Spatial Analysis of Infiltration in an Oxisol of the Eastern Plains of Colombia

Studies that involve soil attributes variability help the analysis of the behavior of hydrophysical attributes in space, to support the decision-making process within the conception of precision agriculture. The aim of the present paper was to characterize the spatial variability of the surface infi...

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Autores principales: Orjuela-Matta,Helber Milton, Rubiano Sanabria,Yolanda, Camacho-Tamayo,Jesus H
Lenguaje:English
Publicado: Instituto de Investigaciones Agropecuarias, INIA 2012
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Acceso en línea:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-58392012000300015
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spelling oai:scielo:S0718-583920120003000152018-10-01Spatial Analysis of Infiltration in an Oxisol of the Eastern Plains of ColombiaOrjuela-Matta,Helber MiltonRubiano Sanabria,YolandaCamacho-Tamayo,Jesus H Geostatistics hydraulic conductivity infiltration sorptivity Studies that involve soil attributes variability help the analysis of the behavior of hydrophysical attributes in space, to support the decision-making process within the conception of precision agriculture. The aim of the present paper was to characterize the spatial variability of the surface infiltration and its relation to some soil physical attributes. The sampling was done with a rectangular mesh of 64 points with perpendicular distances of 52 m x 45 m between sampling points. The attributes studied were bulk density, contents of sand, silt and clay, soil moisture, cumulative infiltration, basic infiltration, sorptivity, and saturated hydraulic conductivity (Ks). Data were analyzed using descriptive statistics and geostatistics, identifying the relationship between attributes, using the Pearson correlation and cluster analysis. Results suggest a behavior of parameters close to normal, attributes related to soil water movement had greater variability, with low basic infiltration (1.46 cm h-1) and Ks (0.80 cm h-1), which together with high values of bulk density (1.87 g cm-3) show limitations by compaction. Cumulative infiltration and Ks attributes did not fit to models of spatial distribution, finding ranges of 150 m for the other attributes, distance to optimize future sampling for the study of spatial variability. Pearson correlation and cluster analysis allowed establishing relationships between soil attributes; spatial relationships were corroborated in contour maps, where we observed the influence of clay and sand content in the behavior of bulk density, and the influence of these attributes in processes of water infiltration into the soil.info:eu-repo/semantics/openAccessInstituto de Investigaciones Agropecuarias, INIAChilean journal of agricultural research v.72 n.3 20122012-09-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-58392012000300015en10.4067/S0718-58392012000300015
institution Scielo Chile
collection Scielo Chile
language English
topic Geostatistics
hydraulic conductivity
infiltration
sorptivity
spellingShingle Geostatistics
hydraulic conductivity
infiltration
sorptivity
Orjuela-Matta,Helber Milton
Rubiano Sanabria,Yolanda
Camacho-Tamayo,Jesus H
Spatial Analysis of Infiltration in an Oxisol of the Eastern Plains of Colombia
description Studies that involve soil attributes variability help the analysis of the behavior of hydrophysical attributes in space, to support the decision-making process within the conception of precision agriculture. The aim of the present paper was to characterize the spatial variability of the surface infiltration and its relation to some soil physical attributes. The sampling was done with a rectangular mesh of 64 points with perpendicular distances of 52 m x 45 m between sampling points. The attributes studied were bulk density, contents of sand, silt and clay, soil moisture, cumulative infiltration, basic infiltration, sorptivity, and saturated hydraulic conductivity (Ks). Data were analyzed using descriptive statistics and geostatistics, identifying the relationship between attributes, using the Pearson correlation and cluster analysis. Results suggest a behavior of parameters close to normal, attributes related to soil water movement had greater variability, with low basic infiltration (1.46 cm h-1) and Ks (0.80 cm h-1), which together with high values of bulk density (1.87 g cm-3) show limitations by compaction. Cumulative infiltration and Ks attributes did not fit to models of spatial distribution, finding ranges of 150 m for the other attributes, distance to optimize future sampling for the study of spatial variability. Pearson correlation and cluster analysis allowed establishing relationships between soil attributes; spatial relationships were corroborated in contour maps, where we observed the influence of clay and sand content in the behavior of bulk density, and the influence of these attributes in processes of water infiltration into the soil.
author Orjuela-Matta,Helber Milton
Rubiano Sanabria,Yolanda
Camacho-Tamayo,Jesus H
author_facet Orjuela-Matta,Helber Milton
Rubiano Sanabria,Yolanda
Camacho-Tamayo,Jesus H
author_sort Orjuela-Matta,Helber Milton
title Spatial Analysis of Infiltration in an Oxisol of the Eastern Plains of Colombia
title_short Spatial Analysis of Infiltration in an Oxisol of the Eastern Plains of Colombia
title_full Spatial Analysis of Infiltration in an Oxisol of the Eastern Plains of Colombia
title_fullStr Spatial Analysis of Infiltration in an Oxisol of the Eastern Plains of Colombia
title_full_unstemmed Spatial Analysis of Infiltration in an Oxisol of the Eastern Plains of Colombia
title_sort spatial analysis of infiltration in an oxisol of the eastern plains of colombia
publisher Instituto de Investigaciones Agropecuarias, INIA
publishDate 2012
url http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-58392012000300015
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