4.7 Article

Study on the pore structure and oxygen-containing functional groups devoting to the hydrophilic force of dewatered lignite

Journal

APPLIED SURFACE SCIENCE
Volume 324, Issue -, Pages 90-98

Publisher

ELSEVIER
DOI: 10.1016/j.apsusc.2014.10.126

Keywords

Dewatered lignite; Pore structure; Oxygen-containing functional groups; Hydrophilicity

Funding

  1. National Basic Research Program of China [2012CB214902]
  2. International S&T Cooperation Program of China [2013DFG61490]
  3. Shanxi Province Basic Conditions Platform for Science and Technology Project [2012091018]

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In order to explore the water-holding capacity of dewatered lignite and the contribution of pore structure and oxygen-containing functional groups to it, a kind of typical Chinese lignite was dried under the atmosphere of nitrogen for different temperatures and times, and then was subjected to a process of moisture re-adsorption at the temperature of 25 degrees C and relative humidity of 75%. Nitrogen adsorption and chemical titration methods were used to examine the pore structure parameters and amounts of oxygen-containing functional groups, respectively. The results indicate that the porous structure and oxygen-containing functional groups in lignite are two main factors influencing the hydrophilicity of dewatered coal, and their contributions are varied with the change of drying conditions. The change of water-holding capacity of pore structure is primarily attributed to the shrinkage or collapse of macro- and mesoporous and it decreases with the increase of drying temperature. The oxygen-containing functional groups mainly include phenolic hydroxyl, carbonyl, carboxyl and methoxyl groups, and the order of their hydrophilicity is: carboxyl group > phenolic hydroxyl group > carbonyl group > methoxyl group. Moreover, the water-holding capacity for the same kind of oxygen-containing functional groups in dewatered coal obtained at different temperature is not a fixed one, their hydrophilic forces decrease with the increase of drying temperature. For the coal samples dried for 60 min under different temperature, the contribution of pore structure and oxygen-containing functional groups to the equilibrium moisture content (EMC) of dewatered lignite is: pore structure > phenolic hydroxyl group > carboxyl group > carbonyl group > methoxyl group. The contribution of total oxygen-containing functional groups to the EMC at below 280 degrees C is more obvious, and that of pore structure is the principal factor thereafter. (C) 2014 Elsevier B.V. All rights reserved.

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