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天然石英砂的表面络合模型研究
引用本文:黄磊,方红卫,王靖宇,陈明洪,何国建.天然石英砂的表面络合模型研究[J].环境科学学报,2014,34(5):1141-1149.
作者姓名:黄磊  方红卫  王靖宇  陈明洪  何国建
作者单位:清华大学水利水电工程系, 水沙科学与水利水电工程国家重点实验室, 北京 100084;清华大学水利水电工程系, 水沙科学与水利水电工程国家重点实验室, 北京 100084;清华大学水利水电工程系, 水沙科学与水利水电工程国家重点实验室, 北京 100084;中国农业大学水利与土木工程学院, 北京 100083;清华大学水利水电工程系, 水沙科学与水利水电工程国家重点实验室, 北京 100084
基金项目:国家自然科学基金重点基金(No.51139003)
摘    要:天然泥沙颗粒表面特性复杂,其与营养物质及重金属之间的相互作用,是研究天然水体水环境效应的关键科学问题之一.本文以石英砂为例,在考虑天然泥沙表面形貌引起的电荷非均匀分布的基础上,建立了统计意义上的表面电荷分布-表面电位数学关系,并修正表面络合模型,对表面络合常数采用更合理的静电力校正,模拟营养物质及重金属在天然泥沙颗粒表面的吸附-解吸关系.同时,表面滴定实验及吸附实验数据被用来进行模型验证.结果表明,泥沙颗粒的吸附特性受pH值、水相平衡浓度和背景离子强度等影响,考虑颗粒表面电荷非均匀分布的修正模型,更接近天然泥沙的吸附特性,相比传统表面络合模型,能够更好地模拟吸附结果.

关 键 词:石英砂  电荷分布  表面络合模型
收稿时间:2013/8/17 0:00:00
修稿时间:2013/11/5 0:00:00

Surface complexation model for quartz sand particles
HUANG Lei,FANG Hongwei,WANG Jingyu,CHEN Minghong and HE Guojian.Surface complexation model for quartz sand particles[J].Acta Scientiae Circumstantiae,2014,34(5):1141-1149.
Authors:HUANG Lei  FANG Hongwei  WANG Jingyu  CHEN Minghong and HE Guojian
Institution:Department of Hydraulic Engineering, the State Key Laboratory of Hydro-science and Engineering, Tsinghua University, Beijing 100084;Department of Hydraulic Engineering, the State Key Laboratory of Hydro-science and Engineering, Tsinghua University, Beijing 100084;Department of Hydraulic Engineering, the State Key Laboratory of Hydro-science and Engineering, Tsinghua University, Beijing 100084;College of Water Resources and Civil Engineering, China Agricultural University, Beijing 100083;Department of Hydraulic Engineering, the State Key Laboratory of Hydro-science and Engineering, Tsinghua University, Beijing 100084
Abstract:The interaction between sediment and pollutants, such as nutrients and heavy metals, is one of the key issues related to the effects of water environment. This paper modified the surface complexation model with quartz sand as an example, considering the non-uniform distribution of surface charge. The surface morphology and charge distribution were observed using the electrical force microscope and the statistics of micro-morphology and surface charge distribution were obtained. Through the potential calculation, a statistical relationship between surface charge distribution and surface potential was established. The surface complexation model was then modified using a more reasonable correction of electrostatic factor, including the effects of non-uniform charge distribution. Data from titration experiment and adsorption experiment were used for the model validation. Results show that the adsorption characteristics of sediment particles are influenced by pH, equilibrium concentration, and ionic strength. The modified surface complexation model can better simulate the adsorption of pollutants on sediment particles.
Keywords:quartz sand  surface charge distribution  surface complexation model
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