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同位素分馏理论计算新进展

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  • 中国科学院地球化学研究所
方涛,男,1965年2月出生,副研究员,主要从事同位素地球化学的研究。

收稿日期: 1996-06-04

  修回日期: 1996-10-21

  网络出版日期: 1997-06-01

基金资助

国家自然科学基金项目“磷灰石氧同位素分馏高压实验研究(项目编号:49303040)资助.

DEVELOPMENT ON THE THEORETICAL CALCULATION OF ISOTOPE

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  • Institute of Geochemistry,Chinese Academy of Sciences,Guizhou  550002

Received date: 1996-06-04

  Revised date: 1996-10-21

  Online published: 1997-06-01

摘要

稳定同位素分馏的理论计算,既是同位素理论研究的重要方面,也是矿物物理研究的重要课题,它涉及矿物的宏观性质和微观性质两个方面。自从Urey(1947)以来,人们提出了许多计算模式,但绝大多数模式都是以还原配分函数比作为出发点,以自由能变化为基础。从方法上表现出两种趋势,一是简化的趋势,以尽可能少的参数得到尽可能合理的结果;二是大型化和精确化趋势,以复杂的晶格动力学模式和计算机的大量应用为特征。随着这方面研究的深入,理论计算将成为人们了解矿物同位素分馏性质的重要途径。

本文引用格式

方涛 . 同位素分馏理论计算新进展[J]. 地球科学进展, 1997 , 12(3) : 253 -258 . DOI: 10.11867/j.issn.1001-8166.1997.03.0253

Abstract

The theoretical calculation of stable isotope fractionation is an important aspect of both stable isotopic theory and mineral's thermodynamic research because it deals with mineral's property in both microscope and macroscope. Many models have been proposed since Urey(1947)and most of them are based on the change in free energy and calculated from the reduced partition function ratios. Two trendecies have been displayed in recent models:simplication-getting reasonable results with less index;accuratif ication-characterized by the widely used of computer and the complicated thermodynamic calculation. With the developement in this area,the theoretical calculation could become an important way to understand mineral's isotopic fractionation properties in future.

参考文献

1 方涛. a-U03氧同位素分馏理论计算.科学通报,1995,40(20):1881 - 84.
2 方涛.黑铜矿氧同位素分馏理论计算.地球化学,1996.25(3):221 - 227.
3 方涛.硅烷氢同位素分馏理论计算.矿物岩石,1997,17(2).
4 卢武长.根据矿物的氧键估计矿物一水氧同位素分馏方程.成都地质学院院报,1981.2:10-15.
5 Bachinski J. Bond strength and sulfur isotopic fractionation in coexisting sulfides. Econ Geol,1969,64:56-65.
6 Bottinga Y. Carbon isotope fractionation between graphite.diamond and carbon dioxide. Earth Planet Sci Lett, 1969,5:301-306.
7 Chacko T,et al. Oxygen and carbon fractionation between CO2 and calcite, Geocltim Cosmochim Acta,1991,(3):2870-2884.
8  Elcombe M. Calculation of sulphur isotope fractionation between sphalerite and g1ena using Lattice dynamics. Earth Planet Sci Lett,1975,28:172-180.
9 Kieffer S W. Thermodynamic and lattice vibrations of minerals 5:Applications to phase equilibria,isotopic fractionation and high-pressure thermodynamic properties. Rev Geophys Space Phys,1982,20:827-849.
10 O'Neil J R, Clayton R N,Mayeda T K. Oxygen. isotope fractionation in divalent metal carbonates.  J Chem Phys,1969,51:5547-5558.
11 Atul Patel,Geoffrey D Price,et al. A computer simulation approach to modelling the structure, thermodynamics and oxygen isotope equilihria of silicates.  Phys Chem Minerals,1991,17:690-699.
12 Richet P, $ottinga Y,Javoy M. A review of hydrogen,carbon,nitrogen,oxygen, sulfur and chlorine stable isotope fractionation among gaseous molecules. Ann Rev Earth Planet Sci,1977,5:85-110.
13 Urey H C. The thermodynamic properties of isotopic substances.  J Chem Soc,1947,562-581.
14 Wesolowsski D. Calculated oxygen isotope fractionation factors between water and the mineral scheelite and powellite. Econ Geol,Isas,81:471-477.
15 Zheng Y F.Calculation of oxygen isotope fractionation in metal oxides. Geochim Cosmochim Acta, 1991,55:2299-2307.
16 Zheng Y F. Oxygen isotope fractionation in woliramite.  European J Mineral,1992,4:1331-1335.
17 Zheng Y F. Calculation of oxygen isotope fractionation in anhydrous silicate minerals. Geochim Cosmochim Acta,1993,57:1079-1091.

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