An Seongnam, Kim Sang Hyun, Woo Heesoo, Choi Jae Woo, Yun Seong-Taek, Chung Jaeshik, Lee Seunghak
Water Cycle Research Center, Korea Institute of Science and Technology (KIST), Seoul 02792, Republic of Korea.
Water Cycle Research Center, Korea Institute of Science and Technology (KIST), Seoul 02792, Republic of Korea; Division of Energy and Environmental Technology, KIST School, Korea University of Science and Technology (UST), Seoul 02792, Republic of Korea.
J Hazard Mater. 2024 Feb 5;463:132837. doi: 10.1016/j.jhazmat.2023.132837. Epub 2023 Oct 21.
Despite the role of the vadose zone protecting groundwater from contamination, the non-stationarity in this zone makes it difficult to predict the behavior of petroleum hydrocarbons (PH) therein. In laboratory soil columns with sandy and sandy loam soils, we simulated a vadose zone subjected to repeated groundwater-level fluctuation (GLF) to evaluate the behavior of PH under hydrodynamic conditions. The GLF vertically redistributed the PH, the extent of which was pronounced in the sandy soil with a high initial concentration due to the enhanced transport of the immiscible PH through the larger pores. The frequency of GLF did not show a substantial effect on the extent of PH redistribution but largely affected their attenuation. The greater GLF hindered PH volatilization by maintaining a high degree of water saturation, while the subsequent development of a local anaerobic regime inhibited biodegradation, which was more apparent in the sandy loam. Finally, a specific potential risk index was introduced to quantitatively compare the potential risk of PH contamination in different vadose zones exposed to GLF. Overall, the sandy soil contaminated with the higher total PH (TPH) concentration showed markedly higher potential risk indices (i.e., 18.4-29.0%), while the ones comprised of the sandy loam showed 0.6-4.9%, which increased under the greater number of GLF cycles.
尽管包气带在保护地下水免受污染方面发挥着作用,但该区域的非平稳性使得预测其中石油烃(PH)的行为变得困难。在装有砂土和砂壤土的实验室土柱中,我们模拟了一个经历反复地下水位波动(GLF)的包气带,以评估水动力条件下PH的行为。GLF使PH在垂直方向上重新分布,由于互不相溶的PH通过较大孔隙的传输增强,这种重新分布的程度在初始浓度较高的砂土中更为明显。GLF的频率对PH重新分布的程度没有显著影响,但在很大程度上影响了它们的衰减。较大的GLF通过保持高度的水饱和度阻碍了PH的挥发,而随后局部厌氧状态的发展抑制了生物降解,这在砂壤土中更为明显。最后,引入了一个特定的潜在风险指数,以定量比较暴露于GLF的不同包气带中PH污染的潜在风险。总体而言,总PH(TPH)浓度较高的砂土显示出明显更高的潜在风险指数(即18.4 - 29.0%),而由砂壤土组成的包气带显示出0.6 - 4.9%,在更多的GLF循环下会增加。