长江科学院院报 ›› 2023, Vol. 40 ›› Issue (1): 37-42.DOI: 10.11988/ckyyb.20220824

• 水资源 • 上一篇    下一篇

基于IHA-RAV法的长江源区生态水文情势变化

李光录1, 樊立娟2   

  1. 1.青海省水文水资源测报中心,西宁 810000;
    2.青海省海东市水务局,青海 海东 810600
  • 收稿日期:2022-07-11 修回日期:2022-08-20 出版日期:2023-01-01 发布日期:2023-02-24
  • 通讯作者: 樊立娟(1987-),女,甘肃张掖人,工程师,硕士研究生,主要从事生态流量分析研究。E-mail:Fanlj87@hotmail.com
  • 作者简介:李光录(1970-),男,青海湟中人,高级工程师,主要从事江源水文分析计算研究。E-mail:1035810227@qq.com
  • 基金资助:
    青海省科技计划资助项目(2020-SF-151)

Study on Ecohydrological Regime Change in Headwaters of the Yangtze River by Using Indicators of Hydrologic Alteration and Range of Variability Approach

LI Guang-lu1, FAN Li-juan2   

  1. 1. Qinghai Hydrology and Water Resources Survey and Forecasting Department of Qinghai Province,Xining 810000,China;
    2. Haidong Water Resources Bureau,Haidong 810600,China
  • Received:2022-07-11 Revised:2022-08-20 Online:2023-01-01 Published:2023-02-24

摘要: 为评估长江源区河流水文情势变化及其生态效应,选用长江源区直门达水文站1957—2021年逐日流量资料,使用贝叶斯变点检验方法分析直门达水文站年平均流量突变发生时间,采用水文改变指标变化范围法(IHA-RVA)综合评价直门达水文站在突变点前后改变程度,使用趋势坡度、Kendall趋势检验以及去趋势波动分析法评价月均流量、年极值流量时间序列变化情况。结果表明:①长江源区直门达水文站年平均流量在2004年发生变异。②2004年前后直门达水文站水文综合改变度为37.2%,属于中度改变。③月均流量综合为中度改变,各月流量均有不同程度的增加,增大了河道内水生生物栖息所需水量。④流量极值综合改变度为低度改变,表明极端流量事件处于一个稳定的范围,在一定程度上维持了长江源区生态系统的稳定性;最小流量的增加更好地保障了流域生态流量。⑤极端值出现时间为低改变度,对水生生物栖息地以及鱼类洄游影响较小。⑥高、低流量脉冲频次均为低度改变,反映出长江源区干旱和洪涝发生次数减少,使得长江源区河道、河滩的受水情况趋于稳定;高、低脉冲历时变化又给源区河道及沿岸生态环境带来不确定的影响。⑦流量上升率、下降率及逆转率均为低改变度,反映出长江源区流量改变程度较低,维持在生态系统相对稳定的状态。总体而言,长江源区河道生态环境有转好的趋势,增加的生态流量有利于维持长江源区生物多样性和生态系统的健康可持续发展。

关键词: 长江源区, 生态流量, IHA指标, 水文情势, 水文改变度, 去趋势波动分析

Abstract: The aim of this study is to assess the changes in eco-hydrological regime and its ecological effect in the headwaters of the Yangtze River.According to the daily flow data of Zhimenda Hydrological Station from 1957 to 2021,we obtained the time of abrupt change in annual average flow of Zhimenda hydrological station via Bayesian change-point test,evaluated the abrupt change degree by using IHA-RVA (Indicators of Hydrologic Alteration and Range of Variability Approach),and then assessed the time-series changes of monthly average flow and annual extreme flow by using trend slope,Kendall trend test and detrended fluctuation analysis.We found that 1) the average annual flow of Zhimenda hydrological station changed abruptly in 2004.2) The comprehensive hydrologic change degree reached 37.2%,implying a moderate change.3) The average monthly flow was moderately changed,and the average monthly flow increased in different degrees,which added to the available water for aquatic life in the river.4) The extreme values of flow were slightly changed,indicating that extreme flow events remained in a stable range,which maintained the stability of the ecosystem in the headwaters.The increase of minimum flow better guaranteed the ecological flow of the watershed.5) The occurrence time of extreme values was slightly changed,posing little impact on aquatic habitats and fish migration.6) The pulse frequency of high and low flows both changed to low degrees,which reflected that the frequency of drought and flood decreased in the headwaters of the Yangtze River,sustaining the water reception of the river and riverbanks.The high and low flow pulse duration also brought about uncertain influence to the ecological environment of river and riverbanks in the source region.7) The rising rate,declining rate and reversal rate of flow all changed to low degrees,which indicated that the change degree of flow in the headwaters of the Yangtze River was low and maintained in a relatively stable state of the ecosystem.In general,the ecological environment in the headwaters of the Yangtze River showed a trend of improvement,and the increased ecological flow was conducive to maintaining the biodiversity and the healthy and sustainable development of the ecosystem in the source region.

Key words: headwaters of the Yangtze River, ecological flow, IHA indicators, hydrological regime, hydrologic change degree, detrended fluctuation analysis

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