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Versión aceptada (postprint) disponible en el espacio personal del siguiente repositorio: https://www.ucm.es/carlos-martinez-hernandez/publications-repository Afiliación del autor Carlos Martínez-Hernández en el momento de publicación del artículo: Departamento de Geografía, Universidad de Murcia. The study was supported by the RECARE Project (No. 603498) from the European Union Seventh Framework Programme (No. FP7/2007-2013). Referencias bibliográficas: • Al-Kaisi, M M, Yin, X H, Licht, M A, Soil carbon and nitrogen changes as influenced by tillage and cropping systems in some Iowa soils. Agr Ecosyst Environ 105 (2005), 635–647. • Arnáez, J, Lasanta, T, Errea, M P, Ortigosa, L, Land abandonment, landscape evolution, and soil erosion in a Spanish Mediterranean mountain region: the case of Camero Viejo. Land Degrad Dev 22 (2011), 537–550. • Bell, S, Alves, S, de Oliveira, E S, Zuin, A, Migration and land use change in Europe: A review. Living Rev Landscape Res, 4, 2010, 2. • Bienes, R, Marqués, M J, Sastre, B, García-Díaz, A, Ruiz-Colmenero, M, Eleven years after shrub revegetation in semiarid eroded soils. Influence in soil properties. Geoderma 273 (2016), 106–114. • Breton, V, Crosaz, Y, Rey, F, Effects of wood chip amendments on the revegetation performance of plant species on eroded marly terrains in a Mediterranean mountainous climate (Southern Alps, France). Solid Earth 7 (2016), 599–610. • Cammeraat, E, van Beek, R, Kooijman, A, Vegetation succession and its consequences for slope stability in SE Spain. Plant Soil 278 (2005), 135–147. • Cerdà A, Soil erosion after land abandonment in a semiarid environment of southeastern Spain. Arid Soil Res Rehab 11 (1997), 163–176. • Cerdà A, Effects of rock fragment cover on soil infiltration, interrill runoff and erosion. Eur J Soil Sci 52 (2001), 59–68. • Cerdà A, González-Pelayo, Ó Giménez-Morera, A, Jordán, A, Pereira, P, Novara, A, Brevik, E C, Prosdocimi, M, Mahmoodabadi, M, Keesstra, S, Orenes, F G, Ritsema, C J, Us, Abandonment of agricultural land results in on- and off-site consequences for the ecosystem. In this study, 105 rainfall simulations were carried out in agriculture lands of the Mediterranean belt in Spain (vineyards in Málaga, almond orchards in Murcia, and orange and olive orchards in Valencia) and in paired abandoned lands to assess the impact of land abandonment on soil and water losses. After abandonment, soil detachment decreased drastically in the olive and orange orchards, while vineyards did not show any difference and almond orchards registered higher erosion rates after the abandonment. Terraced orchards of oranges and olives recovered a dense vegetation cover after the abandonment, while the sloping terrain of almond orchards and vineyards enhanced the development of crusts and rills and a negligible vegetation cover resulted in high erosion rates. The contrasted responses to land abandonment in Mediterranean agricultural lands suggest that land abandonment should be programmed and managed with soil erosion control strategies for some years to avoid land degradation., Unión Europea, Depto. de Didáctica de las Ciencias Experimentales , Sociales y Matemáticas, Fac. de Educación, TRUE, pub

Versión aceptada (postprint) disponible en el espacio personal del siguiente repositorio: https://www.ucm.es/carlos-martinez-hernandez/publications-repository -Premio Wiley al artículo más citado en la revista "Hidrological Processess" (JCR-Q1) en 2017. -Afiliación del autor Carlos Martínez-Hernández en el momento de publicación del artículo: Departamento de Geografía, Universidad de Murcia. Referencias bibliográficas: • Abaci, O., & Papanicolaou, A. N. T. (2009). Long-term effects of management practices on water-driven soil erosion in an intense agricultural sub-watershed: Monitoring and modelling. Hydrological Processes, 23, 2818–2837. https://doi.org/10.1002/hyp.7380 • Alonso Sarría, F., & López Bermúdez, F. (1994). Rainfall time and space variability during short storms in South-East Spain. Geoökodynamik, 15(3), 261–278. • Alonso Sarría, F., Martínez Hernández, C., Belmonte Serrato, F., & Fernández Carrillo, M. A. (2016). Principales causas del abandono de cultivos en la Región de Murcia. In A. Romero Díaz (Ed.), Abandono de cultivos en la Región de Murcia. Consecuencias Ecogeomorfológicas (pp. 203–226). Murcia: Servicio de Publicaciones de la Universidad de Murcia. • Arnaez, J., Lasanta, T., Errea, M. P., & Ortigosa, L. (2011). Land abandonment, landscape evolution, and soil erosion in a Spanish Mediterranean mountain region: The case of Camero Viejo. Land Degradation and Development, 22, 537–550. https://doi.org/10.1002/ldr.1032 • Belmonte Serrato, F., Ruiz Sinoga, J. D., Romero Díaz, A., Martínez Hernández, C., & Robledano Aymerich, F. (2013). Medida de la conductividad hidráulica mediante infiltrómetros de minidisco en suelos agrícolas cultivados y en abandono (Región de Murcia). In Espacios insulares y de frontera, una visión geográfica (pp. 287–296). Palma de Mallorca: Universitat de les Illes Balears. • Bienes, R., Marques, M. J., Sastre, B., García-Díaz, A., & Ruiz-Colmenero, M. (2016). Eleven years after shrub revegetation in semiarid eroded soils. In, Soil erosion by water in abandoned dry terraces is one of the most important environmental problems in semiarid areas, enhancing biological degradation and reducing possible resources that can be obtained. However, little is known about the effects of the types of lithology and soil properties on the early stages of soil erosion. Therefore, the main aim of this research was to assess the effect of different lithologies (marls, limestones, and metamorphic—phyllites, schists, and greywackes—materials) and soil properties on the early stages of soil erosion by water in abandoned dry terraces, compared with similar terraces still in agricultural use. Soil analyses (texture, aggregate stability, and bulk density) and 22 rainfall simulations were carried out under dry conditions. During the experiments, local inclination, vegetation and stone cover, total organic matter, and antecedent soil moisture were also quantified. The results showed that the highest soil loss (41.41 g/m2 in cultivated plots and 17.05 g/m2 in the abandoned plots) and runoff (3.79 L/m2 in the abandoned plot) occurred on marl substrata. Marls also showed the shallowest infiltration front (9 cm) and lowest infiltration rate (4.3 cm/min). Limestones and, especially, metamorphic areas, showed a lower degree of soil erosion, higher infiltration rates, and deeper infiltration fronts., Fundación Séneca, Ministerio de Educación, Cultura y Deporte del Gobierno de España, Depto. de Didáctica de las Ciencias Experimentales , Sociales y Matemáticas, Fac. de Educación, TRUE, pub