Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Wen-yau Chen"'
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 29, Iss 1, Pp 87-103 (2018)
Given a large block of fine-grained sediment that overlies a 1° continental slope, if the entire sediment deposit is shaken by an earthquake to slide down the slope with an initial velocity (referred to as "submarine landslide" hereinafter), our blo
Externí odkaz:
https://doaj.org/article/e5f28b3f2fec477a96bc13db87238a5c
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 29, Iss 1, Pp 87-103 (2018)
Given a large block of fine-grained sediment that overlies a 1° continental slope, if the entire sediment deposit is shaken by an earthquake to slide down the slope with an initial velocity (referred to as "submarine landslide" hereinafter), our blo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::23bf0ddfe05343d330012ada653c324d
https://doaj.org/article/e5f28b3f2fec477a96bc13db87238a5c
https://doaj.org/article/e5f28b3f2fec477a96bc13db87238a5c
Publikováno v:
Journal of Mountain Science. 13:1333-1344
When a block of dense sandy soil moves downhill, the shear-induced soil dilatancy along the basal shear boundary produces a negative value of excess pore pressure that increases the basal frictional resistance. Dilatancy angle, , the degree to which
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::00c97ef8724516ec78fd286bc58c0ffd
https://doi.org/10.1007/s11629-015-3698-0
https://doi.org/10.1007/s11629-015-3698-0
Publikováno v:
International Journal of Multiphase Flow. 38:27-34
Asymptotic and transient stability analyses of unbounded uniform shear flows of dense, slightly inelastic, spherical particles were carried out using a frictional–kinetic theory. This model proposed for describing dense flows is based on a critical
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1e43007d1ce21b4802c35694873e4e29
https://doi.org/10.1016/j.ijmultiphaseflow.2011.08.010
https://doi.org/10.1016/j.ijmultiphaseflow.2011.08.010
Publikováno v:
Journal of Fluid Mechanics. 455:1-19
The three-dimensional motion observed by Chen & Chen (1997) in the convection cells generated by sideways heating of a solute gradient is further examined by experiments and linear stability analysis. In the experiments, we obtained visualizations an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::51ef95281ab68a33abe87b635159f6cd
https://doi.org/10.1017/s0022112001007297
https://doi.org/10.1017/s0022112001007297
Autor:
Wen-Yau Chen, C. F. Chen
Publikováno v:
Journal of Fluid Mechanics. 395:327-344
The nature of instability occurring in a differentially heated infinite slot under steady gravity depends only on the Prandtl number of the contained Boussinesq fluid. For fluids with Pr < 12.5, the instability is shear dominated and onsets in a stea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc37ff3b8bd945f3b3cd41daa03b078c
https://doi.org/10.1017/s0022112099006011
https://doi.org/10.1017/s0022112099006011
Publikováno v:
Physics of Fluids. 22:113304
Asymptotic and transient stability analyses of unbounded uniform granular shear flow at high solids volume fractions were carried out in the paper, based on a model composed of the viscoplastic constitutive law [P. Jop, Y. Forterre, and O. Pouliquen,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3a9dec26343bcf54cfdfb6e96a3dbfc6
https://doi.org/10.1063/1.3488225
https://doi.org/10.1063/1.3488225