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Comparison of calcined illitic clays (brick clays) and low- grade kaolinitic clays as supplementary cementitious materials

机译:煅烧的硅质粘土(砖状粘土)与低品位高岭土作为辅助胶凝材料的比较

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摘要

The use of calcined clays as supplementary cementitious materials (SCMs) has been identified as a viable option to decrease the CO2 emissions related to cement production. However, while extensive data is available about kaolinitic clays in this context, other clays such as illitic clays appear to be under-studied. Therefore, in the present study, two illitic clays were compared to two low-grade kaolinitic clays in terms of transformations in the calcination temperature range 650-900 degrees C, and performance of the calcined clays in blended cement pastes as measured by strength evolution, heat release, hydrated phase formation and portlandite consumption. The illitic clays required a higher calcination temperature for complete dehydroxylation of their illite than what is necessary for dehydroxylation of kaolinite. These higher calcination temperatures also led to particle sintering, significantly decreasing the specific surface area of the illitic clays, particularly for the clay with the higher Fe2O3 content. Nevertheless, while the kaolinitic clays generally exhibited the best performance as SCM, the illitic clay with lower Fe2O3 content performed similar to the kaolinitic clays when calcined at optimum temperature and applied at a moderate substitution rate. These findings demonstrate that several different clays have the potential to be used as SCM and indicate possible routes to identify suitable deposits for this purpose.
机译:使用煅烧粘土作为补充胶结材料(SCM)已被确定为减少与水泥生产相关的CO2排放的可行选择。但是,尽管在这种情况下可以获得有关高岭土的大量数据,但其他粘土(例如硅质粘土)的研究似乎仍未得到充分研究。因此,在本研究中,就煅烧温度范围650-900℃的转化率以及通过强度演变测量的混合水泥浆中煅烧粘土的性能,将两种硅藻土与两种低品位高岭土进行了比较,放热,水合相形成和硅酸盐消耗。硬质粘土要求其伊利石完全脱羟基的煅烧温度高于高岭石脱羟基所需的煅烧温度。这些较高的煅烧温度也导致了颗粒烧结,显着降低了硬质粘土的比表面积,特别是对于具有较高Fe 2 O 3含量的粘土而言。尽管如此,尽管高岭土通常表现出最好的SCM性能,但在最佳温度下煅烧并以中等取代率施用时,Fe2O3含量较低的高岭土的性能与高岭土相似。这些发现表明,几种不同的粘土有可能被用作SCM,并指出了为此目的确定合适矿床的可能途径。

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