黄河"几字弯"水沙变化与系统治理OA
Water and sediment discharge evolution in the Ordos Loop of the Yellow River and its systematic governance
治黄百难,唯沙为首,破解症结在于通过生态与水利工程等措施来协调水沙异源,驱动河道与流域协同演化.为探究黄河"几字弯"河道冲淤演变及未来水沙调控方向,本文基于水文序列分析法及泥沙平衡法量化了宁蒙段过去 70年水沙演变、河道冲淤和泥沙空间来源变化,解析了其影响并提出区域治理对策.结果表明:(1)宁蒙河段耗水显著,年均耗水量 86.72 亿m3,其中宁夏河段和内蒙河段年均耗水分别贡献 28%和 72%;宁蒙河段年均淤积 0.135 亿t,其中宁夏河段总体冲刷,内蒙河段持续淤积.(2)宁夏河段输沙波动主控因子为支流来沙及灌区引水携沙,内蒙河段则系十大孔兑来沙及河道累积性淤积;1951-1985年宁蒙河段泥沙变率由河床冲淤主导,1986-2020年则转为支流来沙和引水沙量共同驱动.(3)宁蒙河段"水减沙增、冲少淤多"的水沙失衡格局对"几字弯"生态、防洪与产业发展产生连锁冲击,未来需系统性恢复河道输沙能力、全链条消减支流沙源与风沙入黄、多维度维系水沙匹配效率,并以制度保障治理长效,实现宁蒙河段系统治沙、精准控沙和协同调沙,确保水沙治理从"攻坚战"转向"长效治",为"几字弯"生态保护和高质量发展提供持久保障.
Among the numerous challenges in the management of the Yellow River,sediment control stands as the foremost.The key to addressing this lies in reconciling the disparate sources of water and sediment through eco-engineering measures,thereby driving the coordinated evolution of the river channel and the basin.To explore the erosion and deposition evolution of the river channel in the Yellow River's Ordos Loop and the future direction of water and sediment discharge regulation,this study quantified the changes in water and sediment discharge evolu-tion,river channel erosion and deposition,and spatial sources of sediment discharge in the Ningxia-Inner Mongolia reach over the past 70 years using hydrological sequence analysis and sediment balance methods.It also analyzed the impacts of these changes and proposed regional management countermeasures.The results show that:(1)Water con-sumption in the Ningxia-Inner Mongolia reach is significant,with an annual average water consumption of 8.672 bil-lion m³,of which the Ningxia section and the Inner Mongolia section account for 28%and 72%of the annual average water consumption respectively;the Ningxia-Inner Mongolia reach has an annual average siltation of 13.5 million tons,among which the Ningxia section is generally eroded while the Inner Mongolia section is continuously silted.(2)The dominant factors influencing sediment discharge fluctuations in the Ningxia section are sediment from tribu-taries and sediment carried by water diversion in irrigation areas,whereas for the Inner Mongolia section,they are sediment from the Ten Kongdui Tributaries and cumulative siltation in the river channel.From 1951 to 1985,the sediment variability in the Ningxia-Inner Mongolia reach was dominated by riverbed erosion and deposition,whereas from 1986 to 2020,it was jointly driven by sediment from tributaries and sediment from water diversion.(3)The water-sediment imbalance pattern of"decreasing water,increasing sediment,less erosion,and more siltation"in the Ningxia-Inner Mongolia reach has triggered chain impacts on the ecology,flood control,and industrial development of the Ordos Loop.In the future,it is necessary to systematically restore the sediment transport capacity of the river channel,reduce sediment sources from tributaries and wind-blown sand entering the Yellow River through the entire chain,maintain water-sediment matching efficiency from multiple dimensions,and ensure the long-term effective-ness of governance through institutional guarantees.This will enable systematic sediment control,precise sediment regulation,and coordinated sediment adjustment in the Ningxia-Inner Mongolia reach,ensuring that water-sediment management shifts from"intensive campaigns"to"sustained governance"and providing enduring guarantees for the ecological protection and high-quality development of the Ordos Loop.
胡春宏;张晓明;缪今典;李锦荣
中国水利水电科学研究院 流域水循环模拟与水安全全国重点实验室,北京 100038中国水利水电科学研究院 流域水循环模拟与水安全全国重点实验室,北京 100038福建农林大学 林学院,福建 福州 350002内蒙古阴山北麓草原生态水文国家野外科学观测研究站,内蒙古 呼和浩特 010020
农业科技
黄河"几字弯"水沙变化河道冲淤空间来源治理对策
Ordos Loop of the Yellow Riverwater and sediment changesriver erosion and depositionspatial sourcesgovernance strategies
《水利学报》 2026 (1)
38-48,11
国家重点研发计划项目(2022YFF1300801)国家自然科学基金项目(52379082)内蒙古自治区"揭榜挂帅"项目(2024JBGS0013)
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