2022
DOI: 10.1016/j.agwat.2022.107943
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Modeling strategies to balance salt leaching and nitrogen loss for drip irrigation with saline water in arid regions

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Cited by 12 publications
(4 citation statements)
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“…The filtration coefficient of the calculated layer is 0.2-0.4 m per day. The porosity of the soil of the study area is 48.61-55.64%, the density is 1.21-1.35 g/cm 3 . At a depth of 0.2m, there is a significant compaction of the soil of 0.6 m, the density increases to 1.42 g/cm3, the porosity decreases to 46%.…”
Section: Resultsmentioning
confidence: 93%
See 1 more Smart Citation
“…The filtration coefficient of the calculated layer is 0.2-0.4 m per day. The porosity of the soil of the study area is 48.61-55.64%, the density is 1.21-1.35 g/cm 3 . At a depth of 0.2m, there is a significant compaction of the soil of 0.6 m, the density increases to 1.42 g/cm3, the porosity decreases to 46%.…”
Section: Resultsmentioning
confidence: 93%
“…Artificial irrigation was first used in the 1980s of the 20th century as a way to enhance food production, but for many years traditional systems' water consumption efficiency did not reach 30%. A proactive shift to drip irrigation, also known as trickling irrigation, micro-irrigation, or localized irrigation, was observed in response to the traditional irrigation techniques' low efficacy (sprinkling, furrow irrigation) [3]. Through a system of pipelines, valves, drip lines, and emitters, the drip irrigation system enables to conserve water and nutrients (dispenser-droppers).…”
Section: Introductionmentioning
confidence: 99%
“…where X m is the maximum horizontal distance of the root distribution, which was set to 40 cm; Z m is the maximum depth of the root distribution, which was set to 70 cm, according to field observations; x * is the horizontal coordinates of the maximum root density, which was set to 20 cm; and z * is the vertical coordinates of the maximum root density, which was set to 10 cm. This was in reference to the related research conducted by Che et al [13]. P x and P z are the empirical parameters of root asymmetry, which are typically set to 1.0.…”
Section: Water Flowmentioning
confidence: 99%
“…The mechanisms of physical improvement measures for Water 2024, 16, 719 2 of 21 saline soil are reduction in surface evaporation, moderation of the rise of groundwater, the creation of a relatively favorable water-salt environment in the root zone, and reduction in the water-salt stress suffered by crops during their growth periods to achieve the goals of increasing crop yields and efficient use of water resources. Through long-term research and practical exploration, film mulching, salt barrier layers, and ridge-furrow planting reduce root-zone salt accumulation and increase crop yields [13][14][15]. The mechanism of the film mulch system is its breaking the exchange of water and heat between soil and the atmosphere, working like a water vapor barrier in the soil surface [10].…”
Section: Introductionmentioning
confidence: 99%