钙芒硝水溶过程结构变化的细观研究
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TD871

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Research on the Microstructural Change of Glauberite in Solution
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    摘要:

    通过实验,研究了钙芒硝在水溶过程中结构上的细观变化。实验结果分析,得出了以下结论:钙芒硝的水溶过程既包含晶体的溶解过程也包含晶体的析出过程;溶液是顺着裂隙进行渗流的,并首先溶解裂隙处的钙芒硝,钙芒硝溶解后空出一定的空间,然后溶液再顺着所产生的空间向裂隙周围流动;水溶后的固体残留物可以认为是多孔介质,其渗透性和力学特性在不断的变化;水溶过程中,溶液在钙芒硝矿石中的流动可以认为是溶液在多孔介质中的渗流;溶质在溶液中的运输过程可以看成是溶质在溶液中的扩散过程。

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    By experiment the micromechanical change of glauberite during its solving was investigated.After analyzing the results of experiment some conclusions were drawn out.In the dissolution process of glauberite both dissolution and crystallization take place at the same time.Solution seeps in along fissures,the dissolution of glauberite happens in cracks at first and some open space forms,then solution expands around the formed space.The remains of glauberite body after dissolution can be looked as pore-medium,and its seepage and mechanical characteristics are variety during solution.The flow of solution in glauberite can be looked as a seepage in pore-medium in the solving process.The process of solute’s convection can be looked as solute’s diffusion in water.

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邓庆阳,刘中华.钙芒硝水溶过程结构变化的细观研究[J].矿业研究与开发,2009,(2):10-12

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  • 在线发布日期: 2012-06-18
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