Acid and thermal treatment of natural heulandite

V. Tsitsishvili, N. Dolaberidze, M. Nijaradze, N. Mirdzveli, Z. Amiridze, B. Khutsishvili
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Abstract

Acid treatment of natural zeolites is considered to be an effective method of “improving” their structure and properties, among which thermal stability occupies a special place, especially for catalytic applications of zeolites. The influence of hydrochloric acid solutions with concentrations up to 2 mol/L and calcination at temperatures up to 1100 °C on the structure and properties of heulandite-containing tuff from the Georgian Dzegvi-Tedzami deposit, selected for the creation of new bactericidal zeolite filter materials for purification and desinfection of water from various sources, was studied by the X-ray energy dispersion spectra, diffraction patterns and thermal analysis, as well as by adsorption of water, benzene and nitrogen methods. It has been found that an acidic environment leads to significant dealumination (Si/Al molar ratio increases from 3.6 to 9.5) and decationization (total charge of metal ions per Al atom decreases from 1 to 0.68) of the sample; solutions of hydrochloric acid do not lead to amorphization of the zeolite microporous crystal structure, but gradually dissolve it. As a result of acid treatment, there is also a sharp increase in the volume of micropores available for large molecules (from ≈ 7 to 80–90 mm3/g) and surface area (from ≈ 13 to 120–175 m2/g), as well as changes in the mesoporous system, leading to the prevalence of pores with a diameter of up to 4 nm. Heulandite heating leads to stepwise dehydration proceeding up to ≈ 800 °C, amorphization starting at ≈ 250 °C, and structural changes: the transition to methastable heulandite B phase at ≈ 340 °C is not fixed, but at ≈ 500 °C wairakite (Ca(Al2Si4O12)·2H2O) is formed, at temperatures above ≈ 1000 °C, amorphous aluminosilicate contains crystalline inclusions of cristobalite (polymorph of SiO2), α-quartz, albite (Na(AlSi3O8), hematite (Fe2O3) and magnetite (FeO·Fe2O3); heating-induced changes in micro- and mesopore systems are insignificant. It is also shown that heat treatment increases the acid resistance of heulandite, which is expressed in a decrease in the degree of dealumination after acid treatment of calcined samples. Thus, acid and heat treatment of heulandite make it possible to obtain materials with different sorption and ion-exchange properties.
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天然乌云石的酸处理和热处理
对天然沸石进行酸处理被认为是 "改善 "其结构和性能的有效方法,其中热稳定性占有特殊地位,尤其是在沸石的催化应用方面。我们通过 X 射线能量色散光谱、衍射图样、热分析以及水、苯和氮的吸附方法,研究了浓度高达 2 mol/L 的盐酸溶液和温度高达 1100 °C 的煅烧对格鲁吉亚 Dzegvi-Tedzami 矿床含海泡石凝灰岩的结构和特性的影响。研究发现,酸性环境会导致样品显著脱铝(硅/铝摩尔比从 3.6 升至 9.5)和脱钙(每个铝原子的金属离子总电荷从 1 降至 0.68);盐酸溶液不会导致沸石微孔晶体结构的非晶化,而是逐渐溶解。酸处理的结果是,大分子可利用的微孔体积(从≈ 7 增加到 80-90 mm3/g)和表面积(从≈ 13 增加到 120-175 m2/g)也急剧增加,介孔系统也发生了变化,导致直径达 4 nm 的孔洞普遍存在。Heulandite 加热会导致逐步脱水,最高温度可达 ≈ 800 °C,从 ≈ 250 °C开始发生非晶化,并导致结构变化:在温度≈ 340 °C时,向可甲烷化的海泡石B相的转变并不固定,但在≈ 500 °C时,会形成怀来石(Ca(Al2Si4O12)-2H2O),温度高于≈ 1000 °C、无定形铝硅酸盐中含有霞石(SiO2 的多晶体)、α-石英、白云石(Na(AlSi3O8))、赤铁矿(Fe2O3)和磁铁矿(FeO-Fe2O3)等结晶包裹体;加热引起的微孔和中孔系统变化不大。研究还表明,热处理可提高海泡石的耐酸性,这表现在煅烧样品经酸处理后的脱矾程度降低。因此,对绿泥石进行酸处理和热处理可以获得具有不同吸附和离子交换特性的材料。
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