TERMINOLOGY FOR TRACE-ELEMENT PARTITIONING

被引：112

作者：

BEATTIE, P

DRAKE, M

JONES, J

LEEMAN, W

LONGHI, J

MCKAY, G

NIELSEN, R

PALME, H

SHAW, D

TAKAHASHI, E

WATSON, B

机构：

[1] LYNDON B JOHNSON SPACE CTR,HOUSTON,TX 77058

[2] UNIV HAWAII MANOA,DIV PLANETARY SCI,HONOLULU,HI 96822

[3] RICE UNIV,DEPT GEOL & GEOPHYS,HOUSTON,TX 77251

[4] RENSSELAER POLYTECH INST,DEPT EARTH & ENVIRONM SCI,TROY,NY 12180

[5] MCMASTER UNIV,DEPT GEOL,HAMILTON L8S 4M1,ONTARIO,CANADA

[6] TOKYO INST TECHNOL,MEGURO KU,TOKYO 152,JAPAN

[7] MAX PLANCK INST CHEM,W-6500 MAINZ,GERMANY

[8] COLUMBIA UNIV,LAMONT DOHERTY GEOL OBSERV,PALISADES,NY 10964

[9] OREGON STATE UNIV,COLL OCEANOG,CORVALLIS,OR 97331

来源：

GEOCHIMICA ET COSMOCHIMICA ACTA | 1993年 / 57卷 / 07期

关键词：

D O I：

10.1016/0016-7037(93)90015-O

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

A self-consistent terminology for partitioning data is presented. Ratios of the concentration of a component in two phases are termed partition coefficients and given the symbol D. Ratios of partition coefficients are termed exchange coefficients and given the symbol K(D). The prefix ''bulk'' implies that these coefficients are weighted according to the proportions of coexisting phases. Bulk partition and bulk exchange coefficients are denoted by DBAR and K(D)BAR, respectively.

引用

页码：1605 / 1606

页数：2

共 9 条

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