Geomicrobiology, Center for Applied Geoscience, University of Tuebingen, Germany.
Quantitative Biology Center (QBiC), University of Tuebingen, Germany.
Sci Total Environ. 2022 Sep 10;838(Pt 4):156496. doi: 10.1016/j.scitotenv.2022.156496. Epub 2022 Jun 3.
Household sand filters (SFs) are widely applied to remove iron (Fe), manganese (Mn), arsenic (As), and ammonium (NH) from groundwater in the Red River delta, Vietnam. Processes in the filters probably include a combination of biotic and abiotic reactions. However, there is limited information on the microbial communities treating varied groundwater compositions and on whether biological oxidation of Fe(II), Mn(II), As(III), and NH contributes to the overall performance of SFs. We therefore analyzed the removal efficiencies, as well as the microbial communities and their potential activities, of SFs fed by groundwater with varying compositions from low (3.3 μg L) to high (600 μg L) As concentrations. The results revealed that Fe(II)-, Mn(II)-, NH-, and NO-oxidizing microorganisms were prevalent and contributed to the performance of SFs. Additionally, groundwater composition was responsible for the differences among the present microbial communities. We found i) microaerophilic Fe(II) oxidation by Sideroxydans in all SFs, with the highest abundance in SFs fed by low-As and high-Fe groundwater, ii) Hyphomicropbiaceae as the main Mn(II)-oxidizers in all SFs, iii) As sequestration on formed Fe and Mn (oxyhydr)oxide minerals, iv) nitrification by ammonium-oxidizing archaea (AOA) followed by nitrite-oxidizing bacteria (NOB), and v) unexpectedly, the presence of a substantial amount of methane monooxygenase genes (pmoA), suggesting microbial methane oxidation taking place in SFs. Overall, our study revealed diverse microbial communities in SFs used for purifying arsenic-contaminated groundwater, and our data indicate an important contribution of microbial activities to the key functional processes in SFs.
家用砂滤器(SFs)广泛应用于去除越南红河三角洲地下水中的铁(Fe)、锰(Mn)、砷(As)和铵(NH)。过滤器中的过程可能包括生物和非生物反应的组合。然而,关于处理不同地下水中成分的微生物群落的信息有限,以及生物氧化 Fe(II)、Mn(II)、As(III)和 NH 是否有助于 SFs 的整体性能的信息也有限。因此,我们分析了 SFs 的去除效率,以及微生物群落及其潜在活性,这些 SFs 以低浓度(3.3μg/L)至高浓度(600μg/L)As 的地下水为食。结果表明,Fe(II)-、Mn(II)-、NH-和 NO-氧化微生物普遍存在,并为 SFs 的性能做出贡献。此外,地下水成分是造成当前微生物群落差异的原因。我们发现:i)所有 SFs 中都存在微需氧的 Fe(II)氧化,在以低 As 和高 Fe 地下水为食的 SFs 中含量最高,ii)所有 SFs 中都是 Hyphomicropbiaceae 作为主要的 Mn(II)-氧化菌,iii)As 被形成的 Fe 和 Mn(氢)氧化物矿物固定,iv)氨氧化古菌(AOA)进行硝化作用,然后是亚硝酸盐氧化细菌(NOB),v)出乎意料的是,存在大量甲烷单加氧酶基因(pmoA),表明微生物甲烷氧化发生在 SFs 中。总体而言,我们的研究揭示了用于净化砷污染地下水的 SFs 中的多样微生物群落,我们的数据表明微生物活性对 SFs 中的关键功能过程有重要贡献。