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在不同水化学条件下,铵和胶体在饱和多孔介质中的共运移行为。

Co-transport behavior of ammonium and colloids in saturated porous media under different hydrochemical conditions.

机构信息

Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun, 130021, China.

College of Environment and Resources, Jilin University, Changchun, 130021, China.

出版信息

Environ Sci Pollut Res Int. 2020 May;27(13):15068-15082. doi: 10.1007/s11356-020-07835-z. Epub 2020 Feb 17.

Abstract

To investigate co-transport behavior of ammonium and colloids in saturated porous media under different hydrochemical conditions, NH was selected as the target contaminant, and silicon and humic acid (HA) were selected as typical organic and inorganic colloids in groundwater. Column experiments were then conducted to investigate the transport of NH colloids under various hydrochemical conditions. The results showed that because of the different properties of colloidal silicon and HA after combining with NH, the co-transport mechanism became significantly different. During transport by the NH-colloid system, colloidal silicon occupied the adsorption sites on the medium surface to promote the transport of NH, while humic acid (HA) increased the number of adsorption sites of the medium to hinder the transport of NH. The co-transport of NH and colloids is closely related to hydrochemical conditions. In the presence of HA, competitive adsorption and morphological changes of HA caused NH to be more likely to be transported at a higher ionic strength (IS = 0.05 m, CaCl) and alkalinity (pH = 9.3). In the presence of colloidal silicon, blocking action caused the facilitated transport to be dependent on higher ionic strength and acidity (pH = 4.5), causing the recovery of NH to improve by 7.99%, 222.25% (stage 1), and 8.63%, respectively. Moreover, transport increases with the colloidal silicon concentrations of 20 mg/L then declines at 40 mg/L, demonstrating that increased concentrations will lead to blocking and particle aggregation, resulting in delayed release in the leaching stage. Graphical abstract.

摘要

为了研究不同水化学条件下铵和胶体在饱和多孔介质中的共运移行为,选择 NH 作为目标污染物,硅和腐殖酸(HA)作为地下水中典型的有机和无机胶体。然后进行了柱实验来研究各种水化学条件下 NH 胶体的迁移。结果表明,由于与 NH 结合后的胶体硅和 HA 的性质不同,共运移机制有很大差异。在 NH-胶体体系的运移过程中,胶体硅占据介质表面的吸附位,促进 NH 的运移,而腐殖酸(HA)增加了介质的吸附位数量,阻碍 NH 的运移。NH 和胶体的共运移与水化学条件密切相关。在存在 HA 的情况下,竞争吸附和 HA 的形态变化导致 NH 在更高的离子强度(IS=0.05 m,CaCl)和碱性(pH=9.3)下更有可能被运移。在存在胶体硅的情况下,堵塞作用导致易位运输取决于更高的离子强度和酸度(pH=4.5),使 NH 的回收率分别提高了 7.99%、222.25%(第 1 阶段)和 8.63%。此外,随着胶体硅浓度从 20mg/L 增加到 40mg/L,运输量增加,然后减少,表明浓度增加会导致堵塞和颗粒聚集,从而导致浸出阶段的延迟释放。图表摘要。

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