OXYGEN DIFFUSION IN FORSTERITE

被引：105

作者：

REDDY, KPR ^{[1
]}

OH, SM ^{[1
]}

MAJOR, LD ^{[1
]}

COOPER, AR ^{[1
]}

机构：

[1] CASE WESTERN RESERVE UNIV,DEPT MET & MAT SCI,CLEVELAND,OH 44106

来源：

JOURNAL OF GEOPHYSICAL RESEARCH | 1980年 / 85卷 / NB1期

关键词：

OXYGEN; -; Diffusion;

D O I：

10.1029/JB085iB01p00322

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：

Oxygen self-diffusion coefficients for forsterite single crystals were determined in different orientations by the single-spectrum proton activation technique. In the temperature range 1275 degree - 1625 degree C the diffusion coefficients in b direction can be represented by D//b equals 3. 5 multiplied by 10** minus **3 exp left bracket ( minus 89 plus or minus 3 kcal/mol)/RT right bracket cm**2/s. right bracket

引用

页码：322 / 326

页数：5

共 11 条

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[3] 2
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