Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Shezad Nilamdeen"'
Autor:
Shezad Nilamdeen, David Switchenko
Publikováno v:
Handbook of Numerical Simulation of In-Flight Icing ISBN: 9783030647254
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb73e4968577f5a7e279d5bab1781e52
https://doi.org/10.1007/978-3-030-64725-4_22-1
https://doi.org/10.1007/978-3-030-64725-4_22-1
Autor:
Isik A. Ozcer, Cristhian Aliaga, Alberto Pueyo, Yue Zhang, Habibollah Fouladi, Shezad Nilamdeen, Jeyatharsan Selvanayagam, Shoaib Shah
Publikováno v:
AIAA AVIATION 2022 Forum.
Autor:
Jennifer L. Chalmers, Craig R. Davison, Shoaib Shah, Martin Neuteboom, Shezad Nilamdeen, Dan Fuleki, Cristhian Aliaga, John Stokes
Crystal icing in the engine core has been identified as a significant potential threat to operational aircraft safety, and therefore understanding and mitigating the associated risk is of paramount importance to engine manufacturers. Its importance h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::de1335615476a2e06bddf1bc438ba95c
https://doi.org/10.2514/6.2021-2663
https://doi.org/10.2514/6.2021-2663
Publikováno v:
SAE Technical Paper Series.
Publikováno v:
SAE Technical Paper Series.
Publikováno v:
SAE Technical Paper Series.
Autor:
Vinod Rao, Isik Ozcer, David Switchenko, Jeyatharsan Selvanayagam, Shezad Nilamdeen, Guido S. Baruzzi
Publikováno v:
SAE Technical Paper Series.
Autor:
Shezad Nilamdeen, Wagdi G. Habashi
Publikováno v:
Journal of Propulsion and Power. 27:959-969
ap = particle acceleration vector b = ice crystal semiminor-axis length, m ch = convective heat transfer coefficient Cd = particle drag coefficient cp;air = specific heat capacity of air, J= kgK cp;ice = specific heat capacity of ice, J= kgK cp;w = s
Publikováno v:
1st AIAA Atmospheric and Space Environments Conference.
A series of high-altitude turbofan engine malfunctions characterized by flameouts and rollbacks have been reported in recent years. The source of these incidents has been related to the presence of ice crystals at high altitudes and, consequently, to