Effect of Mineral N on C and N Dynamics of Rice and Wheat Residues under Different Moisture Levels

ljaz Ali, G. Nabi
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Abstract

Crop residue mineralization affects soil carbon (C) and nitrogen (N) dynamics during crop residue management in crop production. C and N mineralization dynamics of rice and wheat residues incorporated with and without mineral N under two moisture conditions were evaluated under laboratory conditions. Mineral N was applied @ 0.015 g/Kg (»30 Kg/ha), whereas soil moisture was maintained at high (» – 15 KPa, near field capacity) and at low (» – 500 KPa)moisture levels during course of study.Periodic determinations on CO2 – C and N mineralized were performed over a period of 120 days. The highest peaks for CO2 – C occurred during first week of the study which then reduced gradually until it attained an equilibrium. High moisture level enhanced CO2 – C flux by 14% than low moisture level. Combined application of crop residues and mineral N released 17% more CO2 – C than crop residue treatments without mineral N.In residue applied treatments, immobilization was 40% higher at high moisture level than that at low moisture level. Application of rice and wheat residues in combination with mineral N caused both immobilizations followed by mineralization phases at both moisture levels. At high moisture level, maximum immobilization occurred during initial 15 days, while at low moisture level it continued till about 30 days. After day15, mineralization started which continued to increase during remaining period of study at high moisture and at low moisture mineralization initiated from day 60 onward. Mineralization in rice residue was faster than that in wheat residues. Immobilization of N continued progressively in residue alone treated soils at both moisture levels during study period. In residue treated soils, increase in soil moisture increased soil organic carbon (SOC) and soil water stable aggregates (WSA) significantly by 14% and 55% over control respectively.Combined application of crop residues and mineral N increased SOC by 43% and WSA by 59%. This study indicated that incorporation of crop residues along with addition of mineral N in the presence of optimum moisture promoted its faster decomposition with a quicker mineral N release, more organic matter build up and soil structure improvement than crop residues incorporated without mineral N.
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不同水分水平下矿质氮对稻麦秸秆碳氮动态的影响
作物残茬矿化影响作物生产中作物残茬管理过程中土壤碳(C)和氮(N)动态。在实验室条件下,研究了水稻和小麦秸秆在含氮和不含氮条件下的碳氮矿化动态。在研究过程中,施用0.015 g/Kg (30 Kg/ha)矿物氮,而土壤湿度保持在高(近田容量> > 15 KPa)和低(> > 500 KPa)的水平。在120天内对CO2 - C和N矿化进行周期性测定。CO2 - C的峰值出现在研究的第一周,然后逐渐降低,直到达到平衡。高湿度比低湿度提高了14%的CO2 - C通量。作物残茬与矿质氮联合施用比不施用矿质氮的作物残茬处理释放的CO2 - C多17%。在作物残茬处理中,高水分条件下固定化效果比低水分条件下高出40%。水稻和小麦秸秆与矿质氮结合施用在两种水分水平下都引起了固定和矿化阶段。在高湿度条件下,最大的固定化发生在最初的15天,而在低湿度条件下,固定化持续到30天左右。在第15天之后,矿化开始,在剩余的研究期间,高湿度矿化继续增加,从第60天开始,低湿度矿化开始。水稻渣矿化速度快于小麦渣矿化速度。在研究期间,在两种水分水平下,残渣单独处理的土壤中,氮的固定化都在逐步进行。在残茬处理的土壤中,土壤水分的增加使土壤有机碳(SOC)和土壤水稳定团聚体(WSA)分别比对照显著增加14%和55%。作物残茬与矿质氮配施可使土壤有机碳增加43%,使土壤水分减少59%。本研究表明,在最佳水分条件下,与不施用矿质氮的作物秸秆相比,施用矿质氮的作物秸秆分解更快,矿质氮释放更快,有机质积累更多,土壤结构改善更明显。
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