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Effects of long-term fertilisation on soil organic carbon sequestration after a 34-year rice-wheat rotation?in Taihu Lake Basin

机译:长期施肥对34岁米 - 小麦旋转后土壤有机碳封存的影响?在太湖盆地

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To evaluate the long-term effects of fertilisation on soil organic carbon (SOC) sequestration in rice-wheat cropping ecosystems, SOC dynamics, stocks and fractionation were determined. The treatments included no fertiliser, mineral N and P, mineral N, P and K, organic fertiliser (OF), OF plus NP and OF plus NPK. The results showed that the average carbon inputs that derived from crop stubble, root residues and organic fertilisers were between 1.47 and 4.33 t/ha/year over the past 34 years. The average SOC stocks measured in the samples collected in 2011–2013 ranged from 31.20 to 38.52 t/ha. The range of the SOC sequestration rate was 0.11–0.40 t/ha/year with a SOC sequestration efficiency of 6.3%. Overall, organic fertilisation significantly promoted C-input, SOC and the sequestration rate compared to mineral fertilisation. The "active pool" (very labile and labile fractions) and "passive pool" (less labile and recalcitrant fractions) accounted for about 71.0% and 29.0% of the SOC fractions, respectively. Significant positive relationships between C-inputs and SOC fractions indicated that SOC was not saturated in this typical rice-wheat cropping system, and fertilisation, especially organic amendment, is an effective SOC strategy sequestration.
机译:为了评估施肥对稻米种植生态系统,SOC动力学,股票和分馏中土壤有机碳(SOC)螯合的长期影响。该治疗包括没有肥料,矿物质N和P,矿物质N,P和K,有机肥(OF)的加入NP和加上NPK。结果表明,在过去34年内,源自作物茬,根残留物和有机肥的平均碳投入源于1.47%至4.33吨/公顷。在2011-2013中收集的样品中测量的平均SOC股,范围为31.20至38.52吨/公顷。 SOC螯合率的范围为0.11-0.40t / ha /年,SOC螯合效率为6.3%。总体而言,与矿物精相比,有机施肥显着促进了C型,SOC和螯合率。 “活动池”是指“活动池”。 (非常不稳定和不稳定的分数)和“被动池”。 (较少的不稳定和醋酸分数)分别占SOC级分的约71.0%和29.0%。 C型和SOC分数之间的显着阳性关系表明,SOC在这种典型的稻米种植系统中没有饱和,施肥,尤其是有机修正,是一种有效的SOC策略封存。

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