首页> 外文期刊>Acta Agriculturae Scandinavica. Section B, Soil and Plant Science >Effect of different fertilization modes on soil organic carbon sequestration in acid soils
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Effect of different fertilization modes on soil organic carbon sequestration in acid soils

机译:不同施肥方式对酸性土壤有机碳固存的影响

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A meta-analysis of 297 treatment data from the Vezaiciai Branch of the Lithuanian Research Centre for Agriculture and Forestry long-term field experiment published from 2006 to 2015 was used to characterize the changes in SOC under different fertilization treatments and residue management practices in Lithuania's acid soil. A meta-analysis was performed to quantify the relative annual change (RAC) of SOC content and the average RAC rate of SOC under four fertilization modes (farmyard manure (FYM) (40 t ha(-1))); alternative organic fertilizers (in the manure background (40 t ha(-1))); FYM (60 t ha(-1)); alternative organic fertilizers (in the manure background (60 t ha(-1))) in two soil backgrounds (naturally acid and limed soil). The average RAC under four fertilization modes was 1.46 g kg(-1) yr(-1), indicating that long-term fertilization had considerable SOC sequestration potential. Incorporation of alternative organic fertilizers in unlimed soil showed negative effects (-0.39 and -0.66 g kg(-1) yr(-1)) in the observed long-term experiment. The RAC in the limed soil with incorporated organic fertilizers (FYM and alternative organic fertilizers), compared to the control, and varied from 0.25 g kg(-1) yr(-1) in the treatment with incorporated alternative organic fertilizers (in the manure background (40 t ha(-1))) to 0.71 g kg(-1) yr(-1) in the soil with FYM (60 t ha(-1)). In this study, the average RAC rate of SOC under organic fertilization treatments in limed soil (5.07-6.54%) was longer than organic fertilization in unlimed soil (2.11-3.49%), which might be attributed to the application of organic manure that would result in a slow release of fertilizer efficiency. Our results indicate that the application of manure (40 or 60 t ha(-1)) showed the greatest potential for C sequestration in agricultural soil and produced the longest SOC sequestration duration.
机译:2006年至2015年发布的立陶宛农林研究中心长期试验的Vezaiciai分支对297种处理数据的荟萃分析用于表征立陶宛酸中不同施肥处理和残留管理实践下SOC的变化。泥。进行荟萃分析,以量化四种施肥模式(农家肥(FYM)(40 t ha(-1)))下SOC含量的相对年变化(RAC)和SOC平均RAC率。替代有机肥料(在肥料背景下(40 t ha(-1))); FYM(60吨ha(-1));在两种土壤背景(天然酸和石灰土)中使用替代性有机肥料(在肥料背景下(60 t ha(-1)))。四种施肥模式下的平均RAC为1.46 g kg(-1)yr(-1),表明长期施肥具有相当大的SOC螯合潜力。在观察到的长期实验中,在未加盐的土壤中掺入替代有机肥料显示出负面影响(-0.39和-0.66 g kg(-1)yr(-1))。与对照相比,掺入有机肥料(FYM和替代有机肥料)的石灰土壤中的RAC在掺入替代有机肥料的处理中(粪肥中)为0.25 g kg(-1)yr(-1) FYM(60 t ha(-1))土壤中的背景(40 t ha(-1))至0.71 g kg(-1)yr(-1)。在这项研究中,石灰土壤有机肥处理下SOC的平均RAC速率(5.07-6.54%)比非石灰土壤有机肥处理下的平均RAC速率(2.11-3.49%)要长,这可能归因于有机肥的应用导致肥料效率缓慢释放。我们的结果表明,施用肥料(40或60 t ha(-1))在农业土壤中表现出最大的C固存潜力,并产生了最长的SOC固存持续时间。

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