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鹽酸改性對天然斜發沸石孔道特征、成分、表面電位及陽離子交換性能的影響

Effects of hydrochloric acid modification on the channel characteristics,composition,surface potential and cation exchange behavior of natural clinoptilolite

  • 摘要: 采用不同濃度鹽酸對天然斜發沸石進行改性,并系統地研究了改性沸石的孔道特征、化學成分、表面電位及陽離子交換性能的變化.鹽酸改性后,沸石晶體結構破壞較小,表面變得疏松粗糙,K+、Na+、Ca2+和Mg2+元素含量均小幅下降;表面負電荷增加,陽離子交換容量減小;比表面積和總孔體積均有所提高,最高分別從原沸石的35.97 m2·g-1和0.0761 m3·g-1提高至64.46 m2·g-1和0.1156 m3·g-1.鹽酸改性對沸石微孔、介孔和大孔的分布影響明顯.從遲滯回線形狀判斷沸石孔道類型均為不均勻狹縫型孔道,鹽酸改性不會改變沸石孔道類型.

     

    Abstract: Natural clinoptilolite was modified by different concentrations of hydrochloric acid. Systemic investigations were performed on the channel characteristics, chemical composition, surface potential, and cation exchange behavior of the modified clinoptilolite. It is found that the surface of the modified clinoptilolite becomes loose and rough, the contents of K+, Na+, Ca2+, and Mg2+ slightly decrease, the surface negative charges increases, and the cation exchange capacity decreases to some extent. The specif-ic surfaee area and total pore volume are improved and the maximum values of them increase from 35.97 m2·g-1 and 0.0761 m3·g-1 to 64.46 m2·g-1 and 0.1156 m3·g-1, respectively. The distribution of micropores, mesopores, and macropores is obviously impacted, and the type of zeolite cavities is determined to be uneven slits by the hysteresis loop shape, indicating that this aeid modification cannot change zeolite cavities.

     

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