机构地区:[1]北京师范大学环境学院,水环境模拟国家重点实验室,北京100875 [2]环境保护部东北环境保护督查中心,沈阳110014
出 处:《生态学报》2011年第23期7218-7226,共9页Acta Ecologica Sinica
基 金:国家自然科学基金项目(50909004),国家自然科学基金重点资助项目(50939001);国家水体污染控制与治理科技重大专项(2008ZX07209-009);高等学校博士学科点专项科研基金(20090003120014)
摘 要:水是湿地生态系统最重要的影响因子,生态需水核算是对湿地进行生态保护,恢复重建的前提与基础。提出一种基于生态系统受扰动程度评价的适宜生态需水量计算方法。首先根据湿地水面面积变化率最大时对应的关键水位构建初始生态水位方案并将其离散得到一系列离散值;然后应用Mann-Kendall(M-K)法分析历史水位时间序列,找出水位发生突变前自然条件下的水位状态;最后对不同情景水位方案与自然水位状态的差异程度进行修正水文指数(APPFD)评价,确定生态系统受扰动程度在可接受范围之内的多个生态水位方案,进而确定相对应的生态需水量方案。将该方法应用于白洋淀湿地得出了7种可接受的生态水位方案,其中汛期的适宜生态水位在8.31—10.62 m之间,非汛期的适宜生态水位在7.51—9.60 m之间,全年的适宜生态需水量在3.10×108—6.47×108m3之间。该方法能够为实际的水资源管理和分配提供多种备选方案,有较强的实用性和可操作性。Hydrological regime is the driving factor degradation of wetlands. Assessment of ecological in wetland ecosystems. Its excessive alteration will lead to severe water demands is essential for wetland protection, recovery and restoranon. To solve the existing problems arose in the traditional methods such as simple interval range and lack ecological information, in this paper a new method was developed to determine wetlands' appropriate ecological water demands. This method can maintain the resultant hydrological regime alteration within ecologically acceptable threshold. Firstly, the key water level was determined by analyzing the water level-area curve, and a series of discrete initial water level scenarios were generated based on the preliminary water level. Then, to identify the natural water level condition in a wetland, the time series of historical water level were analyzed by using the Mann-Kendall approach. A hydrological alteration assessment indicator, amended annual proportional flow deviation (AAPFD) , was recommended to quantify the hydrological differences between the generated discrete initial water level scenarios and the identified natural water level condition. Each generated discrete initial water level scenarios was evaluated according to its corresponding AAPFD value. Finally, several appropriate ecological water level schemes were identified, which can ensure the corresponding hydrological alteration degree within the ecologically acceptable threshold, and their corresponding ecological water demands can be determined. We applied the proposed method to the Baiyangdian Wetland, the largest shallow lake and wetland complex in the North China Plain, which is now seriously suffered from water crisis. The key water levels were 7.5 m in dry periods ( October to May) and 8.3 m in wet periods (June to September). Seven initial water level scenarios were set up depending on the disperse results of the preliminary water level and actual status of water resources. Hydrological regime befo
关 键 词:关键水位 适宜生态需水量 AAPFD指数 白洋淀湿地
分 类 号:X171[环境科学与工程—环境科学] TV213.4[水利工程—水文学及水资源]
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