Polanams Jup, Ray Alisha D, Watt Richard K
Department of Chemistry, University of New Mexico, Albuquerque, New Mexico 87131-0001, USA.
Inorg Chem. 2005 May 2;44(9):3203-9. doi: 10.1021/ic048819r.
Nanoparticles of iron phosphate, iron arsenate, iron molybdate, and iron vanadate were synthesized within the 8 nm interior of ferritin. The synthesis involved reacting Fe(II) with ferritin in a buffered solution at pH 7.4 in the presence of phosphate, arsenate, vanadate, or molybdate. O2 was used as the oxidant to deposit the Fe(III) mineral inside ferritin. The rate of iron incorporation into ferritin was stimulated when oxo-anions were present. The simultaneous deposition of both iron and the oxo-anion was confirmed by elemental analysis and energy-dispersive X-ray analysis. The ferritin samples containing iron and one of the oxo-anions possessed different UV/vis spectra depending on the anion used during mineral formation. TEM analysis showed mineral cores with approximately 8 nm mineral particles consistent with the formation of mineral phases inside ferritin.
磷酸铁、砷酸铁、钼酸铁和钒酸铁纳米颗粒在铁蛋白8纳米的内部合成。合成过程包括在pH值为7.4的缓冲溶液中,在磷酸盐、砷酸盐、钒酸盐或钼酸盐存在的情况下,使Fe(II)与铁蛋白反应。使用O2作为氧化剂将Fe(III)矿物沉积在铁蛋白内部。当存在含氧阴离子时,铁掺入铁蛋白的速率会加快。通过元素分析和能量色散X射线分析证实了铁和含氧阴离子的同时沉积。含有铁和一种含氧阴离子的铁蛋白样品根据矿物形成过程中使用的阴离子不同而具有不同的紫外/可见光谱。透射电子显微镜分析显示矿物核心具有约8纳米的矿物颗粒,这与铁蛋白内部矿物相的形成一致。