论文标题
三角结构中的一阶过渡$ {\ textbf {ca}}} {\ textbf {mn}} _ {2} {\ textbf {p}} _ {2} _ {2} $
First order transition in trigonal structure ${\textbf{Ca}}{\textbf{Mn}}_{2}{\textbf{P}}_{2}$
论文作者
论文摘要
我们报告了单晶$ {\ mathrm {ca}} {\ Mathrm {Mn}} _ {2} {\ Mathrm {p}} _ {2} $的结构和物理属性。 X射线衍射(XRD)结果表明$ {\ Mathrm {ca}} {\ Mathrm {Mn}} _ {2} {2} {\ Mathrm {p}} _ {2} _ {2} $采用Trigonal $ {\ mathrm {ca}}} {\ mathrm {al}} _ {2} {\ mathrm {si}} _ {2} $ - 类型结构。与温度相关的电阻率$ρ(t)$测量表明,$ {\ Mathrm {Ca}}} {\ MathRM {Mn}} _ {2} {\ Mathrm {p}} _ {2} _ {2} $具有40 mev和0.64 mev的启动能量的绝缘基态。磁化测量值在400 K下没有明显的磁相过渡。与其他$ {\ Mathrm {a}} {\ Mathrm {Mn}} _ {2} {\ Mathrm {pn}} $C_{\mathrm{p}}(T)$ and $ρ(T)$ reveal that ${\mathrm{Ca}}{\mathrm{Mn}}_{2}{\mathrm{P}}_{2}$ has a first-order transition at $T$ = 69.5 K and the transition temperature shifts to high temperature upon压力增加。在过渡下方的许多新拉曼模式的出现清楚地表明,伴随过渡的对称性发生了变化。结构,传输,热和磁性测量的组合表明了过渡的异常起源。
We report structural and physical properties of the single crystalline ${\mathrm{Ca}}{\mathrm{Mn}}_{2}{\mathrm{P}}_{2}$. The X-ray diffraction(XRD) results show that ${\mathrm{Ca}}{\mathrm{Mn}}_{2}{\mathrm{P}}_{2}$ adopts the trigonal ${\mathrm{Ca}}{\mathrm{Al}}_{2}{\mathrm{Si}}_{2}$-type structure. Temperature dependent electrical resistivity $ρ(T)$ measurements indicate an insulating ground state for ${\mathrm{Ca}}{\mathrm{Mn}}_{2}{\mathrm{P}}_{2}$ with activation energies of 40 meV and 0.64 meV for two distinct regions, respectively. Magnetization measurements show no apparent magnetic phase transition under 400 K. Different from other ${\mathrm{A}}{\mathrm{Mn}}_{2}{\mathrm{Pn}}_{2}$ (A = Ca, Sr, and Ba, and Pn = P, As, and Sb) compounds with the same structure, heat capacity $C_{\mathrm{p}}(T)$ and $ρ(T)$ reveal that ${\mathrm{Ca}}{\mathrm{Mn}}_{2}{\mathrm{P}}_{2}$ has a first-order transition at $T$ = 69.5 K and the transition temperature shifts to high temperature upon increasing pressure. The emergence of plenty of new Raman modes below the transition, clearly suggests a change in symmetry accompanying the transition. The combination of the structural, transport, thermal and magnetic measurements, points to an unusual origin of the transition.