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Soil moisture regimes under point irrigation.

机译:点灌条件下的土壤水分状况。

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摘要

The main objective of this paper is determination of principal relationships influencing the distribution of moisture content in a soil profile under an emitter in point irrigation. Research was carried out by conducting field experiments. They determined geometry of wetted soil volume in a soil profile under point irrigation. Infiltration of water from a single emitter and the resulting spatial distribution is a typical feature of localized irrigation technology. The field experiments using different emitter discharges and various periods of irrigation on haplic Luvisol (ha LV) (ALFISOLS Udalfs) on loess were conducted in a soil profile 1 m deep. Admissible duration of irrigation in relation to discharge rates has been calculated and illustrated in a graph. Incorrect irrigation practices can cause serious environmental damage. A method for determining the width and depth of the wetted soil volume under the point irrigation was developed. This method is rapid and simple, and it gives consistent results.
机译:本文的主要目的是确定影响点灌溉下喷头下土壤剖面中水分含量分布的主要关系。通过进行现场实验进行了研究。他们确定了点灌条件下土壤剖面中湿润土壤体积的几何形状。来自单个排放源的水渗入及其产生的空间分布是局部灌溉技术的典型特征。在1 m深的土壤剖面上,使用不同的发射器排放量和在黄土上的Luvisol(ha LV)(ALFISOLS Udalfs)上进行不同灌溉时间的田间试验。已经计算出了相对于流量的允许灌溉持续时间,并在图表中进行了说明。不正确的灌溉方式会造成严重的环境破坏。提出了一种确定点灌条件下湿润土壤体积的宽度和深度的方法。此方法快速,简单,并且结果一致。

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