Search Results - "Salinas, Jorge S."

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  1. 1

    Peering inside a cough or sneeze to explain enhanced airborne transmission under dry weather by Liu, Kai, Allahyari, Majid, Salinas, Jorge S., Zgheib, Nadim, Balachandar, S.

    Published in Scientific reports (10-05-2021)
    “…High-fidelity simulations of coughs and sneezes that serve as virtual experiments are presented, and they offer an unprecedented opportunity to peer into the…”
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    Journal Article
  2. 2

    Anatomy of subcritical submarine flows with a lutocline and an intermediate destruction layer by Salinas, Jorge S., Balachandar, S., Shringarpure, M., Fedele, J., Hoyal, D., Zuñiga, S., Cantero, M. I.

    Published in Nature communications (12-03-2021)
    “…Turbidity currents are sediment-laden flows that travel over a sloping bed under a stagnant ambient fluid, driven by the density difference between the current…”
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    Journal Article
  3. 3

    Properties of the Body of a Turbidity Current at Near‐Normal Conditions: 1. Effect of Bed Slope by Salinas, Jorge S., Cantero, M. I., Shringarpure, M., Balachandar, S.

    Published in Journal of geophysical research. Oceans (01-11-2019)
    “…We study the body of turbidity currents in normal flow conditions by means of highly resolved direct numerical simulations of a homogeneous model. We focus on…”
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    Journal Article
  4. 4

    Mixing at a sediment concentration interface in turbulent open channel flow by Salinas, Jorge S., Shringarpure, Mrugesh, Cantero, Mariano I., Balachandar, S.

    “…In this work we address the role of turbulence on mixing of clear layer of fluid with sediment-laden layer of fluid at a sediment concentration interface. This…”
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  5. 5

    Properties of the Body of a Turbidity Current at Near‐Normal Conditions: 2. Effect of Settling by Salinas, Jorge S., Cantero, M. I., Shringarpure, M., Balachandar, S.

    Published in Journal of geophysical research. Oceans (01-11-2019)
    “…Turbidity currents are sediment‐laden flows that move over a sloping surface. These flows are driven by the density difference between the sediment‐laden…”
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    Journal Article
  6. 6