Estimation of the 2D cross-sectional area of the wetting pattern under drip irrigation and spatio-temporal variation of the components of the wetting pattern

IF 1 4区 环境科学与生态学 Q4 WATER RESOURCES Water SA Pub Date : 2023-04-24 DOI:10.17159/wsa/2023.v49.i2.3942
Murat Kilic
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Abstract

The wetting pattern which occurs under surface drip irrigation is an important component for the optimum design of the system and for irrigation programming. The aim of this investigation was to devise a model which enables estimation of the 2D cross-sectional area of the wetting pattern which occurs under a surface dripper by an analytical method. The main parameters of the wetting pattern are the wetting diameter on the soil surface, the maximum wetted depth and maximum wetted width in the soil profile, and the depth of this maximum wetted width from the soil surface. In the laboratory experiments, water applications were carried out on two soil textures (clay loam and clay) with homogeneous soil profiles at two discharge rates over 125 min and 170 min periods. The sizes of the parameters of the wetting pattern were measured as consecutive series over 5-min intervals during the water application period. The general/main shape which represents the wetting patterns which occur under different irrigation conditions was defined and mathematically modelled. When the results were evaluated statistically, a correlation of 0.9128 was found between the momentary rates of change of the maximum depth of the wetting pattern predicted by the model and those measured in the experiment. The correlation between the momentary variations of accelerations of the same parameter was 0.9205. In addition, the size of the wetting pattern showed an increment in reducing velocities during the water application period. The results indicate that the model devised in this investigation can be used in the prediction of the cross-sectional area of the wetting pattern which occurs under a surface dripper.
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滴灌条件下湿润型二维截面积估算及湿润型各组成部分的时空变化
地表滴灌下的湿润模式是滴灌系统优化设计和灌溉规划的重要组成部分。本研究的目的是设计一个模型,该模型可以通过分析方法估计表面滴管下发生的润湿模式的二维横截面积。湿化模式的主要参数是土壤表面的湿化直径、土壤剖面上的最大湿化深度和最大湿化宽度以及最大湿化宽度距离土壤表面的深度。在室内试验中,以两种土壤质地(粘壤土和粘土)为研究对象,在125 min和170 min的排水速率下进行了水处理。在施水期间,以连续5分钟的间隔测量润湿模式参数的大小。定义了在不同灌溉条件下发生的湿润模式的一般/主要形状,并建立了数学模型。结果表明,模型预测的最大润湿型深度瞬时变化率与实验测量值的相关系数为0.9128。同一参数下加速度瞬时变化的相关系数为0.9205。此外,在加水期间,润湿模式的大小表现出减少速度的增加。结果表明,所设计的模型可用于预测表面滴管下的润湿模式的横截面积。
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来源期刊
Water SA
Water SA 环境科学-水资源
CiteScore
2.80
自引率
6.70%
发文量
46
审稿时长
18-36 weeks
期刊介绍: WaterSA publishes refereed, original work in all branches of water science, technology and engineering. This includes water resources development; the hydrological cycle; surface hydrology; geohydrology and hydrometeorology; limnology; salinisation; treatment and management of municipal and industrial water and wastewater; treatment and disposal of sewage sludge; environmental pollution control; water quality and treatment; aquaculture in terms of its impact on the water resource; agricultural water science; etc. Water SA is the WRC’s accredited scientific journal which contains original research articles and review articles on all aspects of water science, technology, engineering and policy. Water SA has been in publication since 1975 and includes articles from both local and international authors. The journal is issued quarterly (4 editions per year).
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