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洞庭湖出口径流变化及对生态系统的影响
引用本文:程俊翔,徐力刚,姜加虎,朱乾德,于丹丹.洞庭湖出口径流变化及对生态系统的影响[J].长江流域资源与环境,2019,28(5):1225-1234.
作者姓名:程俊翔  徐力刚  姜加虎  朱乾德  于丹丹
作者单位:中国科学院南京地理与湖泊研究所,中国科学院流域地理学重点实验室,江苏南京210008;中国科学院大学,北京100049;南京水利科学研究院,水文水资源与水利工程科学国家重点实验室,江苏南京210029;生态环境部南京环境科学研究所,江苏南京,210042
基金项目:中国科学院战略性先导科技专项;国家重点实验室开放基金;国家自然科学基金;国家自然科学基金;流域水循环模拟与调控国家重点实验室开放基金
摘    要:为了阐明洞庭湖出口径流变化及生态效应,根据城陵矶1960~2016年的日径流量数据,采用生态盈余和生态赤字两个生态径流指标,分别从年和季节尺度分析了洞庭湖出口径流变化,并讨论了其对洞庭湖生态系统的影响。研究结果表明:年生态盈余和年生态赤字的变化范围分别为0~0.39和0~0.47,且年生态赤字比年生态盈余的波动更加剧烈和频繁;季节生态径流指标差异较大,春季和冬季生态盈余波动比较频繁,夏季和秋季生态盈余变化不大;除冬季外,春季、夏季和秋季生态赤字在水文变异后呈明显上升趋势,且高于生态盈余;季节生态变化总值整体呈上升趋势,且在水文变异后更加离散,表明生态系统受到了较大的扰动。气候变化和人类活动是导致径流变异的主要影响因素。降水对生态赤字的影响较大;人类活动导致了高流量减少、低流量增加,使季节生态径流指标发生较大改变。径流变化与生态系统关系的基本准则表明,洞庭湖出口径流与生态系统具有紧密的联系,且径流改变对生态系统产生了负面影响。

关 键 词:洞庭湖  径流  生态盈余  生态赤字  生态系统影响

Changes in Streamflow at the Outlet of Dongting Lake and Their Impacts on Ecosystems
CHENG Jun-xiang,XU Li-gang,JIANG Jia-hu,ZHU Qian-de,YU Dan-dan.Changes in Streamflow at the Outlet of Dongting Lake and Their Impacts on Ecosystems[J].Resources and Environment in the Yangtza Basin,2019,28(5):1225-1234.
Authors:CHENG Jun-xiang  XU Li-gang  JIANG Jia-hu  ZHU Qian-de  YU Dan-dan
Institution:(1. Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; 2. University of Chinese Academy of Sciences, Beijing 100049, China; 3. State Key Laboratory of Hydrology Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China; 4. Nanjing Institute of Environmental Sciences, Ministry of Ecology and Environment, Nanjing 210042, China)
Abstract:Based on the daily streamflow data of Chenglingji station from 1960 to 2016, two eco-flow metrics, ecosurplus and ecodeficit, were used to evaluate the changes in streamflow and their related ecological effects at the outlet of Dongting Lake. Both annual and seasonal eco-flow metrics were analyzed and the ecosystem influences were also discussed. The results indicated that the average annual ecosurplus and ecodeficit fell in the range of 0-0.39 and 0-0.47, respectively, and the annual ecodeficit had a more frequent fluctuation than the annual ecosurplus. Changes of seasonal eco-flow metrics differed greatly. Ecosurplus had frequent fluctuations in spring and winter, while had no significant fluctuations in summer and autumn. Seasonal ecodeficit showed an increased trend in all seasons except for winter, and were higher than the values of seasonal ecosurplus. The total seasonal ecochange increased during the whole period, and became more discrete during the post-impact period, which indicated a severely disturbance on the ecosystem. Climate change and human activities are two main factors of the eco-flow alteration at the outlet of Dongting Lake. Furthermore, precipitation had greater impact on ecodeficit. Human activities may lead to a large alteration of seasonal eco-flow metrics, through reducing high flow and increasing low flow. According to the four basic principles of flow regimes and ecosystems, Streamflow of Dongting Lake outlet had a close relationship with the ecosystems, and streamflow alteration had negative impacts on the ecosystems.
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