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Physico-chemical characterization of thermally treated bentonite

机译:热处理膨润土的理化特性

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Samples of original and thermally treated bentonite at 650 ℃ 4 h were characterized with chemical analysis, X-ray diffraction, thermal analysis, mercury porosimetry, differential scanning calorimetry, physisorption measurement and scanning electron microscopy. These consequence of the heating have been found. The chemical analysis shows high silica and alumina contents and small quantities of Fe~(+3), Ca~(+2) and Mg~(+2). XRD analysis shown the presence the main minerals are montmorillonite and opal CT, in the subordinate quantity illite. The result of the heating was the decomposition of clay minerals. Further, the increase in silica and alumina contents. A significant changes in the original pore structure have been found. The changes were characterized by the expressed increase in the content of total porosity caused by the achieved occurence of the pores covering pore radius area over 2000 nm. This effect represents the increased openness of the pore structure which may have the significant role in the intensity of alkali-activation process as a factor contributing to the increase of the contact of alkali activator solution with the activated solid. As a possible consequence of the increased openness could be the acceleration of alkali-activation process resulting, for example, in the acceleration of the strength development of binding system based on the thermally treated bentonite.
机译:通过化学分析,X射线衍射,热分析,水银孔隙率法,差示扫描量热法,物理吸附测量和扫描电子显微镜对650℃×4h的原始和热处理过的膨润土样品进行表征。已经发现了加热的这些后果。化学分析表明,二氧化硅和氧化铝的含量较高,而Fe〜(+3),Ca〜(+2)和Mg〜(+2)的含量较少。 XRD分析表明,主要矿物为蒙脱石和蛋白石CT,次要含量为伊利石。加热的结果是粘土矿物的分解。此外,二氧化硅和氧化铝含量的增加。已发现原始孔结构发生了重大变化。这些变化的特征在于,由于覆盖2000nm以上的孔半径区域的孔的出现而导致的总孔隙率的含量明显增加。该作用表示孔结构的开放性增加,这可能在碱活化过程的强度中起重要作用,这是导致碱活化剂溶液与活化的固体接触增加的因素。开放性增加的可能结果可能是碱活化过程的加速,例如,这导致了基于热处理膨润土的粘结体系强度发展的加速。

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