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Reactivity of dealuminated kaolin and burnt kaolin using cement kiln dust or hydrated lime as activators

机译:以水泥窑粉尘或熟石灰为活化剂的脱铝高岭土和烧高岭土的反应性

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Pozzolanic activity of dealuminated kaolin (DK) and burnt kaolinite clay (BK) was studied using cement kiln dust (CKD) or hydrated lime (CH) as activators. The different solid dry mixtures made of DK-CKD, BK-CKD, DK-CH, BK-CH, SF-CKD and SF-CH were hydrated in the suspension form, while paste hydra-tion was done using DK-BK-CKD mix. Chemically combined water and free lime contents were determined at various ages of hydration and the hydrated samples were characterized using DSC, XRD and FTIR techniques. Combined water contents of the blends containing DK activated with CKD or CH are higher than those of mixes containing BK and SF activated with CKD or CH. Evidently, the suspensions containing DK possess relatively lower values of free lime contents than those of mixes containing BK and SF; this is due to the higher pozzolanic activity of DK as compared to BK and SF. The results of DSC and XRD analysis of suspension hydrated samples indicated the formation and later stabilization of calcium silicates hydrates (CSH) and calcium aluminosilicate hydrates (C_3ASH4 and C_2ASH_8) as the main hydration products in addition to free calcium hydroxide (CH), which is completely consumed at 12 h for mixes containing DK. Compressive strength and SEM examination were done for paste hydrated specimens made of mix IV (35% DK, 35% BK and 30% CKD) as an application. The microstructure of the hardened paste after 7 days of hydration displayed the formation of nearly amorphous and microcrystal-line CSH products as well as rod-like crystals of ettringite with a partial filling of the available pore spaces of the hardened paste. On prolonged hydration the microstructure displayed crumpled foils and dense structure of tobermorite-like CSH as the main hydration product which deposited in the originally water-filled space; this kind of CSH product is mainly formed as a result of interaction of active DK and BK with CH of CKD.
机译:用水泥窑粉尘(CKD)或熟石灰(CH)作为活化剂研究了脱铝高岭土(DK)和烧成高岭石粘土(BK)的火山灰活性。将由DK-CKD,BK-CKD,DK-CH,BK-CH,SF-CKD和SF-CH制成的不同固体干燥混合物以悬浮液形式水合,而使用DK-BK-CKD进行糊状水合混合。在不同的水合年龄测定化学结合的水和游离石灰的含量,并使用DSC,XRD和FTIR技术对水合样品进行表征。含有由CKD或CH活化的DK的掺合物的混合水含量高于含有由CKD或CH活化的BK和SF的掺合物的含水量。显然,与含有BK和SF的混合物相比,含有DK的悬浮液具有较低的游离石灰含量。这是由于DK的火山灰活性高于BK和SF。悬浮水合样品的DSC和XRD分析结果表明,除游离氢氧化钙(CH)外,作为主要水合产物的硅酸钙水合物(CSH)和铝硅酸钙水合物(C_3ASH4和C_2ASH_8)的形成和后期稳定化。含有DK的混合物在12小时内被完全消耗。对混合物IV(35%DK,35%BK和30%CKD)制成的糊状水合样品进行了抗压强度和SEM检查。水合7天后,硬化糊的微观结构显示出几乎无定形和微晶线的CSH产物以及钙矾石的棒状晶体的形成,部分填充了硬化糊的可用孔隙空间。在长时间的水合作用中,微观结构显示出皱巴巴的箔片和作为主要水合作用的水辉石状CSH的致密结构,它们沉积在最初充满水的空间中。这种CSH产物主要是由于活性DK和BK与CKD的CH相互作用而形成的。

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