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README.md
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## Description
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The dataset captures the time-evolving behavior of 3D spherical droplets subjected to an external shock wave in air.
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Here we investigate a scenario with symmetric boundary conditions at the north, south, top and bottom walls.
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<div style="display:flex;justify-content:center;gap:20px;flex-wrap: wrap;">
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<div>
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<video style="width:100%;max-width:800px" src="https://huggingface.co/datasets/FluidVerse/3D_SDBA_SSOOSS/resolve/main/SDBA_SSOOSS_RTP_Mas1.20.mp4" loop autoplay muted controls></video>
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<p style="position:relative;top:-30px;font-size:14px">Shock-Induced Droplet RTP-
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<video style="width:100%;max-width:800px" src="https://huggingface.co/datasets/FluidVerse/3D_SDBA_SSOOSS/resolve/main/SDBA_SSOOSS_SIE_Mas1.20.mp4" loop autoplay muted controls></video>
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<p style="position:relative;top:-30px;font-size:14px">Shock-Induced Droplet SIE-
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## Description
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The dataset captures the time-evolving behavior of 3D spherical droplets subjected to an external shock wave in air.
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When a shock wave impacts a droplet, the initial response—largely independent of the Weber number—is a deformation phase in which the droplet flattens.
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This interaction with the shock wave results in two different breakup-modes of the droplet (SIE and RTP).
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In the SIE regime, breakup is driven mainly by strong shear forces acting along the droplet surface.
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After the droplet has flattened, shear-induced disturbances emerge near the equator; these instabilities originate near the droplet equator after the droplet has flattened out in the first phase and are advected along the droplet surface.
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As the relative velocity between the droplet and the surrounding gas increases, these disturbances grow due to Kelvin–Helmholtz instability, eventually stripping liquid from the droplet and producing fine droplets downstream.
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In contrast, in the RTP regime, relatively stronger surface tension suppresses the growth of such shear instabilities, maintaining a smoother interface.
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As deformation progresses, the upstream side of the droplet becomes concave as the surrounding gas penetrates and pierces the liquid.
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Unlike RTP, the SIE regime is characterized by a continuous and gradual loss of mass, often resulting in a mist of droplets downstream.
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Here we investigate a scenario with symmetric boundary conditions at the north, south, top and bottom walls.
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<div style="display:flex;justify-content:center;gap:20px;flex-wrap: wrap;">
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<div>
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<video style="width:100%;max-width:800px" src="https://huggingface.co/datasets/FluidVerse/3D_SDBA_SSOOSS/resolve/main/SDBA_SSOOSS_RTP_Mas1.20.mp4" loop autoplay muted controls></video>
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<p style="position:relative;top:-30px;font-size:14px">Shock-Induced Droplet RTP-Breakup in Air (Mach 1.20)</p>
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</div>
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<div>
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<video style="width:100%;max-width:800px" src="https://huggingface.co/datasets/FluidVerse/3D_SDBA_SSOOSS/resolve/main/SDBA_SSOOSS_SIE_Mas1.20.mp4" loop autoplay muted controls></video>
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<p style="position:relative;top:-30px;font-size:14px">Shock-Induced Droplet SIE-Breakup in Air (Mach 1.20)</p>
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</div>
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</div>
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