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Formation and stabilization of aggregates by the grass root system in an Oxisol

Grasses take direct action in the formation and stabilization of soil aggregates due to the density of roots and the release of organic exudates in soil. The objective of this study was to evaluate the effects of the root system of Brachiaria ruziziensis Germain et Evrard in the formation and stabilization of aggregates of an Oxisol. The experiment was conducted under greenhouse, using soil collected in the upper 0-20cm depth. Loosening the soil was manually and passed through a sieve of 2.00mm mesh size and subsequently separated by diameter classes of aggregates from 2.00-1.00, 1.00-0.50 and 0.50-0.25mm, with the help of specific mesh sieves. The experimental design was completely randomized in factorial 3x2x2x4, corresponding to three diameter classes of aggregates (2.00-1.00, 1.00-0.50 and from 0.50-0.25mm), two conditions crop (with and without grass), two moisture contents (100% and 60% of available water), and four sampling times (90, 180, 270 and 360 days after planting the grass), with four repetitions. The aggregate samples were packed in polyethylene vessels with a capacity of 10kg. The moisture content was balanced through irrigation every two days. Samples were taken every three months, determining the mean diameter of air-dried aggregates (DMPAs), the mean weight diameter of stable aggregates in water (DMPAu) and aggregate stability index (IAS = DMPAu/DMPAs). It was found higher values of DMPAu and IAS to treatment with grass, indicating that the root system of Brachiaria ruziziensis favored increased formation and stabilization of soil aggregates.

Brachiaria ruziziensis; roots; soil aggregation; water available


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