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Supersaturation-controlled morphology and phase evolution of NiCo LDH in controllable and continuous flow synthesis. [PDF]
Hu Y.
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Enhanced phosphorus elimination from aquatic systems employing modified granular waterworks derived sludge composite materials: Mechanistic evaluation and process optimization. [PDF]
He L +8 more
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Modelling of coupled convective energy and mass fluxes in hydrothermal systems
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Hydrothermal convection in a thin porous ring
Fluid Dynamics, 1994zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Magomedbekov, Kh. G., Ramazanov, M. M.
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Hydrothermal convection in carbonaceous chondrite parent bodies
Earth and Planetary Science Letters, 2005Abstract Numerical simulations of the thermal evolution of carbonaceous chondrite parent bodies indicate a period of several million years during which convective motion of water could occur. The present study considers variations of permeability, radiogenic heating, and body radius.
Bryan J. Travis, Gerald Schubert
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Convective Rolls and Hydrothermal Waves in Evaporating Sessile Drops
Langmuir, 2012Recent experiments on the evaporation of sessile droplets have revealed the spontaneous formation of various patterns including the presence of hydrothermal waves. These waves had previously been observed, in the absence of evaporation, in thin liquid layers subjected to an imposed, uniform temperature gradient.
George, Karapetsas +3 more
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A model of hydrothermal convection in an aquifer
Journal of Geophysical Research: Solid Earth, 1980Numerical calculations have been carried out to determine the temperature field due to the steady state hydrothermal flow of water through a smoothly curved cylindrical aquifer. It is found that the outflow water temperature relative to the ambient temperature at the base of the aquifer has a maximum at intermediate flow rates.
K. E. Torrance +2 more
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Hydrothermal convection at slow-spreading mid-ocean ridges
Tectonophysics, 1979Abstract The discrepancy observed between measured heat flow data and the heat flow predicted by thermal models of mid-ocean ridges is commonly explained by the presence of hydrothermal convection in young oceanic crust. Numerical modelling of fluid flow through porous media has been used to investigate what permeability, depth of penetration and ...
Udo Fehn, Lawrence M. Cathles
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