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Hiroki Suzuki

Researcher at Yamaguchi University

Publications -  67
Citations -  535

Hiroki Suzuki is an academic researcher from Yamaguchi University. The author has contributed to research in topics: Turbulence & Direct numerical simulation. The author has an hindex of 11, co-authored 67 publications receiving 436 citations. Previous affiliations of Hiroki Suzuki include Nagoya Institute of Technology & University of Tokyo.

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Turbulence structure and turbulence kinetic energy transport in multiscale/fractal-generated turbulence

TL;DR: In this article, the turbulence structure and turbulence kinetic energy transport in multiscale/fractal-generated turbulence in a wind tunnel are investigated, where a low-blockage, space-filling square-type fractal grid is placed at the inlet of the test section.
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Relevance of turbulence behind the single square grid to turbulence generated by regular- and multiscale-grids

TL;DR: In this article, direct numerical simulations were carried out to study the turbulence generated by a fractal square grid at a Reynolds number of ReL0 = 20000 (based on the inlet velocity Uin and length of the largest grid bar L0).
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Direct numerical simulation of turbulent mixing in grid-generated turbulence

TL;DR: In this article, a turbulence-generating grid, on which the velocity components are set to zero, is located downstream of the channel entrance, and it is numerically constructed on the staggered mesh arrangement using the immersed boundary method.
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High-Schmidt-number scalar transfer in regular and fractal grid turbulence

TL;DR: In this paper, the mixing of high-Schmidt-number passive scalars in regular and fractal grid turbulence is experimentally investigated using a water channel, where a turbulence-generating grid is installed at the entrance of the test section, which is 1.5 m in length and 0.1 m×0.1m in cross section.
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Direct numerical simulation of fractal-generated turbulence

TL;DR: In this paper, the authors simulate fractal-generated turbulence by means of a direct numerical simulation and address its fundamental characteristics, and examine whether the fractal generated turbulence in the upstream region has a nature similar to that of a wake.