2012
DOI: 10.1590/s0100-06832012000600007
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Atributos físicos relacionados à compactação de solos sob vegetação nativa em região de altitude no Sul do Brasil

Abstract: RESUMOA compactação causada por atividades antrópicas altera os atributos físicos do solo, causando redução na produtividade e impactos ao ambiente. Muitos estudos sobre esse tema têm sido realizados em solos agrícolas, porém poucas são as informações em áreas com vegetação nativa, nas quais, geralmente, os teores de matéria orgânica são mais elevados. Assim, é oportuno avaliar a relação entre os atributos físicos relacionados à compactação, nessas condições, a fim de estabelecer valores de referência para pro… Show more

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Cited by 39 publications
(27 citation statements)
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“…This way, soil density elevation comes from grain-size related factors such as a large amount of fine sand (FS) within total sand fraction in contrast to the other fractions as medium sand fraction (MS), coarse sand (CS) and very coarse sand (VCS) ( Table 1). This result validate the findings of LUCIANO et al (2012), who worked with two Humic Cambisols and two Litholic Neosols (Humic Litholic Nitosol and Dystrophic Litholic Neosol). Soil total porosity (Pt), which is another important indicative of soil quality, was also not influenced by TWW applications in this present study.…”
Section: Resultssupporting
confidence: 90%
“…This way, soil density elevation comes from grain-size related factors such as a large amount of fine sand (FS) within total sand fraction in contrast to the other fractions as medium sand fraction (MS), coarse sand (CS) and very coarse sand (VCS) ( Table 1). This result validate the findings of LUCIANO et al (2012), who worked with two Humic Cambisols and two Litholic Neosols (Humic Litholic Nitosol and Dystrophic Litholic Neosol). Soil total porosity (Pt), which is another important indicative of soil quality, was also not influenced by TWW applications in this present study.…”
Section: Resultssupporting
confidence: 90%
“…proporcional desses parâmetros que também foi verificado por Braida et al (2006) Luciano et al (2012) observaram uma faixa mais ampla de 1,02 a 1,81 g cm -3 para Dsmáx e de 0,14 a 0,48 g g -1 para Ugc, na camada de 5 a 10 cm, ao analisarem Neossolos, Nitossolos, e Cambissolos. Os autores relataram que a variação na Dsmáx foi maior nos solos com menor teor de carbono orgânico total (12 a 40 g kg -1 ).…”
Section: Resultsunclassified
“…Pois com o aumento no teor de água, ocorre redução da coesão. A água atua como lubrificante entre as partículas de solo, permitindo o deslizamento e o empacotamento das partículas quando este é submetido a algum tipo de pressão (Luciano et al, 2012).…”
Section: Introductionunclassified
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“…In the constructed minesoil, the aggregation results are likely also derived from soil particle cohesion, due to intense machine traffic carried out in soil construction, as already discussed by Stumpf et al (2014). This type of condition was also reported in minesoils by Sencindiver and Ammons (2000) and in agricultural soils by Rev Bras Cienc Solo 2016;40:e0150482 Voorhees (1983), Carpenedo and Mielniczuk (1990), Topp et al (1997), Bergamin et al (2010), and Conte et al (2011).The soil used in recomposition of the mined area can reach its final construction stage in varying degrees of disintegration and compaction (Akala and Lal, 2001), and the use of machines at soil moisture close to the plastic limit is the main factor that causes compaction, since water reduces cohesion and acts as a lubricant between soil particles, allowing sliding and packing of particles when the soil is subjected to some sort of pressure (Luciano et al, 2012).…”
Section: Resultsmentioning
confidence: 99%