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Multi-Physics and Multi-Scale Modeling and Simulation Methods for Nuclear Reactor Application
A nuclear reactor operates in an environment where complex multi-physics and multi-scale phenomena exist, and it requires consideration of coupling among neutronics, thermal hydraulics, fuel performance, chemical dynamics, and coupling between the reactor core and first circuit. Safe, reliable, and economical operation can be achieved by leveraging high-fidelity numerical simulation, and proper considerations for coupling among different physics and required to provide powerful numerical simulation tools. In the past simplistic models for some of the physics phenomena are used, with the recent development of advanced numerical methods, software design, and high-performance computing power, the appeal of multi-physics and multi-scale modeling and simulation has been broadened.
Metallogenic Theory and Exploration Technology of Multi-Arc-Basin-Terrane Collision Orogeny in “Sanjiang” Region, Southwest China
This open access book presents a new structural model of “multi-arc-basin-terrane system” based on the in-depth research of the Nujiang-Lancangjiang-Jinshajiang region, especially several Paleo-Tethys ophiolitic mélange belts and sets of arc-basin systems, and a new orogenic model of “The Hengduan shan Mountains” based on penetrated research on spatial-temporal framework and orogenic models of different orogenic belts under large-scale strike-slip-shear-nappe structures evolution. The authors paid special attention on the coupling relation between orogeny and metallogenesis. The metallogenesis and dynamic process are probed under the crust–mantle interaction and material-energy ex...
Ofioliti
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Scientific Programme
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The Geology of China
The first published account in forty years, this up-to-date survey of the geology of China, written by three prominent Chinese scientists, makes available to the West a vast body of information hitherto difficult to obtain, including data gleaned from many papers and unpublished reports produced in China since 1949. The core of the book is a fourteen-chapter survey of the geological history of China, from the Archaean to the Quaternary. The book also features a consideration of igneous and metamorphic rock, and concludes with a description of the geotectonics of China. This landmark volume will be an integral part of all library collections in geology.
