2023
DOI: 10.1016/j.agwat.2023.108236
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Simulation of water balance and irrigation strategy of typical sand-layered farmland in the Hetao Irrigation District, China

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Cited by 15 publications
(8 citation statements)
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“…The lack of isotope data with high temporal resolution along the soil-plant-atmosphere axis and the effects of isotope fractionation complicated our analysis of yellow willow water sources. To increase the accuracy of water source identification, future studies should examine the isotope fractionation mechanisms in yellow willow water sources [49], specifically the differences between various plant tissues and soil layers [50][51][52][53], and consider other models and/or data correction factors. To more precisely record short-term changes in the isotopic compositions of soil, plants, and atmospheric water, high-precision isotope analyzers should be employed with a higher sample frequency.…”
Section: Discussionmentioning
confidence: 99%
“…The lack of isotope data with high temporal resolution along the soil-plant-atmosphere axis and the effects of isotope fractionation complicated our analysis of yellow willow water sources. To increase the accuracy of water source identification, future studies should examine the isotope fractionation mechanisms in yellow willow water sources [49], specifically the differences between various plant tissues and soil layers [50][51][52][53], and consider other models and/or data correction factors. To more precisely record short-term changes in the isotopic compositions of soil, plants, and atmospheric water, high-precision isotope analyzers should be employed with a higher sample frequency.…”
Section: Discussionmentioning
confidence: 99%
“…Compared with that in the other vertical soil layers, RL in the 10-20 cm soil layer had a better correlation with yield and WUE (r = 0.847, p < 0.01); in contrast, RL in the 40-50 cm layer showed little or no correlation with yield and WUE. This may be because capillary water remained in the sand layer when the fine sand layer exceeded 35 cm, thus interrupting the hydraulic connection between the layers above and below the sand layer [62][63][64]. Given that roots cannot effectively absorb soil moisture below the sand layer, the growth of deep roots may not significantly increase maize yield.…”
Section: Discussionmentioning
confidence: 99%
“…The treatments included various irrigation schedules, crop planting patterns, etc., to investigate their impact on crop growth and output. The soil in the experimental locations was categorized into two layers: the topsoil layer (0 to 40 cm) was chalky loam with a soil bulk density of 1.43 g/cm 3 , and the subsoil layer (40 to 100 cm) was chalky loam with a soil bulk density of 1.40 g/cm 3 .…”
Section: Experimental Site and Field Trialsmentioning
confidence: 99%
“…Recently, the imbalance between availability and demand for water resources has become noticeable, leading to water shortages. Asynchronous irrigation scheduling and varying water levels in the Yellow River have resulted in inconsistent irrigation dates and volumes, which are not aligned with crop water requirements, exacerbating the issue of water scarcity [1][2][3]. The irrigation schedules are not consistently optimized, resulting in water wastage and worsening the water shortage.…”
Section: Introductionmentioning
confidence: 99%