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水平可渗透反应屏障在快速渗滤进行管理补给期间刺激硝酸盐去除并改变微生物生态。

A horizontal permeable reactive barrier stimulates nitrate removal and shifts microbial ecology during rapid infiltration for managed recharge.

机构信息

Earth and Planetary Sciences, University of California Santa Cruz, Santa Cruz, CA, 95064, USA.

Earth and Planetary Sciences, University of California Santa Cruz, Santa Cruz, CA, 95064, USA.

出版信息

Water Res. 2018 Nov 1;144:274-284. doi: 10.1016/j.watres.2018.07.039. Epub 2018 Jul 17.

Abstract

We present results from field experiments linking hydrology, geochemistry, and microbiology during infiltration at a field site that is used for managed aquifer recharge (MAR). These experiments measured how a horizontal permeable reactive barrier (PRB) made of woodchips impacted subsurface nitrate removal and microbial ecology. Concentrations of dissolved organic carbon consistently increased in infiltrating water below the PRB, but not in un-amended native soil. The average nitrate removal rate in soils below the PRB was 1.5 g/m/day NO-N, despite rapid infiltration (up to 1.9 m/d) and a short fluid residence time within the woodchips (≤6 h). In contrast, 0.09 g/m/day NO-N was removed on average in native soil. Residual nitrate in infiltrating water below the PRB was enriched in δN and δO, with low and variable isotopic enrichment factors that are consistent with denitrification during rapid infiltration. Many putative denitrifying bacteria were significantly enhanced in the soil below a PRB; Methylotenera mobilis and genera Microbacterium, Polaromonas, and Novosphingobium had log fold-changes of +4.9, +5.6, +7.2, and +11.8, respectively. These bacteria were present before infiltration and were not enhanced in native soil. It appears that the woodchip PRB contributed to favorable conditions in the underlying soil for enhanced nitrate removal, quantitatively shifting soil microbial ecology. These results suggest that using a horizontal PRB could improve water quality during rapid infiltration for MAR.

摘要

我们展示了在一个用于管理含水层补给(MAR)的现场进行的水文、地球化学和微生物学渗透实验的结果。这些实验测量了水平可渗透反应屏障(PRB)对地下硝酸盐去除和微生物生态的影响。在 PRB 下方的渗透水中,溶解有机碳的浓度持续增加,但在未改良的原生土壤中没有增加。尽管快速渗透(高达 1.9 m/d)和木材内的短流体停留时间(≤6 h),但 PRB 下方土壤中的平均硝酸盐去除率为 1.5 g/m/天 NO-N。相比之下,原生土壤的平均去除率为 0.09 g/m/天 NO-N。PRB 下方渗透水中残留的硝酸盐在δN 和 δO 中富集,同位素富集因子低且变化大,与快速渗透过程中的反硝化作用一致。许多假定的反硝化细菌在 PRB 下方的土壤中显著增强;甲基营养菌(Methylotenera mobilis)和微杆菌属(Microbacterium)、极性菌属(Polaromonas)和新鞘氨醇单胞菌属(Novosphingobium)的对数折叠变化分别为+4.9、+5.6、+7.2 和+11.8。这些细菌在渗透前就存在,并且在原生土壤中没有增强。似乎木屑 PRB 有助于改善快速渗透 MAR 过程中地下土壤中增强硝酸盐去除的有利条件,定量改变了土壤微生物生态。这些结果表明,使用水平 PRB 可以在 MAR 快速渗透过程中提高水质。

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