19 research outputs found

    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

    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

    Hypogene Speleogenesis in the Piedmont Crimea Range

    No full text
    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

    Hydrothermal epitaxy growth of self-organized vanadium dioxide 3D structures with metal–insulator transition and THz transmission switch properties

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    The hydrothermal method is the most effective approach for the synthesis of VO2 metastable polymorphs with unique powder crystallite morphology. In this work, we expanded the capabilities of this method, directing it to the growth of oriented crystallites in self-organized systems on single crystal substrates. According to our investigations, a large variety of 3D structures of vanadium dioxide can be obtained using one single crystal substrate r-sapphire by fine tuning of synthesis parameters. The orientation growth of six-pointed vanadium dioxide crystallites fits into an epitaxial growth model describing unit cell relations between the VO2(M1) film and r-sapphire substrate. We describe the process of VO2(M1) phase stabilization in the films and the changes of resistivity and terahertz transparency of the films based on the metal–insulator transition (MIT)

    COLLOID-CHEMICAL PROPERTIES OF SILICONE SURFACTANTS USED IN THE SYNTHESIS OF POLYSTYRENE LATEXES

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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
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