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首页> 外文期刊>Irrigation & Drainage Systems Engineering >Estimation of Deep Percolation in Sandy-Loam Soil using Water-balance Approach
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Estimation of Deep Percolation in Sandy-Loam Soil using Water-balance Approach

机译:水平衡法估算砂壤土的深层渗流

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The most reliable method used to estimate deep percolation is using Lysimeter which proves to be expensive and time consuming as well. In this study, deep percolation has been estimated by using water balance method. The experimental setup consisted of two lysimeters in the Hydraulic Engineering field lab, I.I.T., Roorkee in which maize crop was grown. Regular measurements of soil moisture were made at the depths 0-20 cm, 20-40 cm, 40- 60 cm, 60-80 cm and 80-100 cm using gravimetric method. The evapotranspiration estimates were determined using Penman-Moneith equation. The deep percolation is calculated using the water-balance approach. The deep percolation calculated using the water-balance approach is comparable to the observed values of deep percolation which are obtained from the lysimeters.
机译:用于估计深度渗滤的最可靠方法是使用Lysimeter,事实证明该方法既昂贵又耗时。在这项研究中,已通过使用水平衡法估算了深度渗滤。该实验装置由位于Roorkee的I.I.T.水利工程野外实验室中的两个测力计组成,玉米作物在其中生长。使用重量分析法在0-20厘米,20-40厘米,40-60厘米,60-80厘米和80-100厘米的深度进行常规土壤湿度测量。蒸发蒸腾估算值是使用Penman-Moneith方程确定的。使用水平衡方法计算深层渗滤。使用水平衡法计算得出的深层渗滤与从溶渗仪获得的深层渗滤观察值相当。

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