背景:水煤浆(CWS)是一种低污染的新型液态煤产品,主要用于化学工业生产合成气(CO+H2)。研究CWS气化反应的微观机理对提高煤气化效率具有重要意义。在本文中,采用基于反应力场的分子动力学方法(ReaxFF-MD)研究了CWS/O2体系在不同温度下的气化过程。结果表明,在1600-2400K的范围内,褐煤的大分子网络结构被分解成大量的小分子结构和少量的轻质焦油自由基片段,反应产物的种类和数量迅速增加。在2400-4000K,轻质焦油的自由基片段进一步分解并与气化剂反应,但反应产物的种类和数量变化不大。在3600K,系统中发生了完全气化反应,合成气的含量最高。
方法:通过MaterialsStudio(MS)软件建立模型并进行优化。基于ReaxFF-MD方法,采用Lammps软件模拟CWS/O2系统的气化过程,和包含C的反作用力场文件,H,O,N,使用S元素。通过计算气化反应的活化能,说明了模型和计算方法的合理性。使用OVITO对结果进行后处理,ChemDraw软件,和自编程的Python脚本。
BACKGROUND: Coal water slurry (CWS) is a new type of liquid coal product with low pollution, which is mainly used in the chemical industry to produce syngas (CO + H2). It is of great significance to study the microscopic mechanism of CWS gasification reaction for improving the efficiency of coal gasification. In this paper, the method of molecular dynamics based on reaction force fields (
ReaxFF-MD) is used to study the gasification process of CWS/O2 system at different temperatures. The results show that, in the range of 1600-2400 K, the macromolecular network structure of lignite is decomposed into a large number of small molecular structures and a small number of light tar free radical fragments, and the types and quantities of reaction products increased rapidly. At 2400-4000 K, the free radical fragments of light tar are further decomposed and reacted with gasification agents, but the types and quantities of reaction products have little change. At 3600 K, a full gasification reaction occurred in the system, and the content of syngas is the highest.
METHODS: The model was established and optimized by Materials Studio (MS) software. Based on
ReaxFF-MD method, Lammps software was used to simulate the gasification process of CWS/O2 system, and the reaction force field files containing C, H, O, N, and S element were used. By calculating the activation energy of gasification reaction, the rationality of the model and calculation method was illustrated. The post-processing of the results was implemented using OVITO, ChemDraw software, and self-programmed Python scripts.