GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室
氧化石墨烯共存条件下水铁矿转化机理探讨
闫丽霞; 朱润良; 刘晶; 陈情泽; 朱建喜; 何宏平
Source Publication中国矿物岩石地球化学学会第九次全国会员代表大会暨第16届学术年会文集
2017-04-18
Conference Date2017-04-18
Conference Place中国陕西西安
Country中国
Indexed By其他
Language中文
Keyword水铁矿 氧化石墨烯 共存条件
Abstract氧化石墨烯是一种新型的人造碳纳米材料,表面具有多种含氧官能团,性质活泼,在声、光、热、电等方面均具有优良性能,被广泛应用于各个行业。当其释放到水体、土壤及沉积物中,可与天然矿物相互作用而改变其物理化学性质。水铁矿是自然界中广泛存在的天然的纳米矿物,比表面积大,表面羟基丰富,结晶弱。前人研究普遍认为水铁矿易通过脱水聚集形成赤铁矿,或者通过溶解再结晶形成针铁
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35547
Collection中国科学院矿物学与成矿学重点实验室
Recommended Citation
GB/T 7714
闫丽霞,朱润良,刘晶,等. 氧化石墨烯共存条件下水铁矿转化机理探讨[C],2017.
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