13年轮作和草地管理下磷储量耗竭与土壤C:N:P化学计量特征

IF 2.1 Q3 SOIL SCIENCE
André Somavilla, L. Caner, I. B. D. da Silva, D. Rheinheimer, A. Chabbi
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引用次数: 0

摘要

磷(P)营养对植物产量和土壤有机质(SOM)输入都至关重要。然而,植物对磷的持续提取和生物量收获会导致土壤磷储量枯竭,作物产量下降,最终导致土壤有机质输入减少。本研究分析了13年来永续耕地(CC)和刈割永续草地(GG)在0 ~ 30 cm表层土壤中磷、碳、氮的变化趋势。此外,我们用31P-NMR表征了P有机形态的变化。结果表明,在13年内,GG的磷排泄量比CC多10%(分别为295和268 kg hm -1)。在CC和GG管理体系下(分别为0.30和0.25 Mg ha-1),总磷储量均有所减少。这种减少主要发生在总Pi形态中,GG和CC分别减少了0.75和0.29 Mg ha-1。GG组Po总存量增加42.6%;这些结果与GG中C和N储量增加(分别为2.6和0.19 Mg ha-1)和CC储量减少(分别为-4.2和-0.38 Mg ha-1)相一致。尽管磷耗竭主要影响稳定性最高的磷库(不稳定磷),但13年后由于磷库的缓冲能力较弱(中等不稳定磷),这种耗竭对植物产量没有负面影响。刈割永久性草地导致稳定磷库从无机形态向有机形态转变,土壤C和N储量增加。基于31P-NMR技术,永久性草地比永久性农田显著降低α-甘油磷酸,显著增加myo-IHP和单磷酸腺苷。尽管生产力没有显著下降,但应长期监测速效磷的耗竭,特别是在刈割的永久性草地作物中,以防止潜在的养分胁迫。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Phosphorus Stock Depletion and Soil C:N:P Stoichiometry Under Annual Crop Rotations and Grassland Management Systems Over 13 Years
Phosphorus (P) nutrition is essential to both plant yield and soil organic matter (SOM) input. However, continuous extraction of P by plants and biomass harvesting can lead to soil P stock depletion, a reduction in crop yields and ultimately a reduction in organic matter input to the soil. In this work, we analysed P, C and N stock trends in the 0-30 cm topsoil layer cultivated with permanent cropland (CC) and mowed permanent grassland (GG) for 13 years. In addition, we characterized the changes in P organic forms by using 31P-NMR. The results showed that the amount of P exported within 13 years was 10% greater in GG than in CC (295 and 268 kg ha-1, respectively). The total P stocks decreased under both the CC and GG management systems (0.30 and 0.25 Mg ha-1, respectively). This depletion was mainly observed in total Pi forms, which recorded reductions of 0.75 and 0.29 Mg ha-1 in GG and CC, respectively. The total Po stock increased by 42.6% in GG; these results were consistent with the increase in C and N stocks in GG (2.6 and 0.19 Mg ha-1, respectively) and their reduction in CC (-4.2 and -0.38 Mg ha-1, respectively). Although P depletion mainly affected the P pool presenting the highest lability (labile P), this depletion did not have a negative effect on plant yield after 13 years due to the buffering capacity of P pools presenting less lability (moderately labile P). Mowing permanent grasslands led to a change in the pool of labile P from inorganic to organic forms and an increase in soil C and N stocks. Based on the 31P-NMR technique, permanent grasslands significantly reduced α-glycerophosphate and increased myo-IHP and adenosine monophosphate more than the permanent cropland. Although there was no significant decrease in productivity, the depletion of available P should be monitored over time, especially in mown permanent grassland crops, to prevent potential nutrient stress.
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