121 research outputs found
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Organic geochemistry of the crater-fill sediments from Boltysh impact crater, Ukraine
The Boltysh impact crater, is a complex structure formed on the basement rocks of the Ukrainian shield which has been dated at 65.17Β±0.64 Ma [1]. The Boltysh crater has been know for several decades and was originally drilled in the 1960s-1980s in a study of economic oil shale deposits. Unfortunately, the cores were not curated and have been lost. However we have recently re-drilled the impact crater and have recovered a near continuous record of ~400 m of organic rich sediments deposited in a deep isolated lake which overlie the basement rocks spanning a period ~10 Ma. At 24km diameter, Boltysh will not have contributed substantially to the worldwide devastation at the end of the
Cretaceous. However, the precise age of the Boltysh impact relative to the Chicxulub impact and its location on a stable low lying coastal plain which allowed formation of the postimpact crater lake make it a particularly important locality. After the impact, the crater quickly filled with water in a short marine phase but returned to fresh water which persisted for >10Ma [2]. These strata contain a valuable record of Paleogene environmental change in central Europe, and one of very few terrestrial records of the KT event. This pre-eminent record of the Paleogene can help us to answer several related scientific questions including the relative age of Boltysh compared with Chicxulub, recovery from the impact, and later climate signals. The organic geochemistry and playnology indicate main inputs to be algal and higher plant within most of the core although there are some marked changes in inputs in some sections. A number of carbon isotope excursions are also present within the core which are currently being further investigated
THE RECURRENT ALGORITHM FOR INTERFEROMETRIC SIGNALS PROCESSING BASED ON MULTI-CLOUD PREDICTION MODEL
The paper deals with modification of the recurrent processing algorithm for discrete sequence of interferometric signal samples. The algorithm is based on subsequent reference signal prediction at specifying a set (βcloudβ) of values for signal parameters vector by Monte Carlo method, comparison with the measured signal value and usage of the residual for enhancing the values of signal parameters at each discretization step. The concept of multi-cloud prediction model is used in the proposed modified algorithm. A set of normally distributed clouds is created with expectation values selected on the base of criterion of minimum residual between prediction and observation values. Experimental testing of the proposed method applied to estimation of fringe initial phase in the phase shifting interferometry has been conducted. The estimate variance of the signal reconstructed according to estimated initial phase from initial signal does not exceed 2% of the maximum signal value. It has been shown that the proposed algorithm application makes it possible to avoid the 2Ο-ambiguity and ensure sustainable recovery of interference fringes phase of a complicated type without involving a priori information about interference fringe phase distribution. The usage of the proposed algorithm applied to estimation of interferometric signals parameters gives the possibility for improving the filter stability with respect to influence of random noise and decreasing requirements for accuracy of a priori filtration parameters setting as compared with conventional (single-cloud) implementation of the sequential Monte Carlo method
STATISTICAL CHARACTERISTICS INVESTIGATION OF PREDICTION ERRORS FOR INTERFEROMETRIC SIGNAL IN THE ALGORITHM OF NONLINEAR KALMAN FILTERING
Basic peculiarities of nonlinear Kalman filtering algorithm applied to processing of interferometric signals are considered. Analytical estimates determining statistical characteristics of signal values prediction errors were obtained and analysis of errors histograms taking into account variations of different parameters of interferometric signal was carried out. Modeling of the signal prediction procedure with known fixed parameters and variable parameters of signal in the algorithm of nonlinear Kalman filtering was performed. Numerical estimates of prediction errors for interferometric signal values were obtained by formation and analysis of the errors histograms under the influence of additive noise and random variations of amplitude and frequency of interferometric signal. Nonlinear Kalman filter is shown to provide processing of signals with randomly variable parameters, however, it does not take into account directly the linearization error of harmonic function representing interferometric signal that is a filtering error source. The main drawback of the linear prediction consists in non-Gaussian statistics of prediction errors including cases of random deviations of signal amplitude and/or frequency. When implementing stochastic filtering of interferometric signals, it is reasonable to use prediction procedures based on local statistics of a signal and its parameters taken into account
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Two large meteorite impacts at the CretaceousβPaleogene boundary
The end-Cretaceous mass extinction has been attributed by most to a single asteroid impact at Chicxulub on the YucatΓ‘n Peninsula, Mexico. The discovery of a second smaller crater with a similar age at Boltysh in the Ukraine has raised the possibility that a shower of asteroids or comets impacted Earth close to the Cretaceous-Paleogene (K-Pg) boundary. Here we present palynological and Ξ΄13C evidence from crater-fill sediments in the Boltysh impact crater. Our analyses demonstrate that a post-impact flora, formed on the ejecta layer, was in turn devastated by the K-Pg event. The sequence of floral recovery from the K-Pg event is directly comparable with that in middle North America. We conclude that the Boltysh crater predated Chicxulub by βΌ2β5 k.y., a time scale that constrains the likely origin of the bodies that formed the two known K-Pg craters
Fractional Systems and Fractional Bogoliubov Hierarchy Equations
We consider the fractional generalizations of the phase volume, volume
element and Poisson brackets. These generalizations lead us to the fractional
analog of the phase space. We consider systems on this fractional phase space
and fractional analogs of the Hamilton equations. The fractional generalization
of the average value is suggested. The fractional analogs of the Bogoliubov
hierarchy equations are derived from the fractional Liouville equation. We
define the fractional reduced distribution functions. The fractional analog of
the Vlasov equation and the Debye radius are considered.Comment: 12 page
Fractional Liouville and BBGKI Equations
We consider the fractional generalizations of Liouville equation. The
normalization condition, phase volume, and average values are generalized for
fractional case.The interpretation of fractional analog of phase space as a
space with fractal dimension and as a space with fractional measure are
discussed. The fractional analogs of the Hamiltonian systems are considered as
a special class of non-Hamiltonian systems. The fractional generalization of
the reduced distribution functions are suggested. The fractional analogs of the
BBGKI equations are derived from the fractional Liouville equation.Comment: 20 page
ANTIBODIES TO BENZO[A]PYRENE IN SERUM OF PATIENTS WITH NON-SMALL CELL LUNG CANCER
The features of immune response to chemical carcinogen benzo[a]pyrene (Bp) at the patients with non-small cell lung cancer (NSCLC) are investigated. The isotypical distinctions in formation of antibodies (Ab) to Bp at the men with NSCLC in comparison with healthy are revealed. There were more often observed the high levels of IgG Ab-Bp at the men with NSCLC. Thus risk of occurrence NSCLC grows almost in 2 times at high levels of Ab-Bp of a class G
The Large Enriched Germanium Experiment for Neutrinoless Double Beta Decay (LEGEND)
The observation of neutrinoless double-beta decay (0)
would show that lepton number is violated, reveal that neutrinos are Majorana
particles, and provide information on neutrino mass. A discovery-capable
experiment covering the inverted ordering region, with effective Majorana
neutrino masses of 15 - 50 meV, will require a tonne-scale experiment with
excellent energy resolution and extremely low backgrounds, at the level of
0.1 count /(FWHMtyr) in the region of the signal. The
current generation Ge experiments GERDA and the MAJORANA DEMONSTRATOR
utilizing high purity Germanium detectors with an intrinsic energy resolution
of 0.12%, have achieved the lowest backgrounds by over an order of magnitude in
the 0 signal region of all 0
experiments. Building on this success, the LEGEND collaboration has been formed
to pursue a tonne-scale Ge experiment. The collaboration aims to develop
a phased 0 experimental program with discovery potential
at a half-life approaching or at years, using existing resources as
appropriate to expedite physics results.Comment: Proceedings of the MEDEX'17 meeting (Prague, May 29 - June 2, 2017
Inhibition of microbial film at the surface of the structural material nanostructuring
The research objective was to find effective option of inhibition of formation of a microbic film on constructional material from dioxide of the titan. Control and experimental groups were made by samples of dioxide of the titan (n=6) and samples of dioxide of the titan with the nanostructured surface (n=6). The control group was processed a rich nutrient mediurruof LB. Added to experimental group S.epidermidis 33 in the environment of LB. After 48 hours of an incubation the planktonic culture was deleted and carried out coloring for biomass definition (0,1% solution gentsianviolet) and amounts of living cells (water-soluble tetrazoliya) in a biofilm. All experiments are made three times and have taken place statistical processing. On control samples the nanostructured covering of dioxide of the titan doesn't exert impact on binding of dye in the environment of LB, but almost three times authentically reduces amount of Staphylococcus epidermidis 33 living cells on experimental samples. The superficial nanostructured covering of dioxide of the titan authentically reduces process of formation of biofilms by 2,5 times and leads to more than triple reliable decrease in biomass of films of Staphylococcus epidermidis 33 at cultivation within 48 hours. These facts have practical value for use of the obtained data of experiment in clinical stomatology as a way of inhibition of formation of bacterial films on surfaces of the offered constructional materials from dioxide of the titan with the nanomodified surface treatment.Π¦Π΅Π»ΡΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ Π±ΡΠ»ΠΎ Π½Π°ΠΉΡΠΈ ΡΡΡΠ΅ΠΊΡΠΈΠ²Π½ΡΠΉ Π²Π°ΡΠΈΠ°Π½Ρ ΠΈΠ½Π³ΠΈΠ±ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ ΠΌΠΈΠΊΡΠΎΠ±Π½ΠΎΠΉ ΠΏΠ»Π΅Π½ΠΊΠΈ Π½Π° ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠΎΠ½Π½ΠΎΠΌ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»Π΅ ΠΈΠ· Π΄ΠΈΠΎΠΊΡΠΈΠ΄Π° ΡΠΈΡΠ°Π½! ΠΠΎΠ½ΡΡΠΎΠ»ΡΠ½ΡΡ ΠΈ ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΡΡ Π³ΡΡΠΏΠΏΡ ΡΠΎΡΡΠ°Π²ΠΈΠ»ΠΈ ΠΎΠ±ΡΠ°Π·ΡΡ ΠΈΠ· Π΄ΠΈΠΎΠΊΡΠΈΠ΄Π° ΡΠΈΡΠ°Π½Π° (n=6) ΠΈ ΠΎΠ±ΡΠ°Π·ΡΡ Π΄ΠΈΠΎΠΊΡΠΈΠ΄Π° ΡΠΈΡΠ°Π½Π° Ρ Π½Π°Π½ΠΎΡΡΡΡΠΊΡΡΡΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠΉ ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΡΡ (n=6). ΠΠΎΠ½ΡΡΠΎΠ»ΡΠ½ΡΡ Π³ΡΡΠΏΠΏΡ ΠΎΠ±ΡΠ°Π±Π°ΡΡΠ²Π°Π»ΠΈ Π±ΠΎΠ³Π°ΡΠΎΠΉ ΠΏΠΈΡΠ°ΡΠ΅Π»ΡΠ½ΠΎΠΉ ΡΡΠ΅Π΄ΠΎΠΉ J_B. Π ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΡΡ Π³ΡΡΠΏΠΏΡ Π΄ΠΎΠ±Π°Π²Π»ΡΠ»ΠΈ ΠΈΠ½ΠΎΠΊΡΠ»ΡΠΌ S.epidermidis 33 Π² ΡΡΠ΅Π΄Π΅ LB. ΠΠΎΡΠ»Π΅ 48 ΡΠ°Ρ. ΠΈΠ½ΠΊΡΠ±Π°ΡΠΈΠΈ ΠΏΠ»Π°Π½ΠΊΡΠΎΠ½Π½ΡΡ ΠΊΡΠ»ΡΡΡΡΡ ΡΠ΄Π°Π»ΡΠ»ΠΈ ΠΈ ΠΏΡΠΎΠ²ΠΎΠ΄ΠΈΠ»ΠΈ ΠΎΠΊΡΠ°ΡΠΈΠ²Π°Π½ΠΈΠ΅ Π΄Π»Ρ ΠΎΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ Π±ΠΈΠΎΠΌΠ°ΡΡΡ (0,1 %-Π½ΡΠΉ ΡΠ°ΡΡΠ²ΠΎΡ Π³Π΅Π½ΡΠΈΠ°Π½Π²ΠΈΠΎΠ»Π΅Ρ) ΠΈ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π° ΠΆΠΈΠ²ΡΡ
ΠΊΠ»Π΅ΡΠΎΠΊ (Π²ΠΎΠ΄ΠΎΡΠ°ΡΡΠ²ΠΎΡΠΈΠΌΡΠΉ ΡΠ΅ΡΡΠ°Π·ΠΎΠ»ΠΈΠΉ) Π² Π±ΠΈΠΎΠΏΠ»Π΅Π½ΠΊΠ΅. ΠΡΠ΅ ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΡ ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½Ρ ΡΡΠΎΠ΅ΠΊΡΠ°ΡΠ½ΠΎ ΠΈ ΠΏΡΠΎΡΠ»ΠΈ ΡΡΠ°ΡΠΈΡΡΠΈΡΠ΅ΡΠΊΡΡ ΠΎΠ±ΡΠ°Π±ΠΎΡΠΊΡ. ΠΠ° ΠΊΠΎΠ½ΡΡΠΎΠ»ΡΠ½ΡΡ
ΠΎΠ±ΡΠ°Π·ΡΠ°Ρ
Π½Π°Π½ΠΎΡΡΡΡΠΊΡΡΡΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠ΅ ΠΏΠΎΠΊΡΡΡΠΈΠ΅ Π΄ΠΈΠΎΠΊΡΠΈΠ΄Π° ΡΠΈΡΠ°Π½Π° Π½Π΅ ΠΎΠΊΠ°Π·ΡΠ²Π°Π΅Ρ Π²Π»ΠΈΡΠ½ΠΈΡ Π½Π° ΡΠ²ΡΠ·ΡΠ²Π°Π½ΠΈΠ΅ ΠΊΡΠ°ΡΠΈΡΠ΅Π»Ρ Π² ΡΡΠ΅Π΄Π΅ LB, Π½ΠΎ ΠΏΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠΈ Π² ΡΡΠΈ ΡΠ°Π·Π° Π΄ΠΎΡΡΠΎΠ²Π΅ΡΠ½ΠΎ ΡΠ½ΠΈΠΆΠ°Π΅Ρ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²ΠΎ ΠΆΠΈΠ²ΡΡ
ΠΊΠ»Π΅ΡΠΎΠΊ Staphylococcus epideimidis 33 Π½Π° ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΡΡ
ΠΎΠ±ΡΠ°Π·ΡΠ°Ρ
. ΠΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠ½ΠΎΠ΅ Π½Π°Π½ΠΎΡΡΡΡΠΊΡΡΡΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠ΅ ΠΏΠΎΠΊΡΡΡΠΈΠ΅ Π΄ΠΈΠΎΠΊΡΠΈΠ΄Π° ΡΠΈΡΠ°Π½Π° Π΄ΠΎΡΡΠΎΠ²Π΅ΡΠ½ΠΎ ΡΠ½ΠΈΠΆΠ°Π΅Ρ Π² 2,5 ΡΠ°Π·Π° ΠΏΡΠΎΡΠ΅ΡΡ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ Π±ΠΈΠΎΠΏΠ»Π΅Π½ΠΎΠΊ ΠΈ ΠΏΡΠΈΠ²ΠΎΠ΄ΠΈΡ ΠΊ Π±ΠΎΠ»Π΅Π΅ ΡΠ΅ΠΌ ΡΡΠ΅Ρ
ΠΊΡΠ°ΡΠ½ΠΎΠΌΡ Π΄ΠΎΡΡΠΎΠ²Π΅ΡΠ½ΠΎΠΌΡ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΡ Π±ΠΈΠΎΠΌΠ°ΡΡΡ ΠΏΠ»Π΅Π½ΠΎΠΊ Staphylococcus epideimidis 33 ΠΏΡΠΈ ΠΊΡΠ»ΡΡΠΈΠ²ΠΈΡΠΎΠ²Π°Π½ΠΈΠΈ Π² ΡΠ΅ΡΠ΅Π½ΠΈΠΈ 48 ΡΠ°ΡΠΎΠ². ΠΠ°Π½Π½ΡΠ΅ ΡΠ°ΠΊΡΡ ΠΈΠΌΠ΅ΡΡ ΠΏΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠΎΠ΅ Π·Π½Π°ΡΠ΅Π½ΠΈΠ΅ Π΄Π»Ρ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΡ ΠΏΠΎΠ»ΡΡΠ΅Π½Π½ΡΡ
Π΄Π°Π½Π½ΡΡ
ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ° Π² ΠΊΠ»ΠΈΠ½ΠΈΡΠ΅ΡΠΊΠΎΠΉ ΡΡΠΎΠΌΠ°ΡΠΎΠ»ΠΎΠ³ΠΈΠΈ Π² ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅ ΡΠΏΠΎΡΠΎΠ±Π° ΠΈΠ½Π³ΠΈΠ±ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ Π±Π°ΠΊΡΠ΅ΡΠΈΠ°Π»ΡΠ½ΡΡ
ΠΏΠ»Π΅Π½ΠΎΠΊ Π½Π° ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΡΡ
ΠΏΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½Π½ΡΡ
ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠΎΠ½Π½ΡΡ
ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»ΠΎΠ² ΠΈΠ· Π΄ΠΈΠΎΠΊΡΠΈΠ΄Π° ΡΠΈΡΠ°Π½Π° Ρ Π½Π°Π½ΠΎΠΌΠΎΠ΄ΠΈΡΠΈΡΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠΉ ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠ½ΠΎΠΉ ΠΎΠ±ΡΠ°Π±ΠΎΡΠΊΠΎΠΉ
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