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Further studies of the hydration of MgO-hydromagnesite blends

机译:进一步研究MgO - 水质岩混合物的水合

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The hydration of magnesium oxide in the presence of hydromagnesite (Mg-5(CO3)(4)(OH)(2)center dot 4H(2)O) was investigated. The hydration products are a poorly-crystalline form of brucite (Mg(OH)(2)) and an unknown amorphous or poorly crystalline hydrate, which was evidenced by X-ray diffraction analyses and Raman spectroscopy. By thermogravimetry it was found that in the presence of hydromagnesite more water is bound in hydrate phases than can be explained by the formation of brucite only. The unknown hydrate is hypothesized to lead to cohesive binding in MgO-hydromagnesite blends. Due to thermodynamic predictions artinite (Mg-2(CO3)(OH)(2)center dot 3H(2)O) should be the stable hydrate in this system. The addition of artinite crystal seeds, however, had no significant effect on hydration kinetics or nature of the reaction products. The hypothesis that the addition of sodium bicarbonate (NaHCO3) could modify or accelerate the hydration reactions due to its high solubility and the supply of additional HCO3- ions was also not supported by the experiments.
机译:研究了含氢镁(Mg-5(4)(4)(2)中心点4H(2)O)存在下氧化氢氧化镁的水合。水合产物是一种良好的结晶形式的Brucite(Mg(OH)(2))和未知的无定形或结晶水合物,其通过X射线衍射分析和拉曼光谱证明。通过热重量测定,发现在水质石存在下,水合物相对于水合物相结合,其仅仅可以通过形成布鲁氏石块的形成。未知的水合物被假设以导致MgO - 水质石共混物中的内聚结合。由于热力学预测,Artinite(Mg-2(CO 3)(OH)(2)中心点3h(2)O)应该是该系统中的稳定水合物。然而,添加型晶体种子对反应产物的水合动力学或性质没有显着影响。添加碳酸氢钠(NaHCO 3)的假设可以通过其高溶解度来修饰或加速水化反应,并且实验也不支持供应另外的HCO3-离子。

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