Critical limits of the degree of compactness and soil penetration resistance for the soybean crop in N Brazil |
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| Authors: | Pedro Daniel De Oliveira Michel Keisuke Sato Herdjania Veras de Lima Sueli Rodrigues Alvaro Pires da Silva |
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| Affiliation: | 1. Universidade Federal Rural da Amaz?nia– UFRA, Research of Soil Physics, Institute of Agricultural Sciences, Av. Presidente Tancredo Neves, 2501, Belém, Pará, P.O. Box 66077‐830, Brazil.;2. Escola Superior de Agricultura Luiz de Queiro–ESALQ/USP, Research of Soil Physics, Department of Soil Science, Av. Pádua Dias, 11, Piracicaba, S?o Paulo, P.O. Box 13418‐900, Brazil. |
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| Abstract: | In agricultural fields soil compaction is a major cause of physical degradation. Degree of compactness (DC) is a useful parameter for characterizing compaction and the response of crops for different soils. The objectives of this study were: (1) to identify the critical DC and PR values for soybean Glycine max (L.) Merrill] using plant growth variables and (2) to verify the relationship between DC and PR, and assess which parameter is recommended for the evaluation of soil compaction. The study was conducted in a greenhouse in a completely randomized factorial design of 4 textures × 5 compaction levels for sandy loam and sandy clay loam soils, and 3 compaction levels for the clayey and very clayey soils. Soil samples were collected from the surface of a Xantic Kandiudox from the NE region of the State of Pará, Brazil. The DC was calculated from the maximum bulk density obtained by the Proctor test, and the PR curve was determined in undisturbed samples equilibrated in different matric potentials. The growth and development of the soybean was favored in the DC range of 80 to 85%, regardless of soil texture. The critical degree of compactness for the growth of soybean was around 98% regardless of soil texture, while the critical values for penetration resistance at field capacity varied according to soil texture and bulk density and were 28.2, 5.6, 3.5, and 5.2 MPa for the sandy loam, sand clay loam, clayey and very clayey soils, respectively. The root length was the plant growth variable most susceptible to soil compaction. Change in soil penetration resistance was poorly related with change in degree of compactness showing that one parameter cannot be replaced by the other. Because PR is quickly determined in field and have a direct relationship with plant growth, for the soils evaluated in this study we recommend the use of soil PR to assess the state of soil compaction. |
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| Keywords: | root growth proctor test maximum bulk density Amazonian soils |
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