投稿中心

审稿中心

编辑中心

期刊出版

网站地图

友情链接

引用本文:杨薇,赵彦伟,刘强,孙涛.白洋淀生态需水:进展及展望.湖泊科学,2020,32(2):294-308. DOI:10.18307/2020.0202
YANG Wei,ZHAO Yanwei,LIU Qiang,SUN Tao.A systematic literature review and perspective on water-demand for ecology of Lake Baiyangdian. J. Lake Sci.2020,32(2):294-308. DOI:10.18307/2020.0202
【打印本页】   【HTML】   【下载PDF全文】   查看/发表评论  【EndNote】   【RefMan】   【BibTex】
←前一篇|后一篇→ 过刊浏览    高级检索
本文已被:浏览 7585次   下载 4716 本文二维码信息
码上扫一扫!
分享到: 微信 更多
白洋淀生态需水:进展及展望
杨薇1,2, 赵彦伟1,2, 刘强1,3, 孙涛1,2
1.北京师范大学环境学院, 北京 100875;2.北京师范大学水环境模拟国家重点实验室, 北京 100875;3.北京师范大学水沙科学教育部重点实验室, 北京 100875
摘要:
采用文献计量、统计分析等手段收集了国内外关于白洋淀生态需水核算的研究成果,系统梳理了15种白洋淀生态需水核算方法,获得了白洋淀不同时间尺度、不同等级生态需水核算结果,并结合雄安新区规划对白洋淀生态需水核算存在的问题及未来的需求提出了展望.统计结果表明,白洋淀最小生态水位为7.45±0.66 m,适宜水位为8.61±0.52 m,最大水位为9.46±0.51 m;各等级生态需水月际变化趋势大致相同,8-9月最大,5月最小,但各月不同等级生态需水量的变幅较大;白洋淀最小生态补水量为1.35亿m3,适宜补水量2.40亿m3,最大生态补水量6.20亿m3.从支撑雄安新区规划建设的角度来看,目前白洋淀生态需水核算中面临的不足主要集中在生态管理目标和方法选择导致核算结果差异较大、缺乏淀区生态需水机制的阐释、生态需水核算时间尺度较粗略、未考虑淀区空间异质性的需水差异以及忽略河湖水文连通关系与过程5个方面;最后,以恢复白洋淀良性生态系统为导向,从分级分区开展白洋淀生态需水精细核算、分时分段淀区生态需水量质耦合模拟和考虑河湖沼连通的淀区水动力过程恢复3个方面提出了未来研究的建议与展望.
关键词:  白洋淀  生态需水  流量调控  生态补水  雄安新区
DOI:10.18307/2020.0202
分类号:
基金项目:国家自然科学基金项目(51439001)、国家重点基础研发计划项目(2017YFC0404505)和国家水体污染控制与治理科技重大专项(2018ZX07110001)联合资助.
A systematic literature review and perspective on water-demand for ecology of Lake Baiyangdian
YANG Wei1,2, ZHAO Yanwei1,2, LIU Qiang1,3, SUN Tao1,2
1.School of Environment, Beijing Normal University, Beijing 100875, P. R. China;2.State Key Laboratory of Water Environment Simulation, Beijing Normal University, Beijing 100875, P. R. China;3.Key Laboratory for Water and Sediment Science, Ministry of Education, Beijing Normal University, Beijing 100875, P. R. China
Abstract:
We collected the 35 literatures about water-demand for eco-environment of Lake Baiyangdian and systematically reviewed the methodologies and the corresponding calculation results. We identified the existing problem, and proposed research directions in the future according to the planning of the Xiong'an New Area. The statistical results shows that the lowest, suitable and highest water levels of Lake Baiyangdian are 7.45±0.66 m, 8.61±0.52 m and 9.46±0.51 m, respectively. Among the above three grades, water levels are highest in August and September, while lowest in May. In addition, extra water with the range of (1.35-6.20)×108 m3 should be supplied to the Lake Baiyangdian annually to maintain the ecosystem status. However, the existing research on environmental water in Lake Baiyangdian is insufficient to support the construction of the New Area, such as significant differences in water-demand for eco-environment from various methods, the mechanism deficiency and rough time scales (year and month) in the ecological water demand calculation, without consideration the spatial heterogeneity in the lake and the connection of the lake and upstream rivers. Therefore, we proposed three research expectations, including the gridding and fine calculation, water quantity and quality simulation by restoring stages, as well as the recovering of the lake hydrodynamic process.
Key words:  Lake Baiyangdian  water for the environment  flow regulation  environmental flow releases  Xiong'an New Area
分享按钮