2015
DOI: 10.1016/j.agwat.2014.12.005
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Field analysis of water and nitrogen fate in lowland paddy fields under different water managements using HYDRUS-1D

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Cited by 102 publications
(65 citation statements)
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“…Therefore, soil salinity has been shown to reduce the µ w1 value under irrigation. Compared with µ w1 , the µ w2 value in our study ranged from 0.04 to 0.12 day -1 among the different soil salinity levels, and this result was similar to that of the studies by Li et al [31] and Tan et al [32]. Therefore, under irrigation, the effects of soil salinity on µ w2 could not be directly compared to the effects of irrigation water levels.…”
Section: Discussionsupporting
confidence: 71%
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“…Therefore, soil salinity has been shown to reduce the µ w1 value under irrigation. Compared with µ w1 , the µ w2 value in our study ranged from 0.04 to 0.12 day -1 among the different soil salinity levels, and this result was similar to that of the studies by Li et al [31] and Tan et al [32]. Therefore, under irrigation, the effects of soil salinity on µ w2 could not be directly compared to the effects of irrigation water levels.…”
Section: Discussionsupporting
confidence: 71%
“…1 ranged from 0.0024 to 0.1992 day -1 , which was reduced from 99.63% to 73.08% compared with that of the studies of Li et al [31] and Tan et al [32], respectively. The µ w1 value in Tan et al [32] ranged from 0.65 to 0.7 day -1 and the value in Li et al [31] was even larger at 0.74 day -1 , and these phenomena may have been caused by soil salinity because the study sites of Li et al [31] and Tan et al [32] are usually regarded as non-saline soils. Therefore, soil salinity has been shown to reduce the µ w1 value under irrigation.…”
Section: Discussionmentioning
confidence: 74%
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“…In the present study, the optimized parameter values by Singh et al [30] for rice crops (h 1 = 100 cm, h 2 = 55 cm, h 3 (high) = −160 cm, h 3 (low) = −250 cm, and h 4 = −15,000 cm were used to parameterize the water stress response proposed [29]. These parameters were also used by [2,19,20]. The parameters h 1 , h 2 , h 3 , and h 4 represent different pressure heads.…”
Section: Calculation Of Reference Evapotranspirationmentioning
confidence: 99%
“…As the water movement in a rice field is vertical due to constant ponding water condition, the one-dimensional model can be used effectively [12]. Furthermore, since the seepage in paddy plots is minimized, and water and solute transport can be simplified to a vertical movement [19], thus, the Hydrus-1D model can be used in the present study, even though it has been often used by many researchers to simulate water flow and solute transport in flooded rice fields [18,20]. Indeed, no study is reported yet on this important aspect in Malaysia.…”
Section: Introductionmentioning
confidence: 99%