Monitoring soil sealing in Guadarrama River basin, Spain, and its potential impact in agricultural areas

This study analyzes soil sealing and its repercussions in the loss of fertile soils, which are more appropriate for agriculture use. Also, soil sealing increases flood risk. The main objective is to estimate soil loss by sealing in the Guadarrama River Basin (Madrid, Spain) between 1961 and 2011. Th...

Descripción completa

Detalles Bibliográficos
Autores: Pérez González, María Eugenia, García Rodríguez, María Del Pilar
Tipo de recurso: artículo
Fecha de publicación:2016
País:España
Institución:Universidad Complutense de Madrid (UCM)
Repositorio:Docta Complutense
Idioma:español
OAI Identifier:oai:docta.ucm.es:20.500.14352/24358
Acceso en línea:https://hdl.handle.net/20.500.14352/24358
Access Level:acceso abierto
Palabra clave:528.9
911.2
910.2:004
Soil sealing
Impact
Remote sensing
Madrid
Sellado de suelos
Impacto
Teledetección
Cartografía
Geografía física
Sistemas de información geográfica
2505.02 Cartografía Geográfica
2505.07 Geografía Física
Descripción
Sumario:This study analyzes soil sealing and its repercussions in the loss of fertile soils, which are more appropriate for agriculture use. Also, soil sealing increases flood risk. The main objective is to estimate soil loss by sealing in the Guadarrama River Basin (Madrid, Spain) between 1961 and 2011. The combination of digital rocessing (Normalized Difference Vegetation Index (NDVI), principal components and convolution filters) of satellite imagery with the digital terrain model helps to detect risk areas and allows quick updating of sealed soil mapping. The supervised classifications of the images were used to estimate the actual soil loss by sealing (9% in 2011) in the Guadarrama River Basin and the types and agrologic classes that have been lost. Soil loss occurs to a greater extent in highly permeable soils (sands) and in the most fertile soils. The main sealed soil associations are luvisols (alfisols), regosols (entisols) and cambisols (inceptisols).