海泡石坡缕石的有机吸附研究
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国家自然科学基金项目!(编号 :4 950 2 0 2 5)的资助


Study on Adsorption of Organic Vapors by Palygorskite and Sepiolite
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    摘要:

    本研究采用红外光谱分析、X射线衍射分析和电泳等方法对坡缕石和海泡石吸附有机气体进行了研究。实验表明,这种吸附是因静电力的作用而产生的。矿物表面的吸附水可减弱静电力的作用。坡缕石、海泡石对有机气体的吸附量与气体温度、蒸气压、气体分子偶极矩,样品纯度、矿物结晶度有关。温度升高,气体分子热运动将加剧,吸附数量随之减少;若气体分子偶极矩加大,则吸附量增加;增大蒸气压能提高气体分子与矿物微粒间的接触频率,从而增强吸附;其他离子对Si4+的置换率增大,则静电力增强,对有机气体的吸附亦增强;样品愈纯吸附量愈大。坡缕石、海泡石对有机气体的吸附为物理吸咐。

    Abstract:

    Adsorption of organic vapors by palygorskite and sepiolite was studied with IR spectrometry, XRD analysis and electrophoresis in this article. It was proved that the adsorption is produced by the static electric force .The adsorbed water on the surface of the minerals which can weaken the static electric force will hinder palygorskite and sepiolite from adsorbing organic vapors, and after drying at 110℃, the absorbed vapors increase obviously.The absorptive capacity is related to the temperature and pressure of vapors, dipole moments of vapor molecules, purity of the samples and crystallinily of the minerals. The adsorbed vapors will be reduced if the temperature rises because the strengthened molecular movement of vapors makes it more difficult for palygorskite and sepiolite to adsorb vapor molecules. If the dipole moment of vapors is enhanced the amount of adsorbed vapors will increase accordingly.Increasing vapor pressure can increase the frequency of collision between vapor molecules and minerals and then increase the adsorptive capacity. The increase of the rate of substitution of the ion Si4+by other ions will intensify the static force and will also increase the adsorptive ca- pacity of organic vapors. The purity of samples can affect the adsorbed amount too, i.e. the purer the samples, the larger the adsorbed amount. The organic molecules were proved to be physically absorbed on the surface of palygorskite and sepiolite through experiments. It is very easy to desorb.

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万 朴,李 平,董发勤,等, 2000. 海泡石坡缕石的有机吸附研究[J]. 岩石矿物学杂志, 19(3):258~263.
Wan Pu, Li Ping, Dong Faqin, et al, 2000. Study on Adsorption of Organic Vapors by Palygorskite and Sepiolite[J]. Acta Petrologica et Mineralogica, 19(3): 258~263.

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  • 最后修改日期:1999-12-21
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