蒂夫顿85灌溉草地施氮后土壤物理质量

M. L. A. D. Melo, Eduardo Vieira Guimarães, B. M. Silva, É. L. D. Costa, Samuel Petraccone Caixeta
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摘要

蒂夫顿85 (Cynodon sp.)是一种广泛用于批量生产的饲料作物,但如果管理得当,它也有可能促进土壤结构质量的保存或改善。本研究的目的是评价巴西MG Prudente de Morais地区Tifton 85轮牧区施用无机氮肥和有机氮肥对土壤物理质量的影响。处理包括不同形式的氮供应:尿素400 kg / h1;400公斤/公顷牛粪;尿素和粪肥按1:1的比例施用,不施氮肥。施氮2年后,测定了0.00 ~ 0.05 m和0.05 ~ 0.10 m土层的土壤物理质量指标:保水性曲线、总孔隙度、大孔隙度、微孔隙度、土壤容重、有效水容量、土壤体积空气容量、土壤基质空气容量和相对水容量。两层处理之间存在差异。总的来说,牛粪处理促进了土壤水分的储存和有效性,这与有机质效应导致土壤微孔隙度增加有关。然而,这些相同的处理呈现出相对的压实,这与保持较高的土壤湿度有关。结论是,即使在集约放牧的影响下,土壤的物理质量一般也很好,但建议特别注意土壤对压实的易感性。
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SOIL PHYSICAL QUALITY AFTER NITROGEN FERTILIZERS USE IN IRRIGATED PASTURE OF TIFTON 85
Tifton 85 ( Cynodon sp.) is a forage crop widely used for the voluminous production, but it has also the potential to promote preservation or improvement in soil structural quality, when well managed. The aim of this work was to evaluate the soil physical quality in a rotational grazing area of Tifton 85 under irrigation in Prudente de Morais, MG, Brazil, due to the application of mineral and organic nitrogen fertilizers. The treatments included different forms of N supply: 400 kg ha -1 of urea; 400 kg ha -1 of bovine manure; 400 kg ha -1 of urea and manure, in proportion 1:1 and the control, without nitrogen fertilization. The following soil physical quality indicators were determined in the layers 0.0-0.05 m and 0.05-0.10 m after two years of N application: water retention curve, total porosity, macroporosity, microporosity, soil bulk density, available water capacity, bulk soil air capacity, soil matrix air capacity and relative water capacity. There were differences among the treatments, in both layers. In general, the treatments using bovine manure promoted greater water storage and availability, which was related to the increase of the microporosity, due to the organic matter effect. However, these same treatments presented a relative compaction, which was associated to the maintenance of higher soil moistures. It was concluded that, even under the effects of intensive grazing, there was generally adequate soil physical quality, but a special attention is recommended to the soil susceptibility to compaction.
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