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[三峡水库汉丰湖蓄水前水文水质变化特征]

[Hanfeng Pre-reservoir Commissioning Time Variation Feature of the Hydrology and Water Quality in Three Gorges Reservoir].

作者信息

Yang Bing, He Bing-Hui, Wang De-Bao

机构信息

Key Laboratory of Eco-environments in the Three Gorges Reservoir Region, Ministry of Education, College of Resources and Environment, Southwest University, Chongqing 400715, China.

出版信息

Huan Jing Ke Xue. 2017 Apr 8;38(4):1366-1375. doi: 10.13227/j.hjkx.201607173.

Abstract

Hanfeng Pre-reservoir is very rare in the world which is specially designed to reduce the impact of Fluctuating Zone, and it is formed in Hanfeng Lake of Three Gorges reservoir. The Hanfeng Pre-reservoir has many special hydrological characteristics and ecological environment features based on its unique "pre-reservoir" control mode, the wide seasonal wetland of Fluctuating Zone, the huge life pollution and agricultural pollution, and the pressure of huge city and excessive population. HanFeng Lake has a variety of morphological features such as lakes, rivers, and other backwater bay, for the effect of water level regulation in Three Gorges, since the successful commissioning of the Hanfeng Lake pre-dam system in 2015. The change of Hanfeng Lake hydrology and water quality during the commissioning was divided into four periods by combining Hydrological and Morphological Variation characteristics with Water quality indicators time clustering analysis:May to August as T1 (river period); January, March and November to December as T2 (lake period); February, April and September as T3 (water level fluctuation period); October as T4 (algal blooms period) in 2015. Principal component analysis and stepwise regression analysis showed that Eutrophication of Hanfeng Lake was dominated by different dominant components at different times and the water quality index factor which has a significant effect on the Chl-a was also different. Cumulative contribution rates of principal components were 82.93%, 77.61%, 78.32%, 88.40% for each period, respectively. The main water quality indicators of T1 (river period) were DP, TP, SD, pH and the significant influencing index of Chl-a was PC, so Chl-a was mainly affected by water nitrogen content. The main water quality indicators of T2 (lake period) were TN, DN, DP, TP, NO-N and the significant influencing index of Chl-a was PC, so Chl-a was mainly affected by water eutrophication including nitrogen and phosphorus nutrient status. The main water quality indicators of T3 (water level fluctuation period) were SD, NH-N, DN, and the significant influencing index of Chl-a was PC. so Chl-a was mainly affected by water level fluctuation. The main water quality indicators of T4 (algal blooms period) were TN, DN, DO, NH-N, pH, permanganate index, , NO-N and the significant influencing index of Chl-a was PC. so Chl-a was mainly affected by flow rate and hydrodynamic conditions. As mentioned in the review, the frequent and significant water level changes during the commissioning of Hanfeng Lake were the important factors influencing the change of hydrological and water quality characteristics.

摘要

汉丰湖前置库在世界上极为罕见,它是专门为减轻消落带影响而设计的,形成于三峡水库的汉丰湖中。基于其独特的“前置库”控制模式、消落带广阔的季节性湿地、巨大的生活污染和农业污染以及大城市和过多人口带来的压力,汉丰湖前置库具有许多特殊的水文特征和生态环境特点。自2015年汉丰湖大坝前系统成功调试以来,受三峡水位调节影响,汉丰湖呈现出湖泊、河流及其他回水湾等多种形态特征。结合水文形态变化特征与水质指标时间聚类分析,将2015年汉丰湖调试期间的水文和水质变化分为四个时期:5月至8月为T1(河流期);1月、3月以及11月至12月为T2(湖泊期);2月、4月和9月为T3(水位波动期);10月为T4(水华期)。主成分分析和逐步回归分析表明,汉丰湖不同时期的富营养化主导成分不同,对叶绿素a有显著影响的水质指标因子也不同。各时期主成分累积贡献率分别为82.93%、77.61%、78.32%、88.40%。T1(河流期)的主要水质指标为溶解性总磷(DP)、总磷(TP)、透明度(SD)、pH值,对叶绿素a有显著影响的指标为总磷(PC),因此叶绿素a主要受水体氮含量影响。T2(湖泊期)的主要水质指标为总氮(TN)、溶解性总氮(DN)、DP、TP、亚硝酸盐氮(NO-N),对叶绿素a有显著影响的指标为PC,所以叶绿素a主要受包括氮磷营养状况在内的水体富营养化影响。T3(水位波动期)的主要水质指标为SD、氨氮(NH-N)、DN,对叶绿素a有显著影响的指标为PC,因此叶绿素a主要受水位波动影响。T4(水华期)的主要水质指标为TN、DN、溶解氧(DO)、NH-N、pH值、高锰酸盐指数、亚硝酸盐氮(NO-N),对叶绿素a有显著影响的指标为PC,所以叶绿素a主要受流速和水动力条件影响。如综述中所述,汉丰湖调试期间频繁且显著的水位变化是影响水文和水质特征变化的重要因素。

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