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Hydrothermal decomposition of K-feldspar in KOH-NaOH-H2O medium

机译:KOH-NaOH-H2O介质中钾长石的水热分解

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The hydrothermal decomposition of K-feldspar in mixed alkaline solutions containing NaOH and KOH at a concentration of 8.5 M was studied. As the mole fraction of KOH (chi(KOH) = KOH/(KOH + NaOH) in mole) in the mixed alkaline solution decreased, metastable kalsilite, kalsilite and hydroxyl-cancrinite crystallized progressively at 240 degrees C. The metastable kalsilite disappeared when reaction temperature increased from 240 degrees C to 280 degrees C, while the crystallization zone of kalsilite was extended from chi(KOH) = 0.8-03 to chi(KOH) = 1.0-0.4, and the crystallization zone of hydroxyl-cancrinite was enlarged from chi(KOH) = 0 to chi(KOH) = 0.2-0. The K-feldspar dissolved under the action of OH- and released K+, Al(OH)(4)(-) and H2SiO42-. The kalsilite or hydroxyl-cancrinite was precipitated from solution. (C) 2015 Elsevier B.V. All rights reserved.
机译:研究了钾长石在浓度为8.5 M的NaOH和KOH混合碱溶液中的水热分解。随着混合碱溶液中KOH的摩尔分数(chi(KOH)= KOH /(KOH + NaOH)以摩尔计)的降低,亚稳钾晶石,钾铝石和羟基钙铝石在240摄氏度下逐渐结晶。温度从240摄氏度增加到280摄氏度,而钙硅石的结晶区从chi(KOH)= 0.8-03扩展到chi(KOH)= 1.0-0.4,而羟基钙锰矿的结晶区从chi(KOH)= 0.8-0.4扩大。 (KOH)= 0至chi(KOH)= 0.2-0。钾长石在OH-的作用下溶解并释放出K +,Al(OH)(4)(-)和H2SiO42-。从溶液中沉淀出钙硅石或羟基钙硅石。 (C)2015 Elsevier B.V.保留所有权利。

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