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通过对产自海南岛石碌铁矿的红帘石进行偏振吸收光谱测量和晶体场理论计算,说明了红帘石具有多色性的本质和 Mn~(-)在红帘石结构M(3)中 d 轨道能级分裂的特征以及稳定的原因.
By means of polarization absorption spectroscopy and crystal field theory calculation of the red cordite from Shilu iron ore from Hainan Island, it is demonstrated that the Cu (Ⅱ) ), The characteristics of d-orbital level splitting and the reasons for its stability.