2016
DOI: 10.1007/s11368-016-1443-0
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Assessing chemical soil tests for predicting nitrogen mineralization in paddy soils of the Dongting Lake region in China

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Cited by 3 publications
(2 citation statements)
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“…However, the reverse was true in the case of the higher proportion (more than 45%) of organic fertilizer treatment, such as GM 6 in this study. The delaying effect of the combined fertilizer with higher proportion of organic nitrogen affected the normal color change of leaves at late growth stage, and even led to stay‐green and yield reduction, which is consistent with the previous studies in conventional rice cultivation (Li et al., 2014, 2015; Lv et al., 2001; Qiu et al., 2005; Ren et al., 2005; Tang et al., 2019; Tian et al., 2012; Zhang et al., 2009). Further analysis of 13 CO 2 pulse labeling test confirmed that different configurations of organic and inorganic fertilizers used in the main crop season had a carryover effect on its ratooning rice (Table 6, Zang et al., 2019).…”
Section: Discussionsupporting
confidence: 91%
“…However, the reverse was true in the case of the higher proportion (more than 45%) of organic fertilizer treatment, such as GM 6 in this study. The delaying effect of the combined fertilizer with higher proportion of organic nitrogen affected the normal color change of leaves at late growth stage, and even led to stay‐green and yield reduction, which is consistent with the previous studies in conventional rice cultivation (Li et al., 2014, 2015; Lv et al., 2001; Qiu et al., 2005; Ren et al., 2005; Tang et al., 2019; Tian et al., 2012; Zhang et al., 2009). Further analysis of 13 CO 2 pulse labeling test confirmed that different configurations of organic and inorganic fertilizers used in the main crop season had a carryover effect on its ratooning rice (Table 6, Zang et al., 2019).…”
Section: Discussionsupporting
confidence: 91%
“…The values of the SON mineralization rate constant (k0) ranged from 0.1026 to 0.1207, with little overall variation at 30% and 60% WHC, but was different at 90% WHC. Further, k0 was mainly affected by the physical and chemical properties of the soil when external conditions changed little (Li et al, 2019). In this study, RM and RC soils were tidal paddy soil developed from lacustrine deposits such that k0 of RM and RC had no difference at 30% and 60% WHC, while large k0 existed at 90% WHC.…”
Section: Effects Of Rc On Soil Organic N Mineralizationmentioning
confidence: 78%