Leidenfrost heat engine
Posted: Fri Jun 12, 2020 4:55 am
https://youtu.be/UAMNDdOho8E
I came across this idea recently.
One thing that came to mind: a Stirling heat engine or "hot air" engine, using ordinary atmospheric air as the "working fluid", is really using a rather complex mixture of various gasses, all having different properties at different temperatures, different "critical temperatures" different boiling points, and may include water vapor or degrees of humidity or partial liquid.
Ordinary air, lowered in temperature, to the point of liquifaction, condenses, or having condensed, reheated slightly, expands 800x.
That is, air as a gas is 800x the volume of a drop of liquid air. And the reverse. A volume of air shrinks down 800x smaller when it condenses.
What about all the individual gases of which air is composed?
This Leidenfrost heat engine illustrates how "dry ice", normally a gas at Earth atmospheric temperatures could power an "ambient heat engine".
What gas/liquid undergoes phase change at or near ordinary atmospheric temperature and pressure?
I was wondering, if water vapor (and/or other gas/liquid) condensation or phase change in a heat engine plays a role, could a heat engine run TOO HOT resulting in a kind of Leidenfrost effect, inhibiting normal, rapid expansion/contraction.
Heat engines often seem to lag, or not run at all until they reach some certain temperature, possibly(?) where some component of the air or "working fluid" is undergoing rapid phase change induced by relatively slight temperature variations.
Perhaps it is only some relatively minor component in the air that is responsible for the majority of the expansion/contraction, or different components may come into play at different operating temperatures.
Lots of room for exploration and research.
I came across this idea recently.
One thing that came to mind: a Stirling heat engine or "hot air" engine, using ordinary atmospheric air as the "working fluid", is really using a rather complex mixture of various gasses, all having different properties at different temperatures, different "critical temperatures" different boiling points, and may include water vapor or degrees of humidity or partial liquid.
Ordinary air, lowered in temperature, to the point of liquifaction, condenses, or having condensed, reheated slightly, expands 800x.
That is, air as a gas is 800x the volume of a drop of liquid air. And the reverse. A volume of air shrinks down 800x smaller when it condenses.
What about all the individual gases of which air is composed?
This Leidenfrost heat engine illustrates how "dry ice", normally a gas at Earth atmospheric temperatures could power an "ambient heat engine".
What gas/liquid undergoes phase change at or near ordinary atmospheric temperature and pressure?
I was wondering, if water vapor (and/or other gas/liquid) condensation or phase change in a heat engine plays a role, could a heat engine run TOO HOT resulting in a kind of Leidenfrost effect, inhibiting normal, rapid expansion/contraction.
Heat engines often seem to lag, or not run at all until they reach some certain temperature, possibly(?) where some component of the air or "working fluid" is undergoing rapid phase change induced by relatively slight temperature variations.
Perhaps it is only some relatively minor component in the air that is responsible for the majority of the expansion/contraction, or different components may come into play at different operating temperatures.
Lots of room for exploration and research.