Measured and simulated soil wetting patterns under porous clay pipe sub-surface irrigation

被引:72
|
作者
Siyal, A. A. [1 ]
Skaggs, T. H. [2 ]
机构
[1] Sindh Agr Univ, Dept Land & Water Management, Tandojam, Pakistan
[2] ARS, US Salin Lab, USDA, Riverside, CA 92507 USA
关键词
Porous clay pipe; Sub-surface irrigation; Micro-irrigation; Soil wetting; Hydraulic conductivity; HYDRUS; DRIP IRRIGATION; WATER DISTRIBUTION;
D O I
10.1016/j.agwat.2008.11.013
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Sub-surface irrigation with porous clay pipe can be an efficient, water saving method of irrigation for many less developed and and semi-arid regions. Maximizing the efficiency of clay pipe irrigation requires guidelines and criteria for system design and operation. In this study, experimental and simulated (with HYDRUS (2D/3D)) soil wetting patterns were investigated for sub-surface pipe systems operating at different water pressures. Predictions of the soil water content made with HYDRUS were found to be in good agreement (R-2 = 0.98) with the observed data. Additional simulations with HYDRUS were used to study the effects of various design parameters on soil wetting. Increasing the system pressure increased the size of the wetted zone. The installation depth affects the recommended lateral spacing as well as the amount of evaporative water loss. For a given water application, the potential rate of surface evaporation affected the shape of the wetted region only minimally. Soil texture, due to its connection to soil hydraulic conductivity and water retention, has a larger impact on the wetting geometry. In general, greater horizontal spreading occurs in fine texture soils, or in the case of layered soils, in the finer textured layers. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:893 / 904
页数:12
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