none10noA recent study (Aielli et al. 2017) about sand boil reactivations in the major Po river banks (Italy) has demonstrated how a structured database of historic information can significantly contribute to better understanding of seepage phenomena and provide a practical tool for safe management of hydraulic works. The primary aim of the present work is to enhance the information collected in the database (DB), which cover the whole course the Po river, to the beginning of the delta. In particular, an improved estimation of the critical height (i.e. height of the water level in the river which causes a sand boil reactivation) for sand boil phenomena is discussed herein. The maximum height without reactivation and the minimum height with ...
Scientists and public administrators are devoting increasing attention to the Po River, in Italy, in...
Archaeological sites are extremely vulnerable to the impacts of weather-related events, which may le...
The effects of human activities on flood propagation, during the period 1878\u20132005, in a 190-km ...
A recent study (Aielli et al. 2017) about sand boil reactivations in the major Po river banks (Italy...
The river Po is the main river of Italy, and crosses the entire North Italy from the Western Alps to...
Backward erosion piping is one of the most critical issues for the stability of the Po River embankm...
Sand boils are the surface manifestation of an erosion process, known as backward erosion piping, wh...
none6noArticolo contenuto negli atti di: VI ITALIAN CONFERENCE OF RESEARCHERS IN GEOTECHNICAL ENGINE...
Piping induced by seepage is a frequent cause of failure for earthen levees. The probability that th...
The article presents a three-dimensional (3D) finite element (FE) model of the groundwater flow bene...
none4noThe Po River, which flows eastward through the Northern of Italy, is the largest and most imp...
Extensive flooding can be the result of levee system failures most frequently caused by the piping p...
Extensive flooding can be the result of levee system failures most frequently caused by the piping p...
The reliability of river embankments is essential for flood risk management. The Po River, which flo...
Alluvial events in Italy are a constant and continuous problem due to the peculiar orographic and cl...
Scientists and public administrators are devoting increasing attention to the Po River, in Italy, in...
Archaeological sites are extremely vulnerable to the impacts of weather-related events, which may le...
The effects of human activities on flood propagation, during the period 1878\u20132005, in a 190-km ...
A recent study (Aielli et al. 2017) about sand boil reactivations in the major Po river banks (Italy...
The river Po is the main river of Italy, and crosses the entire North Italy from the Western Alps to...
Backward erosion piping is one of the most critical issues for the stability of the Po River embankm...
Sand boils are the surface manifestation of an erosion process, known as backward erosion piping, wh...
none6noArticolo contenuto negli atti di: VI ITALIAN CONFERENCE OF RESEARCHERS IN GEOTECHNICAL ENGINE...
Piping induced by seepage is a frequent cause of failure for earthen levees. The probability that th...
The article presents a three-dimensional (3D) finite element (FE) model of the groundwater flow bene...
none4noThe Po River, which flows eastward through the Northern of Italy, is the largest and most imp...
Extensive flooding can be the result of levee system failures most frequently caused by the piping p...
Extensive flooding can be the result of levee system failures most frequently caused by the piping p...
The reliability of river embankments is essential for flood risk management. The Po River, which flo...
Alluvial events in Italy are a constant and continuous problem due to the peculiar orographic and cl...
Scientists and public administrators are devoting increasing attention to the Po River, in Italy, in...
Archaeological sites are extremely vulnerable to the impacts of weather-related events, which may le...
The effects of human activities on flood propagation, during the period 1878\u20132005, in a 190-km ...