Double diffusive convection
id:
double-diffusive-convection-322-16089205
title:
Double diffusive convection
text:
Double diffusive convection is a fluid dynamics phenomenon that describes a form of convection driven by two different density gradients, which have different rates of diffusion. Convection in fluids is driven by density variations within them under the influence of gravity. These density variations may be caused by gradients in the composition of the fluid, or by differences in temperature. Thermal and compositional gradients can often diffuse with time, reducing their ability to drive the conv
brand slug:
wiki
category slug:
encyclopedia
description:
Convection with two density gradients
original url:
https://en.wikipedia.org/wiki/Double_diffusive_convection
date created:
date modified:
2024-02-17T05:38:09Z
main entity:
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image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/c/c9/Salt_fingers.png","width":472,"height":349}
fields total:
13
integrity:
15