High-Pressure Experimental Studies on Geo-Liquids Using Synchrotron Radiation at the Advanced Photon Source

查看全文 作　　者：Yanbin [1]Wang;Guoyin [2]Shen

机构地区：[1]Center for Advanced Radiation Sources, The University of Chicago;[2]HPCAT, Geophysical Laboratory, Carnegie Institution of Washington

出　　处：《Journal of Earth Science》索引2014年第25卷第6期,共20页

基　　金：support from the National Science Foundation (Nos. EAR-0001088, 0711057, and 1214376);Guoyin Shen acknowledges support from the DOE (Nos. DE-NA0001974 and DE-FG02-99ER45775);COMPRES for the support in developing the PEP system. Portions of this work were performed at GeoS oilE nviroC ARS (Sector 13), Advanced Photon Source (APS), Argonne National Laboratory;Geo Soil Enviro CARS is supported by the National Science Foundation-Earth Sciences (No. EAR-1128799);Department of Energy-Geo Sciences (No. DE-FG02-94ER14466);HPCAT operations are supported by DOE-NNSA under Award (Nos. DE-NA0001974);DOE-BES under Award (No. DE-FG02-99ER45775), with partial instrumentation funding by NSF;Use of the Advanced Photon Source was supported by the U. S. Department of Energy, Office of Science, Office of Basic Energy Sciences, under Contract (No. DE-AC02-06CH11357) 摘　　要：We review recent progress in studying silicate, carbonate, and metallic liquids of geological and geophysical importance at high pressure and temperature, using the large-volume high-pressure devices at the third-generation synchrotron facility of the Advanced Photon Source, Argonne National Laboratory. These integrated high-pressure facilities now offer a unique combination of experimental techniques that allow researchers to investigate structure, density, elasticity, viscosity, and interfacial tension of geo-liquids under high pressure, in a coordinated and systematic fashion. Experimental techniques are described, along with scientific highlights. Future developments are also discussed. 关键词：国家实验室高温高压同步辐射光子源液体地理实验技术液态金属

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High-Pressure Experimental Studies on Geo-Liquids Using Synchrotron Radiation at the Advanced Photon Source

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