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Spatial and daily variability of soil moisture content in three agroforestry systems/Variabilidad espacial y diaria del contenido de humedad en el suelo en tres sistemas agroforestales

The objective of this study was to determine the level of soil spatial variability in an area consisting of the land uses: Quesungual slash and mulch agroforestry system with less than two years (QSMASQ), Slash-and-burn traditional system (SB) and Secondary forest (SF). Soil samples were taken in th...

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Published in:Acta agronomica (Palmira) 2009-04, Vol.58 (2), p.75
Main Authors: Rivera Pena, Mariela, Collazos, Edgar Amezquita, Rao, Idupulapati, Menjivar Flores, Juan Carlos
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Collazos, Edgar Amezquita
Rao, Idupulapati
Menjivar Flores, Juan Carlos
description The objective of this study was to determine the level of soil spatial variability in an area consisting of the land uses: Quesungual slash and mulch agroforestry system with less than two years (QSMASQ), Slash-and-burn traditional system (SB) and Secondary forest (SF). Soil samples were taken in three parallel transects of 102 m in length, separated 9 meters. The profile was sampled in the depths from 0 to 5 cm, 5 to 10 cm, 10 to 20 cm and 20 to 40 cm in 6 points (09, 11 am and 05) during 9 days. Coefficient of variation for soil properties varied for bulk density (0.76 and 15.1 %), organic carbon (30.4 and 54.3%), volumetric moisture (9.5 and 23.5%), sand (12.8 and 22.5%) and clay (14.0 and 29.2%). The geo-statistical analysis showed that the random component of the spatial dependence was predominant over the nugget effect. The functions of semivariograms, structured for each variable were used to generate maps of interpolated contours at a fine scale. The Moran (1) autocorrelation indicated that sampling ranges less than 9 m would be adequate to detect spatial structure of the volumetric moisture variable. Keywords: Spatial variability; soil moisture; bulk density; organic carbon. En seis puntos de tres transectos (102 m) paralelos (9 m) en tres sistemas de uso del terreno (Quesungual menor de dos anos, SAQ
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Soil samples were taken in three parallel transects of 102 m in length, separated 9 meters. The profile was sampled in the depths from 0 to 5 cm, 5 to 10 cm, 10 to 20 cm and 20 to 40 cm in 6 points (09, 11 am and 05) during 9 days. Coefficient of variation for soil properties varied for bulk density (0.76 and 15.1 %), organic carbon (30.4 and 54.3%), volumetric moisture (9.5 and 23.5%), sand (12.8 and 22.5%) and clay (14.0 and 29.2%). The geo-statistical analysis showed that the random component of the spatial dependence was predominant over the nugget effect. The functions of semivariograms, structured for each variable were used to generate maps of interpolated contours at a fine scale. The Moran (1) autocorrelation indicated that sampling ranges less than 9 m would be adequate to detect spatial structure of the volumetric moisture variable. Keywords: Spatial variability; soil moisture; bulk density; organic carbon. En seis puntos de tres transectos (102 m) paralelos (9 m) en tres sistemas de uso del terreno (Quesungual menor de dos anos, SAQ&lt;2, Tradicional de Tala y Quema, TQ y Bosque Secundario, BS) se tomaron muestras de suelo a cuatro profundidades (0-5 cm, 5-10 cm, 10-20 cm y 20 a 40 cm) y tres horas (09, 11 y 15) durante 9 dias. Se modelo el analisis estructural de la variacion de los parametros humedad volumetrica, densidad aparente, carbono organico, arena y arcilla. El coeficiente de variacion de los parametros evaluados presento rangos para densidad aparente (0.76 y 15.1 %), carbono organico (30.4 y 54.3%), humedad volumetrica (9.5 y 23.5%), arena (12.8 y 22.5%) y arcilla (14.0 y 29.2%). En los analisis geoestadisticos el componente al azar de la dependencia espacial predomino sobre el efecto pepita (nugget). Con las funciones de los semivariogramas estructurados para cada variable se generaron mapas de contorno interpolados a escala fina los cuales mostraron heterogeneidad en las propiedades evaluadas. La autocorrelacion de Moran (1) indico que rangos de muestreo menores a 9 m podrian ser adecuados para detectar la estructura espacial de la variable humedad volumetrica. 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Soil samples were taken in three parallel transects of 102 m in length, separated 9 meters. The profile was sampled in the depths from 0 to 5 cm, 5 to 10 cm, 10 to 20 cm and 20 to 40 cm in 6 points (09, 11 am and 05) during 9 days. Coefficient of variation for soil properties varied for bulk density (0.76 and 15.1 %), organic carbon (30.4 and 54.3%), volumetric moisture (9.5 and 23.5%), sand (12.8 and 22.5%) and clay (14.0 and 29.2%). The geo-statistical analysis showed that the random component of the spatial dependence was predominant over the nugget effect. The functions of semivariograms, structured for each variable were used to generate maps of interpolated contours at a fine scale. The Moran (1) autocorrelation indicated that sampling ranges less than 9 m would be adequate to detect spatial structure of the volumetric moisture variable. Keywords: Spatial variability; soil moisture; bulk density; organic carbon. En seis puntos de tres transectos (102 m) paralelos (9 m) en tres sistemas de uso del terreno (Quesungual menor de dos anos, SAQ&lt;2, Tradicional de Tala y Quema, TQ y Bosque Secundario, BS) se tomaron muestras de suelo a cuatro profundidades (0-5 cm, 5-10 cm, 10-20 cm y 20 a 40 cm) y tres horas (09, 11 y 15) durante 9 dias. Se modelo el analisis estructural de la variacion de los parametros humedad volumetrica, densidad aparente, carbono organico, arena y arcilla. El coeficiente de variacion de los parametros evaluados presento rangos para densidad aparente (0.76 y 15.1 %), carbono organico (30.4 y 54.3%), humedad volumetrica (9.5 y 23.5%), arena (12.8 y 22.5%) y arcilla (14.0 y 29.2%). En los analisis geoestadisticos el componente al azar de la dependencia espacial predomino sobre el efecto pepita (nugget). Con las funciones de los semivariogramas estructurados para cada variable se generaron mapas de contorno interpolados a escala fina los cuales mostraron heterogeneidad en las propiedades evaluadas. La autocorrelacion de Moran (1) indico que rangos de muestreo menores a 9 m podrian ser adecuados para detectar la estructura espacial de la variable humedad volumetrica. 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Soil samples were taken in three parallel transects of 102 m in length, separated 9 meters. The profile was sampled in the depths from 0 to 5 cm, 5 to 10 cm, 10 to 20 cm and 20 to 40 cm in 6 points (09, 11 am and 05) during 9 days. Coefficient of variation for soil properties varied for bulk density (0.76 and 15.1 %), organic carbon (30.4 and 54.3%), volumetric moisture (9.5 and 23.5%), sand (12.8 and 22.5%) and clay (14.0 and 29.2%). The geo-statistical analysis showed that the random component of the spatial dependence was predominant over the nugget effect. The functions of semivariograms, structured for each variable were used to generate maps of interpolated contours at a fine scale. The Moran (1) autocorrelation indicated that sampling ranges less than 9 m would be adequate to detect spatial structure of the volumetric moisture variable. Keywords: Spatial variability; soil moisture; bulk density; organic carbon. En seis puntos de tres transectos (102 m) paralelos (9 m) en tres sistemas de uso del terreno (Quesungual menor de dos anos, SAQ&lt;2, Tradicional de Tala y Quema, TQ y Bosque Secundario, BS) se tomaron muestras de suelo a cuatro profundidades (0-5 cm, 5-10 cm, 10-20 cm y 20 a 40 cm) y tres horas (09, 11 y 15) durante 9 dias. Se modelo el analisis estructural de la variacion de los parametros humedad volumetrica, densidad aparente, carbono organico, arena y arcilla. El coeficiente de variacion de los parametros evaluados presento rangos para densidad aparente (0.76 y 15.1 %), carbono organico (30.4 y 54.3%), humedad volumetrica (9.5 y 23.5%), arena (12.8 y 22.5%) y arcilla (14.0 y 29.2%). En los analisis geoestadisticos el componente al azar de la dependencia espacial predomino sobre el efecto pepita (nugget). Con las funciones de los semivariogramas estructurados para cada variable se generaron mapas de contorno interpolados a escala fina los cuales mostraron heterogeneidad en las propiedades evaluadas. La autocorrelacion de Moran (1) indico que rangos de muestreo menores a 9 m podrian ser adecuados para detectar la estructura espacial de la variable humedad volumetrica. Palabras clave: Variabilidad espacial; humedad de suelo; densidad aparente; carbono organico.</abstract><pub>Universidad Nacional de Colombia - Sede Palmira</pub></addata></record>
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title Spatial and daily variability of soil moisture content in three agroforestry systems/Variabilidad espacial y diaria del contenido de humedad en el suelo en tres sistemas agroforestales
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