Department of Chemistry and Biochemistry, Florida State University, Tallahassee, Florida 32306, United States.
J Am Chem Soc. 2012 Mar 28;134(12):5577-85. doi: 10.1021/ja210285p. Epub 2012 Mar 14.
Herein we report doping of ZnSe by Cr ions leads to formation of small ZnCr(2)Se(4) spinel inclusions within the cubic sphalerite lattice of a 2.8 nm CrZnSe quantum dot (QD). The Cr ion incorporates as a pair of Cr(III) ions occupying edge-sharing tetragonal distorted octahedral sites generated by formation of three Zn ion vacancies in the sphalerite lattice in order to charge compensate the QD. The site is analogous to the formation of a subunit of the ZnCr(2)Se(4) spinel phase known to form as inclusions during peritectoid crystal growth in the ternary CrZnSe solid-state compound. The oxidation state and site symmetry of the Cr ion is confirmed by X-ray absorption near edge spectroscopy (XANES), crystal field absorption spectroscopy, and electron paramagnetic resonance (EPR). Incorporation as the Cr(III) oxidation state is consistent with the thermodynamic preference for Cr to occupy an octahedral site within a II-VI semiconductor lattice with a half-filled t(2g) d-level. The measured crystal field splitting energy for the CrZnSe QD is 2.08 eV (2.07 eV form XANES), consistent with a spinel inclusion. Further evidence of a spinel inclusion is provided by analysis of the magnetic data, where antiferromagnetic (AFM) exchange, a Curie-Weiss (C-W) temperature of θ = -125 K, and a nearest-neighbor exchange coupling constant of J(NN) = -12.5 K are observed. The formation of stable spinel inclusions in a QD has not been previously reported.
在此,我们报告了通过 Cr 离子掺杂 ZnSe,导致在 2.8nm CrZnSe 量子点(QD)的立方闪锌矿晶格内形成小的 ZnCr(2)Se(4)尖晶石包裹体。Cr 离子以一对 Cr(III)离子的形式掺入,占据由闪锌矿晶格中形成的三个 Zn 离子空位产生的共边四面体扭曲八面体位置,以补偿 QD 的电荷。该位置类似于 ZnCr(2)Se(4)尖晶石相的亚单位的形成,众所周知,在三元 CrZnSe 固态化合物的包晶晶体生长过程中,该尖晶石相作为包裹体形成。Cr 离子的氧化态和点群对称性通过 X 射线吸收近边光谱(XANES)、晶体场吸收光谱和电子顺磁共振(EPR)得到证实。以 Cr(III)氧化态掺入是与 Cr 占据 II-VI 半导体晶格中填满一半的 t(2g)d 能级的八面体位置的热力学偏好一致的。测量的 CrZnSe QD 的晶体场分裂能为 2.08eV(XANES 形式为 2.07eV),与尖晶石包裹体一致。通过对磁性数据的分析进一步提供了尖晶石包裹体的证据,其中观察到反铁磁(AFM)交换、居里-魏斯(C-W)温度θ=-125K 和最近邻交换耦合常数 J(NN)=-12.5K。在 QD 中形成稳定的尖晶石包裹体以前尚未报道过。