首页> 外文期刊>Journal of soils & sediments >Organic residue and agricultural lime interactions on CO_2 emissions from two contrasting soils: implications for carbon management in acid soils
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Organic residue and agricultural lime interactions on CO_2 emissions from two contrasting soils: implications for carbon management in acid soils

机译:两种对比土的CO_2排放的有机残留物和农业石灰相互作用:酸性土壤中碳管理的影响

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Purpose Agricultural lime (aglime) has been recognised to promote the production of CO(2)from acid soils. However, the role of organic residues in controlling the magnitude of these emissions is poorly understood. This study, therefore, investigated the interactive effects of aglime and organic residues on inorganic- and organic-derived CO(2)emissions from two contrasting acid soils. Materials and methods The experiment was carried out as a completely randomised 2 x 2 x 4 factorial design where two contrasting acid soils (Nariva clay series, Mollic Fluvaquents and Piarco loam series, Typic Kanhaplaquults) were amended with varying rates of(13)C-enriched aglime (0% w/w and 0.230% w/w (CaCO3,C)-C-13-C-13 5.99% atom abundance) and organic residues (0% w/w and 1% w/w corn stover, poultry litter, or glucose) to give a total of 16 treatment combinations. These treatments were triplicated, resulting in 48 experimental units that were incubated for 103 days in 1-L media bottles. Results and discussion The mineralisation of carbon (C) in the Piarco soil increased by 27% with aglime addition relative to the no-organic residue control but decreased (by as much as 13.2%) when applied to the organic residue-amended soils. This interaction was, however, not evident in the Nariva soil, which may be attributed to the fact that aglime-induced priming effects were negligible in this soil. Results also show that the rate of aglime-CO(2)emissions decreased with the application of poultry litter and corn stover, and increased with the application of glucose. This effect was particularly evident in the Piarco soil and is likely related to the organic residue-induced changes in the soil pH. Conclusions Overall, our results highlight the importance of considering organic residue addition when assessing the global warming effect associated with aglime use. In addition to crop nutrition benefits, our results further emphasise the need to optimise liming and organic residue management practices to enhance C sequestration in acid soils.
机译:目的,农业石灰(Alllime)已被认识到促进酸性土壤的CO(2)的生产。然而,有机残留在控制这些排放量的范围中的作用是较差的。因此,本研究研究了来自两个对比酸性土壤的无机 - 和有机衍生的CO(2)排放对无机和有机衍生的CO(2)排放的互动影响。实验的材料和方法是作为完全随机的2×2×4因子设计进行的,其中两个对比酸性土壤(Nariva Clay系列,Mollic Flyva和Piarco Loam系列,典型Kanhaplaquards)被修改,不同的速率(13)C-富含搅拌(0%w / w和0.230%w / w(caco3,c)-c-13-c-13 5.99%原子丰度)和有机残留物(0%w / w和1%w / w玉米秸秆,家禽垃圾或葡萄糖)总共提供16种治疗组合。这些治疗是一式三份,导致48个实验单元在1-L介质瓶中孵育103天。结果与讨论Piarco土壤中的碳(C)的矿化在施加到有机残留物修正的土壤中时,Piarco土壤中的碳(C)中的碳(C)增加了27%,并且相对于无有机残留对照减少(通过多达13.2%)。然而,这种相互作用在Nariva土壤中没有明显,这可能归因于在这种土壤中止痛引起的引发效应可以忽略不计的事实。结果还表明,随着家禽凋落物和玉米秸秆的应用,Aglime-Co(2)排放率降低,并随着葡萄糖的应用而增加。这种效果在Piarco土壤中特别明显,并且可能与有机残留物诱导的土壤pH的变化有关。结论总体而言,我们的结果突出了考虑在评估与哑铃使用相关的全球变暖效果时考虑有机残留的重要性。除了作物营养效益外,我们的结果还强调需要优化雷明和有机残留管理实践,以增强酸性土中的C螯合。

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