GYIG OpenIR  > 地球内部物质高温高压实验室  > 期刊论文
In-situ synchrotron X-ray diffraction study of scorodite at high pressure
DAWEI FAN; MAINING MA; SHUYI WEI; BAOSHENG LI; ZHIQIANG CHEN; HONGSEN XIE
2013
发表期刊High Temperatures -- High Pressures
卷号42期号:3页码:203-209
摘要The compression behavior of a natural scorodite has been investigated to about 8.21 GPa at 300 K for the fist time using in situ angle-dispersive X-ray diffraction and a diamond anvil cell at beamline X17C, National Synchrotron Light Source, Brookhaven National Laboratory. Over this pressure range, no phase change or disproportionation has been observed. The isothermal equation of state was determined for the first time. The values of V-0, K-0, and K'(0) refined with a third-order Birch-Murnaghan equation of state are V-0 = 934.2 +/- 0.3 angstrom(3), K-0 = 61.8 +/- 2.5 GPa, and K'(0)= 6.6 +/- 0.9. Furthermore, we confirm that the linear compressibilities (beta) along a, b and c directions of scorodite is elastically anisotropic.
学科领域地球深部物质与流体作用地球化学
收录类别SCI
语种英语
文献类型期刊论文
条目标识符http://ir.gyig.ac.cn/handle/352002/5049
专题地球内部物质高温高压实验室_地球内部物质高温高压实验室_期刊论文
地球深部物质与流体作用地球化学研究室
推荐引用方式
GB/T 7714
DAWEI FAN,MAINING MA,SHUYI WEI,et al. In-situ synchrotron X-ray diffraction study of scorodite at high pressure[J]. High Temperatures -- High Pressures,2013,42(3):203-209.
APA DAWEI FAN,MAINING MA,SHUYI WEI,BAOSHENG LI,ZHIQIANG CHEN,&HONGSEN XIE.(2013).In-situ synchrotron X-ray diffraction study of scorodite at high pressure.High Temperatures -- High Pressures,42(3),203-209.
MLA DAWEI FAN,et al."In-situ synchrotron X-ray diffraction study of scorodite at high pressure".High Temperatures -- High Pressures 42.3(2013):203-209.
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
查看访问统计
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[DAWEI FAN]的文章
[MAINING MA]的文章
[SHUYI WEI]的文章
百度学术
百度学术中相似的文章
[DAWEI FAN]的文章
[MAINING MA]的文章
[SHUYI WEI]的文章
必应学术
必应学术中相似的文章
[DAWEI FAN]的文章
[MAINING MA]的文章
[SHUYI WEI]的文章
相关权益政策
暂无数据
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。