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Layer: MUESTRAS SUELOS (3)

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Layer: MAPA SUELOS CYL 1987 IRNASA-CSIC (5)

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Layer: Fases (6)

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Description: Las fases indican caracteres limitantes relacionados con características superficiales o subsuperficiales de los suelos. No están relacionadas directamente con la formación del suelo y normalmente sobrepasan y cruzan los límites adoptados para las unidades de suelo (Mapa de Suelos del Mundo, leyenda revisada FAO-Unesco de 1988). La fase lítica indica suelos en los que predomina la presencia de una roca continua, dura y coherente, que es limitante para el desarrollo de algunos cultivos. La fase de gravas indica suelos en los que predomina un horizonte superficial con más del 30% de gravas en peso. Las fases representadas en esta capa son las del Mapa de suelos a escala 1/500.000 del IRNASA-CSIC.

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Layer: Clasificación FAO 1974 modificada (7)

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Description: Clasificación de los suelos de Castilla y León según la Base de Referencia Mundial para Recursos de Suelos (WRB). El color aplicado a cada tesela del mapa, se ha establecido para el gran Grupo de Suelo de Referencia (GSR) y su calificador correspondiente (segundo nivel en la estructura de la WRB), más abundante en la asociación de suelos descrita en la unidad cartográfica (SMU). Mapa de suelos a escala 1/500.000 del IRNASA-CSIC, del año 1988, reeditado por el ITACyL en el año 2011. La información completa de las SMU se puede consultar haciendo clic con el ratón sobre la tesela.

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Description: Contenido de arcilla expresado como porcentaje del peso total de la tierra fina de la muestra. Según el criterio USDA (United States Department of Agriculture), son partículas de arcilla las que tienen un diámetro menor de 0,002 mm. La capa se ha obtenido mediante interpolación de 6.924 muestras de suelo realizada mediante el método geoestadístico Universal Kriging. En el modelo entran variables explicativas climáticas (régimen de temperatura, pluviometría, período libre de heladas y suma de grados día), derivadas del Modelo Digital de Elevaciones e intensidad de la actividad agraria. En el proceso de interpolación se generan en algunos casos valores imposibles para la variable considerada; estas zonas se agrupan en la clase “No interpolado”. La imagen resultante tiene una resolución de 500 metros de pixel.

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Layer: Humedad de Saturación (17)

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Description: Contenido de humedad en la matriz del suelo cuando todos sus poros están llenos de agua. Está expresado como humedad volumétrica en porcentaje, es decir, el volumen de la fracción líquida con respecto al volumen de la muestra de suelo. La capa se ha obtenido mediante álgebra de mapas con las imágenes interpoladas de textura y materia orgánica siguiendo las fórmulas empíricas de Saxton y Rawls que relacionan el contenido de arcilla, arena, limo y materia orgánica de un suelo con sus características hidráulicas, entre ellas la humedad de saturación. Todas estas fórmulas así como su obtención se describen en la publicación de 2006 “Soil Water Characteristic Estimates by Texture and Organic Matter for Hydrologic Solutions” de estos mismos autores.

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Layer: Capacidad de Campo (18)

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Description: Contenido de humedad presente en la matriz del suelo tras drenar libremente durante 2 o 3 días después de una lluvia o un riego abundante. Está expresado como humedad volumétrica en porcentaje, es decir, el volumen de la fracción líquida con respecto al volumen de la muestra de suelo. La capa se ha obtenido mediante álgebra de mapas con las imágenes interpoladas de textura y materia orgánica siguiendo las fórmulas empíricas de Saxton y Rawls que relacionan el contenido de arcilla, arena, limo y materia orgánica de un suelo con sus características hidráulicas, entre ellas la capacidad de campo. Todas estas fórmulas así como su obtención se describen en la publicación de 2006 “Soil Water Characteristic Estimates by Texture and Organic Matter for Hydrologic Solutions” de estos mismos autores.

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Layer: Punto de Marchitez (19)

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Description: Contenido de agua de un suelo retenida tan firmemente que las plantas no pueden extraerla causándoles una marchitez irreversible. Está expresado como humedad volumétrica en porcentaje, es decir, el volumen de la fracción líquida con respecto al volumen de la muestra de suelo. La capa se ha obtenido mediante álgebra de mapas con las imágenes interpoladas de textura y materia orgánica siguiendo las fórmulas empíricas de Saxton y Rawls que relacionan el contenido de arcilla, arena, limo y materia orgánica de un suelo con sus características hidráulicas, entre ellas el punto de marchitez. Todas estas fórmulas así como su obtención se describen en la publicación de 2006 “Soil Water Characteristic Estimates by Texture and Organic Matter for Hydrologic Solutions” de estos mismos autores.

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Layer: Capacidad de Rentención de Agua (20)

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Description: Representa la máxima cantidad de agua disponible para las plantas que puede almacenar un determinado suelo. Es la diferencia entre el contenido de agua a capacidad de campo y el contenido de agua a punto de marchitez. Está expresado como humedad volumétrica en porcentaje, es decir, el volumen de la fracción líquida con respecto al volumen de la muestra de suelo. Para el cálculo de este parámetro se utilizan los mapas de Capacidad de Campo y Punto de Marchitez calculados a su vez, a partir de los mapas interpolados de arcilla, limo, arena y materia orgánica. Este mapa se calcula como diferencia de los mapas de Punto de Marchitez y de Capacidad de Campo.

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Layer: Permeabilidad (21)

Name: Permeabilidad

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Description: La permeabilidad define la velocidad con la que un suelo saturado transmite el agua a su través bajo la influencia de la gravedad. Un suelo está saturado cuando todos sus poros están llenos de agua y, por lo tanto, el valor de la permeabilidad está en su máximo. Este valor se expresa en mm por día. La capa se ha obtenido mediante álgebra de mapas con las imágenes interpoladas de textura y materia orgánica siguiendo las fórmulas empíricas de Saxton y Rawls que relacionan el contenido de arcilla, arena, limo y materia orgánica de un suelo con sus características hidráulicas, entre ellas la permeabilidad. Todas estas fórmulas así como su obtención se describen en la publicación de 2006 “Soil Water Characteristic Estimates by Texture and Organic Matter for Hydrologic Solutions” de estos mismos autores.

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Layer: pH (22)

Name: pH

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Description: El pH se define como el logaritmo decimal negativo de la actividad de los protones en la fase líquida del suelo, de manera que, cuanto menor es el valor del pH, mayor es la acidez o la actividad de los protones. La reacción del suelo (o grado de acidez, basicidad o neutralidad) es una propiedad físico-química que se expresa por medio del pH. Para la obtención de la capa, se ha realizado una interpolación espacial de los datos de pH mediante el método geoestadístico Ordinary Kriging. Para esta interpolación se utilizaron 6.859 muestras de la Base de Datos de suelos de Castilla y León.

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Layer: Fósforo Olsen en ppm (23)

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Layer: Potasio en ppm (24)

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Layer: Contenido Nitratos Agua Riego en mg/l (25)

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Layer: Nivel de P Olsen en ppm. Valoración en suelos de secano. (26)

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Description: El mapa se ha obtenido estimando las ppm de P mediante el algoritmo de aprendizaje por computación Random Forest. La estimación de la variable se realizó a partir de 10.312 muestras de suelo georreferenciadas a nivel de parcela. Las variables auxiliares utilizadas han sido las derivadas del Modelo Digital del Terreno (altimetría, pendiente, orientación, rugosidad), las asociadas a la textura del suelo (contenido de arcilla, limo y arena), las asociadas al contenido y movimiento de agua en el suelo (por ejemplo, la capacidad de campo, el punto de marchitez y la permeabilidad en saturación) y aquellas relacionadas con la climatología de la zona (por ejemplo, precipitación media, temperatura media y amplitud térmica, entre otras).

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Layer: Nivel de K en ppm. Valoración en suelos de secano. (27)

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Description: Estimación de las ppm de K mediante el algoritmo de aprendizaje por computación Random Forest. La estimación de la variable se realizó a partir de 11.402 muestras de suelo georreferenciadas a nivel de parcela. Las variables auxiliares utilizadas fueron las derivadas del Modelo Digital del Terreno (altimetría, pendiente, orientación, rugosidad), las asociadas a la textura del suelo (contenido de arcilla, limo y arena), las asociadas al contenido y movimiento de agua en el suelo (por ejemplo, la capacidad de campo, el punto de marchitez y la permeabilidad en saturación) y aquellas relacionadas con la climatología de la zona (por ejemplo, precipitación media, temperatura media y amplitud térmica, entre otras).

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