长江科学院院报 ›› 2018, Vol. 35 ›› Issue (10): 30-35.DOI: 10.11988/ckyyb.20170189

• 水资源与环境 • 上一篇    下一篇

变化环境下通江湖泊江水倒灌年内分配变化规律研究

许斌1, 陈广才1,2   

  1. 1.长江科学院 水资源综合利用研究所,武汉 430010;
    2.长江水利委员会规划计划局,武汉 430010
  • 收稿日期:2017-02-27 出版日期:2018-10-01 发布日期:2018-10-22
  • 通讯作者: 陈广才(1981-),男,湖北汉川人,高级工程师,博士,主要研究方向为变化环境下的水文水资源。E-mail:cgc07@163.com
  • 作者简介:许 斌(1985-),男,河南焦作人,工程师,博士,主要研究方向为变化环境下的水文水资源。E-mail:taibaidugu@163.com
  • 基金资助:
    国家重点研发计划项目(2017YFC0405304);国家自然科学基金项目(51809009,51409014);中央级公益性科研院所基本科研业务费资助项目(20150914091245)

Inner-annual Allocations of Backward Flow ofRiver-connected Lake in Changing Environment

XU Bin1, CHEN Guang-cai1,2   

  1. 1.Water Resources Department, Yangtze River Scientific Research Institute, Wuhan 430010, China;
    2.Planning Bureau of Changjiang Water Resources Commission, Wuhan 430010, China
  • Received:2017-02-27 Published:2018-10-01 Online:2018-10-22

摘要: 长江中下游的通江湖泊具有调蓄洪水和涵养水源等重要作用,针对目前通江湖泊分析中将三峡工程作为节点又缺乏支撑性分析的情况,以及对变化环境下江水倒灌年内分配变化规律研究较少的问题,以鄱阳湖为研究对象,采用水文变异诊断系统对鄱阳湖湖口站水位进行变异诊断,并以诊断结果为依据对湖口站实测倒灌序列进行变异前后年内分配变化规律研究。结果显示:变异后汛期鄱阳湖江水倒灌的流量均值上升,但月平均倒灌天数减少,倒灌水量呈减少的态势,且倒灌流量的极值有较大幅度降低,有利于鄱阳湖的防洪安全;非汛期江水倒灌的流量均值、平均天数、流量极值比变异前总体大幅度下降,对于鄱阳湖枯期水位会有较大的影响。研究结果对变化环境下通江湖泊的水情分析具有一定的参考作用。

关键词: 环境变化, 倒灌流量, 水位, 年内分配, 鄱阳湖

Abstract: River-connected lakes in the midstream and downstream of Changjiang River have functions of flood storage and water resources conservation. With the Three Gorges Project as node, current research on river-connected lakes in the midstream and downstream of Changjiang River is in lack of supportive analysis. Research on the annual evolution of backward flow in river-connected lakes under changing environment is insufficient as well. In view of this, the backward flow measured at Hukou Station, Poyang Lake was divided into the series before alteration point and the series after alteration point to study the inner-annual allocation of backward flow. Hydrological Alteration Diagnose System was adopted to analyze the water level series of Hukou Station to uncover the alteration point. Results show that despite increased monthly mean backward flow rate after alteration point, the duration and backflow flow volume both decreased, and the extreme value of backward flow declined dramatically, which was conducive to the safety of flood control of Poyang Lake. The monthly mean backward flow rate, duration, and extreme value of backward flow rate in non-flood season were greatly smaller than those before the alteration point, posing large impact on the water level of Poyang Lake in dry season. The results offer reference for analyzing the water regime of river-connected lakes in changing environment.

Key words: changing environment, backward flow rate, water level, inner-annual allocation, Poyang Lake

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