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Benjamin Gebhart

Researcher at University of Pennsylvania

Publications -  139
Citations -  6603

Benjamin Gebhart is an academic researcher from University of Pennsylvania. The author has contributed to research in topics: Natural convection & Combined forced and natural convection. The author has an hindex of 42, co-authored 139 publications receiving 6390 citations. Previous affiliations of Benjamin Gebhart include State University of New York System & Cornell University.

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Buoyancy-Induced Flows And Transport

TL;DR: In this paper, a general formulation of buoyancy-induced fluid flows is presented, including external Vertical Thermally Induced Flows and Vertical Axisymmetric Flows.
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The nature of vertical natural convection flows resulting from the combined buoyancy effects of thermal and mass diffusion

TL;DR: In this article, a set of Boussinesq approximations were shown to have solutions of similarity form for combined buoyancy effects, for vertical flows adjacent to surfaces and in plumes, and the resulting equations were integrated for air and water for various practical values of the Schmidt number.
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Effects of viscous dissipation in natural convection

TL;DR: In this paper, the effect of viscous dissipation in natural convection is considered for vertical surfaces subject to both isothermal and uniform-flux surface conditions, and the first temperature perturbation function is calculated for Prandtl numbers from 10−2 to 104.
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A new density relation for pure and saline water

TL;DR: In this article, an equation for the density of pure and saline water was developed and the density variation was fitted in the temperature, salinity and pressure ranges to 20°C, 40%, and 1000 bars abs.
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Organ pipe radiant modes of periodic micromachined silicon surfaces.

TL;DR: A study of emittance from deep gratings of heavily phosphorus doped silicon with pronounced resonant periodicities with a characteristic length of ∼42 µm and the resonant amplitude of the s polarization does not depend significantly on Λ, but it does for the p polarization.