CAS OpenIR
K-H3OFe3(SO4)2(OH)6铁矾的XRD研究
许涛1; 邹来昌1; 阮仁满2; 廖占丕1; 苏秀珠1; 苏妤芸1; 黄丽娟1
2013
Source Publication岩石矿物学杂志
ISSN1000-6524
Volume32.0Issue:006Pages:995
Abstract根据X射线衍射(XRD)分析发现:A Fe3(SO4)2(OH)6(A=K+、H3O+)系列铁钒的XRD数据十分相近,难以用XRD区别,需通过能谱(EDS)辅助分析,才能区分此类铁矾.另外,此类铁矾的003和107面网间距d随K+含量增大而增大,且呈一元三次方程的关系;而033和220面网间距d随K+含量增大而减小,呈一元二次方程的关系.对该现象从铁矾晶体结构方面进行解释:K+、H3O+离子位于较大空隙中,且沿着Z轴方向排列,当K+、H3O+离子之间相互替换时,会导致该铁矾晶体结构在Z轴方向有较明显的变化.
Keyword铁矾 XRD 晶体结构 鉴别
Language英语
Document Type期刊论文
Identifierhttp://ir.ipe.ac.cn/handle/122111/45347
Collection中国科学院过程工程研究所
Affiliation1.紫金矿业低品位难处理黄金资源综合利用国家重点实验室
2.中国科学院过程工程研究所
Recommended Citation
GB/T 7714
许涛,邹来昌,阮仁满,等. K-H3OFe3(SO4)2(OH)6铁矾的XRD研究[J]. 岩石矿物学杂志,2013,32.0(006):995.
APA 许涛.,邹来昌.,阮仁满.,廖占丕.,苏秀珠.,...&黄丽娟.(2013).K-H3OFe3(SO4)2(OH)6铁矾的XRD研究.岩石矿物学杂志,32.0(006),995.
MLA 许涛,et al."K-H3OFe3(SO4)2(OH)6铁矾的XRD研究".岩石矿物学杂志 32.0.006(2013):995.
Files in This Item:
There are no files associated with this item.
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[许涛]'s Articles
[邹来昌]'s Articles
[阮仁满]'s Articles
Baidu academic
Similar articles in Baidu academic
[许涛]'s Articles
[邹来昌]'s Articles
[阮仁满]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[许涛]'s Articles
[邹来昌]'s Articles
[阮仁满]'s Articles
Terms of Use
No data!
Social Bookmark/Share
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.