基于多同位素和Simmr模拟的华北城乡岩溶地下水系统硝酸盐污染源及其转化

IF 5 1区 地球科学 Q2 ENVIRONMENTAL SCIENCES
Jie Zhang, Lin Zhang, Tianyuan Zheng, Menggui Jin, Fengxin Kang, Jinde Jiang, Zhouwei Yuan, Jian Luo
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引用次数: 0

摘要

在人为影响强烈且异质性高的温带喀斯特含水层中,地下水污染追踪主要集中在硝酸盐上,但对共发生铵源的证据不足,影响了氮污染的准确评估。本研究率先将同位素方法应用于济南泉集水区地下水流动框架中,构建了一种新的硝酸铵同位素示踪系统(、、和),用于全形式的水源跟踪,并实施贝叶斯混合模型(Simmr)来定量分配岩溶地下水中的硝酸盐来源。该集成系统能够同时识别NH4+‐N和NO3−−N污染源,增强了关键氮循环途径的分辨率,特别是铵态硝化。NO3−N是岩溶地下水中无机氮的主要形态(0.4 ~ 42.2 mg/L), 1958 ~ 2019年总体呈上升趋势。NH4+‐N和NO3−‐N主要来源于铵肥和土壤氮。Simmr模型量化了铵肥(28.4% ~ 58.3%)和土壤氮(23.1% ~ 62.7%)是地下水NO3−‐N的主要贡献者。水化学和双氮同位素证据表明,土壤氮的矿化和再硝化、铵态肥料的硝化和硝态肥料的矿化-固定化-周转都促进了岩溶地下水中硝酸盐的积累。地下水流量分析表明,浅层和深层岩溶地下水混合是城市排水区泉水硝酸盐衰减的主要机制,反硝化作用可以忽略不计。这些发现为研究温带岩溶地下水中氮的行为提供了新的认识,为类似岩溶系统的水资源管理和保护提供了有价值的指导。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tracing Nitrate Contamination Sources and Transformations in a Rural−Urban Karst Groundwater System in North China Using Multiple Isotopes and Simmr Modeling
In temperate karst aquifers under intensive anthropogenic impacts and high heterogeneity, groundwater contamination tracking has predominantly focused on nitrate, but inadequate evidence for co‐occurring ammonium sources undermines accurate nitrogen pollution assessments. This study pioneered the application of a isotope approach within the groundwater flow framework of the Jinan Spring Catchment, constructed a novel ammonium‐nitrate isotope tracing system (, , and ) for full‐form source tracking, and implemented the Bayesian mixing model (Simmr) to quantitatively apportion nitrate sources in karst groundwater. This integrated system enabled simultaneous NH4+‐N and NO3‐N pollution source identification, enhancing the resolution of key nitrogen cycling pathways, particularly ammonium‐dominated nitrification. The NO3‐N was the dominant form of inorganic nitrogen in karst groundwater (0.4−42.2 mg/L), and demonstrated an overall upward trend from 1958 to 2019. and nitrate isotope both confirmed that NH4+‐N and NO3‐N primarily originated from ammonium fertilizer and soil nitrogen. The Simmr model quantified ammonium fertilizer (28.4%−58.3%) and soil nitrogen (23.1%−62.7%) as primary contributors to groundwater NO3‐N. Hydrochemical and dual nitrogen isotope evidences revealed that mineralization and re‐nitrification of soil nitrogen, nitrification of ammonium fertilizers, and mineralization‐immobilization‐turnover of nitrate fertilizers all promoted nitrate accumulation in karst groundwater. Groundwater flow analysis identified mixing between shallow and deep karst groundwater as the primary mechanism for nitrate attenuation of spring waters in the urban discharge area, with denitrification playing a negligible role. These findings provide new insights into nitrogen behavior in temperate karst groundwater, offering valuable guidance for water resource management and protection in similar karst systems.
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来源期刊
Water Resources Research
Water Resources Research 环境科学-湖沼学
CiteScore
8.80
自引率
13.00%
发文量
599
审稿时长
3.5 months
期刊介绍: Water Resources Research (WRR) is an interdisciplinary journal that focuses on hydrology and water resources. It publishes original research in the natural and social sciences of water. It emphasizes the role of water in the Earth system, including physical, chemical, biological, and ecological processes in water resources research and management, including social, policy, and public health implications. It encompasses observational, experimental, theoretical, analytical, numerical, and data-driven approaches that advance the science of water and its management. Submissions are evaluated for their novelty, accuracy, significance, and broader implications of the findings.
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