黄河小北干流水量和水质的时空变化及污染物通量特征

IF 3 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Water Pub Date : 2024-09-15 DOI:10.3390/w16182616
Zhenzhen Yu, Xiaojuan Sun, Li Yan, Yong Li, Huijiao Jin, Shengde Yu
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引用次数: 0

摘要

小北主流位于黄河中游,在调节河水水质方面发挥着重要作用。我们的研究利用了 73 年(1951-2023 年)的水文数据,调查了小北主流及其两条主要支流(渭河和汾河)的长期径流趋势和季节变化。结果表明,随着时间的推移,径流量明显减少,年际波动显著,年内径流分布不均。渭河和汾河的径流分别占主流径流总量的 19.75% 和 3.59%。我们在小北河调查河段的 11 个地点进行了实地监测,评估了 8 项水质参数(温度、pH 值、溶解氧、化学需氧量、氨氮、总磷、高锰酸盐指数和 5 天生化需氧量)。长期监测结果表明,监测期间小北主流水质总体为 III 类。与主流相比,渭河和汾河与黄河汇合点的水质参数较高。这些支流汇入主流后,局部断面浓度有所上升,水质参数呈现空间波动。考虑到水量和水质传输的质量通量过程,汾河和卫河每年输入黄河的 NH3-N 分别占 11.5%和 67.1%,TP 分别占 6.8%和 66.18%。这些发现强调了支流污染物负荷的重要性,突出表明迫切需要针对这些支流制定有效的污染管理策略,以改善黄河的整体水质。本研究揭示了小北主流及其支流径流、水质和污染物通量的时空变化,为加强黄河水环境的保护和管理提供了有价值的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatiotemporal Changes in the Quantity and Quality of Water in the Xiao Bei Mainstream of the Yellow River and Characteristics of Pollutant Fluxes
The Xiao Bei mainstream, located in the middle reaches of the Yellow River, plays a vital role in regulating the quality of river water. Our study leveraged 73 years of hydrological data (1951–2023) to investigate long-term runoff trends and seasonal variations in the Xiao Bei mainstream and its two key tributaries, the Wei and Fen Rivers. The results indicated a significant decline in runoff over time, with notable interannual fluctuations and an uneven distribution of runoff within the year. The Wei and Fen Rivers contributed 19.75% and 3.59% of the total runoff to the mainstream, respectively. Field monitoring was conducted at 11 locations along the investigated reach of Xiao Bei, assessing eight water quality parameters (temperature, pH, dissolved oxygen (DO), chemical oxygen demand (COD), ammonia nitrogen (NH3-N), total phosphorus (TP), permanganate index (CODMn), and 5-day biochemical oxygen demand (BOD5)). Our long-term results showed that the water quality of the Xiao Bei mainstream during the monitoring period was generally classified as Class III. Water quality parameters at the confluence points of the Wei and Fen Rivers with the Yellow River were higher compared with the mainstream. After these tributaries merged into the mainstream, local sections show increased concentrations, with the water quality parameters exhibiting spatial fluctuations. Considering the mass flux process of transmission of the quantity and quality of water, the annual NH3-N inputs from the Fen and Wei Rivers to the Yellow River accounted for 11.5% and 67.1%, respectively, and TP inputs accounted for 6.8% and 66.18%. These findings underscore the critical pollutant load from tributaries, highlighting the urgent need for effective pollution management strategies targeting these tributaries to improve the overall water quality of the Yellow River. This study sheds light on the spatiotemporal changes in runoff, water quality, and pollutant flux in the Xiao Bei mainstream and its tributaries, providing valuable insights to enhance the protection and management of the Yellow River’s water environment.
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来源期刊
Water
Water WATER RESOURCES-
CiteScore
5.80
自引率
14.70%
发文量
3491
审稿时长
19.85 days
期刊介绍: Water (ISSN 2073-4441) is an international and cross-disciplinary scholarly journal covering all aspects of water including water science and technology, and the hydrology, ecology and management of water resources. It publishes regular research papers, critical reviews and short communications, and there is no restriction on the length of the papers. Our aim is to encourage scientists to publish their experimental and theoretical research in as much detail as possible. Full experimental and/or methodical details must be provided for research articles. Computed data or files regarding the full details of the experimental procedure, if unable to be published in a normal way, can be deposited as supplementary material.
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