4,251 research outputs found
Inversionless light amplification and optical switching controlled by state-dependent alignment of molecules
We propose a method to achieve amplification without population inversion by
anisotropic molecules whose orientation by an external electric field is
state-dependent. It is based on decoupling of the lower-state molecules from
the resonant light while the excited ones remain emitting. The suitable class
of molecules is discussed, the equation for the gain factor is derived, and the
magnitude of the inversionless amplification is estimated for the typical
experimental conditions. Such switching of the sample from absorbing to
amplifying via transparent state is shown to be possible both with the aid of
dc and ac control electric fields.Comment: AMS-LaTeX v1.2, 4 pages with 4 figure
A method for obtaining plastid pigments from the biomass of Chlorella microalgae
Microalgae are distinguished from land plants by the high content of plastid pigments
and the biodiversity of carotenoids. The aim of this study is to develop a technology for extracting
a pigment complex from the biomass of the microalgae of the genus Chlorella and to determine
the extracted pigmentsβ composition. To obtain biomass, a crude cell suspension of microalgae
was used, which was obtained under laboratory conditions for pre-culture cultivation of
C. sorokiniana (strain 211-8k). The extraction of plastid pigments from air-dry biomass after
disintegration of cell membrane was performed in the 40 kHz mode. It was found that the highest
pigment content in ethanol extracts was observed after 30 min (870.0 Β± 27.1 mg L
-1
) at 45β50 Β°C.
The pigmentsβ composition in the resulting total extracts was determined by spectrophotometry
and the Reverse Phase HPLC method. The established content of chlorophyll a in the obtained
extracts was 537.5 Β± 10.0 mg L
-1
, the content of chlorophyll b was 182.5 Β± 27.5 mg L
-1
; the
maximum output of the amount of carotenoids in extracts was 150.0 Β± 10.0 mg L
-1
. Thus, the
main identified forms of carotenoids in extracts from the biomass of microalgae C. sorokiniana
were xanthophylls: lutein and fucoxanthin (18.6 and 4.7% of the amount of pigment in extract,
respectively) and Ξ²-carotene (1.8% of the amount of pigment). It is planned to further fractionate
the obtained total extracts of the pigment complex to obtain various forms of chlorophylls and
carotenoids to study the spectrum of physiological activity of plastid pigments
Optical spectra, crystal-field parameters, and magnetic susceptibility of the new multiferroic NdFe3(BO3)4
We report high-resolution optical absorption spectra for NdFe3(BO3)4 trigonal
single crystal which is known to exhibit a giant magnetoelectric effect below
the temperature of magnetic ordering TN = 33 K. The analysis of the
temperature-dependent polarized spectra reveals the energies and, in some
cases, symmetries and exchange splittings of Nd3+ 84 Kramers doublets. We
perform crystal-field calculations starting from the exchange-charge model,
obtain a set of six real crystal-field parameters, and calculate wave functions
and magnetic g-factors. In particular, the values g(perpendicular) = 2.385,
g(parallel) = 1.376 were found for the Nd3+ ground-state doublet. We obtain
Bloc=7.88 T and |JFN|= 0.48 K for the values of the local effective magnetic
field at liquid helium temperatures at the Nd3+ site and the Nd - Fe exchange
integral, respectively, using the experimentally measured Nd3+ ground-state
splitting of 8.8 cm-1. To check reliability of our set of crystal field
parameters we model the magnetic susceptibility data from literature. A dimer
containing two nearest-neighbor iron ions in the spiral chain is considered to
partly account for quasi-one-dimensional properties of iron borates, and then
the mean-field approximation is used. The results of calculations with the
exchange parameters for Fe3+ ions Jnn = -6.25 K (intra-chain interactions) and
Jnnn = -1.92 K (inter-chain interactions) obtained from fitting agree well with
the experimental data.Comment: 13 pages, 8 figures, 2 table
Mechanisms controlling primary and new production in a global ecosystem model ? Part I: The role of the large-scale upper mixed layer variability
International audienceA global general circulation model coupled to a simple six-compartment ecosystem model is used to study the extent to which global variability in primary and export production can be realistically predicted on the basis of advanced parameterizations of upper mixed layer physics, without recourse to introducing extra complexity in model biology. The ''K profile parameterization'' (KPP) scheme employed, combined with 6-hourly external forcing, is able to capture short-term periodic and episodic events such as diurnal cycling and storm-induced deepening. The model realistically reproduces various features of global ecosystem dynamics that have been problematic in previous global modelling studies, using a single generic parameter set. The realistic simulation of deep convection in the North Atlantic, and lack of it in the North Pacific and Southern Oceans, leads to good predictions of chlorophyll and primary production in these contrasting areas. Realistic levels of primary production are predicted in the oligotrophic gyres due to high frequency external forcing of the upper mixed layer (accompanying paper Popova et al., 2006) and novel parameterizations of zooplankton excretion. Good agreement is shown between model and observations at various JFOFS time series sites: BATS, KERFIX, Papa and station India. One exception is that the high zooplankton grazing rates required to maintain low chlorophyll in high-nutrient low-chlorophyll and oligotrophic systems lessened agreement between model and data in the northern North Atlantic, where mesozooplankton with lower grazing rates may be dominant. The model is therefore not globally robust in the sense that additional parameterizations were needed to realistically simulate ecosystem dynamics in the North Atlantic. Nevertheless, the work emphasises the need to pay particular attention to the parameterization of mixed layer physics in global ocean ecosystem modelling as a prerequisite to increasing the complexity of ecosystem models
Lattice vibrations of alpha'-NaV_2O_5 in the low-temperature phase. Magnetic bound states?
We report high resolution polarized infrared studies of the quarter-filled
spin ladder compound alpha'-NaV_2O_5 as a function of temperature (5K <= T <=
300K). Numerous new modes were detected below the temperature T_c=34K of the
phase transition into a charge ordered nonmagnetic state accompanied by a
lattice dimerization. We analyse the Brillouin zone (BZ) folding due to lattice
dimerization at T_c and show that some peculiarities of the low-temperature
vibrational spectrum come from quadruplets folded from the BZ point (1/2, 1/2,
1/4). We discuss an earlier interpretation of the 70, 107, and 133cm-1 modes as
magnetic bound states and propose the alternative interpretation as folded
phonon modes strongly interacting with charge and spin excitations.Comment: 15 pages, 13 Postscript figure
The future of the subsurface chlorophyll-a maximum in the Canada Basin-A model intercomparison
Six Earth system models and three ocean-ice-ecosystem models are analyzed to evaluate magnitude and depth of the subsurface Chl-a maximum (SCM) in the Canada Basin and ratio of surface to subsurface Chl-a in a future climate scenario. Differences in simulated Chl-a are caused by large intermodel differences in available nitrate in the Arctic Ocean and to some extent by ecosystem complexity. Most models reproduce the observed SCM and nitracline deepening and indicate a continued deepening in the future until the models reach a new state with seasonal ice-free waters. Models not representing a SCM show either too much nitrate and hence no surface limitation or too little nitrate with limited surface growth only. The models suggest that suppression of the nitracline and deepening of the SCM are caused by enhanced stratification, likely driven by enhanced Ekman convergence and freshwater contributions with primarily large-scale atmospheric driving mechanisms. The simulated ratio of near-surface Chl-a to depth-integrated Chl-a is slightly decreasing in most areas of the Arctic Ocean due to enhanced contributions of subsurface Chl-a. Exceptions are some shelf areas and regions where the continued ice thinning leaves winter ice too thin to provide a barrier to momentum fluxes, allowing winter mixing to break up the strong stratification. Results confirm that algorithms determining vertically integrated Chl-a from surface Chl-a need to be tuned to Arctic conditions, but likely require little or no adjustments in the future
Optical spectra, crystal-field parameters, and magnetic susceptibility of multiferroic Nd Fe3 (B O3) 4
We report high-resolution optical absorption spectra for Nd Fe3 (B O3) 4 trigonal single crystal, which is known to exhibit a giant magnetoelectric effect below the temperature of magnetic ordering TN =33 K. The analysis of the temperature-dependent polarized spectra reveals the energies and, in some cases, symmetries and exchange splittings of Nd3+ 84 Kramers doublets. We perform crystal-field calculations starting from the exchange-charge model, obtain a set of six real crystal-field parameters, and calculate wave functions and magnetic g factors. In particular, the values g =2.385 and g =1.376 were found for the Nd3+ ground-state doublet. We obtain Bloc =7.88 T and JFN =0.48 K for the values of the local effective magnetic field at liquid-helium temperatures at the Nd3+ site and the Nd-Fe exchange integral, respectively, using the experimentally measured Nd3+ ground-state splitting of 8.8 cm-1. To check the reliability of our set of crystal-field parameters, we model the magnetic susceptibility data from literature. A dimer containing two nearest-neighbor iron ions in the spiral chain is considered to partly account for quasi-one-dimensional properties of iron borates, and then the mean-field approximation is used. The results of calculations with the exchange parameters for Fe3+ ions Jnn =-6.25 K (intrachain interactions) and Jnnn =-1.92 K (interchain interactions) obtained from fitting agree well with the experimental data. Β© 2007 The American Physical Society
Three Aspects of the Phenomenon of Science: In Search for Unity among Sociologists
Introduction.Β In todayβs globalising world, science acquires a crucial importance: integrating humanity within the framework of solving global problems, it becomes one of the leading factors in social development, facilitating work and diversifying leisure time, as well as serving as an instrument of transformations in the political sphere. Undoubtedly, the social aspects of contemporary science are capturing the attention of a huge number of researchers. However, it is not clear that all areas of the sociology of science treat the object of their study in the same way. Aim.Β A lack of reflection on the unity or otherwise in the understanding of the essence of science in the various fields of sociological research makes it difficult to compare different theories of the institutional, cultural, social and communicative contexts of scientific development. An urgent methodological task therefore consists in developing an understanding of the various definitions of the concept of βscienceβ used in the framework of contemporary sociological analysis of this phenomenon. Results and scientific novelty.Β In this paper, two dominant sociological views on science β as an experimental-mathematical approach to cognising the world and as a system of representations in general β are compared. We conclude that while researchers studying institutional aspects of science tend to interpret it in terms of the βheritageβ of post-Enlightenment European rationalism, constructionist and communicatively-oriented researchers tend to approach science as the system of knowledge and cognition that is formed in any human society, having its own specific sociocultural features in each respective case. While each of these two approaches undoubtedly has its own methodological potential, in order to provide such a diverse field of studies with a common ground, it would be necessary to balance them with a third aspect. We argue that this balancing role, since both common for all mankind and unique for every culture, could be played by Heideggerβs conceptualisation of science as βthe theory of the realβ. Practical significance.Β In order to avoid a pluralism of incompatible theories, it is important to continually pose the question βwhat is the object of study when conducting a sociological study of various scientific phenomena?β β as well as to understand the βlimits of applicabilityβ of the particular interpretation of science on which basis sociological analysis proceeds.ΠΠ²Π΅Π΄Π΅Π½ΠΈΠ΅.Β Π ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΠΎΠΌ Π³Π»ΠΎΠ±Π°Π»ΠΈΠ·ΡΡΡΠ΅ΠΌΡΡ ΠΌΠΈΡΠ΅ Π½Π°ΡΡΠ½ΡΠ΅ Π·Π½Π°Π½ΠΈΡ ΠΏΡΠΈΠΎΠ±ΡΠ΅ΡΠ°ΡΡ Π²ΡΠ΅ Π±ΠΎΠ»ΡΡΡΡ Π·Π½Π°ΡΠΈΠΌΠΎΡΡΡ: ΠΎΠ½ΠΈ ΠΈΠ½ΡΠ΅Π³ΡΠΈΡΡΡΡ ΡΡΠΈΠ»ΠΈΡ ΡΠ΅Π»ΠΎΠ²Π΅ΡΠ΅ΡΡΠ²Π° Π΄Π»Ρ ΡΠ΅ΡΠ΅Π½ΠΈΡ ΠΎΠ±ΡΠΈΡ
ΠΏΡΠΎΠ±Π»Π΅ΠΌ, ΡΡΠ°Π½ΠΎΠ²ΡΡΡΡ ΠΎΠ΄Π½ΠΈΠΌΠΈ ΠΈΠ· Π²Π΅Π΄ΡΡΠΈΡ
ΡΠ°ΠΊΡΠΎΡΠΎΠ² ΡΠ°Π·Π²ΠΈΡΠΈΡ ΠΎΠ±ΡΠ΅ΡΡΠ²Π°, ΠΎΠ±Π»Π΅Π³ΡΠ°ΡΡ ΡΡΡΠ΄ ΠΈ ΡΠ°Π·Π½ΠΎΠΎΠ±ΡΠ°Π·ΡΡ Π΄ΠΎΡΡΠ³ Π»ΡΠ΄Π΅ΠΉ. ΠΡΠΎΠΌΠ΅ ΡΠΎΠ³ΠΎ, ΠΎΠ½ΠΈ ΠΈΡΠΏΠΎΠ»ΡΠ·ΡΡΡΡΡ ΠΈ Π² ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅ ΠΈΠ½ΡΡΡΡΠΌΠ΅Π½ΡΠ° ΡΠΎΡΠΈΠ°Π»ΡΠ½ΠΎ-ΠΏΠΎΠ»ΠΈΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠ°Π½ΡΡΠΎΡΠΌΠ°ΡΠΈΠΉ. ΠΠ΅ ΡΠ»ΡΡΠ°ΠΉΠ½ΠΎ ΡΠ΅Π³ΠΎΠ΄Π½Ρ Π²Π½ΠΈΠΌΠ°Π½ΠΈΠ΅ ΠΎΠ³ΡΠΎΠΌΠ½ΠΎΠ³ΠΎ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π° ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°ΡΠ΅Π»Π΅ΠΉ ΠΏΡΠΈΠΊΠΎΠ²Π°Π½ΠΎ ΠΊ ΡΠΎΡΠΈΠ°Π»ΡΠ½ΡΠΌ Π°ΡΠΏΠ΅ΠΊΡΠ°ΠΌ Π½Π°ΡΠΊΠΈ, Π° ΡΠ°ΠΊΠΆΠ΅ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ ΠΊΠ°ΠΊ Π²Π°ΠΆΠ½Π΅ΠΉΡΠ΅Π³ΠΎ Π²Π·Π°ΠΈΠΌΠΎΡΠ²ΡΠ·Π°Π½Π½ΠΎΠ³ΠΎ Ρ Π½Π΅ΠΉ ΡΠΎΡΠΈΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΈΠ½ΡΡΠΈΡΡΡΠ°. ΠΠ΄Π½Π°ΠΊΠΎ Π²ΠΎΠΏΡΠΎΡ ΠΎ ΡΠΎΠΌ, Π²ΡΠ΅ Π»ΠΈ Π½Π°ΠΏΡΠ°Π²Π»Π΅Π½ΠΈΡ ΡΠΎΡΠΈΠΎΠ»ΠΎΠ³ΠΈΠΈ Π½Π°ΡΠΊΠΈ ΡΡΠ°ΠΊΡΡΡΡ ΠΎΠ±ΡΠ΅ΠΊΡ ΡΠ²ΠΎΠ΅Π³ΠΎ ΠΈΠ·ΡΡΠ΅Π½ΠΈΡ ΠΎΠ΄ΠΈΠ½Π°ΠΊΠΎΠ²ΠΎ, ΠΎΡΡΠ°Π΅ΡΡΡ ΠΎΡΠΊΡΡΡΡΠΌ. ΠΠ΅ΠΆΠ΄Ρ ΡΠ΅ΠΌ ΠΏΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠΈ ΠΏΠΎΠ»Π½ΠΎΠ΅ ΠΎΡΡΡΡΡΡΠ²ΠΈΠ΅ ΡΠ΅ΡΠ»Π΅ΠΊΡΠΈΠΈ ΠΏΠΎ ΠΏΠΎΠ²ΠΎΠ΄Ρ Π΅Π΄ΠΈΠ½ΡΡΠ²Π° Π² ΠΏΠΎΠ½ΠΈΠΌΠ°Π½ΠΈΠΈ ΡΡΡΠ΅ΡΡΠ²Π° Π½Π°ΡΠΊΠΈ Π² ΠΏΠΎΠ»Π΅ ΡΠΎΡΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ Π·Π°ΡΡΡΠ΄Π½ΡΠ΅Ρ ΡΠΎΠΏΠΎΡΡΠ°Π²Π»Π΅Π½ΠΈΠ΅ ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
ΡΠ΅ΠΎΡΠΈΠΉ ΡΠ°Π·Π²ΠΈΡΠΈΡ Π½Π°ΡΡΠ½ΠΎΠ³ΠΎ Π·Π½Π°Π½ΠΈΡ Π² ΠΈΠ½ΡΡΠΈΡΡΡΠΈΠΎΠ½Π°Π»ΡΠ½ΠΎΠΌ, ΠΊΡΠ»ΡΡΡΡΠ½ΠΎΠΌ, ΡΠΎΡΠΈΠ°Π»ΡΠ½ΠΎ-ΠΊΠΎΠΌΠΌΡΠ½ΠΈΠΊΠ°ΡΠΈΠ²Π½ΠΎΠΌ ΠΊΠΎΠ½ΡΠ΅ΠΊΡΡΠ°Ρ
. Π’Π°ΠΊΠΎΠ΅ ΠΏΠΎΠ»ΠΎΠΆΠ΅Π½ΠΈΠ΅ Π΄Π΅Π» Π°ΠΊΡΡΠ°Π»ΠΈΠ·ΠΈΡΡΠ΅Ρ ΠΏΠΎΠΈΡΠΊ ΡΠ΅ΡΠ΅Π½ΠΈΡ ΠΎΠ΄Π½ΠΎΠΉ ΠΈΠ· ΡΠ΅Π½ΡΡΠ°Π»ΡΠ½ΡΡ
ΠΌΠ΅ΡΠΎΠ΄ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
Π·Π°Π΄Π°Ρ ΠΏΠΎ ΠΎΡΠΌΡΡΠ»Π΅Π½ΠΈΡ Π²Π°ΡΠΈΠ°Π½ΡΠΎΠ² ΠΎΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ ΠΏΠΎΠ½ΡΡΠΈΡ Β«Π½Π°ΡΠΊΠ°Β», ΠΈΡΠΏΠΎΠ»ΡΠ·ΡΠ΅ΠΌΡΡ
Π² ΡΠ°ΠΌΠΊΠ°Ρ
ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΠΎΠ³ΠΎ ΡΠΎΡΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ Π°Π½Π°Π»ΠΈΠ·Π° Π΄Π°Π½Π½ΠΎΠ³ΠΎ ΡΠ΅Π½ΠΎΠΌΠ΅Π½Π°. Π¦Π΅Π»ΡΒ ΠΏΡΠ±Π»ΠΈΠΊΠ°ΡΠΈΠΈ Π·Π°ΠΊΠ»ΡΡΠ°Π΅ΡΡΡ Π² ΠΏΠΎΠΏΡΡΠΊΠ΅ ΡΠΎΠΏΠΎΡΡΠ°Π²ΠΈΡΡ ΠΎΡΠ½ΠΎΠ²Π½ΡΠ΅ ΡΡΠ°ΠΊΡΠΎΠ²ΠΊΠΈ Π½Π°ΡΠΊΠΈ β ΠΊΠ°ΠΊ ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΠΎ-ΠΌΠ°ΡΠ΅ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΡΠΏΠΎΡΠΎΠ±Π° ΠΏΠΎΠ·Π½Π°Π½ΠΈΡ ΠΌΠΈΡΠ° ΠΈ ΠΊΠ°ΠΊ ΡΠΈΡΡΠ΅ΠΌΡ ΠΏΡΠ΅Π΄ΡΡΠ°Π²Π»Π΅Π½ΠΈΠΉ ΠΎ ΡΡΡΠ΅ΡΡΠ²ΡΡΡΠΈΡ
ΡΠ΅Π°Π»ΠΈΡΡ
. Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΈ Π½Π°ΡΡΠ½Π°Ρ Π½ΠΎΠ²ΠΈΠ·Π½Π°. Π Ρ
ΠΎΠ΄Π΅ ΠΎΠ±ΡΡΠΆΠ΄Π΅Π½ΠΈΡ ΠΏΡΠΎΠ±Π»Π΅ΠΌΡ Π°Π²ΡΠΎΡΡ ΠΏΡΠΈΡ
ΠΎΠ΄ΡΡ ΠΊ Π²ΡΠ²ΠΎΠ΄Ρ ΠΎ ΡΠΎΠΌ, ΡΡΠΎ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ, ΠΏΠΎΡΠ²ΡΡΠ΅Π½Π½ΡΠ΅ ΠΈΠ·ΡΡΠ΅Π½ΠΈΡ ΠΈΠ½ΡΡΠΈΡΡΡΠΈΠΎΠ½Π°Π»ΡΠ½ΡΡ
Π°ΡΠΏΠ΅ΠΊΡΠΎΠ², ΡΡΠ³ΠΎΡΠ΅ΡΡ ΠΊ ΠΏΠΎΠ½ΠΈΠΌΠ°Π½ΠΈΡ Π½Π°ΡΠΊΠΈ ΠΊΠ°ΠΊ ΡΠ°ΡΠΈΠΎΠ½Π°Π»ΠΈΡΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ Β«Π½Π°ΡΠ»Π΅Π΄ΠΈΡΒ» ΠΠ²ΡΠΎΠΏΡ ΠΠΎΠ²ΠΎΠ³ΠΎ Π²ΡΠ΅ΠΌΠ΅Π½ΠΈ, Π° ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠΎΠ½ΠΈΡΡΡΠΊΠΈ ΠΈ ΠΊΠΎΠΌΠΌΡΠ½ΠΈΠΊΠ°ΡΠΈΠ²ΠΈΡΡΡΠΊΠΈ ΠΎΡΠΈΠ΅Π½ΡΠΈΡΠΎΠ²Π°Π½Π½ΡΠ΅ ΡΠ΅ΡΠ΅Π½ΠΈΡ ΡΠΊΠ»ΠΎΠ½Π½Ρ ΡΠ°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°ΡΡ Π΅Π΅ ΠΊΠ°ΠΊ ΡΠΈΡΡΠ΅ΠΌΡ Π·Π½Π°Π½ΠΈΡ ΠΈ ΠΏΠΎΠ·Π½Π°Π½ΠΈΡ, ΠΊΠΎΡΠΎΡΠ°Ρ ΡΠΎΡΠΌΠΈΡΡΠ΅ΡΡΡ Π² Π»ΡΠ±ΠΎΠΌ ΡΠ΅Π»ΠΎΠ²Π΅ΡΠ΅ΡΠΊΠΎΠΌ ΡΠΎΠΎΠ±ΡΠ΅ΡΡΠ²Π΅, ΠΈΠΌΠ΅Ρ, ΠΎΠ΄Π½Π°ΠΊΠΎ, Π² ΠΊΠ°ΠΆΠ΄ΠΎΠΌ ΡΠ»ΡΡΠ°Π΅ ΡΠ²ΠΎΠΈ ΡΠΏΠ΅ΡΠΈΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΡΠΎΡΠΈΠΎΠΊΡΠ»ΡΡΡΡΠ½ΡΠ΅ ΡΠ΅ΡΡΡ. ΠΠ°ΠΆΠ΄ΠΎΠ΅ ΠΈΠ· Π΄Π²ΡΡ
ΡΠΊΠ°Π·Π°Π½Π½ΡΡ
Π½Π°ΠΏΡΠ°Π²Π»Π΅Π½ΠΈΠΉ, Π½Π΅ΡΠΎΠΌΠ½Π΅Π½Π½ΠΎ, ΠΎΠ±Π»Π°Π΄Π°Π΅Ρ ΡΠ²ΠΎΠΈΠΌ ΠΌΠ΅ΡΠΎΠ΄ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠΌ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»ΠΎΠΌ. Π’Π΅ΠΌ Π½Π΅ ΠΌΠ΅Π½Π΅Π΅ Π² ΡΠ΅Π»ΡΡ
Π²ΡΠ²Π΅Π΄Π΅Π½ΠΈΡ ΡΠ°ΠΊΠΈΡ
ΡΠ°Π·Π½ΠΎΠΏΠ»Π°Π½ΠΎΠ²ΡΡ
ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ Π½Π° Π΅Π΄ΠΈΠ½ΡΡ ΠΏΠΎΡΠ²Ρ ΠΏΡΠ΅Π΄Π»Π°Π³Π°Π΅ΡΡΡ ΡΡΠ°Π²Π½ΠΎΠ²Π΅ΡΠΈΡΡ ΠΈΡ
ΡΡΠ΅ΡΡΠ΅ΠΉ ΡΠΎΡΠΊΠΎΠΉ Π·ΡΠ΅Π½ΠΈΡ, ΡΠΎΠ³Π»Π°ΡΠ½ΠΎ ΠΊΠΎΡΠΎΡΠΎΠΉ Π½Π°ΡΠΊΠ° Π΅ΡΡΡ Β«ΡΠ΅ΠΎΡΠΈΡ Π΄Π΅ΠΉΡΡΠ²ΠΈΡΠ΅Π»ΡΠ½ΠΎΠ³ΠΎΒ», ΠΈΠΌΠ΅ΡΡΠ°Ρ ΡΠ΅ΡΡΡ ΡΠ½ΠΈΠ²Π΅ΡΡΠ°Π»ΡΠ½ΠΎ-ΠΎΠ±ΡΠ΅ΡΠ΅Π»ΠΎΠ²Π΅ΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΈ ΡΠ½ΠΈΠΊΠ°Π»ΡΠ½ΠΎ-ΠΊΡΠ»ΡΡΡΡΠ½ΠΎΠ³ΠΎ ΡΠ΅Π½ΠΎΠΌΠ΅Π½Π°. ΠΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠ°Ρ Π·Π½Π°ΡΠΈΠΌΠΎΡΡΡ. ΠΡΠ²Π΅Ρ Π½Π° Π²ΠΎΠΏΡΠΎΡ: Β«Π§ΡΠΎ ΠΌΡ ΠΈΠ·ΡΡΠ°Π΅ΠΌ, ΠΊΠΎΠ³Π΄Π° ΠΏΡΠΎΠ²ΠΎΠ΄ΠΈΠΌ ΡΠΎΡΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΎΠ΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠ΅ Π½Π°ΡΠΊΠΈ?Β» ΠΏΠΎΠ·Π²ΠΎΠ»ΠΈΡ ΠΈΠ·Π±Π΅ΠΆΠ°ΡΡ ΠΏΠ»ΡΡΠ°Π»ΠΈΠ·ΠΌΠ° Π½Π΅ΡΠΎΠΏΠΎΡΡΠ°Π²ΠΈΠΌΡΡ
ΡΠ΅ΠΎΡΠΈΠΉ ΠΈ ΠΏΠΎΠ½ΡΡΡ Β«Π³ΡΠ°Π½ΠΈΡΡ ΠΏΡΠΈΠΌΠ΅Π½ΠΈΠΌΠΎΡΡΠΈΒ» ΡΠΎΠΉ ΡΡΠ°ΠΊΡΠΎΠ²ΠΊΠΈ Π½Π°ΡΠΊΠΈ, ΠΎΡ ΠΊΠΎΡΠΎΡΠΎΠΉ ΠΌΡ ΠΎΡΡΠ°Π»ΠΊΠΈΠ²Π°Π΅ΠΌΡΡ Π² ΡΠΎΡΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΎΠΌ Π°Π½Π°Π»ΠΈΠ·Π΅
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