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温压条件下不同含水高岭石对NH4+吸附的分子模拟
引用本文:杨有威,王有霖,罗玉霞,刘新棋,郭昌胜,陈明,王春英.温压条件下不同含水高岭石对NH4+吸附的分子模拟[J].中国环境科学,2022,42(8):3720-3727.
作者姓名:杨有威  王有霖  罗玉霞  刘新棋  郭昌胜  陈明  王春英
作者单位:1. 江西省矿冶环境污染控制重点实验室, 江西 赣州 341000;2. 中国南方稀土集团有限公司, 江西 赣州 341000;3. 中国环境科学研究院, 环境基准与风险评估国家重点实验室, 北京 100012
基金项目:国家重点研发计划(2019YFC1805100);国家自然科学基金资助项目(21767012);江西理工大学清江青年英才支持计划项目(JXUSTJYX2016003);江西理工大学研究生创新专项资金项目(XY2021-S013)
摘    要:为研究高岭石对NH4+吸附的微观情况,通过Material Studio软件对高岭石单胞进行收敛性测试后构建了4×2×1不同水化程度高岭石模型,采用量子力学和经典力学方法对模型晶胞进行了理论计算和吸附实验研究.结果显示,在交换关联泛函GGA-PW91,K点4×3×2,截断能600eV条件下,得到了高岭石稳定结构模型(误差<2%);高岭石对NH4+的吸附受温度影响明显,随温度升高,吸附量逐渐减少,与吸附实验结果一致;动力学结果显示吸附类型主要为物理吸附,吸附作用力为范德华力和库仑力.

关 键 词:高岭石  分子模拟  吸附  NH4+  影响因素  
收稿时间:2022-01-10

Molecular simulation of NH4+ adsorption by kaolinite with different water content under temperature and pressure
YANG You-wei,WANG You-lin,LUO Yu-xia,LIU Xin-qi,GUO Chang-sheng,CHEN Ming,WANG Chun-ying.Molecular simulation of NH4+ adsorption by kaolinite with different water content under temperature and pressure[J].China Environmental Science,2022,42(8):3720-3727.
Authors:YANG You-wei  WANG You-lin  LUO Yu-xia  LIU Xin-qi  GUO Chang-sheng  CHEN Ming  WANG Chun-ying
Institution:1. Jiangxi Key Laboratory of Mining and Metallurgy Environmental Pollution Control, Ganzhou 341000, China;2. China South Rare Earth Group Co. LTD, Ganzhou 341000, China;3. State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China
Abstract:In order to study the microscopic situation of NH4+ adsorption by kaolinite, kaolinite models with different hydration degrees of 4×2×1 were constructed after the convergence test of kaolinite monocytes by Material Studio software. The theoretical calculation and adsorption experiment of the model cell were carried out by using the methods of quantum mechanics and classical mechanics. The results showed that the stable structure model of kaolinite is obtained (error < 2%) under the conditions of exchange correlation functional GGA-PW91, K point 4×3×2 and truncation energy 600eV. The adsorption of NH4+ by kaolinite was obviously affected by temperature. With the increase of temperature, the adsorption capacity decreases gradually, which was consistent with the experimental results. The kinetic results showed that the adsorption type was mainly physical adsorption, and the adsorption forces were Van der Waals force and Coulomb force. The research results were helpful to supplement the research on the kaolinite properties and have a guiding role in the control of ammonia nitrogen pollution in soil of rare earth mines.
Keywords:kaolinite  molecular simulation  adsorption  NH4+  influencing factors  
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