19 research outputs found
ΠΠΠΠΠΠΠΠΠ-Π₯ΠΠΠΠ§ΠΠ‘ΠΠΠ Π‘ΠΠΠΠ‘Π’ΠΠ ΠΠ ΠΠΠΠΠΠΠ ΠΠΠΠΠ§ΠΠ‘ΠΠΠ₯ ΠΠΠ, ΠΠ ΠΠΠΠΠ―ΠΠΠ«Π₯ Π Π‘ΠΠΠ’ΠΠΠ ΠΠΠΠΠ‘Π’ΠΠ ΠΠΠ¬ΠΠ«Π₯ ΠΠΠ’ΠΠΠ‘ΠΠ
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 substancesβ 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‘ΠΈΠ½ΡΠ΅Π· ΠΏΠΎΠ»ΠΈΠΌΠ΅ΡΠ½ΡΡ
ΡΡΡΠΏΠ΅Π½Π·ΠΈΠΉ Ρ ΡΠ·ΠΊΠΈΠΌ ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΠ΅ΠΌ ΡΠ°ΡΡΠΈΡ ΠΏΠΎ ΡΠ°Π·ΠΌΠ΅ΡΠ°ΠΌ ΡΠ²Π»ΡΠ΅ΡΡΡ Π°ΠΊΡΡΠ°Π»ΡΠ½ΠΎΠΉ ΠΏΡΠΎΠ±Π»Π΅ΠΌΠΎΠΉ Π² ΡΠΎΠ²ΡΠ΅ΠΌΠ΅Π½Π½ΠΎΠΉ Π½Π°ΡΠΊΠ΅. ΠΠΎΠ»ΠΈΠΌΠ΅ΡΠ½ΡΠ΅ ΠΌΠΈΠΊΡΠΎΡΡΠ΅ΡΡ ΠΏΡΠΈΠΌΠ΅Π½ΠΈΠΌΡ Π² ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
ΠΎΡΡΠ°ΡΠ»ΡΡ
Ρ
ΠΈΠΌΠΈΠΈ, ΡΠ°ΡΠΌΠ°ΡΠ΅Π²ΡΠΈΠΊΠΈ, Π±ΠΈΠΎΠ»ΠΎΠ³ΠΈΠΈ ΠΈ ΠΌΠ΅Π΄ΠΈΡΠΈΠ½Ρ, Π² ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅ Π½ΠΎΡΠΈΡΠ΅Π»Π΅ΠΉ Π±ΠΈΠΎΠ»ΠΈΠ³Π°Π½Π΄ΠΎΠ² ΠΏΡΠΈ ΡΠΎΠ·Π΄Π°Π½ΠΈΠΈ Π΄ΠΈΠ°Π³Π½ΠΎΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΠ΅ΡΡ-ΡΠΈΡΡΠ΅ΠΌ. Π ΡΠ°Π±ΠΎΡΠ΅ ΠΏΡΠΈΠ²Π΅Π΄Π΅Π½Ρ Π΄Π°Π½Π½ΡΠ΅ ΠΏΠΎ ΠΈΠ·ΡΡΠ΅Π½ΠΈΡ ΠΊΠΎΠ»Π»ΠΎΠΈΠ΄Π½ΠΎ-Ρ
ΠΈΠΌΠΈΡΠ΅ΡΠΊΠΈΡ
Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊ Π½Π΅ΡΠ°ΡΡΠ²ΠΎΡΠΈΠΌΡΡ
Π² Π²ΠΎΠ΄Π΅ ΡΡΠΎΡΠΈΡΠΎΠ²Π°Π½Π½ΡΡ
ΠΊΡΠ΅ΠΌΠ½ΠΈΠΉΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΏΠΎΠ²Π΅ΡΡ
Π½ΠΎΡΡΠ½ΠΎ-Π°ΠΊΡΠΈΠ²Π½ΡΡ
Π²Π΅ΡΠ΅ΡΡΠ² (ΠΠΠ) ΠΈ ΠΊΠΈΠ½Π΅ΡΠΈΠΊΠΈ ΠΏΡΠΎΡΠ΅ΡΡΠ° ΠΏΠΎΠ»ΠΈΠΌΠ΅ΡΠΈΠ·Π°ΡΠΈΠΈ Π² ΠΈΡ
ΠΏΡΠΈΡΡΡΡΡΠ²ΠΈΠΈ. ΠΠ·ΡΡΠ΅Π½ΠΈΠ΅ ΡΠ΅ΠΎΠ»ΠΎΠ³ΠΈΠΈ Π΄Π°Π½Π½ΡΡ
Π²Π΅ΡΠ΅ΡΡΠ² ΠΏΠΎΠ·Π²ΠΎΠ»ΠΈΠ»ΠΎ ΠΎΠΏΡΠ΅Π΄Π΅Π»ΠΈΡΡ Π½Π°ΠΈΠ±ΠΎΠ»Π΅Π΅ ΠΏΠΎΠ΄Ρ
ΠΎΠ΄ΡΡΠ΅Π΅ ΠΠΠ Π΄Π»Ρ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΏΡΠΎΡΠ½ΠΎΠ³ΠΎ ΠΌΠ΅ΠΆΡΠ°Π·Π½ΠΎΠ³ΠΎ Π°Π΄ΡΠΎΡΠ±ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΡΠ»ΠΎΡ ΠΏΡΠΈ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΠΈ ΠΏΠΎΠ»ΠΈΠΌΠ΅ΡΠ½ΠΎ-ΠΌΠΎΠ½ΠΎΠΌΠ΅ΡΠ½ΡΡ
ΡΠ°ΡΡΠΈΡ Π² ΠΏΡΠΎΡΠ΅ΡΡΠ΅ ΠΏΠΎΠ»ΠΈΠΌΠ΅ΡΠΈΠ·Π°ΡΠΈΠΈ. Π‘ΠΏΠΎΡΠΎΠ±Π½ΠΎΡΡΡ ΡΡΠΎΡΠΈΡΠΎΠ²Π°Π½Π½ΡΡ
ΠΊΡΠ΅ΠΌΠ½ΠΈΠΉΠΎΡΠ³Π°Π½ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΠΠ ΠΎΠ±ΡΠ°Π·ΠΎΠ²ΡΠ²Π°ΡΡ ΡΡΠ°Π±ΠΈΠ»ΡΠ½ΡΠ΅ ΠΏΠΎΠ»ΠΈΠΌΠ΅ΡΠ½ΡΠ΅ ΡΡΡΠΏΠ΅Π½Π·ΠΈΠΈ Π±ΡΠ»Π° Π΄ΠΎΠΊΠ°Π·Π°Π½Π° ΠΏΡΠΈ ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½ΠΈΠΈ Π³Π΅ΡΠ΅ΡΠΎΡΠ°Π·Π½ΠΎΠΉ ΠΏΠΎΠ»ΠΈΠΌΠ΅ΡΠΈΠ·Π°ΡΠΈΠΈ Π²ΠΈΠ½ΠΈΠ»ΠΎΠ²ΡΡ
ΠΌΠΎΠ½ΠΎΠΌΠ΅ΡΠΎΠ². ΠΠΎΠ»ΡΡΠ΅Π½Π½ΡΠ΅ ΠΏΠΎΠ»ΠΈΠΌΠ΅ΡΠ½ΡΠ΅ ΡΡΡΠΏΠ΅Π½Π·ΠΈΠΈ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΠ·ΠΎΠ²Π°Π»ΠΈΡΡ ΡΠ·ΠΊΠΈΠΌ ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΠ΅ΠΌ ΡΠ°ΡΡΠΈΡ ΠΏΠΎ ΡΠ°Π·ΠΌΠ΅ΡΠ°ΠΌ, Π° ΡΠ°ΠΊΠΆΠ΅ Π²ΡΡΠΎΠΊΠΎΠΉ Π°Π³ΡΠ΅Π³Π°ΡΠΈΠ²Π½ΠΎΠΉ ΡΡΡΠΎΠΉΡΠΈΠ²ΠΎΡΡΡΡ Π² ΠΏΡΠΎΡΠ΅ΡΡΠ΅ ΡΠΈΠ½ΡΠ΅Π·Π° ΠΈ ΠΏΡΠΈ Ρ
ΡΠ°Π½Π΅Π½ΠΈΠΈ
Hypogene Speleogenesis in the Piedmont Crimea Range
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
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 metalβinsulator transition and THz transmission switch properties
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 metalβinsulator transition (MIT)
COLLOID-CHEMICAL PROPERTIES OF SILICONE SURFACTANTS USED IN THE SYNTHESIS OF POLYSTYRENE LATEXES
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 substancesβ 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
Large thickness-dependent improvement of crystallographic texture of CVD silicon films on R-sapphire
Synthesis of Sulfur-Containing Heterocycles by Electrophilic Addition Reactions of Disulfur Dichloride
Novel fused tetrathiocines as antivirals that target the nucleocapsid zinc finger containing protein of the feline immunodeficiency virus (FIV) as a model of HIV infection
A novel series of fused tetrathiocines were prepared for evaluation of activity against the nucleocapsid protein of the feline immunodeficiency virus (FIV) in an in vitro cell culture approach. The results demonstrated that the compounds display potent nanomolar activity and low toxicity against this key model of HIV infection