2017
DOI: 10.1061/(asce)ir.1943-4774.0001206
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Comparison of Effects of Root Water Uptake Functions for Simulating Surface Water and Heat Fluxes within a Corn Farmland Ecosystem in Northeast China

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Cited by 3 publications
(7 citation statements)
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“…The soil is the typical cambisol soil with pH 6.3. The organic carbon content is 8.83 g/kg, and nitrogen, phosphorus, and potassium contents are 1.04, 0.50 and 22.62 g/kg (Cai et al 2017). The soil bulk density, soil field capacity, and wilting coefficient of the soil moisture for each soil layer to a depth of 50 cm were presented in Table 1.…”
Section: Methodsmentioning
confidence: 99%
“…The soil is the typical cambisol soil with pH 6.3. The organic carbon content is 8.83 g/kg, and nitrogen, phosphorus, and potassium contents are 1.04, 0.50 and 22.62 g/kg (Cai et al 2017). The soil bulk density, soil field capacity, and wilting coefficient of the soil moisture for each soil layer to a depth of 50 cm were presented in Table 1.…”
Section: Methodsmentioning
confidence: 99%
“…Maize farmland ecosystems have intense human intervention relative to forests, grasslands and other ecosystems. Nevertheless, few explicit conclusions have been drawn with respect to applicability of land surface models over maize farmland ecosystems, and few studies on the RWU process have been conducted [26].…”
Section: Discussionmentioning
confidence: 99%
“…Root distribution and RWU are important components of any RWU parameterization scheme and have been proven to be the key to improving simulation accuracy of land surface models with rational optimization [16,26]. The optimization for root distribution and RWU both increase model performance by improving the vertical distribution of SWC, but the mechanisms used to realize this and the magnitude of improvement in SWC differ.…”
Section: Discussionmentioning
confidence: 99%
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