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Combined Effects of Water Quality and Slope Gradient on Infiltration Under Simulated Furrow Irrigation for a Soil in North China

机译:华北土壤模拟沟灌水质和坡度对土壤入渗的联合影响

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Furrow irrigation is the main irrigation method in the world, including the developed and developing countries. Its management is important for the improvement of water utilization efficiency. The effects of irrigation water quality and furrow bed slope on infiltration were studied with simulated furrow irrigation experiments in laboratory. The experimental treatments were salt concentration (5, 10, 20, and 30 mmolc L-1), sodium adsorption ratio (SAR) (0.5, 5, and 10 (mmolc L-1)0.5), and slope gradient (1%, 3%, and 5%). Runoff amounts during experimental processes were measured to estimate infiltration amounts under the given inflow rate. The experimental results indicated that soil infiltration rate as a temporal function can be reasonably well represented with Kostiakov equation for various combined conditions of salt concentrations, SAR values, and slope gradients. Total infiltration amount generally increased with salt concentration but decreased with SAR level in irrigation water. It also decreased with the increased slope gradient of irrigation furrow. Different combinations of salt concentration and SAR had different influences on infiltration process. The effects of irrigation water quality on infiltration were promoted with increase in slope gradient. The effects of irrigation water quality and slope gradient on infiltration should be considered together to further improve water utilization efficiency in furrow irrigation practice.
机译:沟灌是包括发达国家和发展中国家在内的世界主要灌溉方式。它的管理对于提高水利用效率非常重要。通过实验室模拟沟灌实验研究了灌溉水质和沟床坡度对入渗的影响。实验处理包括盐浓度(5、10、20和30 mmolc L-1),钠吸附率(SAR)(0.5、5和10(mmolc L-1)0.5)和斜率(1%, 3%和5%)。测量实验过程中的径流量,以估算在给定流入速率下的入渗量。实验结果表明,对于盐浓度,SAR值和坡度的各种组合条件,用Kostiakov方程可以较好地表示土壤入渗速率作为时间函数。总入渗量通常随盐浓度增加而增加,但随SAR水中的SAR含量而降低。随着灌溉沟渠坡度的增加,灌溉面积也随之减小。盐浓度和SAR的不同组合对入渗过程的影响不同。坡度的增加促进了灌溉水质对入渗的影响。应综合考虑灌溉水质和坡度对入渗的影响,以进一步提高沟灌实践中的水分利用效率。

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