1. Structural Equation Modeling of Soil Moisture Effects on Evapotranspiration of Maize in the North China Plain
- Author
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Junfu Xiao, Aiwang Duan, Bin Sun, Zhandong Liu, Anzhen Qin, Ben Zhao, and Dongfeng Ning
- Subjects
0106 biological sciences ,Irrigation ,Topsoil ,02 engineering and technology ,01 natural sciences ,Agronomy ,Evapotranspiration ,Lysimeter ,Soil water ,0202 electrical engineering, electronic engineering, information engineering ,Soil horizon ,Environmental science ,020201 artificial intelligence & image processing ,Stage (hydrology) ,Engineering (miscellaneous) ,Water content ,010606 plant biology & botany - Abstract
Relationships between crop evapotranspiration (ET) and soil water content (SWC) have been studied worldwide. However, traditional data processing has drawbacks in modeling the contribution of SWC to ET on a layer-to-layer basis. To address this issue, large-scale weighing lysimeters were used to monitor the real-time ET along with Insentek sensors to monitor daily SWC dynamics of summer maize at Xuchang Experimental Irrigation Station, North China Plain, in 2016 and 2017. At the vegetative stage of maize (V6 and V12), roots reached 70 cm deep, with an average root length density (RLD) of 0.55 cm cm−3. Mean RLD at reproductive stage (VT and R3) was 1.13 cm cm−3, and the roots reached 100 cm deep. Cumulative percentage of ETi to ET in topsoil (0–30 cm) was from 66% (V6) to 77% (R3), with the lowest proportion of 62% at maturity (R6), indicating > 2/3 of root mass distributed in the 0–30 cm soil layer. Principal component analysis was conducted to extract principal components of SWC. Soil moisture in the top (0–30 cm), middle (30–60 cm), and deep (60–100 cm) soil layers explained 8%, 14%, and 31% of the variances in ET (P
- Published
- 2019
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