Shen Xiong-Fei, Ding Yun-Shuang, Liu Jia, Han Zhao-Hui, Budnick Joseph I, Hines William A, Suib Steven L
Institute of Materials Science, and Departments of Physics and Chemistry, University of Connecticut, 55 North Eagleville Road, Storrs, Connecticut 06269, USA.
J Am Chem Soc. 2005 May 4;127(17):6166-7. doi: 10.1021/ja043406a.
A magnetic route has been applied for measurement of the average oxidation state (AOS) of mixed-valent manganese in manganese oxide octahedral molecular sieves (OMS). The method gives AOS measurement results in good agreement with titration methods. A maximum analysis deviation error of +/-7% is obtained from 10 sample measurements. The magnetic method is able to (1) confirm the presence of mixed-valent manganese and (2) evaluate AOS and the spin states of d electrons of both single oxidation state and mixed-valent state Mn in manganese oxides. In addition, the magnetic method may be extended to (1) determine AOS of Mn in manganese oxide OMS with dopant "diamagnetic" ions, such as reducible V5+ (3d0) ions, which is inappropriate for the titration method due to interference of redox reactions between these dopant ions and titration reagents, such as KMnO4, (2) evaluate the dopant "paramagnetic" ions that are present as clusters or in the OMS framework, and (3) determine AOS of other mixed-valent/single oxidation state ion systems, such as Mo3+(3d3)-Mo4+(3d2) systems and Fe3+ in FeCl3.
一种磁学方法已被应用于测定氧化锰八面体分子筛(OMS)中混合价态锰的平均氧化态(AOS)。该方法给出的AOS测量结果与滴定法高度吻合。对10个样品进行测量得到的最大分析偏差误差为±7%。该磁学方法能够(1)确认混合价态锰的存在,以及(2)评估氧化锰中单一氧化态和混合价态锰的AOS及d电子的自旋态。此外,该磁学方法可扩展用于(1)测定含有掺杂“抗磁性”离子(如可还原的V5+(3d0)离子)的氧化锰OMS中锰的AOS,由于这些掺杂离子与滴定试剂(如KMnO4)之间的氧化还原反应干扰,滴定法不适用于此;(2)评估以簇状形式存在或存在于OMS骨架中的掺杂“顺磁性”离子,以及(3)测定其他混合价态/单一氧化态离子体系,如Mo3+(3d3)-Mo4+(3d2)体系和FeCl3中的Fe3+。