[Spatiotemporal Characteristics of Dissolved Oxygen and Control Mechanism of Hypoxia (Low Oxygen) in the Watershed-Coastal System in Fujian Province].

Ai-Lin Yang, Fang Yang, Shao-Bin Li, Qi-Biao Yu, Neng-Wang Chen
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引用次数: 1

Abstract

Dissolved oxygen is a key parameter to measure water environment quality and ecosystem health. Currently, the problem of hypoxia (low oxygen) is prominent in coastal areas in China, but there is a lack of research on the spatiotemporal characteristics of dissolved oxygen and the control mechanism of hypoxia in the watershed-coastal system. Based on the data of 135 surface water (including estuaries) and 66 coastal water monitoring sites in Fujian Province from 2011 to 2020, this study analyzed the spatiotemporal variation pattern of dissolved oxygen at seasonal and interannual time scales. The data of hypoxia (10% quantile, corresponding to 67% saturation) were selected to study the characteristics and control mechanism of hypoxia in four types of water bodies (i.e., rivers, reservoirs, estuaries, and coastal waters) using mathematical statistics and a random forest model. The results showed that the dissolved oxygen saturation was the highest in the coast[(98.2±10.2)%] and the lowest in the estuary[(79.2±17.9)%]. Compared with that in the 12th Five-Year Plan (2011-2015), the frequency of hypoxia detection in rivers and reservoirs in the 13th Five-Year Plan (2016-2020) was significantly reduced, but the change in estuaries was not significant. Counting the points with hypoxia detection, the multi-year average hypoxia detection frequency of rivers and reservoirs was highest in autumn, and the frequency of estuaries was highest in summer. Hypoxia in reservoirs and estuaries was the most prominent but with different mechanisms. Specifically, hypoxia in reservoir reaches was related to summer runoff carrying large amounts of organic matter input, stratification leading to continuous oxygen depletion in the bottom water, and vertical mixing or discharge through dams in autumn, whereas hypoxia in estuaries was associated with strong pollution inputs and reductive materials. Systematic management and regionalized control mechanisms need to be established to further strengthen watershed-coastal pollution abatement to help mitigate eutrophication and hypoxia problems.

福建流域-海岸系统溶解氧时空特征及缺氧(低氧)控制机制[j]。
溶解氧是衡量水环境质量和生态系统健康的重要指标。目前,中国沿海地区缺氧(低氧)问题比较突出,但对流域-沿海系统溶解氧时空特征及缺氧控制机制的研究还比较缺乏。基于2011 - 2020年福建省135个地表水(含河口)和66个近岸水体监测点的数据,分析了溶解氧在季节和年际时间尺度上的时空变化格局。选取低氧数据(10%分位数,对应67%饱和度),采用数理统计和随机森林模型研究河流、水库、河口、沿海4类水体的低氧特征及控制机制。结果表明:溶解氧饱和度以海岸最高[(98.2±10.2)%],河口最低[(79.2±17.9)%];与“十二五”(2011-2015年)相比,“十三五”(2016-2020年)江河、水库缺氧检测频次明显减少,河口缺氧检测频次变化不显著。从低氧检测点来看,河流和水库的多年平均低氧检测频率在秋季最高,河口的低氧检测频率在夏季最高。水库和河口缺氧最为突出,但机制不同。具体而言,水库河段缺氧与夏季径流携带大量有机物输入、分层导致底层水体持续缺氧以及秋季通过大坝垂直混合或排放有关,而河口缺氧与强污染输入和还原性物质有关。需要建立系统管理和区域化控制机制,进一步加强流域-沿岸污染治理,帮助缓解富营养化和缺氧问题。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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