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黄河典型支流地表水与地下水中的水化学演化及硝酸盐来源、迁移与转化

Hydrochemical evolution and nitrate sources, migration, and transformation in surface water and groundwater of a typical tributary of the Yellow River.

作者信息

Tong Hui, Gao Ruizhong, Yue Chang, Xie Longmei, Duan Limin, Zhu Yi, Wang Guoqiang

机构信息

Water Conservancy and Civil Engineering College, Inner Mongolia Agricultural University, Hohhot, 010018, China; Autonomous Region Collaborative Innovation Center for Integrated Management of Water Resources and Water Environment in the Inner Mongolia Reaches of the Yellow River, Hohhot, 010018, China; Inner Mongolia Key Laboratory of Ecohydrology and High-Efficient Utilization of Water Resources, College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot, 010018, China.

Water Conservancy and Civil Engineering College, Inner Mongolia Agricultural University, Hohhot, 010018, China; Autonomous Region Collaborative Innovation Center for Integrated Management of Water Resources and Water Environment in the Inner Mongolia Reaches of the Yellow River, Hohhot, 010018, China; Inner Mongolia Key Laboratory of Ecohydrology and High-Efficient Utilization of Water Resources, College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot, 010018, China.

出版信息

J Environ Manage. 2025 Aug;390:126218. doi: 10.1016/j.jenvman.2025.126218. Epub 2025 Jun 21.

Abstract

Nitrate pollution poses a severe threat to ecological security and the sustainable utilization of water resources. Accurately identifying its sources and transformation processes is crucial for water quality protection. This study investigated the hydrochemical evolution, nitrate sources, and transformation mechanisms in surface water and groundwater within the Dahei River Basin, a typical tributary of the Yellow River, across wet and dry seasons. A comprehensive approach integrating hydrochemical analysis, nitrogen-oxygen stable isotope techniques, and the MixSIAR model framework was employed. The results indicated that the water bodies in the study area were weakly alkaline freshwater, with hydrochemical characteristics primarily classified as the HCO-Ca·Mg type. The major hydrochemical ions were governed by silicate and evaporite weathering, with additional influence from cation exchange processes. Nitrate formation was mainly driven by nitrification, while denitrification played a minor role. Quantitative source apportionment using MixSIAR revealed that the dominant sources of nitrate, in descending order of contribution, were manure and sewage wastes (MS), soil organic nitrogen (SON), chemical fertilizers (CF), and atmospheric precipitation (AP). MS accounted for the largest proportion, contributing 32.4 % to surface water and 24.6 % to groundwater during the wet season, and 28.2 % to surface water and 33.5 % to groundwater during the dry season. Its impact was particularly pronounced in urban and agricultural areas, with a notable accumulation effect in groundwater during the dry season. This study highlights the pronounced spatiotemporal variations in nitrate sources and provides scientific guidance for developing region-specific pollution prevention and control strategies in urban, agricultural, and hilly regions. The findings also offer a valuable reference for water quality management in similar watersheds.

摘要

硝酸盐污染对生态安全和水资源的可持续利用构成了严重威胁。准确识别其来源和转化过程对于水质保护至关重要。本研究调查了黄河典型支流大黑河流域地表水和地下水在湿季和干季的水化学演化、硝酸盐来源及转化机制。采用了综合水化学分析、氮氧稳定同位素技术和MixSIAR模型框架的方法。结果表明,研究区水体为弱碱性淡水,水化学特征主要为HCO-Ca·Mg型。主要水化学离子受硅酸盐和蒸发岩风化作用控制,阳离子交换过程也有一定影响。硝酸盐的形成主要由硝化作用驱动,反硝化作用作用较小。利用MixSIAR进行的定量源解析表明,硝酸盐的主要来源按贡献大小依次为粪便和污水废物(MS)、土壤有机氮(SON)、化肥(CF)和大气降水(AP)。MS占比最大,在湿季对地表水的贡献率为32.4%,对地下水的贡献率为24.6%;在干季对地表水的贡献率为28.2%,对地下水的贡献率为33.5%。其影响在城市和农业地区尤为明显,在干季地下水中有明显的累积效应。本研究突出了硝酸盐来源的显著时空变化,为制定城市、农业和山区特定区域的污染防治策略提供了科学指导。研究结果也为类似流域的水质管理提供了有价值的参考。

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