从1998年到2018年,长江流域的水文制度和水质变化
Yunbing Liu1, Chunlei Song2, Xia Yang3
1Changjiang Basin Ecology and Environment Monitoring and Scientific Research Center, Changjiang Basin Ecology and Environment Administration, Ministry of Ecology and Environment, No. 13 Yongqing Road, Wuhan 430010, China.
Water research
|November 28, 2023
概括
三峡大显著改变了长江流域水质,减少了悬浮固体和改善了一些参数. 然而,增加的总和减少的溶解氧构成持续的水质威胁.
科学领域:
- 环境科学 环境科学
- 水文学的水文学
- 水资源管理 水资源管理
背景情况:
- 三峡大等大型水电项目对河流生态系统产生深远影响.
- 有效的流域管理需要了解水建设后的长期环境变化.
研究的目的:
- 评估三峡大对长江流域水文制度和物理化学参数的长期影响.
- 为未来的大型水建设提供参考数据.
主要方法:
- 对长江流域20年 (1998-2018) 的水文和物理化学数据的分析.
- 在大灌之前,期间和之后的参数比较.
主要成果:
- 在灌后观察到水位显著上升和流速下降.
- 沉积过程中溶解氧的初始波动,化学氧需求,导电性,硬度和性,随后是稳定.
- 悬浮固体 (SS),总和水平的大幅降低.
- 总的增加和下游溶解氧的减少,加剧河口的缺氧.
结论:
- 三峡大导致长期的长江流域环境发生重大变化.
- 虽然一些水质指标有所改善,但其他如总和溶解氧等指标需要持续监测和管理.
- 这些发现为未来大型河项目的规划和运营提供了关键的指导.
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