|
Descripción
|
|
|---|---|
| Increased attention has been drawn to the variation of soil surface characteristics on a micro-scale. This is because soil surface constitutes the interface between soil and atmosphere and, consequently, it has implications for understanding water and heat fluxes, emission, and also when using remote sensing for soil evaluation. Soil surface microrelief may undergo rapid changes due to tillage and in tilled soil it may decay considerably under rainfall. As many natural and anthropogenic fractal-like structures, soil surface roughness is determined by a large number of generating processes operating at different scales. Such structures, termed multifractals, are characterized by fractional dimensions that vary in scale, and so require an infinite number of scaling exponents for their description, called a distributional spectrum. | |
|
Internacional
|
Si |
|
Nombre congreso
|
EGU General Assembly 2008 |
|
Tipo de participación
|
960 |
|
Lugar del congreso
|
Viena, Austria |
|
Revisores
|
Si |
|
ISBN o ISSN
|
1029-7006 |
|
DOI
|
|
|
Fecha inicio congreso
|
13/04/2008 |
|
Fecha fin congreso
|
18/04/2008 |
|
Desde la página
|
1 |
|
Hasta la página
|
2 |
|
Título de las actas
|
Geophysical Research Abstracts, Vol. 10, SRef-ID: 1607-7962/gra/EGU2008 |