Mini tornado experiment
It occurred to me that if centrifugal separation activity can occur in a square enclosure, it could also occur without any enclosure. And that prompted me to try to produce a small sort of "tornado" in my workshop. Maybe "tornado" is overstating it a bit, but I have from time to time seen little eddies or twisters that pick up leaves and twigs from the ground in otherwise relatively calm weather conditions. It's one of those that I set out to create. I knew I needed some suction from the top. I first tried it with just a box fan blowing air up, but without success. I then made a cardboard shroud to concentrate the suction on a smaller area.
Some wood shavings spread on the floor give the tornado something to pick up, which makes it visible. A real tornado is visible because there is enough of a pressure drop in the funnel to cause a temperature drop, and that in turn causes water to condense out of the air. But my workshop tornado was not going to be nearly as powerful.
It's possible that I could have formed a twister without the cardboard shroud on the box fan, but I didn't realize I had too much wind from my other fans until after I put a cardboard shroud around the box fan.
What's most interesting is that the air inside the tornado is moving much faster than the circulating breeze or the upward suction that I started with. The high airspeeds get produced by spinning air getting pulled in towards the center. Like a pirouetting figure skater pulling her arms in, the air also accelerates as it is pulled in. Conservation of angular momentum dictates that, for angular momentum to be conserved, the air must speed up as it gets to the middle. But this is counterintuitive --- what pushes the air to go faster, and where does the kinetic energy come from? The energy comes from the upwards suction. With centrifugal force from the spinning air pushing outwards, pressure inside the funnel is lower than in the surrounding air. Lower pressure is lower potential energy, and in the process of getting to the middle, potential energy (through centrifugal force) is converted to kinetic energy, resulting in higher wind speeds. Or you could just use the Bernoulli principle to explain that the air at lower pressure moves at a higher speed. This speeding up of air towards the middle really helps a cyclone work. Centrifugal force on an object moving in a circular motion is given by this formula:
To achieve maximum force on a particle of mass m, we want to maximize speed (V) and minimize radius. And at the middle of the cyclone, r becomes smaller, while air speed (V) increases, achieving maximum force F to pull heavier particles away from the middle where air is sucked out of the cyclone. And that is what makes a dust separating cyclone work so well.
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