摘要
将磁性粒子体积分数为15%和10%的两种Cofe3O4离子型磁性液体静置半年后,为15%的磁性液体中有沉淀产生.TEM分析表明:静置后的两种磁性液体的磁性微粒在物相成分、粒度分布上基本相同,差别表现在团聚程度上——为15%的磁性微粒大量团聚,而为10%的磁性微粒则只有少数团聚.可见,团聚是造成为15%的磁性液体出现沉淀的主要原因.
Two kinds of CoFe2O4 ionic magnetic fluids, with different magnetic Particles volume fraction ψi 15 % and 10%, are discussed. Both of them have self-evolved for half a year in room temperature.As a result of self-evolution, one of them whose is 15 % has many precipitations appearing but the other whose is 10% is still a suspension. The component size distribution and aggregate situation of the magnetie parhcles in these two ionic magnetic fluids are discussed through TEM. As a result, the serious aggregation of the magnetic particles in the ionic magnetic fluids whose is 15 % is the major reason that leads to the precipitations appearance.
出处
《西南师范大学学报(自然科学版)》
CAS
CSCD
1996年第4期344-348,共5页
Journal of Southwest China Normal University(Natural Science Edition)
关键词
磁性液体微粒
沉淀
团聚
透射电子显微镜
离子型
magnetic fluids portides
Precipitation
aggregation
Trans mission electron microscopes(TEM)