含沙量对草地坡面径流泥沙沉积和水力特性的影响

潘成忠; 马岚; 上官周平

含沙量对草地坡面径流泥沙沉积和水力特性的影响

1.
北京师范大学水科学研究院, 水沙科学教育部重点实验室, 北京, 100875;
2.
西北农林科技大学水利与建筑工程学院, 陕西, 杨凌, 712100;
3.
中国科学院水利部, 水土保持研究所黄土高原土壤侵蚀与早地农业国家重点实验室, 陕西, 杨凌, 712100

基金项目: 国家自然科学基金资助项目(50579003;40801103);国家科技支撑计划项目(2006BAD09B04)

详细信息

作者简介:
潘成忠(1980- ),男,江苏灌云人,讲师,博士,主要从事山坡水文与流域生态方面的研究.E-mail:pancz@bnu.edu.cn

中图分类号: P333.4

Influence of sediment concentration on deposition of silt and runoff hydraulics on grassland

1.
Key Laboratory of Water Sediment Sciences, College of Water Sciences, Beijing Normal University, Beijing 100875, China;
2.
College ofWater Resources and Architectural Engineering, Northwest A&F University, Yangling 712100, China;
3.
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, I nstitute of Soil and Water Conservation, CAS, Yangling 712100, China

Funds: The study is financially supported by the National Natural Science Foundation of China (No.50579003 and No.40801103) and the National Key Technology R & D Program of China (No.2006BAD09B04)

摘要: 通过室内模拟试验,在坡度为3°和9°、流量为20和60L/min条件下研究了不同浓度(0～350kg/m³)含沙水流流经草地的泥沙沉积过程及其水力学特性。结果表明,坡面泥沙沉积量随含沙量的增加而增大,3°时泥沙沉积率与含沙量呈正相关,而9°时沉积率与含沙量呈反势。坡度对泥沙沉积影响显著,而在相同坡度条件下,两种流量试验的泥沙沉积量无明显差异。相同坡面坡上部位流速小于坡下部位,且含沙量对坡面流速影响较小。在相同坡度和流量条件下,水流雷诺数随含沙量的增大而减小。3°时水流阻力系数和曼宁糙率均随含沙量的增加而增大,而9°时含沙量对阻力影响不明显,因此在土壤侵蚀较严重地区进行坡面水文过程演算时需考虑含沙量对缓坡糙率的影响。
- 含沙水流 /
- 含沙量 /
- 沉积 /
- 水力学特性 /
- 草地
Abstract: In order to reveal the performance of grass strips on silt-laden flow with high sediment concentration, the experiments were carried out on different sediment concentration of 0-350 kg/m³ in grassplots on the slope of 3° and 9° and discharge of 20 and 60 L/min, and the deposition of sediment and hydraulic characteristics of runoff were analyzed.The results show that the sediment mass deposited on grassplots increase with the concentration.There is a positive relationship between the deposition rate and the sediment concentration at 3°, but a negative relationship at 9°.Under the experimental conditions, the discharge plays a negligible role in the total mass of sediment deposition, but slope significantly affects the sediment deposition.The flow velocities at downslope are greater than that at upslope, and the sediment concentration has a minor influence on the velocity.On the same slope and discharge, the Reynolds number of silt laden flow decreases with the increase of sediment concentration Runoff resistance coeff icient (f) and Manning roughness (n) increase with sediment concentration at 3°, but there is no significant correlation between them at 9°.Therefore, sediment concentration should be considered in the estimation of hydrological processes in the region with severe soil erosion.
- silt-laden flow /
- sediment concentration /
- deposition /
- hydraulics /
- grassland

[1]	TOLLNER E W,BARFIELD B J,HAAN C T,et al.Suspended sediment filtration capacity of simulated vegetation[J].Transacctions of the ASAE,1976,19:678-682.
[2]	TOLLNER E W,BARFIELD B J,VACHIRAKORNWATANA C,et al.Sediment deposition patterns in simulated grass filters[J].Transacctions of the ASAE,1977,20:940-944.
[3]	DELETIC A.Modelling of water and sediment transport over grassed areas[J].J Hydrol,2001,248:168-182.
[4]	蔡强国,黎四龙.植物篱笆减少侵蚀的原因分析[J].土壤侵蚀与水土保持学报,1998,4(2):54-60.(CAI Qiang-guo,LI Si-long.Effect of contour hedgerows on control of soil erosion[J].Journal of Soil and Water Conservation,1998,4(2):54-60.(in Chinese))
[5]	李怀恩,张亚平,蔡明,等.植被过滤带的定量计算方法[J].生态学杂志,2006,25(1):108-112.(LI Huai-en,ZHANG Ya-ping,CAI Ming,et al.Quantitative calculation methods for vegetative filter strips[J].Chinese Journal of Ecology,2006,25(1):108-112.(in Chinese))
[6]	DELETIC A.Sediment transport in urban ruoff over grassed areas[J].J Hydrol,2005,301:108-122.
[7]	钱宁.高含沙水流运动[M].北京:清华大学出版社,1989.(QIAN Ning.Dynamics of high-concentrated mud suspensions[M].Beijing:TsinghUa University Press,1989.(in Chinese))
[8]	GHADIRI H,BOSE C W,HOGARTH W L.The influence of grass and porous barrier strips on runoff hydrology and sediment transport[J].Transactions ofthe ASAE,2001,44(2):259-268.
[9]	ABU-ZREIG M,RUDRA R P,LALONDE M N,et al.Experimental investigation of runoff reduction and segment removal by vegetated filter strips[J].Hydrological Processes,2004,18(11):2029-2037.
[10]	LIGDI E,MORGAN B P C.Contour grass strips:a laboratory simulation oftheir role in soil erosion control[J].Soil Technol,1995,8(1):109-117.
[11]	潘成忠,上官周平.不同坡度草地含沙水流水力学特性及其拦沙机理[J].水科学进展,2007,18(4):490-495.(PAN Cheng-zhong,SHANGGUAN Zhou-ping.Hydraulic characteristics of silt-laden flow on different gradient grassplots and its mechanism of sediment retention[J].Advances in Water Scienee,2007,18(4):490-495.(in Chinese))
[12]	沙玉清.泥沙运动力学引论[M].北京:中国工业出版社,1965.(SHA Yu-qing.Dynamics of sediment movement[M].Beijing:China Industry Press,1965.(in Chinese))
[13]	张瑞瑾.河流泥沙动力学(第二版)[M].北京:中国水利水电出版社,1998.(ZHANG Rui-jing.River Sediment dynamics(2nd)[M].Beijing:China Waterpower Press,1998.(in Chinese))
[14]	JIN C X,RoMKENS M J M.Experimental studies of factors in determining sediment trapping in vegetative filter strips[J].Transactions of the ASAE,2001,44(2):277-288.
[15]	ABRAHAMS A D,PARSONS A J,HIRSCH P J.Field and laboratory studies of resistance to interrill overland flow on semi-arid hillslopes,southern Arizona[A].PARSONS A J,ABRAHAMS A D(eds),Overland flow:Hydraulics and erosion mechanics[C].London:UCL Press,1992.1-23.

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含沙量对草地坡面径流泥沙沉积和水力特性的影响

作者简介:
潘成忠(1980- ),男,江苏灌云人,讲师,博士,主要从事山坡水文与流域生态方面的研究.E-mail:pancz@bnu.edu.cn

Influence of sediment concentration on deposition of silt and runoff hydraulics on grassland

计量

含沙量对草地坡面径流泥沙沉积和水力特性的影响

作者简介:
潘成忠(1980- ),男,江苏灌云人,讲师,博士,主要从事山坡水文与流域生态方面的研究.E-mail:pancz@bnu.edu.cn

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Influence of sediment concentration on deposition of silt and runoff hydraulics on grassland

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含沙量对草地坡面径流泥沙沉积和水力特性的影响

作者简介: 潘成忠(1980- ),男,江苏灌云人,讲师,博士,主要从事山坡水文与流域生态方面的研究.E-mail:pancz@bnu.edu.cn

Influence of sediment concentration on deposition of silt and runoff hydraulics on grassland

计量

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含沙量对草地坡面径流泥沙沉积和水力特性的影响

作者简介: 潘成忠(1980- ),男,江苏灌云人,讲师,博士,主要从事山坡水文与流域生态方面的研究.E-mail:pancz@bnu.edu.cn

English Abstract

Influence of sediment concentration on deposition of silt and runoff hydraulics on grassland

全文HTML

目录

作者简介:
潘成忠(1980- ),男,江苏灌云人,讲师,博士,主要从事山坡水文与流域生态方面的研究.E-mail:pancz@bnu.edu.cn

作者简介:
潘成忠(1980- ),男,江苏灌云人,讲师,博士,主要从事山坡水文与流域生态方面的研究.E-mail:pancz@bnu.edu.cn