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Molecular and Dual-Isotopic Profiling of the Microbial Controls on Nitrogen Leaching in Agricultural Soils under Managed Aquifer Recharge

[Image: see text] Nitrate (NO(3)(–)) leaching is a serious health and ecological concern in global agroecosystems, particularly those under the application of agricultural-managed aquifer recharge (Ag-MAR); however, there is an absence of information on microbial controls affecting NO(3)(–) leaching...

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Detalles Bibliográficos
Autores principales: Huang, Laibin, Levintal, Elad, Erikson, Christian Bernard, Coyotl, Adolfo, Horwath, William R., Dahlke, Helen E., Mazza Rodrigues, Jorge L.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Chemical Society 2023
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10399200/
https://www.ncbi.nlm.nih.gov/pubmed/37467434
http://dx.doi.org/10.1021/acs.est.3c01356
Descripción
Sumario:[Image: see text] Nitrate (NO(3)(–)) leaching is a serious health and ecological concern in global agroecosystems, particularly those under the application of agricultural-managed aquifer recharge (Ag-MAR); however, there is an absence of information on microbial controls affecting NO(3)(–) leaching outcomes. We combine natural dual isotopes of NO(3)(–) ((15)N/(14)N and (18)O/(16)O) with metagenomics, quantitative polymerase chain reaction (PCR), and a threshold indicator taxa analysis (TITAN) to investigate the activities, taxon profiles, and environmental controls of soil microbiome associated with NO(3)(–) leaching at different depths from Californian vineyards under Ag-MAR application. The isotopic signatures demonstrated a significant priming effect (P < 0.01) of Ag-MAR on denitrification activities in the topsoil (0–10 cm), with a 12–25-fold increase of (15)N–NO(3)(–) and (18)O–NO(3)(–) after the first 24 h of flooding, followed by a sharp decrease in the enrichment of both isotopes with ∼80% decline in denitrification activities thereafter. In contrast, deeper soils (60–100 cm) showed minimal or no denitrification activities over the course of Ag-MAR application, thus resulting in 10–20-fold of residual NO(3)(–) being leached. Metagenomic profiling and laboratory microcosm demonstrated that both nitrifying and denitrifying groups, responsible for controlling NO(3)(–) leaching, decreased in abundance and potential activity rates with soil depth. TITAN suggested that Nitrosocosmicus and Bradyrhizobium, as the major nitrifier and denitrifier, had the highest and lowest tipping points with regard to the NO(3)(–) changes (P < 0.05), respectively. Overall, our study provides new insight into specific depth limitations of microbial controls on soil NO(3)(–) leaching in agroecosystems.