饱和土壤填料柱中镉(II)和氧化锌的协同迁移:离子强度和 pH 值的影响

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Acta Geochimica Pub Date : 2023-10-25 DOI:10.1007/s11631-023-00645-3
Min Liao, Guo Bin, Yixin Luo, Yuhao Zhang, Kangyou Hu, Xiongxiong Lu, Xiaomei Xie
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引用次数: 0

摘要

纳米氧化锌(nZnO)在各行各业的快速发展和广泛应用引起了人们对其潜在环境影响的关注。因此,了解 nZnO 在自然环境中的归宿和作用对于减轻其对环境和人类安全的有害影响至关重要。本研究旨在通过揭示镉(II)和纳米氧化锌(nZnO)在不同离子强度(IS)和 pH 值条件下在土壤中的共迁移特性,为了解和消除土壤环境中纳米颗粒和重金属污染的共同风险提供科学支持。本研究调查了在一个长 20 厘米、内径 2.5 厘米、装有 10 厘米高土壤样品的丙烯酸柱中,不同离子强度和 pH 值对 Cd(II) 和 nZnO 协同迁移的影响。在上述系统中,500 μg L-1 的镉(II)负载 nZnO 悬浮脉冲随 IS 或 pH 值的变化被引入土壤柱中浸滤 5 个 PV,然后再浸滤 5 个 PV 不含 nZnO 的背景溶液。IS 为 1、10 或 50 mM NaCl,pH 值为 6;pH 值为 6、7 或 8,含 1 mM NaCl。同时,还进行了 nZnO 的沉降实验、土壤对 Cd(II) 的吸附实验以及相同背景条件下的 nZnO、DLVO 理论计算。由于 nZnO 对与 nZnO 相关的 Cd(II) 有很强的吸附能力,因此 nZnO 的存在大大增加了 Cd(II) 的迁移率。然而,随着 IS 的增加,nZnO 和 Cd(II) 的共迁移率降低,并且由于迁移过程中更多的 nZnO 参与聚集和沉积,以及 nZnO 在 Na+ 的竞争下对 Cd(II) 的吸附能力降低,导致 nZnO 在土柱中的保留率降低。当 pH 值为 6、7 和 8 时,随着 pH 值的升高,nZnO 与 Cd(II)的共迁移量增加,这是因为在较高的 pH 值下,nZnO 与土壤之间的静电吸引力降低。同时,DLVO 理论被拟合用于描述上述 nZnO 和 Cd(II) 的共迁移过程。应更多地关注 nZnO 对自然土壤中 Cd(II) 迁移的影响,以控制纳米粒子和重金属对环境的潜在风险。可通过调节土壤溶液中的 IS 和 pH 值来控制 nZnO 和 Cd(II) 共同迁移的风险。
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The co-transport of Cd(II) and nZnO in saturated soil packed column: effects of ionic strength and pH

The rapid development and widespread use of ZnO nanoparticles (nZnO) in various industries have raised concerns about their potential environmental impact. Therefore, understanding the fate and role of nZnO in the natural environment is crucial for mitigating their hazardous effects on the environment and human safety. The purpose of the present study was to provide scientific support for understanding and eliminating the joint risk of nanoparticle and heavy metal pollution in the soil environment by revealing the co-transport characteristics of Cd(II) and ZnO nanoparticles (nZnO) in soil under different ionic strength (IS) and pH. The impacts of different IS and pH on the co-transport of Cd(II) and nZnO in a 20 cm long with an inner diameter of 2.5 cm acrylic column packed with 10 cm high soil samples were investigated in the present study. In the above system, a 500 μg L−1 Cd(II) loaded nZnO suspension pulse with varying IS or pH was introduced into the soil column for leaching over 5 PVs, followed up by 5 PVs background solutions without nZnO. The IS was 1, 10, or 50 mM NaCl, with pH6, or the pH was 6, 7 or 8 with 1 mM NaCl. Meanwhile, Sedimentation experiments for nZnO, adsorption of Cd(II) on soil, and nZnO, DLVO theory calculation for the same background condition were conducted. The presence of nZnO significantly increased the mobility of Cd(II) as a result of its strong adsorption capacity for nZnO-associated Cd(II). However, with the increase of IS, the co-transport of nZnO and Cd(II) was decreased and the retention of nZnO in the soil column due to more nZnO attended to aggregate and sediment during the transport and the decrease in the adsorption capacity of nZnO for Cd(II) by competition of Na+. When pH was 6, 7, and 8, the co-transport of nZnO and Cd(II) increased with higher pH due to the lower electrostatic attraction between nZnO and soil under higher pH. Meanwhile, the DLVO theory was fitted to describe the above co-transport process of nZnO and Cd(II). More attention should be paid to the presence of nZnO on the migration of Cd(II) in the natural soil to control the potential risk of nanoparticles and heavy metals to the environment. The risk of co-transport of nZnO and Cd(II) might be controlled by adjusting IS and pH in the soil solution.

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来源期刊
Acta Geochimica
Acta Geochimica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
2.80
自引率
6.20%
发文量
1134
期刊介绍: Acta Geochimica serves as the international forum for essential research on geochemistry, the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth‘s crust, its oceans and the entire Solar System, as well as a number of processes including mantle convection, the formation of planets and the origins of granite and basalt. The journal focuses on, but is not limited to the following aspects: • Cosmochemistry • Mantle Geochemistry • Ore-deposit Geochemistry • Organic Geochemistry • Environmental Geochemistry • Computational Geochemistry • Isotope Geochemistry • NanoGeochemistry All research articles published in this journal have undergone rigorous peer review. In addition to original research articles, Acta Geochimica publishes reviews and short communications, aiming to rapidly disseminate the research results of timely interest, and comprehensive reviews of emerging topics in all the areas of geochemistry.
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