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Geochemical rate models :
详细信息    Geochemical rate models :
  • 出版日期:2014.
  • 出版者:Cambridge University Press,
  • 页数:x, 232 p. :
  • 出版地:Cambridge :
  • 第一责任说明:J. Donald Rimstidt.
  • 尺寸:26 cm.
  • 分类号:a270
  • ISBN:978-1-107-02997-2(hdk.) :
MARC全文
02h0047735 20141115092302.0 140905s2014 enka frb |001|||eng | 978-1-107-02997-2(hdk.) : CNY501.00 DLC eng DLC QE515.5.G43 R56 2014 551.9 23 a270 aP59 25 Rimstidt, J. Donald, 1947- Geochemical rate models : an introduction to geochemical kinetics / J. Donald Rimstidt. Cambridge : Cambridge University Press, 2014. x, 232 p. : ill. ; 26 cm. Includes bibliographical references and index. Geochemical models -- Modeling tools -- Rate equations -- Chemical reactors -- Molecular kinetics -- Surface kinetics -- Diffusion and advection -- Quasi-kinetics -- Accretion and transformation kinetics -- Pattern formation. This well-organised, comprehensive reference and textbook describes rate models developed from fundamental kinetic theory and presents models using consistent terminology and notation. Major topics include rate equations, reactor theory, transition state theory, surface reactivity, advective and diffusive transport, aggregation kinetics, nucleation kinetics, and solid-solid transformation rates. The theoretical basis and mathematical derivation of each model is presented in detail and illustrated with worked examples from real-world applications to geochemical problems. The book is also supported by online resources: self-study problems put students' new learning into practice, and spreadsheets provide the full data used in figures and examples, enabling students to manipulate the data for themselves. This is an ideal overview for graduate students, providing a solid understanding of geochemical kinetics. It will also provide researchers and professional geochemists with a valuable reference for solving practical and scientific problems. Geochemical modeling. ; Chemical kinetics. ; Geochemistry Mathematical models. aCN b010001 010001 270 R46 gljx1404 h1 ; rCNY501.00

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