73 research outputs found
Issue of Money Laundering Risks Identification in the Activity of the Organizations and Individual Entrepreneurs Engaged in the Mining, Production, Use and Circulation of Precious Metals and Precious Stones
This article is distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use and redistribution provided that the original author and source are credited.Identification of money laundering risks in the sector of precious metals and precious stones is an important element in building an effective risk-based approach of money laundering risk assessment in the country. The article describes a mechanism of information exchange used in risk assessment of the organizations and individual entrepreneurs engaged in the mining, production, use and circulation of precious metals and precious stones. The mechanism is based on modern digital technologies such as a userβs cabinet on the Federal financial monitoring service website. The risk-score is obtained as a result of the analysis of the information contained in the database of Rosfinmonitoring, as well as monitoring and oversight activities conducted by Federal state institution Β«The risk-score shall be provided to all subjects of the sector allowing them to quickly resolve the shortcomings in their activities.Β Keywords: money laundering risk, sector of precious metals and precious stones, big data, information exchange, risk assessment, internal control
Hard tube pulser for 150 MW klystron
The development of adequate modulators for high peak power klystrons is one of the focus points for linear collider R&D programs. For the DESY/THD Sband linear collider study 150MW RF pulse power at 50Hz repetition rate and 3mks pulse duration is required. Two different modulator schemes were investigated. One is the conventional line type pulser, using a pulse forming network and a step up transformer, the other one is a Hard Tube Pulser, using a DC power source at the full klystron voltage and a switch tube. The main advantages of a Hard Tube Pulser are short rise and fall times of the HV pulse, resulting in high efficiency and simpler design
Large-volume silicic volcanism in Kamchatka: ArβAr and UβPb ages, isotopic, and geochemical characteristics of major pre-Holocene caldera-forming eruptions
The Kamchatka Peninsula in far eastern Russia represents the most volcanically active arc in the world in terms of magma production and the number of explosive eruptions. We investigate large-scale silicic volcanism in the past several million years and present new geochronologic results from major ignimbrite sheets exposed in Kamchatka. These ignimbrites are found in the vicinity of morphologically-preserved rims of partially eroded source calderas with diameters from βΌ 2 to βΌ 30 km and with estimated volumes of eruptions ranging from 10 to several hundred cubic kilometers of magma. We also identify and date two of the largest ignimbrites: Golygin Ignimbrite in southern Kamchatka (0.45 Ma), and Karymshina River Ignimbrites (1.78 Ma) in south-central Kamchatka. We present whole-rock geochemical analyses that can be used to correlate ignimbrites laterally. These large-volume ignimbrites sample a significant proportion of remelted Kamchatkan crust as constrained by the oxygen isotopes. Oxygen isotope analyses of minerals and matrix span a 3β° range with a significant proportion of moderately low-Ξ΄18O values. This suggests that the source for these ignimbrites involved a hydrothermally-altered shallow crust, while participation of the Cretaceous siliceous basement is also evidenced by moderately elevated Ξ΄18O and Sr isotopes and xenocryst contamination in two volcanoes. The majority of dates obtained for caldera-forming eruptions coincide with glacial stages in accordance with the sediment record in the NW Pacific, suggesting an increase in explosive volcanic activity since the onset of the last glaciation 2.6 Ma. Rapid changes in ice volume during glacial times and the resulting fluctuation of glacial loading/unloading could have caused volatile saturation in shallow magma chambers and, in combination with availability of low-Ξ΄18O glacial meltwaters, increased the proportion of explosive vs effusive eruptions. The presented results provide new constraints on PlioceneβPleistocene volcanic activity in Kamchatka, and thus constrain an important component of the Pacific Ring of Fire
The high energy cosmic ray particle spectra measurements with the PAMELA calorimeter
Abstract Up until now there has been limited, contradictive data on the high energy range of the cosmic ray electron-positron, proton and helium spectra. Due to the limitations of the use of a magnetic spectrometer, over 8 years experimental data was processed using information from a sampling electro-magnetic calorimeter, a neutron detector and scintillator detectors. The use of these devices allowed us to successfully obtain the high energy cosmic ray particle spectra measurements. The results of this study clarify previous findings and greaten our understanding of the origin of cosmic rays
Deuteron spectrum measurements under radiation belt with PAMELA instrument
Abstract In this work the results of data analysis of the deuteron albedo radiation obtained in the PAMELA experiment are presented. PAMELA is an international space experiment carried out on board of the satellite Resurs DK-1. The high precision detectors allow to register and identify cosmic ray particles in a wide energy range. The albedo deuteron spectrum in the energy range 70 β 600 MeV/nucleon has been measured
PAMELA Observation of the 2012 May 17 GLE Event
The PAMELA (Payload for Antimatter Matter Exploration and Light-nuclei Astrophysics) satellite-borne experiment has been collecting data in orbit since July 2006, providing accurate measurements of the energy spectra and composition of the cosmic radiation from a few hundred MeVn up to hundred GeVn. This wide interval of measured energies makes PAMELA a unique instrument for Solar Energetic Particle (SEP) observations. Not only does it span the energy range between the ground-based neutron monitor data and the observations of SEPs from space, but also PAMELA carries out the first direct measurements of the composition for the highest energy SEP events, including those causing Ground Level Enhancements (GLEs). PAMELA has registered many SEP events in solar cycle 24 including the 2012 May 17 GLE event (GLE 71), offering unique opportunities to address the question of high-energy SEP origin. Experimental performances and preliminary results on the 2012 May 17 events will be presented. We will discuss the derived particle injection time and compare with other time scales at the Sun including the flare and CME onset times
ΠΠ΅Π»Π΅Π·ΠΎΠ·Π°Π²ΠΈΡΠΈΠΌΠΎΡΡΡ Π±ΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ ΡΠ²ΠΎΠΉΡΡΠ² Π‘andida albicans
Background: Candidal infections occur in individuals with humoral or cell immunity deficiency. Any disorders of iron metabolism promote immune deficiency and abnormal sensitivity to infections. Potential modification of biological properties of Candida spp. in disorders of iron metabolism has not been discussed. Aim: To clarify the effects of iron metabolism disorders on the modification of biological properties of C.Β albicans. Materials and methods: Growth kinetics of reference strain (24433 ΠΠ’Π‘Π‘) and clinical isolates of C.Β albicans (n = 20) depending on the concentration of Fe2+ ions in the broth and serum of blood donors with various types of iron metabolism (n = 2) was studied by turbidimetry. We also assessed the expression of the adhesion gen (als3), hemolytic phospholipaseΒ C genes (plb1, plb2, plΡ) and aspartic protease gene (sap1) in serum of donors with various iron levels. Results: Growth parameters of all C.Β albicans strains studied depends on the iron levels in the medium. The calculated constant of affinity to Fe2+ (Ks) for C.Β albicans strains was in the range from 179.5 to 1863.3 ΞΌM. Clinical isolates are more iron-dependent (179.5 KsΒ 1000 ΞΌM), compared to the reference strain ATCC 24433 (KsΒ = 1199.5 Β± 28.3 ΞΌM). The optimal concentration of iron for the growth in the broth is 30 to 50 ΞΌM. The serum from individuals with normal iron metabolism inhibits the growth activity of C.Β albicans and is associated with overexpression of all virulence genes studied. Incubation of C.Β albicans with iron-deficient and iron-loaded sera results in an increase in the growth rate up to 0.017 h-1 and 0.012 h-1, respectively, but is associated with aΒ reduction in expression of the major virulence genes. Conclusion: Biological properties of C.Β albicans are modified depending on the iron metabolism of the host. In those with normal iron metabolism, immune system suppresses Candida growth. Excess iron levels may promote candidiasis, whereas in iron deficient states the outcome of infection depends on the immune status of the host.ΠΠΊΡΡΠ°Π»ΡΠ½ΠΎΡΡΡ. ΠΠ°Π½Π΄ΠΈΠ΄ΠΎΠ·Ρ Π²ΠΎΠ·Π½ΠΈΠΊΠ°ΡΡ ΡΒ ΠΈΠΌΠΌΡΠ½ΠΎΠΊΠΎΠΌΠΏΡΠΎΠΌΠ΅ΡΠΈΡΠΎΠ²Π°Π½Π½ΡΡ
Π»ΠΈΡ ΡΒ Π΄Π΅ΡΠ΅ΠΊΡΠ°ΠΌΠΈ Π³ΡΠΌΠΎΡΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΈΠ»ΠΈ ΠΊΠ»Π΅ΡΠΎΡΠ½ΠΎΠ³ΠΎ Π·Π²Π΅Π½ΡΠ΅Π² ΠΈΠΌΠΌΡΠ½ΠΈΡΠ΅ΡΠ°. ΠΡΠ±ΡΠ΅ Π½Π°ΡΡΡΠ΅Π½ΠΈΡ ΠΎΠ±ΠΌΠ΅Π½Π° ΠΆΠ΅Π»Π΅Π·Π° ΡΠΏΠΎΡΠΎΠ±ΡΡΠ²ΡΡΡ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΠΈΠΌΠΌΡΠ½ΠΎΠ΄Π΅ΡΠΈΡΠΈΡΠ° ΠΈΒ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ ΠΈΠ½ΡΠ΅ΠΊΡΠΈΠΎΠ½Π½ΠΎΠΉ ΡΡΠ²ΡΡΠ²ΠΈΡΠ΅Π»ΡΠ½ΠΎΡΡΠΈ. ΠΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡΡ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ Π±ΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠ²ΠΎΠΉΡΡΠ² Π³ΡΠΈΠ±ΠΎΠ² ΡΠΎΠ΄Π° Candida ΠΏΡΠΈ Π½Π°ΡΡΡΠ΅Π½ΠΈΡΡ
ΠΎΠ±ΠΌΠ΅Π½Π° ΠΆΠ΅Π»Π΅Π·Π° Π½Π΅ ΠΎΠ±ΡΡΠΆΠ΄Π°Π»Π°ΡΡ. Π¦Π΅Π»ΡΒ β Π²ΡΡΡΠ½ΠΈΡΡ Π²Π»ΠΈΡΠ½ΠΈΠ΅ Π½Π°ΡΡΡΠ΅Π½ΠΈΠΉ ΠΎΠ±ΠΌΠ΅Π½Π° ΠΆΠ΅Π»Π΅Π·Π° Π½Π° ΠΌΠΎΠ΄ΠΈΡΠΈΠΊΠ°ΡΠΈΡ Π±ΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠ²ΠΎΠΉΡΡΠ² C.Β albicans. ΠΠ°ΡΠ΅ΡΠΈΠ°Π» ΠΈΒ ΠΌΠ΅ΡΠΎΠ΄Ρ. Π‘Β ΠΏΠΎΠΌΠΎΡΡΡ ΡΡΡΠ±ΠΈΠ΄ΠΈΠΌΠ΅ΡΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΌΠ΅ΡΠΎΠ΄Π° ΠΈΠ·ΡΡΠ°Π»Π°ΡΡ ΠΊΠΈΠ½Π΅ΡΠΈΠΊΠ° ΡΠΎΡΡΠ° ΡΠ΅ΡΠ΅ΡΠ΅Π½ΡΠ½ΠΎΠ³ΠΎ ΡΡΠ°ΠΌΠΌΠ° (24433 ΠΠ’Π‘Π‘) ΠΈΒ ΠΊΠ»ΠΈΠ½ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΈΠ·ΠΎΠ»ΡΡΠΎΠ² C.Β albicans Π²Β Π±ΡΠ»ΡΠΎΠ½Π΅ (n = 20) Π²Β Π·Π°Π²ΠΈΡΠΈΠΌΠΎΡΡΠΈ ΠΎΡ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠΈ ΠΈΠΎΠ½ΠΎΠ² Fe2+ ΠΈΒ Π² ΡΡΠ²ΠΎΡΠΎΡΠΊΠ΅ ΠΊΡΠΎΠ²ΠΈ Π΄ΠΎΠ½ΠΎΡΠΎΠ² ΡΒ ΡΠ°Π·Π½ΡΠΌ Π²Π°ΡΠΈΠ°Π½ΡΠΎΠΌ ΠΎΠ±ΠΌΠ΅Π½Π° ΠΆΠ΅Π»Π΅Π·Π° (n = 2). ΠΠΏΡΠ΅Π΄Π΅Π»ΡΠ»Π°ΡΡ ΡΠΊΡΠΏΡΠ΅ΡΡΠΈΡ Π³Π΅Π½Π° Π°Π΄Π³Π΅Π·ΠΈΠΈ (als3), Π³Π΅Π½ΠΎΠ² ΡΠΎΡΡΠΎΠ»ΠΈΠΏΠ°Π·Β Π‘Β (plb1, plb2, plΡ), Π³Π΅Π½Π° Π°ΡΠΏΠ°ΡΡΠΈΠ»ΡΠ½ΠΎΠΉ ΠΏΡΠΎΡΠ΅Π°Π·Ρ (sap1) Π²Β ΡΡΠ²ΠΎΡΠΎΡΠΊΠ΅ ΠΊΡΠΎΠ²ΠΈ Π΄ΠΎΠ½ΠΎΡΠΎΠ² ΡΒ ΡΠ°Π·Π½ΡΠΌ ΡΠΎΠ΄Π΅ΡΠΆΠ°Π½ΠΈΠ΅ΠΌ ΠΆΠ΅Π»Π΅Π·Π°. Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ. ΠΠΊΡΠΈΠ²Π½ΠΎΡΡΡ ΡΠΎΡΡΠ° Π²ΡΠ΅Ρ
ΠΈΠ·ΡΡΠ΅Π½Π½ΡΡ
ΡΡΠ°ΠΌΠΌΠΎΠ² C.Β albicans Π·Π°Π²ΠΈΡΠΈΡ ΠΎΡ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠΈ ΠΆΠ΅Π»Π΅Π·Π° Π²Β ΠΏΠΈΡΠ°ΡΠ΅Π»ΡΠ½ΠΎΠΉ ΡΡΠ΅Π΄Π΅. Π Π°ΡΡΠ΅Ρ Π·Π½Π°ΡΠ΅Π½ΠΈΠΉ ΠΊΠΎΠ½ΡΡΠ°Π½ΡΡ ΡΡΠΎΠ΄ΡΡΠ²Π° ΠΊΒ ΠΈΠΎΠ½Π°ΠΌ Fe2+ (Ks) Π΄Π»Ρ ΡΡΠ°ΠΌΠΌΠΎΠ² C.Β albicans ΠΏΠΎΠΊΠ°Π·Π°Π», ΡΡΠΎ ΠΎΠ½ΠΈ ΠΈΠ·ΠΌΠ΅Π½ΡΡΡΡΡ ΠΎΡΒ 179,5 Π΄ΠΎΒ 1863,3 ΠΌΠΊΠ. ΠΠ»ΠΈΠ½ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΈΠ·ΠΎΠ»ΡΡΡ ΠΎΡΠ»ΠΈΡΠ°ΡΡΡΡ Π±ΠΎΠ»ΡΡΠ΅ΠΉ ΠΆΠ΅Π»Π΅Π·ΠΎΠ·Π°Π²ΠΈΡΠΈΠΌΠΎΡΡΡΡ (179,5 Πs 1000Β ΠΌΠΊΠ) ΠΏΠΎ ΡΡΠ°Π²Π½Π΅Π½ΠΈΡ ΡΒ ΡΠ΅ΡΠ΅ΡΠ΅Π½ΡΠ½ΡΠΌ ΡΡΠ°ΠΌΠΌΠΎΠΌ 24433 ΠΠ’Π‘Π‘ (KsΒ = 1199,5 Β± 28,3Β ΠΌΠΊΠ). ΠΠΏΡΠΈΠΌΠ°Π»ΡΠ½Π°Ρ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΡ ΠΆΠ΅Π»Π΅Π·Π° Π΄Π»Ρ ΡΠΎΡΡΠ° Π²Β Π±ΡΠ»ΡΠΎΠ½Π΅ ΡΠΎΡΡΠ°Π²Π»ΡΠ΅Ρ 30β50Β ΠΌΠΊΠ. Π‘ΡΠ²ΠΎΡΠΎΡΠΊΠ° ΠΊΡΠΎΠ²ΠΈ ΡΒ Π½ΠΎΡΠΌΠ°Π»ΡΠ½ΡΠΌ ΠΎΠ±ΠΌΠ΅Π½ΠΎΠΌ ΠΆΠ΅Π»Π΅Π·Π° ΠΈΠ½Π³ΠΈΠ±ΠΈΡΡΠ΅Ρ ΡΠΎΡΡΠΎΠ²ΡΡ Π°ΠΊΡΠΈΠ²Π½ΠΎΡΡΡ C.Β albicans ΠΈΒ ΡΠ²Π΅Π»ΠΈΡΠΈΠ²Π°Π΅Ρ ΡΠΊΡΠΏΡΠ΅ΡΡΠΈΡ Π²ΡΠ΅Ρ
ΠΈΠ·ΡΡΠ΅Π½Π½ΡΡ
Π³Π΅Π½ΠΎΠ² ΠΏΠ°ΡΠΎΠ³Π΅Π½Π½ΠΎΡΡΠΈ. ΠΡΠ»ΡΡΠΈΠ²ΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ C.Β albicans Π²Β ΠΆΠ΅Π»Π΅Π·ΠΎΠ΄Π΅ΡΠΈΡΠΈΡΠ½ΠΎΠΉ ΠΈΒ ΠΆΠ΅Π»Π΅Π·ΠΎΠ½Π°Π³ΡΡΠΆΠ΅Π½Π½ΠΎΠΉ ΡΡΠ²ΠΎΡΠΎΡΠΊΠ°Ρ
ΡΠ²Π΅Π»ΠΈΡΠΈΠ²Π°Π΅Ρ ΡΠΊΠΎΡΠΎΡΡΡ ΡΠΎΡΡΠ° Π΄ΠΎ 0,017 Ρ-1 ΠΈΒ 0,012 Ρ-1 ΡΠΎΠΎΡΠ²Π΅ΡΡΡΠ²Π΅Π½Π½ΠΎ, Π½ΠΎ ΡΠΌΠ΅Π½ΡΡΠ°Π΅Ρ ΡΠΊΡΠΏΡΠ΅ΡΡΠΈΡ ΠΎΡΠ½ΠΎΠ²Π½ΡΡ
Π³Π΅Π½ΠΎΠ² ΠΏΠ°ΡΠΎΠ³Π΅Π½Π½ΠΎΡΡΠΈ. ΠΠ°ΠΊΠ»ΡΡΠ΅Π½ΠΈΠ΅. ΠΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΡΠ²ΠΎΠΉΡΡΠ²Π° C.Β albicans ΠΈΠ·ΠΌΠ΅Π½ΡΡΡΡΡ Π²Β Π·Π°Π²ΠΈΡΠΈΠΌΠΎΡΡΠΈ ΠΎΡ ΡΠΎΡΡΠΎΡΠ½ΠΈΡ ΠΎΠ±ΠΌΠ΅Π½Π° ΠΆΠ΅Π»Π΅Π·Π° ΠΎΡΠ³Π°Π½ΠΈΠ·ΠΌΠ° Ρ
ΠΎΠ·ΡΠΈΠ½Π°. ΠΡΠΈ Π½ΠΎΡΠΌΠ°Π»ΡΠ½ΠΎΠΌ ΠΎΠ±ΠΌΠ΅Π½Π΅ ΠΆΠ΅Π»Π΅Π·Π° ΠΈΠΌΠΌΡΠ½Π½Π°Ρ ΡΠΈΡΡΠ΅ΠΌΠ° ΠΏΠΎΠ΄Π°Π²Π»ΡΠ΅Ρ ΡΠ°Π·Π²ΠΈΡΠΈΠ΅ ΠΊΠ°Π½Π΄ΠΈΠ΄. ΠΠ·Π±ΡΡΠΎΡΠ½ΠΎΠ΅ Π½Π°ΠΊΠΎΠΏΠ»Π΅Π½ΠΈΠ΅ ΠΆΠ΅Π»Π΅Π·Π° ΡΠΏΠΎΡΠΎΠ±ΡΡΠ²ΡΠ΅Ρ Π²ΠΎΠ·Π½ΠΈΠΊΠ½ΠΎΠ²Π΅Π½ΠΈΡ ΠΊΠ°Π½Π΄ΠΈΠ΄ΠΎΠ·Π°, ΠΏΡΠΈ Π΄Π΅ΡΠΈΡΠΈΡΠ΅ ΠΆΠ΅Π»Π΅Π·Π° ΠΈΡΡ
ΠΎΠ΄ ΠΈΠ½ΡΠ΅ΠΊΡΠΈΠΈ Π±ΡΠ΄Π΅Ρ Π·Π°Π²ΠΈΡΠ΅ΡΡ ΠΎΡ ΡΠΎΡΡΠΎΡΠ½ΠΈΡ ΠΈΠΌΠΌΡΠ½Π½ΠΎΠ³ΠΎ ΡΡΠ°ΡΡΡΠ° ΠΎΡΠ³Π°Π½ΠΈΠ·ΠΌΠ° Ρ
ΠΎΠ·ΡΠΈΠ½Π°.
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