2010
DOI: 10.1016/s1002-0160(10)60008-2
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Nitrate and Ammonium Leaching in Variable- and Permanent-Charge Paddy Soils

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Cited by 39 publications
(12 citation statements)
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“…Higher NH 4 + -N leaching has been observed in soil with variable charges and soils with low CEC and a low content of exchangeable base cations (Chen and Zu 2007;Xiong et al 2010). The results of the present study coincided with the findings of Xiong et al (2010) who reported that NH 4 + -N makes up to 92% of the total inorganic N in the leachate. Our results confirmed that NH 4 + -N movement in soil is greatly influenced by irrigation regimes and that the vast potential risk of NH 4 + -N leaching deserves more attention.…”
Section: N Dynamics and Leaching In Paddy Soilsupporting
confidence: 89%
See 1 more Smart Citation
“…Higher NH 4 + -N leaching has been observed in soil with variable charges and soils with low CEC and a low content of exchangeable base cations (Chen and Zu 2007;Xiong et al 2010). The results of the present study coincided with the findings of Xiong et al (2010) who reported that NH 4 + -N makes up to 92% of the total inorganic N in the leachate. Our results confirmed that NH 4 + -N movement in soil is greatly influenced by irrigation regimes and that the vast potential risk of NH 4 + -N leaching deserves more attention.…”
Section: N Dynamics and Leaching In Paddy Soilsupporting
confidence: 89%
“…Furthermore, the changes in soil chemical and mineralogical properties result in significant variations in the NH 4 + -N adsorption capacity (Liu et al 2007). Higher NH 4 + -N leaching has been observed in soil with variable charges and soils with low CEC and a low content of exchangeable base cations (Chen and Zu 2007;Xiong et al 2010). The results of the present study coincided with the findings of Xiong et al (2010) who reported that NH 4 + -N makes up to 92% of the total inorganic N in the leachate.…”
Section: N Dynamics and Leaching In Paddy Soilmentioning
confidence: 99%
“…Another factor that may influence the forms of N that are leached is the type of surface charge of soil colloids. Xiong et al (2010), in an experiment with soil columns, found greater leaching of NH + 4 than of NO − 3 in soils with variable charge, contrary to the results obtained in soils with permanent charge. The soils in our study have mineral composition similar to that of Xiong et al (2010) (hydroxy-Al interlayered vermiculites, kaolinites; data not shown) and high organic matter content, therefore with variable charge also prevailing.…”
Section: Ammonium Nitrate and Phosphorusmentioning
confidence: 56%
“…Xiong et al (2010), in an experiment with soil columns, found greater leaching of NH + 4 than of NO − 3 in soils with variable charge, contrary to the results obtained in soils with permanent charge. The soils in our study have mineral composition similar to that of Xiong et al (2010) (hydroxy-Al interlayered vermiculites, kaolinites; data not shown) and high organic matter content, therefore with variable charge also prevailing. These results can be due to the presence of positive surface charge on some variable-charge compounds when pH value is acid or subacid, then making it difficult for the cations to be adsorbed into the soil, whereas dominate negative charges in soils having a permanent charge are an advantage to cations being retained.…”
Section: Ammonium Nitrate and Phosphorusmentioning
confidence: 56%
“…At the 50 cm depth in the sandy loam soil that we studied, in organic treatments, the presence of the oxidized zone close to the reduced soil zone was conductive for the transformation of NH 4 -N mineralized from organic manure to NO 3 -N. However, the continuous anaerobic conditions (under flood irrigation, until 1 week before harvest) at the 180 cm depth maintained NH 4 -N as the main form of inorganic N, more so than NO 3 -N. Particularly, in continuously flooded paddy soils with abundant organic substrate and a limited availability of electron acceptors, the reduction of NO 3 -N to NH 4 -N would be more efficient than the formation of N 2 , so NH 4 -N concentrations can be an order of magnitude higher than those of NO 3 -N [21], [22], [23], [24]. This situation also occurs in soils with low CEC and a low content of exchangeable base cations [19], [25], [26], [27]. From the depth of 50 cm to 180 cm, average NH 4 -N and NO 3 -N concentrations decreased by about 5–10% and 47–70%, respectively, in fertilized organic treatments (B1A1, B2A1 and B3A1).…”
Section: Discussionmentioning
confidence: 99%