基于变水位静水法的梯形渠道渗漏强度函数构建及验证
变水位静水法受规范中观测方法限制,相邻2次观测时间段的计算只能代表平均水深的平均渗漏强度,且将观测期间渠道渗漏的非线性过程假设为线性变化,该假设将导致计算误差,从而使拟合的渗漏强度幂函数存在系统误差。该文以渠道内水位随时间的渗漏过程拟合函数为基础,建立了关于梯形渠道变水位静水法(dropping head ponding test,DHPT)的渗漏强度函数。以石津灌区6种梯形衬砌渠道的变水位静水法试验为依据进行实例分析,分析获得6种梯形渠道的传统幂函数和DHPT渗漏强度函数,并应用各函数进行了渗漏时长计算。通过渗漏时长计算值与实测值对比表明,DHPT函数平均估计误差0.978 h,最大相对误差...
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Published in | 农业工程学报 Vol. 33; no. 5; pp. 91 - 95 |
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Main Author | |
Format | Journal Article |
Language | Chinese |
Published |
河北农业大学城乡建设学院,保定,071001%天津农学院水利工程学院,天津,300384
2017
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Subjects | |
Online Access | Get full text |
ISSN | 1002-6819 |
DOI | 10.11975/j.issn.1002-6819.2017.05.013 |
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Summary: | 变水位静水法受规范中观测方法限制,相邻2次观测时间段的计算只能代表平均水深的平均渗漏强度,且将观测期间渠道渗漏的非线性过程假设为线性变化,该假设将导致计算误差,从而使拟合的渗漏强度幂函数存在系统误差。该文以渠道内水位随时间的渗漏过程拟合函数为基础,建立了关于梯形渠道变水位静水法(dropping head ponding test,DHPT)的渗漏强度函数。以石津灌区6种梯形衬砌渠道的变水位静水法试验为依据进行实例分析,分析获得6种梯形渠道的传统幂函数和DHPT渗漏强度函数,并应用各函数进行了渗漏时长计算。通过渗漏时长计算值与实测值对比表明,DHPT函数平均估计误差0.978 h,最大相对误差为1.552%;而传统方法平均估计误差为3.997 h,最大相对误差为5.632%。表明DHPT函数能够更好地描述梯形渠道的渗漏过程,可用于计算点水深下的渗漏强度。通过DHPT函数与传统方法的计算结果对比,表明传统方法计算的渗漏强度普遍偏高,实例中平均误差达到0.248 L/(m^2·h),而DHPT函数直接建立于观测数据之间的函数关系,可避免线性假设的影响,提高计算精度,为分析变水位工况下的渠道水利用系数提供依据。 |
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Bibliography: | Chai Chunling1, Su Yanna1, Yang Luhua2, Liu Hongquan1 (1. Institute of Urban and Rural Construction, Agricultural University of Hebei, Baoding 071001, China; 2. College of Water Conservancy Engineering, Tianjin Agricultural University, Tianjin 300384, China) 11-2047/S seepage; canals; functions; dropping head ponding test; lined with concrete; linear variation Dropping head ponding test is a typical method for canal seepage measurement, particularly under variable canal capacities during irrigation. This study analyzed the limitations of traditional method for seepage rate calculation and proposed a new method based on dropping head ponding test(DHPT). Based on dropping head ponding test results and a standard method in Technical Code for Seepage Control Engineering on Canal, seepage rates were calculated, and a power function was established to describe the relationships between water-level and seepage rate. The standard calculation method had two inaccurate hypotheses. One was the linear variation of water-lev |
ISSN: | 1002-6819 |
DOI: | 10.11975/j.issn.1002-6819.2017.05.013 |