately quantify this impact on the Earth’s atmosphere. We use bounce‐averaged pitch angle diffusion coefficients for whistler mode chorus waves, plasmaspheric hiss and atmospheric collisions to calculate magnetic local time (MLT) dependent electron precipitation inside the field of view of the Polar Orbiting Environmental Satellites (POES) T0 detector, between 26‐30 March 2013. These diffusion coefficients are used in the BAS Radiation Belt Model (BAS‐RBM) and this paper is a first step towards testing the loss in this model via comparison with real world data. We find the best agreement between the calculated and measured T0 precipitation at L* > 5 on the dawnside for the > 30keV electron channel, consistent with precipitation driven by lower band chorus. Additional diffusion is required to explain the flux at higher energies and on the dusk side. The POES T0 detector underestimates electron precipitation as its field of view does not measure the entire loss cone. We demonstrate the potential for utilizing diffusion coefficients to reconstruct precipitating flux over the entire loss cone. Our results show that the total precipitation can exceed that measured by the POES > 30 keV electron channel by a factor that typically varies from 1 to 10 for L* = 6, 6.5 and 7
    • …
    corecore