Phosphorus Stock Depletion and Soil C:N:P Stoichiometry Under Annual Crop Rotations and Grassland Management Systems Over 13 Years

IF 2.1 Q3 SOIL SCIENCE Frontiers in soil science Pub Date : 2022-07-22 DOI:10.3389/fsoil.2022.863122
André Somavilla, L. Caner, I. B. D. da Silva, D. Rheinheimer, A. Chabbi
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Abstract

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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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
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。
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