Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Dick R. Mastbergen"'
Publikováno v:
Journal of Marine Science and Engineering, Vol 7, Iss 10, p 368 (2019)
Retrogressive breach failures or coastal flow slides occur naturally in the shoreface in fine sands near dynamic tidal channels or rivers. They sometimes retrogress into beaches, shoal margins and riverbanks where they can threaten infrastructure and
Externí odkaz:
https://doaj.org/article/8fa6b61f29b045a4978fbf4f6c5d115d
Publikováno v:
Canadian Geotechnical Journal. 60:72-85
Although retrogressive flow slides in subaqueous sandy slopes can be very large and cause substantial damage, the failure mechanisms of such slides are not very clear yet. This study analyses two well-monitored flow slides in a shoal margin in the We
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d65c831d0680c2ff367c5391a909226e
https://doi.org/10.1139/cgj-2021-0282
https://doi.org/10.1139/cgj-2021-0282
Publikováno v:
International Journal of Physical Modelling in Geotechnics. 19:37-53
Liquefaction flow slides in sand have been investigated during an extensive experimental research programme during the period 1973–1977 on behalf of the design of the storm surge barrier in the Oosterschelde estuary. The programme included more tha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::908c286dbd13e2f17acf4ed645f6df69
https://doi.org/10.1680/jphmg.16.00026
https://doi.org/10.1680/jphmg.16.00026
Publikováno v:
Journal of Marine Science and Engineering, Vol 7, Iss 10, p 368 (2019)
Journal of Marine Science and Engineering
Volume 7
Issue 10
Journal of Marine Science and Engineering
Volume 7
Issue 10
Retrogressive breach failures or coastal flow slides occur naturally in the shoreface in fine sands near dynamic tidal channels or rivers. They sometimes retrogress into beaches, shoal margins and riverbanks where they can threaten infrastructure and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::576124b772910b0ff70b38f388f02406
https://www.mdpi.com/2077-1312/7/10/368
https://www.mdpi.com/2077-1312/7/10/368
Publikováno v:
Coastal Sediments 2019.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8c3a3d22a4dae41402805d3cacf1c6b6
https://doi.org/10.1142/9789811204487_0261
https://doi.org/10.1142/9789811204487_0261
Publikováno v:
Marine Geology, 280(1-4), 40. Elsevier
Although sediment waves cover many levees and canyon floors of submarine fan systems, their relation to the turbidity currents that formed them is still poorly understood. Over the recent years some large erosional sediment waves have been interprete
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2e26b8f8593befd055ff2ad5c5e6c488
Autor:
André Koelewijn, Geeralt A. van den Ham, M. Azpiroz, Age Vellinga, Matthieu J.B. Cartigny, J. L. Hizzett, Marco de Kleine, Dick R. Mastbergen, Michael A. Clare
Publikováno v:
Submarine Mass Movements and their Consequences ISBN: 9783319209784
Flow slides form a major threat to flood defences along coastlines and riverbanks in the Netherlands. Due to the uncertainties with respect to the process in combination with the severity of the consequences and costs for prevention measures, there i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1b0bc43221001ec2e529c32aaaed0bc
https://doi.org/10.1007/978-3-319-20979-1_24
https://doi.org/10.1007/978-3-319-20979-1_24
Publikováno v:
Sedimentology. 50:625-637
Natural, moderately loosely packed sands can only erode from the surface of the bed after an increase in pore volume. Because of this shear dilatancy, negative pore pressures are generated in the bed. In cases of low permeability, these negative pres
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31581f897834352b9a6ed6fda9a9df31
https://doi.org/10.1046/j.1365-3091.2003.00554.x
https://doi.org/10.1046/j.1365-3091.2003.00554.x
Publikováno v:
Sedimentology. 49:81-95
Large bank failures, comprising up to 10 6 m 3 of sediment, are common features along steep channel banks in estuaries and large rivers that consist of clean, fine sands, and are mostly assumed to be generated by sudden liquefaction of large masses o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7205c6a64c11d5c51c20ea9b30471cde
https://doi.org/10.1111/j.1525-139x.2006.00168.x-i1
https://doi.org/10.1111/j.1525-139x.2006.00168.x-i1
Publikováno v:
Sedimentology. 49:81-95
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c9435a1fcc332551e47286fb6bd00351
https://doi.org/10.1046/j.1365-3091.2002.00433.x
https://doi.org/10.1046/j.1365-3091.2002.00433.x