Sgarlata Caterina, Formia Alessandra, Siligardi Cristina, Ferrari Francesco, Leonelli Cristina
Department of Engineering "Enzo Ferrari", University of Modena and Reggio Emilia, 41125 Modena, Italy.
Sibelco Ankerpoort NV, 6223 EP Maastricht, The Netherlands.
Materials (Basel). 2021 Dec 23;15(1):83. doi: 10.3390/ma15010083.
The aim of this paper is to promote the use of mine clay washing residues for the preparation of alkali activated materials (AAMs). In particular, the influence of the calcination temperature of the clayey by-product on the geopolymerization process was investigated in terms of chemical stability and durability in water. The halloysitic clay, a mining by-product, has been used after calcination and mixed with an alkaline solution to form alkali activated binders. Attention was focused on the influence of the clay's calcination treatment (450-500-600 °C) on the geopolymers' microstructure of samples, remaining in the lower limit indicated by the literature for kaolinite or illite calcination. The mixtures of clay and alkali activators (NaOH 8M and Na-silicate) were cured at room temperature for 28 days. The influence of solid to liquid ratio in the mix formulation was also tested in terms of chemical stability measuring the pH and the ionic conductivity of the eluate after 24-h immersion time in water. The results reported values of ionic conductivity higher for samples made with untreated clay or with low temperature of calcination (≥756 mS/m) compared with values of samples made with calcined clay (292 mS/m). This result suggests that without a proper calcination of the as-received clay it was not possible to obtain 25 °C-consolidated AAMs with good chemical stability and dense microstructure. The measures of integrity test, pH, and ionic conductivity in water confirmed that the best sample is made with calcined clay at 600 °C, being similar (53% higher ionic conductivity of the eluate) or equal (integrity test and pH) to values recorded for the metakaolin-based geopolymer considered the reference material. These results were reflected in term of reticulation and morphology of samples through the analysis with scanning electron microscope (SEM) and X-ray diffraction (XRD), which show a dense and homogeneous microstructure predominantly amorphous with minor amounts of quartz, halloysite, and illite crystalline phases. Special attention was dedicated to this by-product to promote its use, given that kaolinite (and metakaolin), as primary mineral product, has a strong impact on the environment. The results obtained led us to consider this halloysite clay very interesting as an aluminosilicate precursor, and extensively deepening its properties and reactivity for the alkaline activation. In fact, the heart of this work is to study the possibility of reusing this by-product of an industrial process to obtain more sustainable high-performance binders.
本文旨在推广利用矿山粘土洗涤残渣制备碱激发材料(AAMs)。具体而言,从化学稳定性和在水中的耐久性方面,研究了粘土副产品的煅烧温度对地质聚合过程的影响。埃洛石粘土这种采矿副产品在煅烧后与碱性溶液混合,形成碱激发粘结剂。重点关注粘土煅烧处理(450 - 500 - 600℃)对样品地质聚合物微观结构的影响,该温度保持在文献中高岭土或伊利石煅烧下限范围内。粘土与碱激发剂(8M NaOH和硅酸钠)的混合物在室温下养护28天。通过测量在水中浸泡24小时后洗脱液的pH值和离子电导率来评估化学稳定性,进而测试混合配方中固液比对其的影响。结果表明,与煅烧粘土制成的样品(292 mS/m)相比,未处理粘土或低温煅烧(≥756 mS/m)制成的样品离子电导率更高。这一结果表明,如果不对原样粘土进行适当煅烧,就无法获得具有良好化学稳定性和致密微观结构的25℃固化AAMs。完整性测试、pH值和水中离子电导率的测量结果证实,最佳样品是由600℃煅烧的粘土制成,与以偏高岭土为基的地质聚合物(作为参考材料)记录的值相比,洗脱液的离子电导率高出53%,完整性测试和pH值与之相当。通过扫描电子显微镜(SEM)和X射线衍射(XRD)分析,这些结果在样品的网状结构和形态方面得到体现,显示出致密且均匀的微观结构,主要为非晶态,含有少量石英、埃洛石和伊利石晶相。鉴于高岭土(和偏高岭土)作为主要矿产对环境有重大影响,因此对这种副产品给予了特别关注以促进其利用。所得结果使我们认为这种埃洛石粘土作为硅铝酸盐前驱体非常有趣,并广泛深入研究其性质和碱性活化反应性。事实上,这项工作的核心是研究重新利用这种工业过程副产品以获得更具可持续性的高性能粘结剂的可能性。