首页> 外文期刊>Agronomy for Sustainable Development >Plant age and rock phosphate effects on the organic resource quality of herbaceous legume residues and their N and P release dynamics.
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Plant age and rock phosphate effects on the organic resource quality of herbaceous legume residues and their N and P release dynamics.

机译:植株年龄和磷矿粉对草本豆科植物残体有机资源质量的影响及其氮,磷的释放动态。

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摘要

Many tropical agro-ecosystems rely on organic resources for nutrient provision. Various factors affect the nutrient release dynamics of organic resources, including application of external nutrients during their growth and their age or physiological stage at the time of harvest. Understanding relationships between organic resource management factors and the resulting nutrient release dynamics is important for optimizing nutrient recovery by crops and minimizing nutrient losses to the environment. Here, Mucuna pruriens and Lablab purpureus legumes were grown on a 'slope' and 'plateau' field, treated or not with rock phosphate, and sampled from 12 to 30 weeks after planting. These plant residues were then incubated in a sandy soil under laboratory conditions and mineral N and Olsen-extractable P dynamics were measured for 28 days. Our results showed that plant age had an impact on N, P and polyphenol contents. Application of rock phosphate only altered the P content of the legumes on the 'plateau' field, which had a lower soil-available P content. We also observed that mineral N dynamics of the organic resources varied between -62% of the added N released after 28 days, indicating net immobilization, and +23%, indicating net mineralization, with most organic resources showing an initial N immobilization phase. N release was negatively related to the lignin-to-N and (lignin+polyphenol)-to-N ratios of the organic resources. Lastly, we observed that the net release of Olsen P relative to the control soil varied between 0.4 and 4.9 mg kg-1 and that net P release was positively related to the P content of the organic resources. In summary, legume age was the parameter that most strongly influenced the quality of the legume residues, and consequently its N and P release dynamics, with potentially significant consequences for N and P uptake recovery and losses and, ultimately, cropping system sustainability.
机译:许多热带农业生态系统依靠有机资源来提供营养。各种因素都会影响有机资源的养分释放动态,包括外部养分在生长过程中的应用以及收获时的年龄或生理阶段。了解有机资源管理因素与养分释放动态之间的关系,对于优化农作物的养分回收和最大程度地减少对环境的养分流失至关重要。在这里,毛uc豆和扁豆豆科植物生长在“坡地”和“高原”田地上,用或不使用磷酸盐岩处理,并在种植后的12至30周内取样。然后将这些植物残留物在实验室条件下的沙质土壤中温育,并测定N和Olsen可萃取的矿物质磷动力学28天。我们的结果表明,植物年龄对氮,磷和多酚含量有影响。磷酸盐岩的施用仅改变了“高原”田地中豆类的磷含量,而土壤中可利用的磷含量较低。我们还观察到,有机资源的矿质N动态在28天后释放的添加N的-62%(表明净固定化)和+ 23%(表明净矿化)之间变化,大多数有机资源显示出初始N固定阶段。氮的释放与有机资源中木质素对氮的比率和(木质素+多酚)对氮的比率负相关。最后,我们观察到Olsen P相对于对照土壤的净释放量在0.4和4.9 mg kg-1之间变化,并且净P释放量与有机资源中的P含量呈正相关。总而言之,豆科植物年龄是最强烈影响豆科植物残留物质量的参数,因此,其氮和磷的释放动态对氮和磷的吸收恢复和损失以及最终对作物系统的可持续性具有潜在的重大影响。

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