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Simulation of soil water movement and deep drainage from jujube tree orchard in arid areas

机译:干旱区枣园土壤水分运移与深层排水模拟

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In arid areas, water is especially critical for residential, industrial, and agricultural users since the water resources are limited. Consequently, how to increase irrigation efficiency is of high concern to the local agricultural authorities. In arid areas like Aksu in Xijiang Province, China, agricultural irrigation is one of the most important factors which impacts on the water content and also infiltration in the subsurface. For Jujube, the intensity and frequency of irrigation greatly influence the infiltration, which may cause excessive irrigation. As well known, the movement of water during irrigation must be recognized in order to properly evaluate current irrigation patterns and take measures to increase irrigation efficiency and reduce water losses due to evaporation and infiltration In this paper, the code, HYDRUS-1D, which can simulate water, heat, and/or solute movement in one-dimensional, variably-saturated porous media, was used to evaluate the movement of water and the characteristics of infiltration in sandy soil. The infiltration rate during irrigation is very large under traditional border irrigation conditions with a rate of 1124.0 mm/year, which accounts for 60% of the total irrigation water. Therefore, it is not suitable to adopt border irrigation if we plan to reduce infiltration and improve irrigation efficiency. Simulation suggests that furrow irrigation or micro-irrigation technologies which use high frequency and small-ration irrigation methods be used in the arid areas.
机译:在干旱地区,由于水资源有限,水对住宅,工业和农业用户尤为重要。因此,如何提高灌溉效率是当地农业部门高度关注的问题。在中国西江阿克苏等干旱地区,农业灌溉是影响水分和地下渗透的最重要因素之一。对于枣来说,灌溉的强度和频率对渗入有很大影响,这可能导致过度灌溉。众所周知,必须认识到灌溉过程中的水运动,以便正确评估当前的灌溉方式,并采取措施提高灌溉效率并减少由于蒸发和入渗引起的水流损失。本文中的代码HYDRUS-1D可以在一维可变饱和多孔介质中模拟水,热和/或溶质的运移,用于评估水的运移和沙质土壤的入渗特性。在传统的边界灌溉条件下,灌溉期间的入渗率非常高,达到1124.0 mm /年,占总灌溉水的60%。因此,如果我们计划减少渗透并提高灌溉效率,则不宜采用边界灌溉。模拟表明,在干旱地区使用沟灌或微灌溉技术,这些技术使用高频和小剂量灌溉方法。

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