Variation of infiltration rate through karstic surfaces due to land use changes: A case study in Murgia (SE-Italy) |
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| Authors: | Filomena Canora M Dolores Fidelibus Antonella Sciortino Giuseppe Spilotro |
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| Institution: | aDip. Strutture, Geotecnica, Geologia Applicata, Università della Basilicata, Potenza, Italy;bDip. di Ingegneria Civile ed Ambientale, Politecnico di Bari, Bari, Italy;cCalifornia State University, Long Beach, California, USA |
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| Abstract: | Groundwaters of the Murgia carbonate aquifer represent the main groundwater resource of the Apulia region (SE Italy). In the highlands (Alta Murgia) karst crops out in different forms and textures which have been preserved up to the 1970s: little evolved agriculture and sheep rearing produced only a marginal modification of the epikarst while a high degree of division into parcels by drystone walls helped in preserving soils from erosion. In the last years the original scenery of the Alta Murgia changed due to widespread transformations of surface karstic textures for agricultural purposes, with undeniable negative consequences on the hydrogeological balance, concerning both the infiltration and the runoff terms. Stone shattering led to flattening and deep alteration of a large part of the original karstic landscape and to demolition of drystone walls.In a study area of about 139 km2 located in the Alta Murgia, the comparison of aerial photos related to the period 1950–2001 indicated that stone shattering had occurred for about 42% of the area.The hydrological behaviour of the first soil layer of experimental parcels representing both shattered stone and natural karstic surface textures was analysed by using the numerical model Hydrus-2D with the aim of estimating the variation on infiltration rate due to stone shattering. Intensive field and laboratory measurements concerned soil texture, soil water content, pressure head, saturated hydraulic conductivity, pan evaporation and meteorological parameters. |
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| Keywords: | Karst Surface textures Stone shattering Evapotranspiration Infiltration rate Groundwater |
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