On Sat, 03 Jun 2006 11:14:19 -0700, "G.T." <[email hidden]>
Quoted message said:Leo Lichtman said:This argument is theoretical--it has nothing to do with friction.
You haven't watched the rolling ball experiments, have you?
Quoted message said:Carl's
original assumption was that his speed at the conclusion of the dip/hill
returns to the original value, due to conservation of energy.
Yes, in a frictionless world he's right, taking the dip example:
"As the ball on the dipped track goes down, its horizontal velocity
increases, so it gets ahead. When it returns to its original level, it
slows down to its original horizontal speed, but in so doing it never
goes slower than the ball on the flat track, so it never gets behind the
other ball or even allows the flat track ball to catch up. The two balls
then move along at the same speed with the dipped track ball remaining
ahead of the straight track ball by a constant amount."
Quoted message said:
Your problem is more basic than friction, wind drag, or any real-world
details.
No, watch the rolling ball experiments.
Greg
Dear Greg,
Regrettably, for Carl to be right, Carl would have to have a firmer
position than it all seems very fishy.
Those stupid balls show that the dip wins--same final speed, but
faster for a short section.
Others have suggested that this smacks of perpetual motion. Since it's
a physics department demo, I assume that perpetual motion has been
eliminated, but I'm hoping that no one asks me to explain exactly why.
Whether wind drag and steady pedal power alter the case enough to
change things for a bicycle with particular initial speed heading into
a dip with a particular depth or width--well, that's the question.
Jobst seems to be saying that he's seen a pair of riders, one on a dip
and the other on a parallel level path, ending up with the dip rider
ending up ahead as he exits the dip, but going noticeably more slowly
than the level rider, who probably overtakes him.
How deep and wide the dip was and how much speed and power were
involved might affect things.
How steady the power was would require a power meter.
My two dips are so short that I can't really say that my power is
steady.
My speed rises dramatically, but that seems likely to be mostly
gravity, not me unleashing my pathetic reserves.
Since my speed rises from about 20 mph to 25-27 mph and doesn't drop
below 20 mph at any point, it seems as if I'd have to be providing
enough extra power to raise my speed from about 15 mph to 20 mph over
what steady power would provide
You can see why I'm not about to claim that it's all due to my mighty
legs. (Who's going to believe that I have an extra 5 mph on the flats,
much less uphill?)
But since my cadence has to rise about 25%, I don't trust my
impression that I'm putting out the same power.
Still, I'm not clear why wind drag should slow the winner of the
ball-race down so much more than the loser. I suspect that a solution
to this would involve a lot of graphs and curves, but maybe someone
will come up with an elegant explanation.
Any explanation should also handle the reverse case, where a rider
goes over a short hill (the dip upside-down). I don't have anything
like that on my daily ride.
Maybe googling for roller-coasters will turn something up.
Cheers,
Carl Fogel