长江科学院院报 ›› 2021, Vol. 38 ›› Issue (7): 7-13.DOI: 10.11988/ckyyb.20200599

• 江湖泥沙与治理 • 上一篇    下一篇

变化环境下长江上游珍稀特有鱼类国家级自然保护区干流水沙过程演变分析

吴华莉1,2, 金中武1,2, 周银军1,2, 李志晶1,2   

  1. 1.长江科学院 河流研究所,武汉 430010;
    2.长江科学院 水利部长江中下游河湖治理与防洪重点实验室,武汉 430010
  • 收稿日期:2020-06-19 修回日期:2020-10-11 出版日期:2021-07-01 发布日期:2021-07-08
  • 通讯作者: 金中武(1976-),男,湖北崇阳人,教授级高级工程师,博士,主要从事河流泥沙及治河工程研究。E-mail:zhongwujin@163.com
  • 作者简介:吴华莉(1985-),女,湖北襄阳人,高级工程师,硕士,主要从事河流泥沙及河流生态相关研究。E-mail:wuhuali1102@whu.edu.cn
  • 基金资助:
    国家自然科学基金青年基金项目(51809013);国家重点研发计划项目(2018YFF0212201,2016YFC0502201)

Evolution of Water and Sediment Processes in the Mainstream of National Nature Reserve for Rare and Endemic Fishes in the Upper Reaches of the Yangtze River under Changing Environment

WU Hua-li1,2, JIN Zhong-wu1,2, ZHOU Yin-jun1,2, LI Zhi-jing1,2   

  1. 1. River Department, Yangtze River Scientific Research Institute, Wuhan 430010, China;
    2. Key Laboratory of River Lake Regulation and Flood Control for the Middle and Lower Reaches of Yangtze River under Ministry of Water Resources, Yangtze River Scientific Research Institute, Wuhan 430010, China
  • Received:2020-06-19 Revised:2020-10-11 Published:2021-07-01 Online:2021-07-08

摘要: 为了研究环境变化对长江上游珍稀特有鱼类国家级自然保护区河段干流水文过程的影响,运用双累积曲线法和数理统计方法对向家坝水文站和朱沱水文站长时间实测水沙数据进行分析。结果表明:①保护区河段干流年径流量无明显下降趋势,年输沙量则呈明显减少趋势;②径流量和输沙量相关性在1998年和2012年出现明显突变,在突变点为分界点的3个时段(建站至1997年、1999—2011年、2013年以后),向家坝站水沙拟合系数R2分别为0.999、0.996、0.989 5,朱沱站水沙拟合系数R2分别为0.999 6、0.995 6、0.983 6;③在鱼类产卵期3—7月份以及11—12月份,流量均值及峰值明显改变,以3月份为例,以突变点为分界点的3个时段对比分析显示,向家坝站日平均流量分别增加了34.3%、58.5%,朱沱站日均流量分别增加了16.1%、21.1%,此外,蓄水运用后多数月份日均流量变化幅度明显大于水库建设过程中。研究成果可为长江上游河道生境修复及梯级水库生态调度提供理论依据。

关键词: 水沙演变, 梯级水库, 国家级自然保护区, 产卵期, 河道生境修复, 生态调度, 长江上游

Abstract: The impacts of environmental changes on hydrologic processes in the mainstream of national nature reserve for rare and endemic fishes in the upper reaches of the Yangtze River are analyzed based on long series of measured water and sediment data at Xiangjiaba and Zhutuo hydrologic stations by double cumulative curve method and mathematical statistics method. Results suggest that annual runoff of the mainstream in the protected area saw no obvious downcut, but annual sediment discharge slipped sharply. The correlation between runoff and sediment discharge changed abruptly in 1998 and 2012; in the three time periods divided by the abrupt changes, the correlation coefficient R2 is 0.999, 0.996 and 0.989 5 for Xiangjiaba station respectively and 0.999 6, 0.995 6 and 0.983 6 for Zhutuo station respectively. In fish spawning period from March to July and from November to December, the mean value and peak value of flow in the study area changed significantly. Take March for example, the average daily flow in the aforementioned three time periods at Xiangjiaba station increased by 34.3% and 58.5% respectively, and 16.1% and 21.1% respectively at Zhutuo station. In addition, the changes average daily of flow in most months after impoundment are more extensive than those during reservoir construction. The research findings offer theoretical basis for river habitat restoration and ecological dispatch of cascade reservoirs.

Key words: water and sediment process, cascade reservoirs, national nature reserve, spawning period, habitat restoration, ecological scheduling, upper reaches of Yangtze River

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