Antonio Jordán, University of Seville, Sevilla, Spain Most Gypsisols are formed when gypsum (calcium sulfate) from gypsiferous parent materials is dissolved and moves through soil water, precipitating in an accumulation soil horizons. Triassic rock outcrops in almost all Andalusia consist mainly of red and variegated clays and in some cases by clays of different colors are known as the iridescent ...[Read More]
Monday paper: Short-term changes in soil Munsell colour value, organic matter content and soil water repellency after a spring grassland fire in Lithuania
Pereira P, Úbeda X, Mataix-Solera J, Oliva M, Novara A: Short-term changes in soil Munsell colour value, organic matter content and soil water repellency after a spring grassland fire in Lithuania. Solid Earth, 5, 209-225. DOI: 10.5194/se-5-209-2014. Abstract Fire is a natural phenomenon with important implications on soil properties. The degree of this impact depends upon fire severity, the ecosy ...[Read More]
Monday paper: Thermal shock and splash effects on burned gypseous soils from the Ebro Basin (NE Spain)
León J, Seeger M, Badía D, Peters P, Echevarría T: Thermal shock and splash effects on burned gypseous soils from the Ebro Basin (NE Spain). Solid Earth, 5, 131-140. DOI: 10.5194/se-5-131-2014. Abstract Fire is a natural factor of landscape evolution in Mediterranean ecosystems. The middle Ebro Valley has extreme aridity, which results in a low plant cover and high soil erodibility, especially on ...[Read More]
Connectivity: an emerging issue
Antonio Jordán (University of Seville, Spain) Paulo Pereira (Mykolas Romeris University, Lithuania) Saskia Keesstra (Wageningen University, The Netherlands) Artemi Cerdà (University of Valencia, Spain) What is connectivity? Over the recent decades, a growing number of studies have highlighted the role of hydrological and sediment connectivity processes in relation to watershed management, t ...[Read More]