Electron Microscopy for Materials Research (EMAT), University of Antwerp, Groenenborgerlaan 171, B-2020, Antwerp, Belgium.
Inorg Chem. 2010 Oct 18;49(20):9508-16. doi: 10.1021/ic101233s.
A new A(n)B(n)O(3n-2) homologous series of anion-deficient perovskites has been evidenced by preparation of the members with n = 5 (Pb(2.9)Ba(2.1)Fe(4)TiO(13)) and n = 6 (Pb(3.8)Bi(0.2)Ba(2)Fe(4.2)Ti(1.8)O(16)) in a single phase form. The crystal structures of these compounds were determined using a combination of transmission electron microscopy and X-ray and neutron powder diffraction (S.G. Ammm, a = 5.74313(7), b = 3.98402(4), c = 26.8378(4) Å, R(I) = 0.035, R(P) = 0.042 for Pb(2.9)Ba(2.1)Fe(4)TiO(13) and S.G. Imma, a = 5.7199(1), b = 3.97066(7), c = 32.5245(8) Å, R(I) = 0.032, R(P) = 0.037 for Pb(3.8)Bi(0.2)Ba(2)Fe(4.2)Ti(1.8)O(16)). The crystal structures of the A(n)B(n)O(3n-2) homologues are formed by slicing the perovskite structure with (101)(p) crystallographic shear (CS) planes. The shear planes remove a layer of oxygen atoms and displace the perovskite blocks with respect to each other by the 1/2110 vector. The CS planes introduce edge-sharing connections of the transition metal-oxygen polyhedra at the interface between the perovskite blocks. This results in intrinsically frustrated magnetic couplings between the perovskite blocks due to a competition of the exchange interactions between the edge- and the corner-sharing metal-oxygen polyhedra. Despite the magnetic frustration, neutron powder diffraction and Mössbauer spectroscopy reveal that Pb(2.9)Ba(2.1)Fe(4)TiO(13) and Pb(3.8)Bi(0.2)Ba(2)Fe(4.2)Ti(1.8)O(16) are antiferromagnetically ordered below T(N) = 407 and 343 K, respectively. The Pb(2.9)Ba(2.1)Fe(4)TiO(13) and Pb(3.8)Bi(0.2)Ba(2)Fe(4.2)Ti(1.8)O(16) compounds are in a paraelectric state in the 5-300 K temperature range.
一种新的 A(n)B(n)O(3n-2) 同系物阴离子缺陷钙钛矿已经通过制备成员 n = 5(Pb(2.9)Ba(2.1)Fe(4)TiO(13)) 和 n = 6(Pb(3.8)Bi(0.2)Ba(2)Fe(4.2)Ti(1.8)O(16))在单相形式中得到证明。这些化合物的晶体结构通过透射电子显微镜和 X 射线和中子粉末衍射(S.G. Ammm,a = 5.74313(7),b = 3.98402(4),c = 26.8378(4)Å,R(I) = 0.035,R(P) = 0.042 对于 Pb(2.9)Ba(2.1)Fe(4)TiO(13) 和 S.G.Imma,a = 5.7199(1),b = 3.97066(7),c = 32.5245(8)Å,R(I) = 0.032,R(P) = 0.037 对于 Pb(3.8)Bi(0.2)Ba(2)Fe(4.2)Ti(1.8)O(16))来确定。A(n)B(n)O(3n-2) 同系物的晶体结构是通过用(101)(p)晶体剪切(CS)平面切割钙钛矿结构形成的。剪切平面去除了一层氧原子,并通过 1/2110 矢量相对于彼此位移钙钛矿块。CS 平面在钙钛矿块之间的界面处引入了过渡金属-氧多面体的边缘共享连接。由于边缘和角共享金属-氧多面体之间的交换相互作用的竞争,这导致了钙钛矿块之间固有的磁受挫耦合。尽管存在磁受挫,但中子粉末衍射和穆斯堡尔光谱表明,Pb(2.9)Ba(2.1)Fe(4)TiO(13) 和 Pb(3.8)Bi(0.2)Ba(2)Fe(4.2)Ti(1.8)O(16) 在分别为 T(N) = 407 和 343 K 以下呈反铁磁有序。Pb(2.9)Ba(2.1)Fe(4)TiO(13) 和 Pb(3.8)Bi(0.2)Ba(2)Fe(4.2)Ti(1.8)O(16) 化合物在 5-300 K 温度范围内处于顺电状态。