VARIATION CHARACTERISTICS OF FLOW RATE AND WATER DEPTH IN DITCHES WITH UNIFORM INFLOW
-
摘要: 近年来,在城市建设过程中,广场、公园、城市道路等区域大量采用线性排水沟或缝隙排水,有沿程入流的沟渠为非均匀流,因此,在上述排水方式中普遍采用的谢才公式计算方法会产生较大误差。针对上述问题,采用物理模型方法,研究了沿程均匀入流对明渠恒定流水面曲线的影响,提出了不同坡度、渠底宽度和壁面粗糙度条件下的水面曲线,并与谢才公式计算结果进行了比较。结果表明:在各实验工况条件下有沿程入流时,沟渠内水面曲线均沿程增加,与谢才公式计算结果有明显差异,并进一步拟合出流量-水深的计算关系公式。上述研究成果对研究和优化道路边沟、线性排水等沿程均匀入流沟渠的水力断面设计计算具有重要意义。Abstract: In recent years, in view of the fact that the flow along the ditch is non-uniform flow for linear drainage pipe of stormwater runoff, application of Chézy's formula will bring large errors when applied to engineering design. The experimental physical model method was adopt to investigate the effect of the inflow along the way on the constant flow surface curve of the open channel. Meanwhile, the water level was measured by the piezometer, the effect of water surface curve under the conditions of different slopes, width of ditch bottom and wall surface roughness was investigated, and compared with the calculation results by Chézy's formula. The results showed that the water surface curve in the ditch increased along the way when there was inflow along the flow way under different experimental conditions, which was obviously different from the calculation results by Chézy's formula, and the calculation relationship between flow rate and water depth was further fitted. These results will significantly contribute to optimize the design and calculation of the hydraulic cross-section of the even inflow ditches along the road such as side ditches and linear drainage system.
-
Key words:
- channel /
- inflow along the way /
- non-uniform flow /
- water surface curve
-
[1] OLTON R C.Slotted drains cut street ponging[J].American City & County,1977,92(4):13-25. [2] BROWN S A,STEIN S M,WARNER J C.Federal Highway.Administration Urban Drainage Design Manual[Z].[No.01-021] FHWA-NHI-01-021,2001:840-886. [3] BJERKLIE DAVID M,DINGMAND S L,BOLSTER C H.Comparison of constitutive flow resistance equations based on the Manning and Chezy equations applied to natural rivers[J].Water Resources Research,2005,41(11):644-653. [4] STRYPCZEWSKI Witold G,SZYMKIEWICZ R.Analysis of paradoxes arising from the Chezy formula with constant roughness:Ⅰ.Depth-discharge curve[J].Hydrological Sciences Journal,1996,41(5):659-673. [5] GENC O,ARDICLIOGLU M,ARDICLIOGLU N.Calculation of mean velocity and discharge using water surface velocity in small streams[J].Flow Measurement and Instrumentation,2015,41:115-120. [6] BALOUCHI B,ABEDINI M J,MANHART M.A simulation-optimization technique to estimate discharge in open channels based on water level data alone:gradually varied flow condition[J].Iranian Journal of Science and Technology,Transactions of Civil Engineering,2019,43(2):215-229. [7] KARIMI S M.Modeling fluid flow in an open rectangular channel with lateral inflow channel[D].Jkuat-paushi,2018:14-39. [8] 樊铭京,马树升,王贵田.明渠恒定非均匀流渠道流量实时监测方法研究与探讨[J].山东农业大学学报(自然科学版),2010,41(3):440-442. [9] 胡岚平,刘华,覃文文,等.基于MATLAB的明渠恒定非均匀渐变流水面线的数值计算[J].西南民族大学学报(自然科学版),2011,37(5):827-831. [10] 孙建良.明渠恒定非均匀流回水曲线的计算方法[J].安徽建筑工业学院学报(自然科学版),1996,4(4):37-40. [11] 朱科.海城河非均匀流水面线的推算研究[J].水利技术监督,2017(6):90-93,95. [12] 程铁杰,郑佳成,郑佳重,等.考虑底坡影响下的明渠恒定非均匀流水力计算公式研究[J].水利水电技术,2017,48(4):79-81,108. [13] 陈建兴,戎红玉,王惠民.用随机微分方程模型求解明渠渐变流[J].河海大学学报,1994,22(5):43-47. [14] 上海市政工程设计研究总院.室外排水设计规范[M].3版.北京:中国计划出版社,2014.
点击查看大图
计量
- 文章访问数: 229
- HTML全文浏览量: 35
- PDF下载量: 5
- 被引次数: 0