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Organic carbon dynamics in soils with pyrogenic organic matter that received plant residue additions over seven years

机译:七年来接受植物残渣添加的热解有机质土壤中的有机碳动态

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The effect of repeated application of plant residues on mineralization of different organic carbon (OC) pools in a pyrogenic organic matter (PyOM) amended soil was determined using an incubation study conducted over 7.1 years. At five occasions during this period, sugarcane residues (C-4) were mixed with the soil (C-4) with or without PyOM (C-3) amendments. Organic C mineralized during the incubation period or remaining in different physical soil fractions after 7.1 years was partitioned into PyOM carbon (PyOM-C) and native soil organic matter C (nSOM-C) or sugarcane C plus nSOM-C (SC-C + nSOM-C). When compared to the control, total cumulative OC (comprising both nSOM-C and PyOM-C) mineralized in the presence of PyOM was 40% higher after the first 2.5 years, but equal by 6.2 years and 3% lower by the end of the incubation period. The cumulative nSOM mineralization after 7.1 years was 2.57 mg CO2-C g(-1) soil with PyOM compared to 3.16 mg CO2-C g(-1) soil without PyOM addition (p = 0.13; n = 3). More than 60% of the added PyOM-C was present in the free-light fraction by the end of the 7.1 years. In total, 93% of the added PyOM-C remained in soil compared to 25-28% of SC-C + nSOM-C. Sugarcane residues increased the remaining PyOM-C in the occluded-light fraction by 3% (p 0.05) and in the organo-mineral fraction by 4% (p 0.1), suggesting a possible preferential use of SC-C or accumulation of metabolites of decomposed PyOM. However, the addition of sugarcane had no significant effect on overall mineralization of PyOM. The presence of PyOM accelerated the mineralization of SC-C + nSOM-C by 9% (p 0.001). This is probably due to enhanced mineralization of sugarcane residues rather than native SOM. Although PyOM was likely to accelerate mineralization of added plant residues throughout a 7-year period, PyOM did not increase cumulative nSOM mineralization when plant residues were absent (p > 0.05), so PyOM may reduce nSOM mineralization in the long term. (C) 2015 Elsevier Ltd. All rights reserved.
机译:使用一项历时7.1年的孵化研究,确定了重复施用植物残渣对热解有机质(PyOM)改良土壤中不同有机碳(OC)库矿化的影响。在此期间,有五次将甘蔗残渣(C-4)与土壤(C-4)混合,添加或不添加PyOM(C-3)。在孵化期中矿化的有机碳或在7.1年后保留在不同物理土壤碎片中的有机碳被分为PyOM碳(PyOM-C)和天然土壤有机质C(nSOM-C)或甘蔗C加nSOM-C(SC-C + nSOM-C)。与对照相比,在存在PyOM的情况下矿化的总累积OC(包括nSOM-C和PyOM-C)在开始的2.5年后升高了40%,但在6.2年后升高了6.2%,在结束时降低了3%。潜伏期。 7.1年后的累积nSOM矿化为PyOM的土壤为2.57 mg CO2-C g(-1),而未添加PyOM的土壤为3.16 mg CO2-C g(-1)(p = 0.13; n = 3)。到7.1年末,超过60%的添加的PyOM-C均以自由光形式存在。总计93%的PyOM-C残留在土壤中,而SC-C + nSOM-C的25-28%。甘蔗残留物使遮挡光部分的剩余PyOM-C增加了3%(p <0.05),有机矿物质部分的剩余PyOM-C增加了4%(p <0.1),表明可能优先使用SC-C或积累分解的PyOM的代谢产物。但是,添加甘蔗对PyOM的总体矿化作用没有显着影响。 PyOM的存在将SC-C + nSOM-C的矿化速度提高了9%(p <0.001)。这可能是由于甘蔗残渣的矿化作用增强,而不是由于天然SOM。尽管PyOM可能会在整个7年的时间里加速添加的植物残渣的矿化作用,但是当没有植物残渣时,PyOM不会增加累积的nSOM矿化作用(p> 0.05),因此PyOM可以长期降低nSOM的矿化作用。 (C)2015 Elsevier Ltd.保留所有权利。

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