156 research outputs found

    Lidar observations of atmospheric optical characteristics during Sichuan earthquake

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    The results of lidar observations of the atmosphere during the Sichuan (China) earthquake of 2008 are presented. It is shown that atmospheric parameters substantially changed during and after the earthquake. The profile of scattering characteristics formed in the lower troposphere differs from the original, which can serve as a predictor for earthquakes

    TRADE RELATIONS OF RUSSIA AND AUSTRIA-HUNGARY WITH THE LEVANTINE PROVINCES OF THE OTTOMAN EMPIRE IN THE LATE XIX - EARLY XX CENTURIES

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    Π’ прСдставлСнной ΡΡ‚Π°Ρ‚ΡŒΠ΅ рассматриваСтся Ρ€Π°Π·Π²ΠΈΡ‚ΠΈΠ΅ Ρ‚ΠΎΡ€Π³ΠΎΠ²Ρ‹Ρ… ΠΎΡ‚Π½ΠΎΡˆΠ΅Π½ΠΈΠΉ России ΠΈ Австро-Π’Π΅Π½Π³Ρ€ΠΈΠΈ Π² ΠΊΠΎΠ½Ρ†Π΅ XIX - Π½Π°Ρ‡Π°Π»Π΅ Π₯Π₯ Π²Π². Π½Π° Ρ‚Π΅Ρ€Ρ€ΠΈΡ‚ΠΎΡ€ΠΈΠΈ Π‘ΠΈΡ€ΠΈΠΈ, Π›ΠΈΠ²Π°Π½Π° ΠΈ ΠŸΠ°Π»Π΅ΡΡ‚ΠΈΠ½Ρ‹, Π²Ρ…ΠΎΠ΄ΠΈΠ²ΡˆΠΈΡ… Π² состав Османской ΠΈΠΌΠΏΠ΅Ρ€ΠΈΠΈ. На основС ΠΊΠΎΠΌΠΏΠ°Ρ€Π°Ρ‚ΠΈΠ²Π½ΠΎΠ³ΠΎ Π°Π½Π°Π»ΠΈΠ·Π° Π°Π²Ρ‚ΠΎΡ€ ΠΏΡ€ΠΈΡ…ΠΎΠ΄ΠΈΡ‚ ΠΊ Π²Ρ‹Π²ΠΎΠ΄Ρƒ, Ρ‡Ρ‚ΠΎ Австро-ВСнгрия смогла Π΄ΠΎΠ±ΠΈΡ‚ΡŒΡΡ Π±ΠΎΠ»ΡŒΡˆΠΈΡ… успСхов Π² Ρ€Π°Π·Π²ΠΈΡ‚ΠΈΠΈ внСшнСй Ρ‚ΠΎΡ€Π³ΠΎΠ²Π»ΠΈ с Π΄Π°Π½Π½Ρ‹ΠΌ Ρ€Π΅Π³ΠΈΠΎΠ½ΠΎΠΌ, Π½Π΅ΠΆΠ΅Π»ΠΈ Россия. ΠŸΡ€Π΅Π΄ΠΏΡ€ΠΈΠ½ΠΈΠΌΠ°Ρ‚Π΅Π»ΠΈ ΠΈΠ· ΠΈΠΌΠΏΠ΅Ρ€ΠΈΠΈ Габсбургов Ρ‚Ρ‰Π°Ρ‚Π΅Π»ΡŒΠ½ΠΎ ΠΈΠ·ΡƒΡ‡Π°Π»ΠΈ запросы ΠΏΠΎΡ‚Ρ€Π΅Π±ΠΈΡ‚Π΅Π»Π΅ΠΉ Π½Π° Ρ‚Π΅Ρ€Ρ€ΠΈΡ‚ΠΎΡ€ΠΈΠΈ Османской ΠΈΠΌΠΏΠ΅Ρ€ΠΈΠΈ ΠΈ спСцифику ΠΎΡ€Π³Π°Π½ΠΈΠ·Π°Ρ†ΠΈΠΈ Ρ‚ΠΎΡ€Π³ΠΎΠ²Π»ΠΈ Π½Π° Π‘Π»ΠΈΠΆΠ½Π΅ΠΌ ВостокС. РоссийскиС ΠΏΡ€Π΅Π΄ΠΏΡ€ΠΈΠ½ΠΈΠΌΠ°Ρ‚Π΅Π»ΠΈ Π² основном ΠΎΡ€ΠΈΠ΅Π½Ρ‚ΠΈΡ€ΠΎΠ²Π°Π»ΠΈΡΡŒ Π½Π° Π΅ΠΌΠΊΠΈΠΉ Π²Π½ΡƒΡ‚Ρ€Π΅Π½Π½ΠΈΠΉ Ρ€Ρ‹Π½ΠΎΠΊ, удСляя Ρ€Π°Π·Π²ΠΈΡ‚ΠΈΡŽ экспорта второстСпСнноС Π·Π½Π°Ρ‡Π΅Π½ΠΈΠ΅. Россия ΠΈ Австро-ВСнгрия ΡΡ‚ΠΎΠ»ΠΊΠ½ΡƒΠ»ΠΈΡΡŒ с рядом сущСствСнных ΠΏΡ€ΠΎΠ±Π»Π΅ΠΌ ΠΏΡ€ΠΈ ΠΎΡ€Π³Π°Π½ΠΈΠ·Π°Ρ†ΠΈΠΈ Π²Π½Π΅ΡˆΠ½Π΅ΡΠΊΠΎΠ½ΠΎΠΌΠΈΡ‡Π΅ΡΠΊΠΎΠΉ Π΄Π΅ΡΡ‚Π΅Π»ΡŒΠ½ΠΎΡΡ‚ΠΈ Π½Π° Ρ‚Π΅Ρ€Ρ€ΠΈΡ‚ΠΎΡ€ΠΈΠΈ Π‘ΠΈΡ€ΠΈΠΈ, Π›ΠΈΠ²Π°Π½Π° ΠΈ ΠŸΠ°Π»Π΅ΡΡ‚ΠΈΠ½Ρ‹. ΠšΡ€ΠΎΠΌΠ΅ ΠΊΠΎΠ½ΠΊΡƒΡ€Π΅Π½Ρ†ΠΈΠΈ Π΄Ρ€ΡƒΠ³ΠΈΡ… СвропСйских государств ΠΈ БША, ΠΈΠΌ ΠΏΡ€ΠΈΡˆΠ»ΠΎΡΡŒ ΡΡ‚ΠΎΠ»ΠΊΠ½ΡƒΡ‚ΡŒΡΡ с Π½ΠΈΠ·ΠΊΠΈΠΌ ΡƒΡ€ΠΎΠ²Π½Π΅ΠΌ Π΄ΠΎΡ…ΠΎΠ΄ΠΎΠ² мСстного насСлСния, Ρ‡Ρ‚ΠΎ сущСствСнно ΠΎΠ³Ρ€Π°Π½ΠΈΡ‡ΠΈΠ²Π°Π»ΠΎ Π΅Π³ΠΎ ΠΏΠΎΠΊΡƒΠΏΠ°Ρ‚Π΅Π»ΡŒΠ½ΡƒΡŽ ΡΠΏΠΎΡΠΎΠ±Π½ΠΎΡΡ‚ΡŒ ΠΈ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡ‚ΡŒ ΠΏΡ€ΠΈΠΎΠ±Ρ€Π΅Ρ‚Π°Ρ‚ΡŒ высококачСствСнныС ΠΈΠΌΠΏΠΎΡ€Ρ‚Π½Ρ‹Π΅ Ρ‚ΠΎΠ²Π°Ρ€Ρ‹

    Mesofauna influence on hamification process of vegetable oddments with partticipation microarthropod

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    Relevance of the studied problem is caused by the fact that stability of natural ecosystems strongly depends on functioning of their destructive block which closes a biological circulation. The organisms that ensure functioning of the destructive block are very different and numerous. All of them partly supplement, partly duplicate functions of each other that is an important factor of reliability of this ecosystem block. Shallow arthropods are important regulators of fossils mineralization and immobilizations of various biogens. Experiments demonstrate that if there are microarthropods, humification processes amplify and the optical density of humic acids raises. The aim of the article is to show degree and depth of change of mineralization and humification processes at the interaction of microarthropods and some mesofauna representatives in the processes of transformation of organic substance of vegetable oddments on the basis of experimental research. The most popular method to a research of this problem is the creation of laboratory microecosystems which have a clear boundary, which are easily reproduced and convenient for experimenting with subsequent instrumental determination of quantitative and qualitative humification parameters. In the course of experimental work it is revealed that the activity of soil-forming invertebrates results in strengthening humification processes. Humification rates, transformation depth of organic substance directly depend on cenotic organization of destructors. It is obvious that, the more complete the composition of biodegradative agents, the more intensive the decomposition process, the stronger the humification processes prevail over mineralization, the higher their maturity degree. All above-mentioned has a huge value to preserve a long-term fertility and high agronomical soil value, both in agrophitocenosis, and in natural biogeocenosis. Β© 2016 Simono, Svetkina and Kryuchkov

    Remote atomic clock synchronization via satellites and optical fibers

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    In the global network of institutions engaged with the realization of International Atomic Time (TAI), atomic clocks and time scales are compared by means of the Global Positioning System (GPS) and by employing telecommunication satellites for two-way satellite time and frequency transfer (TWSTFT). The frequencies of the state-of-the-art primary caesium fountain clocks can be compared at the level of 10e-15 (relative, 1 day averaging) and time scales can be synchronized with an uncertainty of one nanosecond. Future improvements of worldwide clock comparisons will require also an improvement of the local signal distribution systems. For example, the future ACES (atomic clock ensemble in space) mission shall demonstrate remote time scale comparisons at the uncertainty level of 100 ps. To ensure that the ACES ground instrument will be synchronized to the local time scale at PTB without a significant uncertainty contribution, we have developed a means for calibrated clock comparisons through optical fibers. An uncertainty below 50 ps over a distance of 2 km has been demonstrated on the campus of PTB. This technology is thus in general a promising candidate for synchronization of enhanced time transfer equipment with the local realizations of UTC . Based on these experiments we estimate the uncertainty level for calibrated time transfer through optical fibers over longer distances. These findings are compared with the current status and developments of satellite based time transfer systems, with a focus on the calibration techniques for operational systems

    Studying the compactibility of the VT22 high-strength alloy powder obtained by the PREP method

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    Compression curves are plotted for VT22 high-strength alloy powder under conditions of uniaxial compression at room temperature. The density of the compacted briquette at the loading and unloading stages is determined. It is demonstrated that strong interparticle bonds are formed in the area of the action of shear deformation. The results are supposed to be used to identify the flow model of the material studied and to perform the subsequent numerical modeling of the compaction process. Β© 2017 Author(s)
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