多要素协同下长江中下游华阳河湖群全年生态水位过程构建
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长江水利委员会长江科学院

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国家自然科学基金项目(长江水科学研究联合基金重点支持项目(U2240224));长江中下游河湖动态过程及调控创新团队项目(CKSF2024326/HL)


Establishing the annual ecological water level regime for the Huayanghe Lake Complex through Multi-Objective Coordination, middle-lower reaches of the Yangtze River
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Changjiang River Scientific Research Institute

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National Natural Science Foundation of China Project (Key Support Project of the Yangtze River Water Science Research Joint Fund (U2240224)); Innovation Team Project on Dynamic Processes and Regulation of Rivers and Lakes in the Middle and Lower Reaches of the Yangtze River (CKSF2024326/HL)

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    摘要:

    华阳湖群作为长江中下游典型湿地系统,兼具水鸟保护、水文连通、水质净化等核心生态功能,并承担供水、防洪等社会生产保障功能。现有水位调控聚焦单一要素且缺乏全年动态过程线,难以充分支撑其核心生态功能稳定发挥。本文整合近50年水文、地形、水质及生境数据,采用IHA-RVA法、ArcGIS空间分析、水动力—水质模型及生境适宜面积法,构建“水文—形态—水质—生境”多要素协同计算框架,提出满足湖群水文稳定与生态健康的全年最适生态水位过程线。结果表明:最适生态水位11.86 m(4月) ~ 13.53 m(9月),阈值范围11.56 m(3月) ~ 14.87 m(8月),且在时间分布上呈“冬春收敛、夏秋扩张”特征,各季节水位适配生物生境、水文节律及水质改善需求。该方案可保障重点鸟类越冬、水生生物栖息及水质净化目标,为长江中下游同类闸控湖泊或湖群生态水位调控提供科学借鉴。

    Abstract:

    Huayang Lake Complex is a typical wetland system in the middle and lower reaches of the Yangtze River, with core ecological functions including waterbird protection, hydrological connectivity and water quality purification, as well as social production guarantee functions such as water supply and flood control. Current water level regulation focuses on single factors and lacks an annual dynamic process curve, which is difficult to fully support the stable exertion of its core ecological functions. Based on nearly 50 years of hydrological, topographic, water quality and habitat data, this study establishes a multi-factor collaborative calculation framework of “hydrology–morphology–water quality–habitat” by using the IHA-RVA method, ArcGIS spatial analysis, hydrodynamic-water quality model and habitat suitability area method, and proposes an annual optimal ecological water level hydrograph to satisfy the hydrological stability and ecological health of the lake complex. The results show that the optimal ecological water level ranges from 11.86 m (April) to 13.53 m (September), with a threshold range of 11.56 m (March) to 14.87 m (August). It presents a temporal distribution characteristic of "convergence in winter and spring, expansion in summer and autumn", and the seasonal water levels adapt to the demands of biological habitats, hydrological rhythms and water quality improvement. This scheme can guarantee the overwintering of key waterbirds, inhabitation of aquatic organisms and water quality purification, and provide a scientific reference for ecological water level regulation of similar gate-controlled lakes or lake groups in the middle and lower reaches of the Yangtze River.

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历史
  • 收稿日期:2025-10-26
  • 最后修改日期:2026-05-18
  • 录用日期:2026-05-19
  • 在线发布日期: 2026-06-30
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