不同水文期“引江济淮”工程(安徽段)溶解性有机质来源解析及关联因素分析
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1.合肥大学生物食品与环境学院;2.安徽省巢湖管理局湖泊生态环境研究院;3.中国科学院南京地理与湖泊研究所湖泊与流域水安全全国重点实验室

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安徽省高校杰出青年科研项目、巢湖生物资源调查研究项目、国家自然科学基金资助项目、安徽高校协同创新项目


Deciphering DOM sources and their controlling factors in the Yangtze-to-Huaihe Water Diversion Project: insights from the Anhui Section across hydrological scenarios
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1.School of Biological Food and Environment,Hefei University;2.Lake Ecological Environment Research Institute of Chaohu Lake Administration Bureau of Anhui Province

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    摘要:

    引江济淮工程作为我国长江下游战略性水利枢纽,兼具缓解淮北水资源短缺、改善巢湖及淮河生态、促进流域可持续发展等多重使命。溶解性有机质(DOM)是评估水体健康状况和污染溯源的重要指标,研究其对流域外调水的响应过程能够精准追踪调水引起的水质变化特征,对优化生态调度策略、保障江淮地区水环境安全具有重要意义。本研究选取引江济淮(安徽段)调水工程中引江济巢和江淮沟通段,系统解析2023年12月试通水至2024年6月首次调水试验期间不同水文期干渠和沿线湖泊水体DOM来源、组成和分布特征,并综合考察其潜在影响因素。结果表明:(1) 在不同水文期水体中TN、氨氮和CODMn浓度呈现枯水期<丰水期<平水期变化趋势,调水后其浓度降低,尤其是受氮污染严重的江淮沟通段,TN浓度由平水期4.00±1.45 mg/L降至丰水期2.06±0.58 mg/L;TP浓度在不同水文期和同一水文期空间上均无明显变化;DOC浓度呈现显著的季节性和空间变化特征,枯水期时在湖泊及其河口中DOC浓度相对较高,而河流段DOC较低。(2)识别出四种DOM荧光组分,分别为C1海洋来源类腐殖质、C2富里酸类腐殖质、C3腐殖酸类腐殖质、C4色氨酸组蛋白质;DOM来源受自生源和陆生源的双重影响;在不同水文期水体中自生源和陆生源有机质占比在季节上无显著变化,调水后由于水量交换DOM荧光强度和DOC浓度的空间分布特征无明显差异。(3) TN、CODMn、DO、Chl-a和WT与DOM的组成和浓度变化具有显著相关性,水温和DO升高对藻类生长和有机物降解具有促进作用,TN浓度的增加导致水体富营养化使得DOM进一步积累。本研究评估了引江济淮(安徽段)实施首次调水后沿线水环境质量状况,揭示了跨流域调水初期DOM的响应规律,基于水质安全角度为引江济淮调水工程实施调度提供科学依据。

    Abstract:

    As a strategic water conservancy project in the lower reaches of the Yangtze River in China, the project has multiple missions such as alleviating the shortage of water resources in Huaibei, improving the ecology of Chaohu Lake and Huaihe River, and promoting the sustainable development of the river basin. Dissolved organic matter (DOM) is an important indicator for assessing the health status of water bodies and tracing pollution sources. Study on its response process to inter-basin water transfers can accurately track the characteristics of water quality changes induced by such transfers, which is of great significance for optimizing ecological scheduling strategies and ensuring water environmental security in the Jiang-huai region. In this study, we selected the Yangtze-Chao section and Yangtze-Huai section in the water diversion project from the Yangtze River to Huaihe River (Anhui section), systematically analysed the source, composition and distribution characteristics of dissolved organic matter (DOM) and its influencing factors in the water diversion project (Anhui section) from the Yangtze River to Huaihe River at the different hydrological periods from December 2023 to June 2024. The results show as follows: (1) the concentration of total nitrogen (TN), ammonia nitrogen and permanganate index (CODMn) in the water bodies during the different hydrological periods showed increasing trends in the dry season, wet season and normal flow season, and their concentrations decreased after water diversion, especially in the Yangtze-Huai section the concentration of TN decreasing from 4.00±1.45 mg/L to 2.06±0.58 mg/L. TP concentration did not change with the spatial and seasonal distributions. DOC concentration showed significant seasonal and spatial variation. During the dry season, the concentrations of DOC in lakes and estuaries were relatively high, while DOC in river section was low. (2) Four DOM fluorescent components were identified, namely marine-derived humus C1, funic acid humic C2, humic acid C3, and tryptophan group proteins C4. DOM was both influenced by autogenic and terrestrial sources. There is no significant seasonal variation in the proportion of autogenic and terrestrial organic matter in the water during different hydrological periods. After water regulation, there is no obvious difference in the spatial distribution characteristics of DOM fluorescence intensity and DOC concentration due to water exchange. (3) TN, CODMn, DO, Chl-a and WT had a significant impact on the composition and concentration of DOM, while the increase of water temperature and DO had a promoting effect on algae growth and degradation of organic matter. The increase of TN concentration led to the eutrophication of water body and the accumulation of DOM. This study evaluated the water environment quality along the Anhui section of the Yangtze-to-Huaihe water diversion project after its initial implementation of water diversion. It reveals the response patterns of DOM in the early stages of inter-basin water transfer and provides a scientific basis for scheduling the water diversion project from a water quality safety perspective.

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  • 收稿日期:2025-03-19
  • 最后修改日期:2025-07-10
  • 录用日期:2025-08-21
  • 在线发布日期: 2025-11-05
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