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Effects of long-term chemical fertilization and organic amendments on dynamics of soil organic C and total N in paddy soil derived from barren land in subtropical China

机译:长期化学施肥和有机改良剂对亚热带贫瘠水稻田土壤有机碳和总氮动态的影响

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For better understanding the development of infertile paddy soils in subtropical China, a long-term field experiment of paddy soil was developed from barren land in 1990. Experimental treatments including NPK, NPKRS (NPK and rice straw), NPK2RS (NPK and double amount of rice straw), NPKPM (NPK and pig manure), and NPKGM (NPK and green manure (Astragalus sinicus L.)) were employed with rice-rice (Oryza sativa L.) cropping system. Rice yields, soil organic C (SOC) and total N were analyzed. In all of the treatments, early rice yields increased along cultivation years steadily, however late and annual rice yield was fluctuant between different years. From 1991 to 2006, average annual yield ranged from 7795 to 8572kghap# among different fertilizer treatments. Organic amendments usually enhanced rice yields significantly except for the treatment with NPKRS. SOC and total N contents of surface soil increased linearly with cultivated years from 3.9-5.7gkgp# and 0.46-0.57gkgp# in initial stage to 7.1-9.2gkgp# and 0.87-0.95gkgp# in 2005 respectively. Quantity and quality of input organic matter affected soil C dynamics and N balance. SOC sequestration rates were well correlated to modified organic C input, while SOC mineralization rates were related with either organic C input or SOC contents. Annual soil N accumulation was 13-18% of total input. However the net lost N, which was calculated based on fertilizer inputs, crop outputs, and annual N accumulation, was 44-49% in our study. In general, after 17 years' cultivation and fertilization management, rice yield reached a high level equivalent to the average yield of local high productivity paddy soils, whereas SOC and total N content were still less than half of those in high productivity paddy soils in this region.
机译:为了更好地了解中国亚热带的不育稻田土壤的发展,1990年从贫瘠的土地上进行了稻田土壤的长期田间试验。试验处理包括NPK,NPKRS(NPK和稻草),NPK2RS(NPK和两倍量的稻田)。稻草),NPKPM(NPK和猪粪)和NPKGM(NPK和绿肥(黄芪))与水稻(Oryza sativa L.)种植系统一起使用。分析了水稻的产量,土壤有机碳(SOC)和总氮。在所有处理中,早稻产量随耕作年稳步增长,但是晚稻和年稻产量在不同年份之间波动。从1991年到2006年,不同肥料处理的年平均产量在7795至8572kghap#之间。除用NPKRS处理外,有机改良剂通常可显着提高水稻产量。表层土壤的SOC和总氮含量随着耕种年限从最初的3.9-5.7gkgp#和0.46-0.57gkgp#线性增加,到2005年分别为7.1-9.2gkgp#和0.87-0.95gkgp#。输入有机质的数量和质量影响土壤碳动力学和氮平衡。 SOC的固存率与改良的有机碳输入量密切相关,而SOC矿化率与有机碳输入量或SOC含量相关。每年的土壤氮累积量为总投入量的13-18%。然而,在我们的研究中,根据肥料投入,作物产量和年度氮积累计算出的净氮净损失为44-49%。一般而言,经过17年的耕作和施肥管理,水稻的产量达到了相当于当地高产稻田平均产量的高水平,而SOC和总氮含量仍不到高产稻田的一半。地区。

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