Zakari Sissou, Liu Hui, Li Yan-Xi, He Xi, Tong Lei
State Key Laboratory of Biogeology and Environmental Geology and School of Environmental Studies, China University of Geosciences, Wuhan, 430074, People's Republic of China.
Environ Sci Pollut Res Int. 2016 Aug;23(15):15749-56. doi: 10.1007/s11356-016-6660-y. Epub 2016 May 4.
This work aimed to quantify the transport and sorption behavior of four individual phthalate esters (PAEs) in sandy aquifer using column experiments so as to provide important parameters for the prediction and control of PAEs pollution plume in groundwater system. The transport curves of four individual PAEs were simulated with HYDRUS-1D through fitting linear and nonlinear equilibrium (LE/NO), linear and nonlinear, first-order, one-site non-equilibrium (LO/NO), linear and nonlinear, first-order, two-site non-equilibrium (LFO/NFO) sorption models. Simulation results showed that two-site models (LFO and NFO) displayed similar best fittings. The results from LFO model simulation showed that when water flowed 1000 m in sandy aquifer, PAEs with shorter carbon chains (DMP and DEP) transport 31.6 and 22.2 m, respectively. Unexpectedly for the same water transport distance, PAEs with longer carbon chains (DBP and DiBP) transported 40.2 and 60.7 m, respectively, which were faster than DMP and DEP, mainly due to the limited accessibility of type-2 sorption sites. The retardations were mainly caused by the sorption of PAEs on the time-dependent type-2 sites. DBP and DiBP exhibited higher mass transfer speed to and fro type-2 sites but showed lower total sorption coefficient (K) due to the limited accessibility of sorption sites. Coexistence of PAEs and smaller sorbent particles increased total K values of DBP and DiBP due to synergic development of more sorption sites with DMP and DEP.
本研究旨在通过柱实验量化四种邻苯二甲酸酯(PAEs)在砂质含水层中的迁移和吸附行为,以便为预测和控制地下水系统中PAEs污染羽提供重要参数。利用HYDRUS-1D通过拟合线性和非线性平衡(LE/NO)、线性和非线性、一级、单位点非平衡(LO/NO)、线性和非线性、一级、双位点非平衡(LFO/NFO)吸附模型来模拟四种PAEs的迁移曲线。模拟结果表明,双位点模型(LFO和NFO)显示出相似的最佳拟合效果。LFO模型模拟结果表明,当水流在砂质含水层中流动1000米时,碳链较短的PAEs(DMP和DEP)分别迁移31.6米和22.2米。出乎意料的是,在相同的水流距离下,碳链较长的PAEs(DBP和DiBP)分别迁移40.2米和60.7米,比DMP和DEP快,这主要是由于2型吸附位点的可及性有限。阻滞作用主要是由PAEs在随时间变化的2型位点上的吸附引起的。DBP和DiBP在2型位点之间表现出较高的传质速度,但由于吸附位点的可及性有限,其总吸附系数(K)较低。PAEs与较小的吸附剂颗粒共存会增加DBP和DiBP的总K值,这是因为与DMP和DEP协同形成了更多的吸附位点。