Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Riccardo Rainato"'
Publikováno v:
Journal of Agricultural Engineering, Vol 47, Iss 2, Pp 72-81 (2016)
Riverine environments can be very dynamic and complex systems, particularly because of the interaction between active channel and riparian land during flood events of different magnitude. In recent years increasing attention has been paid to large wo
Externí odkaz:
https://doaj.org/article/a88345d307e2442aa694d71303893410
Publikováno v:
Agriculture, Vol 9, Iss 8, p 184 (2019)
Harrowing is a process that reduces the size of soil clods and prepares the field for seeding. Rotary harrows are a common piece of equipment in North Italy that consists of teeth rotating around a vertical axis with a processing depth of 5−15 cm.
Externí odkaz:
https://doaj.org/article/7ee3d568566947e580d896b668ca7ecc
Publikováno v:
Journal of Agricultural Engineering, Vol 44, Iss 3, Pp e15-e15 (2013)
The European Union (EU) Water Framework Directive (WFD, 2000/60/EC), which came into force in Italy under Decree Law no. 152 of 3rd April 2006, has as its objectives the protection and improvement of aquatic ecosystem status, promoting the sustainabl
Externí odkaz:
https://doaj.org/article/83b63f7dbf9043d7a85bf75c106eaa98
In many environments, climate change causes an increase in the frequency and magnitude of Large Infrequent Disturbances (LIDs). LIDs make fragile areas, as mountain basins, even more vulnerable. Among all LIDs, windthrows are one of the most relevant
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::82fd369828cf57a2df95487743399c12
https://doi.org/10.5194/egusphere-egu22-5456
https://doi.org/10.5194/egusphere-egu22-5456
Autor:
C. Rojas, Bruno Mazzorana, Galo Valdebenito, Lorenzo Picco, Pablo Iribarren-Anacona, Daniel Melnick, Andrés Iroumé, Virginia Ruiz-Villanueva, Riccardo Rainato
Publikováno v:
Science of The Total Environment, vol. 655, pp. 1089-1103
The compound hazard effects of multiple process cascades severely affect Chilean river systems and result in a large variety of disturbances on their ecosystems and alterations of their hydromorphologic regimes leading to extreme impacts on society,
Publikováno v:
CATENA. 216:106398
Mountain basins can be affected by Large Infrequent Disturbances (LIDs) that have the power of changing their forest cover and morphological settings, and supplying high amounts of sediments to river networks. The resulting cascading processes are of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::143362608ace15829b6e6edbad44b707
https://doi.org/10.5194/egusphere-egu21-5397
https://doi.org/10.5194/egusphere-egu21-5397
Publikováno v:
Water; Volume 13; Issue 24; Pages: 3630
Water, Vol 13, Iss 3630, p 3630 (2021)
Water, Vol 13, Iss 3630, p 3630 (2021)
Mountain streams are frequently characterized by step–pool morphology that provides stability and energy dissipation to the channel network. Large flooding events can overturn the equilibrium of the step–pool condition by altering the entire conf
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f988e6e407f06c68cf303ee42b8748fc
http://hdl.handle.net/11577/3409679
http://hdl.handle.net/11577/3409679
To achieve a reliable analysis of the impacts induced in mountain basins by large and infrequent floods, all their main components, from the spatial-temporal distribution of meteorological agents to the hydrological, geomorphic and sedimentological r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0c1097d04d33a2c1903b94231a9d99e1
http://hdl.handle.net/11577/3398148
http://hdl.handle.net/11577/3398148
The transport of coarse material strongly controls the stability and evolution of mountain fluvial systems but, despite this, bedload dynamics are not yet fully understood especially in mountain streams. In this sense, particular attention was paid o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::70922bff56175092936a71eeb148b865
https://eprints.lincoln.ac.uk/id/eprint/42280/1/GEOMOR-9548_R1clean.docx
https://eprints.lincoln.ac.uk/id/eprint/42280/1/GEOMOR-9548_R1clean.docx