铜型蛭石抗菌剂中Cu^2+的赋存状态
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P578.963;TB33

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Modes of Occurrence of Cu~(2 ) in the Cu-vermiculite Antimicrobial Agent
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    摘要:

    利用天然矿物蛭石的阳离子交换特点,通过离子交换法将Cu^2 植入到蛭石中,制得铜含量高达5.5%(相当于蛭石阳离子交换容量的80%)、具良好抗菌性能的铜型蛭石。经XRD、TEM、AAS分析,结合晶胞参数及晶体化学式的计算,铜型蛭石的XRD特征值更接近于标准的Mg^-蛭石,这与Cu^2 与Mg^2 半径相近,电价相等的特点相符合,Cu^2 部分以水合物的形式存在于蛭石层间,部分进入八面体中以六次配位的形式存在。铜型蛭石的a0和b0值无明显变化而c0值略有减小,这对于Cu^2 的稳定是有利的,上述各特点有利于铜型蛭石抗菌剂的稳定性和持久性。

    Abstract:

    The Cu-vermiculite, with 5.5% copper (equal to 80% CEC of vermiculite) and excellent antibacterial performance, was obtained by ion exchange method based on its specialty in cation exchange. On the basis of XRD, TEM and EDS analyses combined with calculation of crystalline parameters and crystal formula, the structure character of Cu-vermiculite was investigated. The similar atom radii and electrovalences of Cu2 and Mg2 suggest that the XRD character of Cu-vermiculite are close to that of standard Mg-vermiculite. A part of Cu2 occupied the interlayer cation sites in the form of hydrate in vermiculite, whereas others turned into octahedral coordinate positions to replace Mg2 . The values of a0 and b0 of the Cu-vermiculite crystal cell had no obvious change compared with that of vermiculite micropowder, but the c0 value slightly decreased, which is desirable for the stabilization of the Cu2 in Cu-vermiculite.

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李博文,于淑会,鲁安怀,等, 2001. 铜型蛭石抗菌剂中Cu^2+的赋存状态[J]. 岩石矿物学杂志, 20(4):495~499.
LI Bo-wen, YU Shu-hui, et al, 2001. Modes of Occurrence of Cu~(2 ) in the Cu-vermiculite Antimicrobial Agent[J]. Acta Petrologica et Mineralogica, 20(4): 495~499.

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