volume 67, issue 1, P78-83 2010
DOI: 10.1590/s0103-90162010000100011
View full text
|
|
Share

Abstract: ABSTRACT: Surface roughness is influenced by type and intensity of soil tillage among other factors, and it changes considerably with rain. In microrelief studies the advantages of using indices such as the fractal dimension, D, and the crossover length, l, is that they allow the partition of the roughness characteristics into properties that depend purely on the scale and on a scale free component, respectively. On the other hand, some geostatistical parameters may provide different ways to understand soil s…

Expand abstract

Search citation statements

Order By: Relevance

Citation Types

0
8
0

Paper Sections

0
0
0
0
0

Publication Types

0
0
0
0

Relationship

0
0

Authors

Journals