42 research outputs found

    Plasma–liquid interactions: a review and roadmap

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    Plasma–liquid interactions represent a growing interdisciplinary area of research involving plasma science, fluid dynamics, heat and mass transfer, photolysis, multiphase chemistry and aerosol science. This review provides an assessment of the state-of-the-art of this multidisciplinary area and identifies the key research challenges. The developments in diagnostics, modeling and further extensions of cross section and reaction rate databases that are necessary to address these challenges are discussed. The review focusses on non-equilibrium plasmas

    Potential Field Studies on the Crustal Structure of the Laptev Sea and the Western Part of the East Siberian Sea

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    Irradiation facility for production of 82Sr isotope on isochronous cyclotron U-240

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    Investigations allowing obtaining of 82Sr isotope upon irradiation of target RbCl by internal proton beam in the cyclotron U-240 were performed. The facility, providing long exposure of the target RbCl upon internal proton beam with the intensity of 150 mA and with energy not less than 70 MeV, was constructed

    Chemical composition, age, and magnetic parameters of igneous rocks from the Franz Josef Land

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    A combined study of magnetic parameters of basalt and andesite samples has been carried out in the framework of geological investigations of the Franz Josef Land. This study has included determination of coercivity, saturation magnetization, Curie points, natural remanent magnetization (NRM), and magnetic susceptibility as well as examination of ferromagnetic minerals with a microscope. Data on chemical composition of the rocks have been obtained for all the samples, and radiological ages have been determined for the majority of the rocks. Thermomagnetic curves of the samples have been subdivided into four types depending on composition of ferromagnetic NRM carriers. Data showing multiple changes in the predominant composition of the igneous rocks have been obtained. Each stage of magmatism is characterized by a specific type of the ferromagnetic component in the rocks and, therefore, magnetomineralogical investigations can be used for differentiation and correlation of the igneous rocks
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