Effect of porous media heterogeneity and FeS re-generation for multiple cycles on arsenic immobilization under in-situ conditions

IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Groundwater for Sustainable Development Pub Date : 2024-06-05 DOI:10.1016/j.gsd.2024.101220
Preetam Kumar Shukla , Vishal Deshpande , Trishikhi Raychoudhury
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Abstract

Arsenic (As) contamination in groundwater is a well-established concern. Several studies have explored the possibility of immobilizing arsenite [As (III)] in-situ within the aquifer. Recent studies show a uniform distribution of ferrous sulfate (FeS) synthesized within homogenous porous media and demonstrated promising performance in immobilizing As(III). Upscaling from bench-scale to field-scale systems involves the integration of physical and chemical heterogeneities. Thus, the distribution of reducing agent (i.e., FeS), subsequent capturing of As(III) in the upscaled heterogeneous porous media system is a complex and uncertain phenomenon. Therefore, this study focuses on assessing the performance of FeS when synthesized for multiple cycles under constant flow and constant head conditions for immobilization of As(III) through a heterogeneous porous media system. A 3-D heterogenous porous media system is first simulated using a sequential indicator simulator model (SISIM). Then, the same heterogeneous media is prepared in the laboratory by packing three different-sized sand within a 3-D tank (0.67 m × 0.40 m × 0.40 m) which is subdivided into a total of 150 grids (0.096 m × 0.08 m × 0.08 m). FeS is synthesized in-situ by sequential injection of sodium sulfide (Na2S) and ferrous sulfate (FeSO4‧6H2O), as detailed in the previous study. The outcome of the study suggests that flow within the model subsurface porous media is non-uniform and follows an inter-connected preferential flow path. The progression of in-situ synthesized FeS is faster in the areas of higher hydraulic conductivity. The immobilization of As (88%) is promising by FeS synthesized within heterogeneous porous media. An overall reduction of porosity (7.7%) and hydraulic conductivity (68.3%) are observed, which is more predominant along the preferential flow path where deposition of FeS is significantly higher. To maintain constant flow rate, 60% increase in head difference is required. Whereas the flow rate decreases by 47.2% when constant head condition is adopted. Overall, the newly synthesized FeS shows promising performance in immobilizing As(III) within heterogeneous model subsurface porous media; however, there might be some possibility of pore-clogging and bypassing of flow due to deposition and subsequent retention of As, which may impact the As removal efficiency in the longer run.

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多孔介质异质性和多次循环铁硫再生成对原位条件下砷固定化的影响
地下水中的砷(As)污染是一个公认的问题。一些研究探讨了在含水层中就地固定亚砷酸[As (III)]的可能性。最近的研究表明,在均质多孔介质中合成的硫酸亚铁(FeS)分布均匀,在固定 As(III)方面表现良好。从工作台规模提升到现场规模的系统涉及物理和化学异质性的整合。因此,还原剂(即 FeS)的分布以及随后在放大的异质多孔介质系统中捕获 As(III)是一个复杂且不确定的现象。因此,本研究重点评估了在恒定流量和恒定水头条件下合成的 FeS 在通过异质多孔介质系统固定 As(III)的多个循环中的性能。首先使用顺序指示器模拟器模型(SISIM)模拟三维异质多孔介质系统。然后,在实验室制备了相同的异质介质,在一个三维水槽(0.67 m × 0.40 m × 0.40 m)中填入三种不同大小的沙子,水槽被细分为总共 150 个网格(0.096 m × 0.08 m × 0.08 m)。根据先前研究的详细说明,硫化亚铁是通过依次注入硫化钠(Na2S)和硫酸亚铁(FeSO4‧6H2O)在原位合成的。研究结果表明,模型地下多孔介质内的流动是不均匀的,并遵循相互连接的优先流动路径。在导水率较高的区域,原位合成的 FeS 的流动速度较快。在异质多孔介质中合成的 FeS 有望固定砷(88%)。据观察,孔隙率(7.7%)和水力传导率(68.3%)总体上有所降低,其中沿优先流道的降低更为显著,因为该处的 FeS 沉积量明显更高。要保持恒定的流速,水头差需要增加 60%。而采用恒定水头条件时,流速会降低 47.2%。总之,新合成的 FeS 在固定异质模型地下多孔介质中的 As(III) 方面表现出良好的性能;但是,由于 As 的沉积和随后的滞留,可能会造成孔隙堵塞和绕流,从而影响长期的 As 去除效率。
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来源期刊
Groundwater for Sustainable Development
Groundwater for Sustainable Development Social Sciences-Geography, Planning and Development
CiteScore
11.50
自引率
10.20%
发文量
152
期刊介绍: Groundwater for Sustainable Development is directed to different stakeholders and professionals, including government and non-governmental organizations, international funding agencies, universities, public water institutions, public health and other public/private sector professionals, and other relevant institutions. It is aimed at professionals, academics and students in the fields of disciplines such as: groundwater and its connection to surface hydrology and environment, soil sciences, engineering, ecology, microbiology, atmospheric sciences, analytical chemistry, hydro-engineering, water technology, environmental ethics, economics, public health, policy, as well as social sciences, legal disciplines, or any other area connected with water issues. The objectives of this journal are to facilitate: • The improvement of effective and sustainable management of water resources across the globe. • The improvement of human access to groundwater resources in adequate quantity and good quality. • The meeting of the increasing demand for drinking and irrigation water needed for food security to contribute to a social and economically sound human development. • The creation of a global inter- and multidisciplinary platform and forum to improve our understanding of groundwater resources and to advocate their effective and sustainable management and protection against contamination. • Interdisciplinary information exchange and to stimulate scientific research in the fields of groundwater related sciences and social and health sciences required to achieve the United Nations Millennium Development Goals for sustainable development.
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