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中国江汉平原第四纪沉积物中的铵和硝酸盐来源及转化机制。

Ammonium and nitrate sources and transformation mechanism in the Quaternary sediments of Jianghan Plain, China.

机构信息

School of Environmental Studies, China University of Geosciences, Wuhan 430078, China.

School of Environmental Studies, China University of Geosciences, Wuhan 430078, China.

出版信息

Sci Total Environ. 2021 Jun 20;774:145131. doi: 10.1016/j.scitotenv.2021.145131. Epub 2021 Feb 9.

Abstract

Excessive inorganic nitrogen (IN) compound content in groundwater is generally attributed to anthropogenic activities. Here, natural nitrogen sources in Quaternary sediments from aquifers and aquitards of Jianghan Plain (JHP), China were identified. Ammonium and nitrate content in groundwater samples collected from 129 well sites were determined through chemical analysis. Subsequent 4 boreholes were drilled at areas with high nitrogen concentration in the Quaternary aquifer. Indicators from hydrochemistry and soil geochemistry analysis, as well as optically stimulated luminescence dating and various of radioactive isotope δC-CO and stable isotopes including δN-NH, δN-total organic nitrogen (TON), δN-NO, δO-NO, δO-HO, δD-HO, and δC-total organic carbon (TOC) were used to identify high-concentration N compound sources and transformation mechanisms (NO: 0.02-770 mg L; NH-N: 0-30.5 mg L) in the porous media. The thick clay layer protected the underlying media. Paleo-precipitation characteristics were preserved in the porewater; that is, it had not been affected by anthropogenic activities. The high nitrate concentration in the shallow oxidized aquifer was mostly attributed to manure and sewage (δN-NO was 14‰). The ammonium-N in the deep strata and part of ammonium-N in the shallow strata (aquifers and aquitards) were from natural sources, mainly from natural TON mineralization. Adsorption was an auxiliary factor for ammonium enrichment in the shallow strata, as were dissimilatory nitrate reduction to ammonium (DNRA) and low ammonia volatilization. Organic matter (OM) involved in mineralization was a mixture of lacustrine algae and terrigenous clastic sediments (from river upstream). The algae were traced to lake formation and frequent evolutionary changes in river environments, as indicated by alterations in sedimentary facies. The present findings may encourage researchers to consider natural IN sources' contribution to N contamination using quantitative models. They also serve as a valuable reference for understanding other pollutants' transformation mechanism in similar environments and provide research ideas for similar areas.

摘要

地下水中超量的无机氮(IN)化合物含量通常归因于人为活动。本研究在中国江汉平原含水层和隔水层的第四纪沉积物中确定了自然氮源。通过化学分析测定了从 129 个井位采集的地下水样本中的铵和硝酸盐含量。随后在第四纪含水层中高氮浓度区域钻了 4 个钻孔。水化学和土壤地球化学分析的指标,以及光激发发光测年和各种放射性同位素 δC-CO 和稳定同位素包括 δN-NH、δN-总有机氮(TON)、δN-NO、δO-NO、δO-HO、δD-HO 和 δC-总有机碳(TOC)用于识别多孔介质中高浓度 N 化合物来源和转化机制(NO:0.02-770 mg L;NH-N:0-30.5 mg L)。厚粘土层保护了下面的介质。古降水特征保存在孔隙水中;也就是说,它没有受到人为活动的影响。浅层氧化含水层中高浓度的硝酸盐主要归因于粪肥和污水(δN-NO 为 14‰)。深部地层中的铵-N 和部分浅层地层(含水层和隔水层)中的铵-N 来自自然源,主要来自天然 TON 矿化。吸附是浅层地层中铵富集的辅助因素,同时还有异化硝酸盐还原为铵(DNRA)和低氨挥发。参与矿化的有机物(OM)是湖泊藻类和陆源碎屑沉积物(来自河流上游)的混合物。藻类是湖泊形成和河流环境频繁演化变化的标志,这反映在沉积相的变化上。本研究结果可能鼓励研究人员使用定量模型考虑自然 IN 来源对 N 污染的贡献。它们也为理解类似环境中其他污染物的转化机制提供了有价值的参考,并为类似地区提供了研究思路。

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