Vereda Fernando, Rodríguez-González Benito, de Vicente Juan, Hidalgo-Alvarez Roque
Grupo de Física de Fluidos y Biocoloides, Departamento de Física Aplicada, Facultad de Ciencias, Universidad de Granada, Granada E-18071, Spain.
J Colloid Interface Sci. 2008 Feb 15;318(2):520-4. doi: 10.1016/j.jcis.2007.11.003. Epub 2007 Nov 13.
We provide new information relevant to the crystallinity and growth mechanism of magnetite particles that were fabricated following the method of Sugimoto and Matijević [J. Colloid Interface Sci. 74 (1980) 227]. These authors observed that in a small excess of Fe(2+), particles grew by aggregation and recrystallization of smaller units, so that until now the resulting particles were thought to be polycrystalline. With the help of transmission electron microscopy (TEM) and selected area electron diffraction (SAED), we also detected the presence of monocrystalline particles, which are strong evidence of the occurrence of direct crystal growth. This growth mechanism seems to coexist with that of the aggregation of primary units proposed by Sugimoto and Matijević. Careful examination of electron microscopy micrographs also revealed the presence of many hollow polycrystalline microspheres.
我们提供了与按照杉本和马蒂耶维奇的方法制备的磁铁矿颗粒的结晶度和生长机制相关的新信息[《胶体与界面科学杂志》74(1980)227]。这些作者观察到,在Fe(2+)略有过量的情况下,颗粒通过较小单元的聚集和重结晶而生长,因此直到现在,所得到的颗粒都被认为是多晶的。借助透射电子显微镜(TEM)和选区电子衍射(SAED),我们还检测到了单晶颗粒的存在,这是直接晶体生长发生的有力证据。这种生长机制似乎与杉本和马蒂耶维奇提出的初级单元聚集机制共存。对电子显微镜显微照片的仔细检查还揭示了许多中空多晶微球的存在。