Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Jan H. van den Berg"'
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
Autor:
Jan H. van den Berg, Jörg Lang
Publikováno v:
Sedimentology. 68:1439-1464
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d793d10ce1b28618931d63953dcc32bf
https://doi.org/10.1111/sed.12833
https://doi.org/10.1111/sed.12833
Publikováno v:
Sedimentology Early View (2020)
Upper-flow-regime bedforms, including upper-stage-plane beds, antidunes, chutes-and-pools and cyclic steps, are ubiquitous in glacigenic depositional environments characterized by abundant meltwater discharge and sediment supply. In this study, the d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4536c93b041619902724d41ed398a00a
https://doi.org/10.1111/sed.12776
https://doi.org/10.1111/sed.12776
Autor:
Jan H. van den Berg
Publikováno v:
Classic Writings for a Phenomenology of Practice ISBN: 9781003011798
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af2db61fcf46df352c51f13d4415e899
https://doi.org/10.4324/9781003011798-3
https://doi.org/10.4324/9781003011798-3
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:
Hans Middelkoop, Jasper T. Dijkstra, Michael A. Shoubin, Dmitry B. Babich, Margriet M. Schoor, Jurgen De Kramer, A. M. Alabyan, Jan H. Van Den Berg
Publikováno v:
Large Rivers. 15:89-103
In recent years, the concept of 'Cyclic Floodplain Rejuvenation' (CFR) has been adopted as a guiding principle for ecological rehabilitation in combination with flood protection of the lower Rhine and Meuse rivers in The Netherlands. This concept is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b2ac68c53ec44e6355879abb0fb852a
https://doi.org/10.1127/lr/15/2003/89
https://doi.org/10.1127/lr/15/2003/89
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
Autor:
Jan H. van den Berg, Brian P. Bledsoe
Publikováno v:
Geomorphology. 53:333-337
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61c427fb1dcf085379e00539f33a919e
https://doi.org/10.1016/s0169-555x(02)00316-1
https://doi.org/10.1016/s0169-555x(02)00316-1
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