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  • 1
    Publication Date: 2021-05-19
    Description: Based on the clay minerals, content analysis from 187 stations in the surface sediments, this paper dealt with the assemblages and the distributions of clay minerals in the surface sediments off the Yangtze River estuary. The research results showed that the illite dominates the surface sediments off the Yangtze River estuary with the smectite or kaolinite the second rank and chlorite the third rank; the illite-smectite- kaolinite- chlorite-assemblage is the main type of the clay minerals assemblage in the area, with the illite-kaolinite-chlorite-smectite -type as the second rank; the source of clay mineral is mainly from the Yellow River and the Yangtze River. The Q-type cluster analysis show that sediments from both recent and ancient Yellow River were deposited mainly in the northeast part of the study area to the north of 29°30′. Substance from the Yangtze River was deposited mainly in the western and middle parts off the Yangtze River estuary.
    Description: Published
    Keywords: Clay minerals ; Distribution
    Repository Name: AquaDocs
    Type: Journal Contribution , Non-Refereed , Article
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  • 2
    Publication Date: 2021-05-19
    Description: Based on the clay minerals, content analysis from 187 stations in the surface sediments, this paper dealt with the assemblages and the distributions of clay minerals in the surface sediments off the Yangtze River estuary. The research results showed that the illite dominates the surface sediments off the Yangtze River estuary with the smectite or kaolinite the second rank and chlorite the third rank; the illite-smectite- kaolinite- chlorite-assemblage is the main type of the clay minerals assemblage in the area, with the illite-kaolinite-chlorite-smectite -type as the second rank; the source of clay mineral is mainly from the Yellow River and the Yangtze River. The Q-type cluster analysis show that sediments from both recent and ancient Yellow River were deposited mainly in the northeast part of the study area to the north of 29°30′. Substance from the Yangtze River was deposited mainly in the western and middle parts off the Yangtze River estuary.
    Description: Published
    Keywords: Clay minerals ; Distribution characteristic
    Repository Name: AquaDocs
    Type: Journal Contribution , Not Known
    Format: pp.56-69
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  • 3
    Publication Date: 2012-04-15
    Description: Perovskite ceramics of Ba [ Ti 1− x ( Co 0.5 W 0.5 ) x ] O 3 ( x  = 0.40–0.90) were synthesized by a conventional solid-state reaction method. Crystal phase, microstructure, and microwave dielectric property of the ceramics were investigated. A phase transition from simple cubic ( x  = 0.40–0.55) to hexagonal and then to cubic double pervoskite ( x  = 0.75–0.90) was detected. A single hexagonal perovskite structure ( P6 3 /mmc ) was obtained at 1425°C and stabilized at room temperature only at x  = 0.61. For ceramics x  = 0.55–0.60 and x  = 0.62–0.75, they are mixtures that consisted of cubic and hexagonal perovskites. With increasing x , Qx f increased from 2800 to 20 700 GHz, whereas dielectric constant (ε r ) decreased from 65 to 18, and temperature coefficient of resonant frequency (τ ƒ ) decreased from 44 to −17 ppm/°C. Hexagonal perovskite (ε r  = 18, Qx f  = 7700 GHz, τ ƒ  = −14 ppm/°C) had decreased ε r , τ ƒ and increased Qx f values, compared with the cubic perovskite phases. The phase formation and the relationship between structures and microwave dielectric properties were discussed.
    Print ISSN: 0002-7820
    Electronic ISSN: 1551-2916
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Published by Wiley
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  • 4
    Publication Date: 2012-01-12
    Description: Perovskite ceramics of Ba [ Ti 1− x ( Co 0.5 W 0.5 ) x ] O 3 ( x  = 0.40–0.90) were synthesized by a conventional solid-state reaction method. Crystal phase, microstructure, and microwave dielectric property of the ceramics were investigated. A phase transition from simple cubic ( x  = 0.40–0.55) to hexagonal and then to cubic double pervoskite ( x  = 0.75–0.90) was detected. A single hexagonal perovskite structure ( P6 3 /mmc ) was obtained at 1425°C and stabilized at room temperature only at x  = 0.61. For ceramics x  = 0.55–0.60 and x  = 0.62–0.75, they are mixtures that consisted of cubic and hexagonal perovskites. With increasing x , Qx f increased from 2800 to 20 700 GHz, whereas dielectric constant (ε r ) decreased from 65 to 18, and temperature coefficient of resonant frequency (τ ƒ ) decreased from 44 to −17 ppm/°C. Hexagonal perovskite (ε r  = 18, Qx f  = 7700 GHz, τ ƒ  = −14 ppm/°C) had decreased ε r , τ ƒ and increased Qx f values, compared with the cubic perovskite phases. The phase formation and the relationship between structures and microwave dielectric properties were discussed.
    Print ISSN: 0002-7820
    Electronic ISSN: 1551-2916
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Published by Wiley
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  • 5
    Publication Date: 2016-11-11
    Description: Anode melting and crater formation significantly affect interruption of high-current vacuum arcs. The primary objective of this paper is to theoretically investigate the mechanism of anode surface crater formation, caused by the combined effect of surface heating during the vacuum arc and pressure exerted on the molten surface by ions and electrons from the arc plasma. A model of fluid flow and heat transfer in the arc anode is developed and combined with a magnetohydrodynamics model of the vacuum arc plasma. Crater formation is observed in simulation for a peak arcing current higher than 15 kA on 40 mm diam. Cu electrodes spaced 10 mm apart. The flow of liquid metal starts after 4 or 5 ms of arcing, and the maximum velocities are 0.95 m/s and 1.39 m/s for 20 kA and 25 kA arcs, respectively. This flow redistributes thermal energy, and the maximum temperature of the anode surface does not remain in the center. Moreover, the condition for the liquid droplet formation on the anode surfaces is developed. The solidification process after current zero is also analyzed. The solidification time has been found to be more than 3 ms after 25 kA arcing. The long solidification time and sharp features on crater rims induce Taylor cone formation.
    Print ISSN: 0021-8979
    Electronic ISSN: 1089-7550
    Topics: Physics
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  • 6
    Publication Date: 2016-07-27
    Print ISSN: 0039-3169
    Electronic ISSN: 1573-1626
    Topics: Architecture, Civil Engineering, Surveying , Geosciences , Physics
    Published by Springer
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