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52篇 您的检索式:作者名="ROYNE"
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1Timescales of interface-coupled dissolution-precipitation reactions oncarbonates显示文摘In the Earth's upper crust, where aqueous fluids can circulate freely, most mineral transformations are controlled by the coupling between the dissolution of a mineral that releases chemical species into the fluid and precipitation of new minerals that contain some of the released species in their crystal structure, the coupled process being driven by a reduction of the total free-energy of the system. Such coupled dissolution-precipitation processes occur at the fluid-mineral interface where the chemical gradients are highest and heterogeneous nucleation can be promoted, therefore controlling the growth kinetics of the new minerals. Time-lapse nanoscale imaging using Atomic Force Microscopy(AFM) can monitor the whole coupled process under in situ conditions and allow identifying the time scales involved and the controlling parameters. We have performed a series of experiments on carbonate minerals(calcite, siderite, dolomite and magnesite) where dissolution of the carbonate and precipitation of a new mineral was imaged and followed through time. In the presence of various species in the reacting fluid(e. g. antimony, selenium, arsenic, phosphate), the calcium released during calcite dissolution binds with these species to form new minerals that sequester these hazardous species in the form of a stable solid phase. For siderite, the coupling involves the release of Fe^(2+) ions that subsequently become oxidized and then precipitate in the form of FeIIIoxyhydroxides. For dolomite and magnesite,dissolution in the presence of pure water(undersaturated with any possible phase) results in the immediate precipitation of hydrated Mg-carbonate phases. In all these systems, dissolution and precipitation are coupled and occur directly in a boundary layer at the carbonate surface. Scaling arguments demonstrate that the thickness of this boundary layer is controlled by the rate of carbonate dissolution,the equilibrium concentration of the precipitates and the kinetics of diffusion of species in a boundary layer. From these parameters a characteristic time scale and a characteristic length scale of the boundary layer can be derived. This boundary layer grows with time and never reaches a steady state thickness as long as dissolution of the carbonate is faster than precipitation of the new mineral. At ambient temperature, the surface reactions of these dissolving carbonates occur on time-scales of the order of seconds to minutes, indicating the rapid surface rearrangement of carbonates in the presence of aqueous fluids. As a consequence, many carbonate-fluid reactions in low temperature environments are controlled by local thermodynamic equilibria rather than by the global equilibrium in the whole system.Francois Renard Anja Royne Christine V.Putnis 2019Geoscience Frontiers2019,10,1:2
2Uterine sarcomas in Norway:a histopathological and prognostic survey of a total population from 1970 to 2000 including419 patients显示文摘Abeler VM Royne O Thoresen S 2009Histopathology2009,54,3:1
3Cooling of photovoltaic cells under concentrated illumination: a critical review 显示文摘ROYNE A DEY C J MILLS D R 2005Solar Energy Materials and Solar Cells2005,86,:1
4Design of a jet impingement cooling device for densely packed PV cells under high concentration显示文摘ROYNE A DEY C J 2007Solar Energy2007,,81:1
5Uterine sarcomas in Norway:A histopathological and prognostic survey of a total population from 1970 to 2000 including 419 patients显示文摘Abeler VM Royne O Thoresen S 2009Histopathology2009,54,3:1
6SuppressionofapoptosisinmammaliancellsbyNAIPandarelatedfamilyofIAPgenes显示文摘ListonP RoyN TamaiK etal 1996Nature1996,379,6563:1
7Controls on rock weathering rates by reaction-induced hierarchical fracturing显示文摘Royne A Jamtveit B Mathiesen J 2008Earth and Planetary Science Letters2008,275,34:1
8Cooling of photovoltaic cells under concentrated illumination:a critical review显示文摘Royne A Dey C J Mill D R 2005Solar Energy Materals & Solar Cells2005,86,:1
9Cooling ofphotovoltaic cells under concen- trated illumination: a critical review 显示文摘Royne A Dey C Mills D 2005Solar Energy Materials and Solar Cells2005,86,:1
10Surgical and psychosocial outcomes in the rural injured a follow-up study of the 2001 earthquake victims显示文摘RoyN Shah H Patel V 0,,08:1
11Technology Acceptance and Satisfaction with Logistics Services显示文摘BIENSTOCK C C ROYNE M B 2010The International Journal of Logistics Management2010,21,2:1
12An expanded model of logistics service quality: Incorporating logistics information technology显示文摘BIENSTOCK C C ROYNE M B SHERRELL D 2007International Journal of Production Economics2007,,7:1
13Cooling of photovoltaic cells under concentrated illumination: a critical review 显示文摘Royne A Dey C J Mill D R 2005Solar Energy Materals & Solar Cells2005,86,:1
14Rapid dingnnosis of infantile spinal muscular atrophy by direct amplificantion of amniocyte and CVS DNA显示文摘MacKennzieA BesnerA RoyN 1993J Med Genet1993,30,2:1
15Design of a jet impingement cooling device for densely packed PV cells under high concentration显示文摘Royne A Dey C J 2007Solar Energy2007,81,8:1
16Self-reported training needs of emergency responders in disasters requiring military interface 显示文摘Levy M Koch RW Royne MB 2013J Emerg Manag2013,11,2:1
17Cooling of photovoltaic cells under concentrated illumination:A critical review显示文摘Royne A Dey C J Mills D R 0,,04:1
18Anexpanded model of logistics service qualityrln-corporating logistics information technology 显示文摘BienstockC C Royne M B Sherrell D 2007International Journal of Production Economics2007,,7:1
19Design of a jet impingement cooling device for densely packed PV cells under high concentration显示文摘Royne A Dey C J 2007Solar Energy2007,81,8:1
20Cooling of photovoltaic cells under concentrated illmnination:a critical review显示文摘Royne Anja Dey Christopher J Mills David R 2005Solar Energy Materials & Solar Cells2005,,86:1
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