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Effects of Hydrothermal Dewatering on Lignite Physico-Chemical Structures and Analysis of Moisture Removal Mechanism

机译:水热脱水对褐煤理化结构的影响及除湿机理分析

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1. Hydrothermal dewatering (HTD) could remove carboxyl and hydroxyl groups in lignite, which begin to decompose after 200 °C and 230 °C respectively. 2. During HTD process, pore volume and surface area increase significantly at first and then decrease. The increase mainly derives from the development of meso-pore and is attributed to the evaporation of water and release of volatiles initially, and the decrease is ascribed to the destruction of lignite structure at high temperature. 3. The removal of free water, capillary water and molecular water is associated with the collapse of macro-pore, the damage of meso-pore and the removal of oxygen functional groups respectively.
机译:1.水热脱水(HTD)可以去除褐煤中的羧基和羟基,它们分别在200°C和230°C后开始分解。 2.在HTD过程中,孔体积和表面积首先显着增加,然后减小。这种增加主要来自中孔的发展,最初归因于水的蒸发和挥发物的释放,而这种减少归因于高温下褐煤结构的破坏。 3.游离水,毛细管水和分子水的去除分别与大孔的破坏,中孔的破坏和氧官能团的去除有关。

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