Costanza Calzolari

Geomorphic features of a badland (biancane) area (Central Italy): characterisation, distribution and quantitative spatial analysis

Abstract The biancana landscapes, rather common in several Italian areas, have a very complex morphology. Different geomorphic features often occur along the same hillslope. From a morphological survey of an experimental site in southern Tuscany, the forms were classified, and their distribution analysed. Spatial analysis of the biancane provided insights into the range of forces responsible for their formation and evolution. The results confirm an evolutionary trend from an original gently sloping surface to a complex biancana landform, emphasising a trend from the taller bean forms to the terminal souffle-like and cone forms. The presence of scarp and sliding forms in the most sloping areas and along the residual surfaces supports the hypothesis of a process influenced by base level, acting initially by small mass movements. Spatial analysis did not reveal any systematic trend in the variability of the erosional features along the slopes. Variographic analysis showed that selected morphological attributes are spatially auto-correlated over a short range, suggesting that the erosive processes responsible for morphogenic evolution of biancane act mostly on a local scale. The strong geometric anisotropy detected in directions parallel to the main jointing systems also indicated a broader scale tectonic control of biancane evolution, probably in an early stage of their formation.

Carbon sequestration and fertility after centennial time scale incorporation of charcoal into soil

The addition of pyrogenic carbon (C) in the soil is considered a potential strategy to achieve direct C sequestration and potential reduction of non-CO2 greenhouse gas emissions. In this paper, we investigated the long term effects of charcoal addition on C sequestration and soil physico-chemical properties by studying a series of abandoned charcoal hearths in the Eastern Alps of Italy established in the XIX century. This natural setting can be seen as an analogue of a deliberate experiment with replications. Carbon sequestration was assessed indirectly by comparing the amount of pyrogenic C present in the hearths (23.3±4.7 kg C m−2) with the estimated amount of charcoal that was left on the soil after the carbonization (29.3±5.1 kg C m−2). After taking into account uncertainty associated with parameters’ estimation, we were able to conclude that 80±21% of the C originally added to the soil via charcoal can still be found there and that charcoal has an overall Mean Residence Time of 650±139 years, thus supporting the view that charcoal incorporation is an effective way to sequester atmospheric CO2. We also observed an overall change in the physical properties (hydrophobicity and bulk density) of charcoal hearth soils and an accumulation of nutrients compared to the adjacent soil without charcoal. We caution, however, that our site-specific results should not be generalized without further study.

Using existing soil databases for estimating retention properties for soils of the Pianura Padano-Veneta region of North Italy

Data collected on benchmark soils from experimental sites in the Pianura Padano-Veneta, Northern Italy, stored in local soil data bases were used to test the reliability of existing pedotransfer functions to derive soil water retention properties, required as input to simulation models of pollutant transport in soils. Eight different algorithms were selected according to their principle of calculation, input variable requirements and in agreement with the different information currently existing in local soil databases. Results were validated against an experimental set of 139 retention curves. In order to assess the validity of the selected pedotransfer functions and to provide operative guidelines for their selection, quantitative error indices mean difference, and square root of the mean squared difference, were calculated and the results evaluated for the whole data set and for subsets of observations classed in terms of soil textural composition, bulk density, organic carbon content and matric potential. Non-parametric significance tests for unbalanced data were applied to assess the significance of the differences among classes. According to the kind of soil on which they were tested, the selected pedotransfer functions showed significantly different responses in terms of accuracy, providing therefore useful indications for their optimal applicability for different levels of available information.

Modelling the impact of increasing soil sealing on runoff coefficients at regional scale: a hydropedological approach

Abstract Soil sealing is the permanent covering of the land surface by buildings, infrastructures or any impermeable artificial material. Beside the loss of fertile soils with a direct impact on food security, soil sealing modifies the hydrological cycle. This can cause an increased flooding risk, due to urban development in potential risk areas and to the increased volumes of runoff. This work estimates the increase of runoff due to sealing following urbanization and land take in the plain of Emilia Romagna (Italy), using the Green and Ampt infiltration model for two rainfall return periods (20 and 200 years) in two different years, 1976 and 2008. To this goal a hydropedological approach was adopted in order to characterize soil hydraulic properties via locally calibrated pedotransfer functions (PTF). PTF inputs were estimated via sequential Gaussian simulations coupled with a simple kriging with varying local means, taking into account soil type and dominant land use. Results show that in the study area an average increment of 8.4% in sealed areas due to urbanization and sprawl induces an average increment in surface runoff equal to 3.5 and 2.7% respectively for 20 and 200-years return periods, with a maximum > 20% for highly sealed coast areas.