1. 西北农林科技大学 水土保持研究所 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西 杨凌,712100
2. 中国科学院 水利部 水土保持研究所, 陕西 杨凌,712100
3. 西北农林科技大学 水利建筑与工程学院, 陕西 杨凌,712100
纸质出版:2020
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穆兴民, 赵广举, 高鹏, 等. 黄河未来输沙量态势及其适用性对策[J]. 水土保持通报, 2020,40(5):328-332.
Mu Xingmin, Zhao Guangju, Gao Peng, et al. Future Trend of Sediment Discharge in Yellow River and Its Adaptation Strategies[J]. Bulletin of Soiland Water Conservation, 2020, 40(5): 328-332.
穆兴民, 赵广举, 高鹏, 等. 黄河未来输沙量态势及其适用性对策[J]. 水土保持通报, 2020,40(5):328-332. DOI: 10.13961/j.cnki.stbctb.2020.05.046.
Mu Xingmin, Zhao Guangju, Gao Peng, et al. Future Trend of Sediment Discharge in Yellow River and Its Adaptation Strategies[J]. Bulletin of Soiland Water Conservation, 2020, 40(5): 328-332. DOI: 10.13961/j.cnki.stbctb.2020.05.046.
[目的
]
探索黄河输沙预测的新思路,预估黄河未来输沙态势与输沙量水平,为黄河流域生态治理规划提供参考。[方法
]
结合黄河流域水土保持生态修复现状,采用单累积曲线法、滑动平均及频率分析方法,分析1950—2019年黄河主要来沙区间的实测输沙量变化特征及其未来态势。[结果
]
1950—2019年黄河输沙量呈现阶梯式减少。1950—2019年黄河中游各站累积实测输沙量随时间的变化可用“左半抛物线”表征。黄河输沙量自1997年以来已进入相对稳定态势,目前已达企稳状态;黄河潼关站未来年输沙量在90%频率下为1.00×10
8
t左右,在10%频率下为5.00×10
8
t左右,未来多年平均输沙量为1.40×10
8
t。[结论
]
为了维持黄河输沙量低稳状态,提升水土保持措施质量与标准,补齐“后水土保持”短板,构建完善的水沙关系调控体系,维持黄河下游河道冲淤平衡,是黄河流域生态保护与高质量发展的保障。
[Objective] New ideas in studying the variations of sediment discharge was explored to predict the future trend of sediment transportation level in the Yellow River
in order to provide a reference for the ecological management and hydraulic planning in this region.[Methods] Cumulative curve
moving average method and frequency analysis were used to analyze the variation characteristics and future trend of sediment discharge at the mainstream stations of the Yellow River from 1950 to 2019
based on the current status of soil and water conservation measures in the basin.[Results] The sediment discharge of the Yellow River decreased step by step from 1950 to 2019. From 1950 to 2019
the variation of cumulative measured sediment discharge at stations in the middle reaches of the Yellow River could be characterized by a “semi parabola”. According to the current status of ecological restoration and soil and water conservation in the Yellow River basin
sediment discharge of the Yellow River remained relative stable after 1997
and has reached a steady state in recent years. The annual sediment discharge at Tongguan station of the Yellow River over the next years was expected to be 1.00×108 tons at 90% frequency and 5.00×108 tons at 10% frequency, and the average annual sediment discharge was expected to be 1.40×108 tons.[Conclusion] In order to maintain a lower and stable state of sediment discharge in the Yellow River
improving the quality and standard of soil and water conservation measures
strengthening the weakness of post soil and water conservation
and establishing a comprehensive runoff-sediment regulation system are crucial to balance the scouring and silting in the lower reaches of the Yellow River
which is the guarantee of ecological protection and high-quality development of the Yellow River basin.
穆兴民,赵广举,高鹏,等.黄土高原水沙变化新格局[M].北京:科学出版社,2019.
穆兴民,胡春宏,高鹏,等.黄河输沙量研究的几个关键问题与思考[J].人民黄河,2017,39(8):1-4,48.
穆兴民,徐学选,陈霁巍.黄土高原生态水文研究[M].北京:中国林业出版社,2001.
比斯瓦斯(Biswas A K).水文学史[M].刘国纬,译.北京:科学出版社,2007:44-59.
胡春宏,张晓明. 论黄河水沙变化趋势预测研究的若干问题[J].水利学报,2018,49(9):1028-1039.
王光谦,钟德钰,吴保生.黄河泥沙未来变化趋势[J].中国水利,2020(1):9-12,32.
穆兴民.双累积曲线及其在水文气象和人类活动效应评价中的应用[EB/O] [2016-12-07] [2020-8-21]. https://wenku.baidu.com/view/54461a37905f804d2b160b4e767f5acfa1c783f5.html.
穆兴民,张秀勤,高鹏,等.双累积曲线方法理论及在水文气象领域应用中应注意的问题[J].水文,2010,30(4):47-51.
Mu Xingmin, Zhang Xiuqin, Shao Hongbo, et al. Dynamic changes of sediment discharge and the influencing factors in the Yellow River, China, for the recent 90 years[J]. Clean-Soil, Air, Water, 2012,40(3):303-309.
Zhao Guangju, Mu Xingmin, Han Mengwei, et al. Sediment yield and sources in dam-controlled watersheds on the Northern Loess Plateau[J]. Catena, 2017,149:110-119.
高健翎,张建国,朱莉莉,等.黄土丘陵沟壑区水土保持关键措施变化特征[J].水土保持通报,2019,39(3):114-118.
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