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Farideh HajyAkbary
Researcher at Delft University of Technology
Publications - 4
Citations - 437
Farideh HajyAkbary is an academic researcher from Delft University of Technology. The author has contributed to research in topics: Martensite & Quenching. The author has an hindex of 4, co-authored 4 publications receiving 269 citations.
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An improved X-ray diffraction analysis method to characterize dislocation density in lath martensitic structures
TL;DR: In this paper, an improved X-ray diffraction line profile analysis method is developed to determine dislocation density of lath martensitic steels, which combines the modified Warren-Averbach (MWA) and the modified Williamson-Hall (MWH) methods.
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Interaction of carbon partitioning, carbide precipitation and bainite formation during the Q&P process in a low C steel
TL;DR: In this paper, the authors investigated the interaction between carbon partitioning, carbide precipitation and carbide-free bainite formation during the quenching and partitioning process of a 0.3C-1.6Si-3.5Mn (wt.%) steel with nonhomogenous distribution of the alloying elements.
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Analysis of the mechanical behavior of a 0.3C-1.6Si-3.5Mn (wt%) quenching and partitioning steel
Farideh HajyAkbary,Jilt Sietsma,Goro Miyamoto,Naoya Kamikawa,Roumen Petrov,Tadashi Furuhara,Maria Jesus Santofimia +6 more
TL;DR: In this paper, a 0.3C-1.6Si-3.5Mn (wt%) steel was subjected to different QP secondary martensite phases and the yield strength of each constituent phase was determined by applying physical models to the data obtained from detailed microstructural characterization.
Journal ArticleDOI
A quantitative investigation of the effect of Mn segregation on microstructural properties of quenching and partitioning steels
Farideh HajyAkbary,Jilt Sietsma,Roumen Petrov,Roumen Petrov,Goro Miyamoto,Tadashi Furuhara,Maria Jesus Santofimia +6 more
TL;DR: In this paper, a 0.3C-1.3Si-3.2Mn steel with Mn segregation is studied experimentally and theoretically, and it is shown that during initial quenching a higher fraction of martensite forms in Mn-poor regions compared to Mn-rich regions.