玉米常规栽培和免耕管理制度下Oxisol的物理性质

Paula Regina de Oliveira, José Frederico Centuron, C. X. D. Almeida, Adilson Pelá, F. D. S. Pereira, M. Centurión
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摘要

寻找旨在保持土壤质量的土壤管理系统,以及可持续农业和农业管理是至关重要的。因此,本研究的目的是评估玉米生产常规和免耕管理制度下土壤的孔隙系统、土壤抗渗透能力、团聚体稳定性、相对土壤密度和S指数等土壤参数。将试验区土壤分为典型的中等质地土(LVd1)和典型的粘土质地土(LVd2)。试验设计为完全随机分割图,6个重复。样地(60 m2)包括6种土壤管理制度(1 - SD1LVd1 = 1年免耕;2 - SD8LVd1 = 8年免耕后;3 - SD10LVd1 = 10年免耕后;4 - CCLVd1 =常规播种;5 - SD12LVd2 = 12年免耕后;6 - CCLVd2 =常规播种),子样分为3个土层(0 ~ 0.10、0.10 ~ 0.20和0.20 ~ 0.30 m)。结果表明,在三个分析层中,中等质地的免耕播种密度较高;中等质地氧化土处理最大土壤密度值较高。这是因为粘土含量影响了大量的表面电荷和比表面积,从而降低了对土壤压实的敏感性。12年免耕播种玉米产量最低(5.9 Mg ha-1),可能是由于土壤表层形成致密层所致。
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Physical properties of Oxisol under conventional corn cultivation and no-till management systems
Searches for soil management systems that aim at maintaining soil quality are fundamental, along with sustainable agricultural and farming management. Thus, the aim of the present research was to assess soil parameters such as porous system, soil resistance to penetration, aggregate stability, relative soil density and the S index of an Oxisol under the conventional and no-till sowing management systems of corn production. They soils of the experimental areas were classified as a typical Oxisol with medium texture (LVd1) and typical Oxisol of clayey texture (LVd2). The experimental design was completely randomized split plot, with six replications. The plots (60 m2) consisted of six soil management systems (1 - SD1LVd1 = after one year no-till sowing; 2 - SD8LVd1 = after 8 years no-till sowing; 3 - SD10LVd1 = after 10 years no-till sowing; 4 - CCLVd1 = conventional sowing; 5 - SD12LVd2 = after 12 years no-till sowing; 6 - CCLVd2 = conventional sowing) and the subplots consisted of three soil layers (0-0.10, 0.10-0.20 and 0.20-0.30 m deep). The results showed that in three analyzed layers, the no-till sowing on medium texture Oxisol had higher densities. Treatments of medium texture Oxisol showed higher values of maximum soil density. This occurred because the clay content influenced a larger quantity of surface charges and specific surface area which decreased the susceptibility to soil compacting. The 12-year-old no-till sowing yielded the lowest corn productivity (5.9 Mg ha-1), probably due to the formation of compact layers, mainly near the soil surface.
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