L. B. Braos, Roberta Souto Carlos, A. C. T. Bettiol, Marina Ali Mere Bergamasco, Maira Caroline Terçariol, Manoel Evaristo Ferreira, Mara Cristina Pessôa da Cruz
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引用次数: 0
Abstract
Cover crops and N fertilization strongly impact the forms of soil organic C and N and their availability, which change the responses of plants to N fertilization and soil organic C accumulation. Our study objectives were to evaluate the effects of cover crops and N doses on soil total and soluble C and N contents, N fractions, and potentially available N in a long-term no-till experiment. The experiment was conducted in a randomized block design with split plots and four replicates. The main treatments were cover crops species, jack bean, lablab bean, millet, velvet bean, and fallow cultivated prior to maize. Secondary treatments included two doses of mineral N (0 and 120 kg ha−1). Soil samples were collected at depths of 0–5, 5–10, 10–20, and 20–40 cm, which were analyzed for total and water-soluble C and N contents, N fractions (acid hydrolysis method), and potentially available N (hot KCl solution and direct steam distillation methods). Cover crop velvet bean resulted in the highest soil organic carbon levels, and cover crop millet plus fertilization resulted in the highest levels of soil total N. The amino sugar was the largest N fraction, which decreased by 8% with N fertilization. The soluble C and N content strongly correlated with total and available N content. The changes in soil N were influenced by cover crop species and fertilization and the interactions of both, so the combination of fertilization regime and cover crops must be chosen with care. Additionally, legumes are a good source of plant and soil N in systems with low input of N via fertilizer; however, the combination of N fertilizer with legumes can reduce soil N reserves, leading to its long-term depletion.
覆盖作物和施氮对土壤有机碳和氮的形态及其有效性产生强烈影响,从而改变植物对施氮和土壤有机碳积累的响应。本研究的目的是评价覆盖作物和施氮量对长期免耕试验土壤总碳和可溶性碳、氮含量、氮组分和潜在有效氮的影响。试验采用随机区组设计,分图4个重复。主要处理为覆盖作物、豆角、小豆、谷子、绒豆和玉米前休耕。二次处理包括两个剂量的无机氮(0和120 kg ha - 1)。在0-5、5-10、10-20和20-40 cm深度采集土壤样品,分析总碳和水溶性碳、氮含量、N组分(酸水解法)和潜在有效氮(热氯化钾溶液和直接蒸汽蒸馏法)。覆盖作物蚕豆导致土壤有机碳含量最高,覆盖作物谷子加施氮肥导致土壤全氮含量最高,氨基糖是最大的氮组分,施氮后降低了8%。可溶性C和N含量与全氮和速效氮含量呈显著正相关。土壤氮的变化受覆盖作物种类和施肥及其相互作用的影响,因此应谨慎选择施肥制度和覆盖作物的组合。此外,在低氮肥输入系统中,豆科植物是植物和土壤氮的良好来源;而豆科作物配施氮肥会使土壤氮储量减少,导致土壤氮储量长期耗竭。