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近60年西洞庭湖生态水位研究

Ecological water level of West Dongting Lake in the past 60 years

  • 摘要: 生态水位是判断湖泊健康的重要指标,西洞庭湖是洞庭湖生态体系的重要组成部分。为了科学识别西洞庭湖生态水位演变特征及影响因素,本研究收集石龟山、牛鼻滩、小河咀和南咀4个水文站近60 a的逐日水位数据,采用IHA-RVA法和年内展布法,计算了生态水位及其保障率,对高、低水位发生时间和历时进行了分析。研究结果表明,受澧水和沅水梯级建设的影响,石龟山站、牛鼻滩站水位突变时间分别为1985年和1992年;小河咀站、南咀站水位突变时间为2003年。4个水文站适宜生态水位、最小生态水位年保障率均呈下降趋势,其中澧水尾闾的石龟山站下降最显著,适宜生态水位保障率由47.21%下降到28.32%,最小生态水位保障率由78.50%下降到48.78%。石龟山站和沅水尾闾的牛鼻滩站的高水位发生时间推后,历时缩短,低水位发生时间提前,历时增长;南咀站和小河咀站低水位发生时间提前,历时增长,高水位发生时间推后,历时缩短。本研究对西洞庭湖生态水位保障度及历时的变化特征开展分析,可以为西洞庭湖生态系统健康评估和生物多样性研究提供参考。

     

    Abstract: The ecological water level serves as a crucial indicator for assessing the health of lakes. Xidongting Lake is a significant component of the Dongting Lake ecosystem. To scientifically identify the evolutionary characteristics and influencing factors of the ecological water level in Xidongting Lake, this study collected daily water level data from four hydrological stations: Shiguishan, Niubitan, Xiaohekou, and Nanchu, spanning over the past 60 years. The IHA-RVA method and intra-annual distribution method were employed to calculate both the ecological water level and its guarantee rate; additionally, an analysis was conducted on the occurrence time and duration of high and low water levels. The research findings indicate that due to the construction of cascade hydropower stations along the Li River and Yuan River, abrupt changes in water levels at Shiguishan Station occurred in 1985, while those at Niubitan Station were noted in 1992. Furthermore, abrupt changes in water levels at Xiaohekou Station and Nanchu Station were observed in 2003. The annual guarantee rates for both the suitable ecological water level and the minimum ecological water level at the four hydrological stations exhibit a downward trend, with the most pronounced changes observed at the Shiguishan Station located in the lower reaches of the Li River. Specifically, the guarantee rate for the suitable ecological water level has decreased from 47.21% to 28.32%, while that for the minimum ecological water level has declined from 78.50% to 48.78%. At both Shiguishan Station and Niubitan Station in the lower reaches of the Yuan River, there has been a postponement in high water levels along with a reduction in their duration; conversely, low water levels have occurred earlier and persisted longer. Similarly, at Nanju Station and Xiaheju Station, low water levels have also advanced in occurrence time and increased in duration, whereas high water levels have been delayed and shortened in duration. This study examines water levels in West Dongting Lake, as well as identifying changing characteristics associated with these metrics. The findings aim to provide valuable insights for assessing ecosystem health within West Dongting Lake's lake and wetland environments as well as contributing to research on biodiversity within these ecosystems.

     

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