Li Haoyang, Wang Yi, He Linyan, Wang Yifei, Liu Miao, Gu Li, Liu Shaowu, Li Jinze, Yang Yushu, Wang Ruizhi, He Qiang
Key laboratory of the Three Gorges Reservoir Region's Eco-environments, Ministry of Education, Institute of Environment and Ecology, Chongqing University, 174 Shapingba Road, Chongqing, 400045, China.
Gastrointestinal Cancer Center, Chongqing University Cancer Hospital, 174 Shapingba Road, 400045, PR China.
Water Res. 2025 Jan 1;268(Pt B):122708. doi: 10.1016/j.watres.2024.122708. Epub 2024 Oct 28.
Vivianite, a notable secondary mineral formed through dissimilatory iron reduction (DIR), demonstrates great potential in addressing both eutrophication and phosphorus deficiency. However, the presence of competition for electrons from the methanogenic pathway and the low rates of Fe(III) reduction limit the creation of vivianite. In this research, H was utilized as electron donor assisted by activated carbon (AC) to promote Fe(Ⅲ) reduction with FePO as electron acceptors. The introduction of H and H/AC increased the Fe(III) reduction by 23.8 % and 34.3 %, respectively. Both also increase the rate of vivianite formation. H acted as an electron donor to promote Fe(III) reduction by both direct Fe(III) reduction and homoacetogenesis-acetate reduction pathways. It also suppressed the process of methanogenesis to avoid extra consumption of electrons. AC increased the rate of electron transfer, increased hydrogenase and homoacetogenesis-related enzyme activities, and enriched more Dissimilatory iron reduction bacteria (DIRB). H promoted the up-regulation of Wood-Ljungdahl pathway, TCA cycle and electron transport chain related genes. AC enhanced H capture and functioned as an electron shuttle. These results offer fresh perspectives on promoting Fe(III) reduction to facilitate vivianite formation.
蓝铁矿是一种通过异化铁还原(DIR)形成的重要次生矿物,在解决富营养化和磷缺乏问题方面具有巨大潜力。然而,甲烷生成途径对电子的竞争以及较低的Fe(III)还原速率限制了蓝铁矿的生成。在本研究中,以H作为电子供体,并借助活性炭(AC),以FePO为电子受体促进Fe(Ⅲ)还原。引入H和H/AC分别使Fe(III)还原率提高了23.8%和34.3%。两者还提高了蓝铁矿的形成速率。H作为电子供体,通过直接Fe(III)还原和同型产乙酸-乙酸还原途径促进Fe(III)还原。它还抑制了甲烷生成过程,以避免电子的额外消耗。AC提高了电子转移速率,增加了氢化酶和同型产乙酸相关酶的活性,并富集了更多的异化铁还原细菌(DIRB)。H促进了伍德-Ljungdahl途径、三羧酸循环和电子传递链相关基因的上调。AC增强了H的捕获,并作为电子穿梭体发挥作用。这些结果为促进Fe(III)还原以利于蓝铁矿形成提供了新的视角。