Use este identificador para citar ou linkar para este item: https://repositorio.ufba.br/handle/ri/6388
Registro completo de metadados
Campo DCValorIdioma
dc.contributor.authorVázquez, E. Vidal-
dc.contributor.authorMiranda, José Garcia Vivas-
dc.contributor.authorAlves, M. C.-
dc.contributor.authorGonzález, A. Paz-
dc.creatorVázquez, E. Vidal-
dc.creatorMiranda, José Garcia Vivas-
dc.creatorAlves, M. C.-
dc.creatorGonzález, A. Paz-
dc.date.accessioned2012-07-10T14:16:19Z-
dc.date.available2012-07-10T14:16:19Z-
dc.date.issued2006-
dc.identifier.issn0016-7061-
dc.identifier.urihttp://www.repositorio.ufba.br/ri/handle/ri/6388-
dc.descriptionRESTRITOpt_BR
dc.description.abstractSoil surface roughness is known to influence water infiltration, runoff and erosion. Soil surface roughness changes with management and weather and its mathematical description still remains an important issue. The main objective of this study was to investigate the effect of tillage on the two fractal indices, fractal dimension, D, and crossover length, l, currently used in characterizing soil surface microrelief. The statistical index random roughness, RR, was also assessed. Field experiments were done on an Alfisol located at Rio Grande do Sul State (Brazil). Two tillage treatments (conventional versus direct drilling) were tested. The soil surface microrelief was assessed by point elevation measurements in 16 plots for each treatment. The sampling scheme was a square grid with 20 × 20 mm between point spacing and the plot size was 280 × 280 mm, so that each data set consisted of 225 individual elevation points. All indices were calculated after trend removal, both by slope correction, i.e., oriented microrelief, and by slope plus tillage marks correction, i.e., random microrelief. The implemented algorithm for estimating D and l consisted in evaluating the roughness around the local root mean square deviation (RMS) of the point elevation values. Irrespective of tillage treatment and detrending procedure, fractal behavior extended only over a bounded range of scales, from 40 to 100 mm, due to the experimental setup. In these conditions, assessing fractal indices was not always straightforward. The statistical index RR and the fractal index l were significantly different between tillage treatments for oriented and random surface conditions. D values of random soil surfaces were not affected by tillage treatment, whereas D values of oriented microrelief were significantly lower in the direct drilled plots. Removal of tillage marks trend resulted in a significant increase in D values. Within each tillage treatment, l and D were significantly correlated.pt_BR
dc.language.isoenpt_BR
dc.publisherGeodermapt_BR
dc.sourcehttp://dx.doi.org/10.1016/j.geoderma.2006.03.012pt_BR
dc.subjectSoil roughnesspt_BR
dc.subjectFractal indicespt_BR
dc.subjectTillagept_BR
dc.subjectRoot mean squarept_BR
dc.subjectAlfisolpt_BR
dc.titleEffect of tillage on fractal indices describing soil surface microrelief of a Brazilian Alfisolpt_BR
dc.title.alternativeGeodermapt_BR
dc.typeArtigo de Periódicopt_BR
dc.identifier.numberv.134, n.3-4pt_BR
Aparece nas coleções:Artigo Publicado em Periódico (FIS)

Arquivos associados a este item:
Arquivo Descrição TamanhoFormato 
AA.pdf909,67 kBAdobe PDFVisualizar/Abrir


Os itens no repositório estão protegidos por copyright, com todos os direitos reservados, salvo quando é indicado o contrário.