Zobrazeno 1 - 10
of 35
pro vyhledávání: '"Gianluca Blois"'
Publikováno v:
Frontiers in Water, Vol 3 (2021)
Resolving pore-scale transient flow dynamics is crucial to understanding the physics underlying multiphase flow in porous media and informing large-scale predictive models. Surface properties of the porous matrix play an important role in controlling
Externí odkaz:
https://doaj.org/article/eec3c48490374155b62c70ff4363cee3
Publikováno v:
Fluids, Vol 6, Iss 6, p 216 (2021)
An experimental investigation into the flow produced by mound-bearing impact craters is reported herein. Both an idealized crater and a scaled model of a real martian crater are examined. Measurements were performed using high-resolution planar parti
Externí odkaz:
https://doaj.org/article/bae149e19cf942feb117fd38ce31a786
Publikováno v:
Water Resources Research. 58
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86370860bf837cba055ea06964ee3133
https://doi.org/10.1029/2021wr031744
https://doi.org/10.1029/2021wr031744
Publikováno v:
Frontiers in Water, Vol 3 (2021)
Resolving pore-scale transient flow dynamics is crucial to understanding the physics underlying multiphase flow in porous media and informing large-scale predictive models. Surface properties of the porous matrix play an important role in controlling
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a2b0c12849ebfa40015b1230b9aa31a0
https://www.frontiersin.org/articles/10.3389/frwa.2021.710370/full
https://www.frontiersin.org/articles/10.3389/frwa.2021.710370/full
Publikováno v:
14th International Symposium on Particle Image Velocimetry. 1
Most modeling studies investigating the flow dynamics in vegetation canopies are limited to rigid models as proxies for vegetation elements. However, most canopies embody some degree of structural flexibility, resulting in aeroelastic mechanisms coup
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::319be2b8b7da6e42aece98c75ddab0f2
https://doi.org/10.18409/ispiv.v1i1.103
https://doi.org/10.18409/ispiv.v1i1.103
Publikováno v:
14th International Symposium on Particle Image Velocimetry. 1
Optical Flow (OF) techniques provide “dense estimation” flow maps (i.e. pixel-level resolution) of timecorrelated images and thus are appealing to applications requiring high spatial resolutions. OF methods revolve around mathematical description
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ca37c5a42f4242ded0b095c4b2a79a5f
https://doi.org/10.18409/ispiv.v1i1.131
https://doi.org/10.18409/ispiv.v1i1.131
Publikováno v:
14th International Symposium on Particle Image Velocimetry. 1
Barchan dunes are crescent-shaped bedforms that form in aeolian (i.e., wind-driven) environments (including both Earth and other planets, such as Mars) as well as subaqueous environments. Under the forcing of the aloft turbulent boundary layer, they
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3d92983868e4e2c55134fbb2f14e6103
https://doi.org/10.18409/ispiv.v1i1.79
https://doi.org/10.18409/ispiv.v1i1.79
Publikováno v:
14th International Symposium on Particle Image Velocimetry. 1
The processes controlling crater mound formation are the subject of ongoing research (Bennett and Bell III, 2016). Several theories exist on the formation of a central mound, with those pointing to wind processes as the predominant driving mechanisms
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::514768af8703ba259c5efe8402743550
https://doi.org/10.18409/ispiv.v1i1.107
https://doi.org/10.18409/ispiv.v1i1.107
Publikováno v:
Journal of Fluid Mechanics. 920
The dynamics of turbulent flow structures in the wakes of barchan dunes is investigated to understand the complex, long-range interactions that occur between these three-dimensional bedforms. High-frame-rate stereo-particle image velocimetry measurem
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f781191de63a541dbf30f3743942ff2e
https://doi.org/10.1017/jfm.2021.476
https://doi.org/10.1017/jfm.2021.476
Publikováno v:
Fluids
Volume 6
Issue 6
Fluids, Vol 6, Iss 216, p 216 (2021)
Volume 6
Issue 6
Fluids, Vol 6, Iss 216, p 216 (2021)
An experimental investigation into the flow produced by mound-bearing impact craters is reported herein. Both an idealized crater and a scaled model of a real martian crater are examined. Measurements were performed using high-resolution planar parti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f4a72840f194c93a40a608c33ef274d5