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方解石晶體結構及表面活性位點第一性原理

The first principles of the crystal structure and active sites of calcite

  • 摘要: 基于密度泛函理論的第一性原理,采用Materials Studio 6.1軟件的CASTEP模塊對方解石的晶體結構及與水分子及水分子簇的吸附作用進行了研究.結果表明,方解石在參與化學反應時O的活性最強,C和Ca次之;其次確定了最穩定解離面為1014切面,其Ca和O位點與單個水分子形成吸附,且與O位點吸附作用較強,H (H2O)-O (CaCO3)鍵與H (H2O)-O (H2O)鍵間形成氫鍵;1014切面水分子簇相互作用,水分子間及水分子與方解石表面均存在氫鍵作用,吸附發生在O位點和Ca位點,且主要發生在O位點.

     

    Abstract: The calcite structure and the adsorption of water molecules as well as water molecule clusters on it were investigated using the CASTEP module, Materials Studio 6.1 based on the first principles of the density functional theory (DFT). Results indicate that the O site of calcite shows the highest activity in the reaction process, followed by the C and Ca sites; 1014 is the most stable cleavage plane, where the adsorption can occur between the water molecule and the Ca and O sites, and the O site shows a more stronger adsorption effect with the hydrogen bond formed through the H(H2O)-O(CaCO3) and H(H2O) -O(H2O) bonds. There are both hydrogen bonds between the water molecules, as well as the water molecules and calcite surface whose adsorption effects are mainly found to be the O site followed by the relative weaker Ca site.

     

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