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高压下岩盐矿和单斜结构AgCl的电子行为

DOI: 10.11858/gywlxb.2007.03.001, PP. 225-230

Keywords: 密度泛函理论,能带结构,金属化

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Abstract:

利用基于密度泛函理论的赝势平面波方法,计算了AgCl在高压下的结构行为和电子性质,交换关联函数采用广义梯度近似(GGA)。通过比较焓随压力的变化关系,从理论上确定了AgCl从岩盐矿结构相变到单斜结构的转变压强。预测了这两种结构在布里渊区中的价带顶和导带底的位置,结果表明:盐岩矿和单斜结构的AgCl都是具有间接带隙的半导体。还计算了这两种结构的带隙和电子态密度随压强的变化情况,发现在这两种结构相变之前都不会发生金属化转变。电荷转移研究发现,随着压强的增加,Ag原子和Cl原子之间成键的共价性增强,离子性减弱。

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