51 research outputs found

    Implementing Automatic Handover Solutions for Linux-based Mobile Devices

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    In a heterogeneous network environment, transparent horizontal and vertical handover is a much desired feature. Effective handover solution would allow mobile device users to stay steadily connected, seamlessly switching between different access networks. If it also consistently connected to networks which offer best quality of service, that would dramatically improve user experience. Expanding upon our work in [1], we present a framework for creating your own custom handover solutions which could run on the clients’ Linux-based mobile devices. The framework consists of three core interacting components: scanners, which detect available networks; measurers, which measure network parameters for every detected network; and evaluators, which rank networks according to the values of the parameters. To provide an example of using the framework, we reimplement parts of our previous signal strength-based handover solution to get improved flexibility, modularity and modifiability

    ΠšΠžΠ›Π›ΠžΠ˜Π”ΠΠž-Π₯Π˜ΠœΠ˜Π§Π•Π‘ΠšΠ˜Π• Π‘Π’ΠžΠ™Π‘Π’Π’Π ΠšΠ Π•ΠœΠΠ˜Π™ΠžΠ Π“ΠΠΠ˜Π§Π•Π‘ΠšΠ˜Π₯ ΠŸΠΠ’, ΠŸΠ Π˜ΠœΠ•ΠΠ―Π•ΠœΠ«Π₯ Π’ Π‘Π˜ΠΠ’Π•Π—Π• ΠŸΠžΠ›Π˜Π‘Π’Π˜Π ΠžΠ›Π¬ΠΠ«Π₯ Π›ΠΠ’Π•ΠšΠ‘ΠžΠ’

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    The synthesis of polymeric suspensions with a narrow particle size distribution is an urgent problem in modern science. The resulting polymeric microspheres are applicable in various fields of chemistry, pharmaceuticals, biology and medicine. In particular, they can be used as carriers of bioligands to create diagnostic test systems. This article presents the results of a study on the colloid-chemical characteristics of water-insoluble fluorinated silicone surfactants and kinetics of the polymerization process in their presence. The results were compared with data from studies on the properties of surfactants of similar structure not containing fluorine atoms in their structure. Studying these substances’ rheology enabled to determine the most suitable surfactants for adsorption forming a strong interfacial layer during the formation of polymermonomer particles during the polymerisation. The ability of fluorinated silicone surfactants to form a stable polymeric slurry was proved during heterophase polymerization of vinyl monomers. The resulting polymeric suspensions were characterized by a narrow particle size distribution and high aggregative stability during the synthesis and in storage.Π‘ΠΈΠ½Ρ‚Π΅Π· ΠΏΠΎΠ»ΠΈΠΌΠ΅Ρ€Π½Ρ‹Ρ… суспСнзий с ΡƒΠ·ΠΊΠΈΠΌ распрСдСлСниСм частиц ΠΏΠΎ Ρ€Π°Π·ΠΌΠ΅Ρ€Π°ΠΌ являСтся Π°ΠΊΡ‚ΡƒΠ°Π»ΡŒΠ½ΠΎΠΉ ΠΏΡ€ΠΎΠ±Π»Π΅ΠΌΠΎΠΉ Π² соврСмСнной Π½Π°ΡƒΠΊΠ΅. ΠŸΠΎΠ»ΠΈΠΌΠ΅Ρ€Π½Ρ‹Π΅ микросфСры ΠΏΡ€ΠΈΠΌΠ΅Π½ΠΈΠΌΡ‹ Π² Ρ€Π°Π·Π»ΠΈΡ‡Π½Ρ‹Ρ… отраслях Ρ…ΠΈΠΌΠΈΠΈ, Ρ„Π°Ρ€ΠΌΠ°Ρ†Π΅Π²Ρ‚ΠΈΠΊΠΈ, Π±ΠΈΠΎΠ»ΠΎΠ³ΠΈΠΈ ΠΈ ΠΌΠ΅Π΄ΠΈΡ†ΠΈΠ½Ρ‹, Π² качСствС носитСлСй Π±ΠΈΠΎΠ»ΠΈΠ³Π°Π½Π΄ΠΎΠ² ΠΏΡ€ΠΈ создании диагностичСских тСст-систСм. Π’ Ρ€Π°Π±ΠΎΡ‚Π΅ ΠΏΡ€ΠΈΠ²Π΅Π΄Π΅Π½Ρ‹ Π΄Π°Π½Π½Ρ‹Π΅ ΠΏΠΎ ΠΈΠ·ΡƒΡ‡Π΅Π½ΠΈΡŽ ΠΊΠΎΠ»Π»ΠΎΠΈΠ΄Π½ΠΎ-химичСских характСристик нСрастворимых Π² Π²ΠΎΠ΄Π΅ Ρ„Ρ‚ΠΎΡ€ΠΈΡ€ΠΎΠ²Π°Π½Π½Ρ‹Ρ… крСмнийорганичСских повСрхностно-Π°ΠΊΡ‚ΠΈΠ²Π½Ρ‹Ρ… вСщСств (ΠŸΠΠ’) ΠΈ ΠΊΠΈΠ½Π΅Ρ‚ΠΈΠΊΠΈ процСсса ΠΏΠΎΠ»ΠΈΠΌΠ΅Ρ€ΠΈΠ·Π°Ρ†ΠΈΠΈ Π² ΠΈΡ… присутствии. Π˜Π·ΡƒΡ‡Π΅Π½ΠΈΠ΅ Ρ€Π΅ΠΎΠ»ΠΎΠ³ΠΈΠΈ Π΄Π°Π½Π½Ρ‹Ρ… вСщСств ΠΏΠΎΠ·Π²ΠΎΠ»ΠΈΠ»ΠΎ ΠΎΠΏΡ€Π΅Π΄Π΅Π»ΠΈΡ‚ΡŒ Π½Π°ΠΈΠ±ΠΎΠ»Π΅Π΅ подходящСС ΠŸΠΠ’ для формирования ΠΏΡ€ΠΎΡ‡Π½ΠΎΠ³ΠΎ ΠΌΠ΅ΠΆΡ„Π°Π·Π½ΠΎΠ³ΠΎ адсорбционного слоя ΠΏΡ€ΠΈ ΠΎΠ±Ρ€Π°Π·ΠΎΠ²Π°Π½ΠΈΠΈ ΠΏΠΎΠ»ΠΈΠΌΠ΅Ρ€Π½ΠΎ-ΠΌΠΎΠ½ΠΎΠΌΠ΅Ρ€Π½Ρ‹Ρ… частиц Π² процСссС ΠΏΠΎΠ»ΠΈΠΌΠ΅Ρ€ΠΈΠ·Π°Ρ†ΠΈΠΈ. Π‘ΠΏΠΎΡΠΎΠ±Π½ΠΎΡΡ‚ΡŒ Ρ„Ρ‚ΠΎΡ€ΠΈΡ€ΠΎΠ²Π°Π½Π½Ρ‹Ρ… крСмнийорганичСских ΠŸΠΠ’ ΠΎΠ±Ρ€Π°Π·ΠΎΠ²Ρ‹Π²Π°Ρ‚ΡŒ ΡΡ‚Π°Π±ΠΈΠ»ΡŒΠ½Ρ‹Π΅ ΠΏΠΎΠ»ΠΈΠΌΠ΅Ρ€Π½Ρ‹Π΅ суспСнзии Π±Ρ‹Π»Π° Π΄ΠΎΠΊΠ°Π·Π°Π½Π° ΠΏΡ€ΠΈ ΠΏΡ€ΠΎΠ²Π΅Π΄Π΅Π½ΠΈΠΈ Π³Π΅Ρ‚Π΅Ρ€ΠΎΡ„Π°Π·Π½ΠΎΠΉ ΠΏΠΎΠ»ΠΈΠΌΠ΅Ρ€ΠΈΠ·Π°Ρ†ΠΈΠΈ Π²ΠΈΠ½ΠΈΠ»ΠΎΠ²Ρ‹Ρ… ΠΌΠΎΠ½ΠΎΠΌΠ΅Ρ€ΠΎΠ². ΠŸΠΎΠ»ΡƒΡ‡Π΅Π½Π½Ρ‹Π΅ ΠΏΠΎΠ»ΠΈΠΌΠ΅Ρ€Π½Ρ‹Π΅ суспСнзии Ρ…Π°Ρ€Π°ΠΊΡ‚Π΅Ρ€ΠΈΠ·ΠΎΠ²Π°Π»ΠΈΡΡŒ ΡƒΠ·ΠΊΠΈΠΌ распрСдСлСниСм частиц ΠΏΠΎ Ρ€Π°Π·ΠΌΠ΅Ρ€Π°ΠΌ, Π° Ρ‚Π°ΠΊΠΆΠ΅ высокой Π°Π³Ρ€Π΅Π³Π°Ρ‚ΠΈΠ²Π½ΠΎΠΉ ΡƒΡΡ‚ΠΎΠΉΡ‡ΠΈΠ²ΠΎΡΡ‚ΡŒΡŽ Π² процСссС синтСза ΠΈ ΠΏΡ€ΠΈ Ρ…Ρ€Π°Π½Π΅Π½ΠΈΠΈ

    Synthesis of 1,4-Dithiins from Pentathiepins.

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    Thienopentathiepins and Pentathiepinofuran.

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    Direct Synthesis of Fused 1,2,3,4,5-Pentathiepins.

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    Hypogene Speleogenesis in the Piedmont Crimea Range

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    Intense development of the theory and criteria for identification of hypogenic speleogenesis during the past few years has stimulated re-interpretation of karst phenomena in many regions of the world. Recent research strongly suggests that solution features in the Piedmont Range of the Crimean Mountains, previously believed to be the result of hypergene (epigene) karstification, were in fact formed in a hypogenic environment due to ascending transverse flow in a stratified artesian system. Tectonically, the Piedmont Range of Crimea is an edge of the Scythian Plate, uplifted and partially eroded along the regional fault separating the plate from the folded region of the Crimea Mountains. The Cretaceous and Paleogene sequence dips 5 to 20o to north and north-west, where it plunges beneath a Neogene cover. It is exposed within the Piedmont Range as a series of distinct cuestas generally facing south-east. Karst features are represented by 26 caves and abundant, diverse solution forms at the cuesta escarps. Most of the karst develops in two distinct limestone units of Paleocene (Danian) and Eocene (Lutetian) but some are present in the underlying Maastrichtian unit of Cretaceous. There are strong and systematic evidences that the caves have a hypogenic origin and that most of the solution features along the scarps are remnants of morphologies of hypogenically karstified fractures, the walls of which are now exposed due to block-fall retreat of the scarp faces. The features in various beds demonstrate strong lithostratigraphic control in their distribution and are vertically stacked into transverse complexes. Caves are fracture-controlled, linear, or crude maze clusters, demonstrating the complete suite of morphologies indicative of hypogenic origin. Isolated cavities, expressed in the contemporary scarps as grottoes, niches and as zones of spongework porosity, developed where laterally conductive beds of higher initial porosity were crossed by vertical fractures that once conducted rising fluids from an underlying r
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