Fractal approach in characterization of spatial pattern of soil properties

The objective of the study was to characterize spatial pattern of soil properties (CaCO3, soil organic carbon, P2O5, K2O, and clay content) using fractal concept. Total of 141 top-soil samples (0-30 cm) were collected on 1850 ha in karst polje (Petrovo polje, Croatia) and analyzed for listed soil pr...

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Main Authors: Boško Miloš, Aleksandra Bensa
Format: Article
Language:English
Published: Federation of Eurasian Soil Science Societies 2017-01-01
Series:Eurasian Journal of Soil Science
Subjects:
Online Access:http://ejss.fesss.org/10.18393/ejss.284260
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spelling doaj-7ce60ff3705b437dabb427261ddd3eac2020-11-25T02:26:13ZengFederation of Eurasian Soil Science SocietiesEurasian Journal of Soil Science 2147-42492147-42492017-01-0161202710.18393/ejss.284260Fractal approach in characterization of spatial pattern of soil propertiesBoško Miloš0Aleksandra Bensa1Institute for Adriatic Crops and Karst Reclamation, Split, CroatiaUniversity of Zagreb, Faculty of Agriculture, Soil Science Department, Zagreb, CroatiaThe objective of the study was to characterize spatial pattern of soil properties (CaCO3, soil organic carbon, P2O5, K2O, and clay content) using fractal concept. Total of 141 top-soil samples (0-30 cm) were collected on 1850 ha in karst polje (Petrovo polje, Croatia) and analyzed for listed soil properties. The semi-variogram method was used to estimate fractal dimension (D) value which was performed from both of isotropic and anisotropic perspective. The D value of soil properties ranged between 1.76 to 1.97, showing a domination of the short-range variations. The SOC and K2O fractal D values 1.79 and 1.76 respectively, exhibited a spatial continuity at the entire analysed range of the scale. The D value for P2O5 (1.97) showed a nearly total absence of the spatial structure at all scales. The CaCO3 and clay content indicated a multifractal behavior mainly attributed to effects of alluviation, differences in geology and its spatial changes and transitions. The results of anisotropic analysis of soil properties pattern have showed strong relations with directions and partial self-similarity over limited ranges of scales defined by scale-break. Finally, our results showed that fractal analysis can be used as a appropriate tool for the characterization of spatial pattern irregularities of soil properties and detection of soil forming factors that cause it.http://ejss.fesss.org/10.18393/ejss.284260Fractal dimensionscale independencyself-similaritysemi-variogram
collection DOAJ
language English
format Article
sources DOAJ
author Boško Miloš
Aleksandra Bensa
spellingShingle Boško Miloš
Aleksandra Bensa
Fractal approach in characterization of spatial pattern of soil properties
Eurasian Journal of Soil Science
Fractal dimension
scale independency
self-similarity
semi-variogram
author_facet Boško Miloš
Aleksandra Bensa
author_sort Boško Miloš
title Fractal approach in characterization of spatial pattern of soil properties
title_short Fractal approach in characterization of spatial pattern of soil properties
title_full Fractal approach in characterization of spatial pattern of soil properties
title_fullStr Fractal approach in characterization of spatial pattern of soil properties
title_full_unstemmed Fractal approach in characterization of spatial pattern of soil properties
title_sort fractal approach in characterization of spatial pattern of soil properties
publisher Federation of Eurasian Soil Science Societies
series Eurasian Journal of Soil Science
issn 2147-4249
2147-4249
publishDate 2017-01-01
description The objective of the study was to characterize spatial pattern of soil properties (CaCO3, soil organic carbon, P2O5, K2O, and clay content) using fractal concept. Total of 141 top-soil samples (0-30 cm) were collected on 1850 ha in karst polje (Petrovo polje, Croatia) and analyzed for listed soil properties. The semi-variogram method was used to estimate fractal dimension (D) value which was performed from both of isotropic and anisotropic perspective. The D value of soil properties ranged between 1.76 to 1.97, showing a domination of the short-range variations. The SOC and K2O fractal D values 1.79 and 1.76 respectively, exhibited a spatial continuity at the entire analysed range of the scale. The D value for P2O5 (1.97) showed a nearly total absence of the spatial structure at all scales. The CaCO3 and clay content indicated a multifractal behavior mainly attributed to effects of alluviation, differences in geology and its spatial changes and transitions. The results of anisotropic analysis of soil properties pattern have showed strong relations with directions and partial self-similarity over limited ranges of scales defined by scale-break. Finally, our results showed that fractal analysis can be used as a appropriate tool for the characterization of spatial pattern irregularities of soil properties and detection of soil forming factors that cause it.
topic Fractal dimension
scale independency
self-similarity
semi-variogram
url http://ejss.fesss.org/10.18393/ejss.284260
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