School of Civil Engineering, Engineering Campus, Universiti Sains Malaysia, Nibong Tebal, Malaysia.
Solid Waste Management Cluster, Engineering Campus, Universiti Sains Malaysia, Nibong Tebal, Malaysia.
Water Environ Res. 2023 Aug;95(8):e10913. doi: 10.1002/wer.10913.
Groundwater is one of the alternatives to surface water that can be used for drinking water; however, it normally exists with high iron and manganese content. In this study, a column study was conducted to observe the elimination of iron (Fe) and manganese (Mn) in the groundwater under different retention times by using zeolite immobilized with iron-oxidizing bacteria (IOB). Rossellomorea sp., representing an IOB, was found from the isolation process and was further cultured in the laboratory for immobilization into the natural zeolite as replacement materials for the sand filter. When the zeolite assisted with the Rossellomorea sp. was used, the elimination of Fe and Mn were 99.34% and 88.92%, respectively, compared to the removal of Fe and Mn, which were 93.62% and 93.73%, respectively, for media without immobilization. The presence of Rossellomorea sp. enhances the Fe oxidation, resulting in high removal of Fe. The Thomas and Yoon-Nelson models were performed in both raw zeolite and zeolite with IOB. The total coliform (most probable number [MPN]) increased from 70.8 to 307.6 MPN/100 mL because of the Rossellomorea sp. present that promotes the growth of coliform bacteria. In conclusion, the immobilization of zeolite with IOB is a potential technique to extract the Fe and Mn in the groundwater. PRACTITIONER POINTS: Zeolite incorporated with Rossellomorea sp. has higher removal performance of Fe, whereas the removal of Mn reduced compared to the raw zeolite. The presence of Rossellomorea sp. enhances the oxidation of ferrous iron and improves the removal of Fe in the groundwater because the ferric iron is the priority ion to be exchanged. The removal of UV254 increase when Rossellomorea sp. present in the zeolite because the Rossellomorea sp. consume the natural organic matter as carbon source.
地下水是可用于饮用水的替代地表水之一;然而,它通常含有高铁和高锰含量。在这项研究中,通过使用固定化铁氧化细菌(IOB)的沸石柱研究来观察不同停留时间下地下水铁(Fe)和锰(Mn)的去除情况。从分离过程中发现了 Rossellomorea sp.,它代表了一种 IOB,并在实验室中进一步培养,将其固定在天然沸石中,作为砂滤器的替代材料。当使用沸石辅助 Rossellomorea sp. 时,Fe 和 Mn 的去除率分别为 99.34%和 88.92%,而没有固定化的介质的去除率分别为 93.62%和 93.73%。Rossellomorea sp. 的存在增强了 Fe 的氧化作用,从而实现了高 Fe 去除率。Thomas 和 Yoon-Nelson 模型分别在原始沸石和固定化 IOB 的沸石上进行。由于存在促进大肠菌群生长的 Rossellomorea sp.,总大肠菌群(最可能数 [MPN])从 70.8 增加到 307.6 MPN/100 mL。综上所述,沸石固定化 IOB 是一种从地下水中提取 Fe 和 Mn 的潜在技术。从业者要点:与原始沸石相比,固定化 Rossellomorea sp. 的沸石对 Fe 的去除性能更高,而对 Mn 的去除性能降低。由于亚铁的氧化作用增强,并且地下水的 Fe 优先被交换,因此 Rossellomorea sp. 的存在提高了地下水的 Fe 去除率。由于 Rossellomorea sp. 消耗天然有机物作为碳源,因此当沸石中存在 Rossellomorea sp. 时,UV254 的去除率会增加。