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Kinetics, equilibrium, and mechanisms of sorption and desorption of 17α-ethinyl estradiol in two natural soils and their organic fractions

机译:两种天然土壤及其有机组分中17α-乙炔雌二醇吸附和解吸的动力学,平衡及机理

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A study was conducted on the kinetics, equilibrium, and mechanisms of sorption and desorption of 17α-ethinyl estradiol (EE2) in six sorbents, which were two natural soils (Bulk1 and Bulk2) and their fractions obtained by alkaline extraction, namely, humic acids (HA1 and HA2), and mineral-bond humins (MHU1 and MHU2). These sorbents, characterized by total organic carbon (TOC), black carbon (BC), gas adsorption and Fourier transform infrared spectra, were shown to be porous solids containing aromatic (hard carbon) and aliphatic carbon (soft carbon). The two-compartment first-order model fitted the kinetics of sorption very well (R~2 > 0.990). The fast and slow sorption rate constants ranged from 1.110 h~(-1) and 0.026 h~(-1) to 2.063 h~(-1) and 0.067 h~(-1) respectively. The slow sorption was attributed to the diffusion of EE2 in micropores rather than organic matter. The Freundlich model fitted the equilibrium of sorption and desorption very well. The nonlinearity of sorption took the order MHU > bulk soil > HA and was positively related to BC/TOC (p <0.01). The hysteresis in MHU2 with higher BC/TOC was stronger than that in Bulk2 with lower BC/TOC, but a contrary observation was found in MHU1 and Bulkl. This contradictory phenomenon could be attributed to the location difference of hard carbon which greatly affected the desorption process. These findings could give an insight into the sorption mechanisms and promote an accurate model for the transport, fate and risk assessment of EE2 in the environment.
机译:对17种α-乙炔雌二醇(EE2)在两种天然土壤(大块1和大块2)及其通过碱性萃取得到的腐殖酸组分中的吸附,解吸的动力学,平衡及其机理进行了研究。 (HA1和HA2),以及矿物质结合的人素(MHU1和MHU2)。这些吸附剂的特征在于总有机碳(TOC),黑碳(BC),气体吸附和傅立叶变换红外光谱,被证明是包含芳香族(硬碳)和脂肪族碳(软碳)的多孔固体。两室一阶模型很好地拟合了吸附动力学(R〜2> 0.990)。快,慢速吸附速率常数分别为1.110 h〜(-1)和0.026 h〜(-1)到2.063 h〜(-1)和0.067 h〜(-1)。缓慢的吸收归因于EE2在微孔而不是有机物中的扩散。 Freundlich模型非常适合吸附和解吸的平衡。吸附的非线性程度依次为MHU>块状土壤> HA,并且与BC / TOC呈正相关(p <0.01)。 BC / TOC较高的MHU2的滞后性强于BC / TOC较低的Bulk2的滞后性,但在MHU1和Bulkl中发现相反的现象。这种矛盾现象可以归因于硬碳的位置差异,这大大影响了脱附过程。这些发现可以提供对吸附机制的深入了解,并为环境中EE2的运输,命运和风险评估提供一个准确的模型。

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