G.R. 1322/2006). The area is also characterized in great part (∼50%) by soils with a high runoff potential (C/D according to the USDA Hydrological Group definition), that in natural condition would have a high water table, but that are drained to keep the seasonal high water table at least 60 cm below the surface. Due to the geomorphic settings, with slopes almost equal to zero and lands below sea level, and due to the settings of the Selleckchem KRX0401 drainage system, this floodplain presents numerous

areas at flooding risk. The local authorities underline how, aside from the risk connected to the main rivers, the major concerns derive mainly from failures of the agricultural ditch network that often results unsufficient to drain rather frequent rainfall events that are not necessarily associated with extreme meteorological condition (Piani Territoriali di Coordinamento Provinciale, 2009). The study site was C59 wnt selected as representative of the land-use

changes that the Veneto floodplain faced during the last half-century (Fig. 3a and b), and of the above mentioned hydro-geomorphological conditions that characterize the Padova province (Fig. 3c–e). The area was deemed critical because here the local authorities often suspend the operations of the water pumps, with the consequent flooding of the territories (Salvan, 2013). The problems have been underlined also by local witnesses and authorities that described the more frequent flood events as being mainly caused by the failures of the minor drainage system, that is

not able to properly drain the incoming rainfall, rather than by the collapsing of the major river system. The study area was also selected because of the availability of different types of data coming from official sources: (1) Historical images of the years 1954, 1981 and 2006; (2) Historical rainfall datasets retrieved from a nearby station (Este) starting from the 1950s; (3) A lidar DTM at 1 m resolution, with a horizontal accuracy selleck chemicals of about ±0.3 m, and a vertical accuracy of ±0.15 m (RMSE estimated using DGPS ground truth control points). For the purpose of this work, we divided the study area in sub-areas of 0.25 km2. This, to speed up the computation time and, at the same time, to provide spatially distributed measures. For the year 1954 and 1981, we based the analysis on the available historical images, and by manual interpretation of the images we identified the drainage network system. In order to avoid as much as possible misleading identifications, local authorities, such as the Adige-Euganeo Land Reclamation Consortium, and local farmers were interviewed, to validate the network maps. For the evaluation of the storage capacity, we estimated the network widths by interviewing local authorities and landowners. We generally found that this information is lacking, and we were able to collect only some indications on a range of average section widths for the whole area (∼0.