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表层沉积物对水中F?吸附及解析过程的影响
Analytical Experiment and Mechanism Study of Surface Sediment on Fluorine Solution

DOI: 10.12677/AEP.2019.95090, PP. 669-676

Keywords: 氟,动力学,吸附解析
Fluorine
, Dynamics, Adsorption Analysis

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Abstract:

地表水受污染后,与表层沉积物接触发生反应,污染物将释放出来,形成二次污染源。为了研究土壤对F?的解析作用,明确F?解析过程中发生的化学反应,本文采用动力学试验和吸附解吸试验,并结合伪二级动力学方程、等温吸附方程,模拟三泉水库底泥与库水之间的反应动力学过程和解析过程,得出当反应时间和初始浓度变化时,水中F?的反应速率,反应历程及其迁移转化规律。结果表明:1) 在表层沉积物上可能以化学反应控制的动力学过程为主,可以用伪二级动力学方程描述,拟合方程为t/qt = 0.7401t + 0.1266,相关系数R2 = 0.9985;2) 表层沉积物对F?的吸附解析等温线符合线性关系,拟合得出F?的饱和解析量为30.56 mg/g;3)土样与氟溶液接触后,溶液pH值随加入F?质量浓度增大而上升,说明随着F?解析的进行不断地有OH?被释放出来;从其他离子的变化可以看出,F?解析过程中发生的化学作用有沉淀–溶解,吸附–解析,离子交换作用。
After the surface water is polluted, it reacts with the surface sediments and releases the pollutants to form the secondary pollution source. In order to study the adsorption and desorption of F? in soils and determine the chemical reactions that happened during the F? analysis, kinetic tests and ad-sorption and desorption experiments were used in this study. Combined with pseudo-second-order kinetic equation and isothermal adsorption equation, the reaction kinetics and adsorption analysis between the mud and the reservoir water show that when the reaction time and the initial concen-tration are changed; the reaction rate, the reaction process and the migration and transformation rules of F? in water are obtained. The results show that: 1) The kinetic process controlled by chemi-cal reaction may be the dominant surface sediment, which can be described by pseudo second-order kinetic equation. The fitting equation is y = 0.7401x + 0.1266 and the correlation coefficient is R2 = 0.9985. 2) The isotherm of F? adsorption by surface sediment is in accordance with the linear relationship, and the saturated analytical volume of F? is 30.56 mg?g?1. 3) After the soil sample is in contact with the fluorine solution, the pH value of the solution increases with the increase of the F-mass concentration, indicating that OH? is continuously released in the F? analysis progresses; it can be seen from the change of other ions. The chemical reactions of F? occurring during the analysis process are precipitation-dissolution, adsorption-analysis, and ion exchange.

References

[1]  曹春, 康宏亮, 李萍萍, 等. 聚丙烯偕胺肟改性羊毛对氟离子的吸附及机理[J]. 高分子学报, 2016(4): 486-493.
[2]  荆秀艳, 袁周燕, 杨红斌, 等. 土氟静态吸附特性及其影响因素[J]. 生态环境学报, 2008, 17(5): 1818-1821.
[3]  杨军耀. 水–土系统氟迁移影响因素分析[J]. 工程勘察, 1998(3): 42-44.
[4]  江霜英, 高廷耀. 粘土对水中氟离子吸附去除机理的研究[J]. 化工环保, 2003, 23(4): 204-208.
[5]  王庆文. 土壤对矿井水中F?的吸附动力学和吸附机理初探[J]. 河南理工大学学报(自然科学版), 2009, 28(6): 807-810.
[6]  梁鹏. 稀土改性壳聚糖树脂的制备、表征及对氟离子的吸附特性研究[D]: [博士学位论文]. 青岛: 中国海洋大学, 2013.
[7]  阮建云, 马立锋, 石元值, 等. 茶园土壤对氟的吸附与解吸特性[J]. 茶叶科学, 2001, 21(2): 161-165.
[8]  Peek, D.C. and Volk, V.V. (1985) Fluoride Sorption and Desorption in Soils. Soil Science Society of America Journal, 49, 583-586.
https://doi.org/10.2136/sssaj1985.03615995004900030010x
[9]  Zhu, M.X., Ding, K.Y., Jiang, X. and Wang, H.-H. (2007) Investigation on Co-Sorption and Desorption of Fluoride and Phosphate in a Red Soil of China. Water Air & Soil Pol-lution, 183, 455-465.
https://doi.org/10.1007/s11270-007-9394-0
[10]  陈男. 天然及合成多孔性粘土材料对地下水中氟化物的吸附性能研究[D]: [博士学位论文]. 北京: 中国地质大学, 2012.
[11]  韩德刚, 高盘良. 化学动力学基础[M]. 北京: 北京大学出版社, 1987.
[12]  董岁明. 氟在土–水系统中的迁移机理与含氟水的处理研究[D]: [博士学位论文]. 西安: 长安大学, 2004.
[13]  梁秀娟. 吉林西部洋沙泡水库水土环境中氟的迁移转化机理研究[D]: [博士学位论文]. 长春: 吉林大学, 2008.
[14]  Nur, T., Loganathan, P., Nguyen, T.C., et al. (2014) Batch and Column Adsorption and Desorption of Fluoride Using Hydrous Ferric Oxide: Solution Chemistry and Modeling. Chemical Engineering Journal, 247, 93-102.
https://doi.org/10.1016/j.cej.2014.03.009
[15]  王洪涛. 多孔介质污染物迁移动力学[M]. 北京: 高等教育出版社, 2008.

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