Evaluating soil water movement and soil water content uniformity under sprinkler irrigation with different soil texture and irrigation uniformity using numerical simulation

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL
Rui Chen, Hong Li, Jian Wang, Xin Guo, Yu Xiang
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Abstract

Water movement and its distribution uniformity in the soil are essential for the design of sprinkler irrigation systems. They are both crucial factors influencing nutrient migration and the productivity of crops. In this study, a new numerical simulation method was proposed to investigate the soil water movement in sprinkler irrigation under nonuniform infiltration boundary conditions using COMSOL software. Besides, two soil tank experiments were conducted to test the reliability of the simulation model. Finally, the model was applied to evaluate the effects of sprinkler irrigation uniformity, soil texture, and initial soil water content on soil wetting patterns and soil water content uniformity. The results showed that the COMSOL-2D predictions of the vertical wetting fronts were in good agreement with the experimental data. The soil texture and initial soil water content influenced the soil wetting pattern and the risks of surface runoff and deep percolation in sprinkler irrigation systems. When the water application rate was 11.35 mm h−1 with an irrigation duration of 10 h, it was easy to cause surface runoff in silty clay loam while deep percolation in loamy sand. Additionally, when the initial soil water content is high, it should be better to avoid irrigation or cut down the irrigation duration to prevent percolation. The water within the soil was more uniformly distributed than that applied through a sprinkler irrigation system. The uniformity coefficient of soil water content distribution (CUs) increased from 87.75 % to 95.56 %, as the uniformity coefficient of sprinkler irrigation (CU) increased from 40.74 % to 82.41 %. Although a higher initial soil water content brought a higher soil CUs value, it also led to a higher risk of percolation. The experimental and simulation results indicated that the COMSOL-2D model could be used to accurately simulate soil water movement in sprinkler irrigation and determine the suitable operation mode of low-pressure sprinklers.

采用数值模拟方法评价不同土壤质地和灌溉均匀度喷灌条件下土壤水分运动和土壤含水量均匀性
水在土壤中的运动及其分布均匀性对喷灌系统的设计至关重要。它们都是影响养分迁移和作物生产力的关键因素。本文提出了一种新的数值模拟方法,利用COMSOL软件对非均匀入渗边界条件下喷灌过程中土壤水分运动进行数值模拟。并进行了两次土槽试验,验证了模拟模型的可靠性。最后,应用该模型评价了喷灌均匀性、土壤质地和土壤初始含水量对土壤湿润模式和土壤含水量均匀性的影响。结果表明,COMSOL-2D对垂直湿润锋的预报与实验数据吻合较好。土壤质地和土壤初始含水量影响喷灌系统土壤湿润模式以及地表径流和深层渗流风险。当施水量为11.35 mm h−1,灌溉时间为10 h时,粉质粘土壤土容易发生地表径流,而壤土砂则容易发生深层渗流。另外,当土壤初始含水量较高时,最好避免灌溉或缩短灌溉时间,防止渗水。土壤中的水分分布比喷灌系统更均匀。土壤含水量分布均匀系数(CU)由87.75%增加到95.56%,喷灌均匀系数(CU)由40.74%增加到82.41%。土壤初始含水量越高,土壤cu值越高,但渗流风险也越大。试验和仿真结果表明,利用COMSOL-2D模型可以准确模拟喷灌过程中土壤水分的运动,确定低压喷灌装置的适宜运行方式。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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