To Brake or not to Brake: The Descender’s Dilemma
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Similar example is holding the speed below a safe threshold. Whichever that particular speed was - depending on road, skill etc. The faster you let the bike go, the more work is done by the wind, less with the brakes.
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You are assuming simple coast down. I'm not. People usually don't just coast all the way down hills. Depending on gearing, they can pedal up from 35 to 50 mph before they simply coast. I will...and have all along... agree that at aerodynamics plays a factor but the degree to which it plays a factor is what I question. If you are doing the speed in the links I posted above...between 70 and 80 mph...in a tuck position and you suddenly untuck, the bike doesn't slow to the mythic terminal velocity of 47 mph. It's hard to say how much the speed slow but, from my experiences with higher than 47mph velocity downhills, setting up and catching the wind provides only marginal speed reduction. You still need the brakes to slow down.
The example I provided earlier of a local 800m hill. Rider starts at the top with over 700,000J of potential energy. If he coasts down the whole hill and ends up travelling 70kph at the bottom he will have dissipated over 680,000J of energy in the form of heat on the way down. If he coasts up to terminal velocity and doesn't brake all the potential energy gets dissipated by aero drag. If he want's to go slower than terminal velocity at say 50kph he will have to burn up a lot of energy by heating up his rims. I think that was the original point. By going faster you can brake less.
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If you start at the top of a hill with a certain amount of potential energy and have to stop at the bottom of the hill at a specific point, the amount of energy you need to scrub off is the same no matter how you get there. At the end of the run, you've converted that potential energy into kinetic energy and then into heat energy through friction of the braking system. It really doesn't matter if you drag your brakes all the way down the hill or brake as hard as you can at the bottom or brake hard in intervals to slow the bike to maintain a specific speed, you are still converting the same amount of kinetic energy into heat so your brakes have to "work" just as hard either way.
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Rediscovering fundamental physics is fun, though slightly off topic. Most of the recent postings do reflect what I take to be the standard view. At the risk of further illustrating the rule that the most wisdom is to be found in the briefest postings, I will try to summarize that.
The force due to gravity in the downhill direction, per unit mass is g sin(angular gradient). For not very extreme gradients this is approximately (g times (% grade) /100 ).
Thus if air resistance is negligible—as it is if you are going very slowly—you pick up 2 mph per second freewheeling down a 10% grade, since g is about 20 mph/s/s.
The gravitational force is opposed by air resistance that increases as the square of your speed, until at some sustained coasting speed (= terminal velocity in the downhill direction) the forces cancel and you stop accelerating. That coasting speed depends on rider mass and posture but is always proportional to the square root of the gradient. For a normal, moderately aero, posture on the drops, mine is around 40mph on a 6% grade. The approximations suggest twice that (80 mph) for a (sufficiently long) 24% grade.
Applying prathmann’s excellent formula above, my worst speed for overheating would be 46 mph on a 24% descent, or 23 mph on a 6% descent.
The force due to gravity in the downhill direction, per unit mass is g sin(angular gradient). For not very extreme gradients this is approximately (g times (% grade) /100 ).
Thus if air resistance is negligible—as it is if you are going very slowly—you pick up 2 mph per second freewheeling down a 10% grade, since g is about 20 mph/s/s.
The gravitational force is opposed by air resistance that increases as the square of your speed, until at some sustained coasting speed (= terminal velocity in the downhill direction) the forces cancel and you stop accelerating. That coasting speed depends on rider mass and posture but is always proportional to the square root of the gradient. For a normal, moderately aero, posture on the drops, mine is around 40mph on a 6% grade. The approximations suggest twice that (80 mph) for a (sufficiently long) 24% grade.
Applying prathmann’s excellent formula above, my worst speed for overheating would be 46 mph on a 24% descent, or 23 mph on a 6% descent.
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I can agree with that speed/ braking chart. I would say the hill needs to be at least 12% to get near limitless speed. On a 6 or 7% hill I have to pedal like mad to get 37 mph. If into a mere 6 mph wind I just can't go more than 30. Same on a short 9% hill where I wizzed up to 47.8 mph with a light tail wind. Into the same wind I get stuck at 35 mph. Air does matter a LOT. I have a video of my top speed there. Maybe these hills are too short to really see, but I doubt it.
I see altitude can make a big difference.
I see altitude can make a big difference.
Last edited by GamblerGORD53; 10-12-16 at 03:47 PM.
#81
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OP , just get comfortable going faster? Sit up more and pulse the brakes, start there. I usually top out at 40- 45 mph.
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A useful linkL the square root relation between coasting speed and gradient can be verified using the calculator for terminal velocity in downhill coasting at Analytic Cycling. To use it, remember to enter zero power for the rider.
https://www.analyticcycling.com/DiffE...lope_Page.html
Another blog has a graph that clearly shows the square root dependence, though it wrongly gives the equation for terminal velocity as linear with slope (a typo I assume)
The Penultimates Cycling Team: The Physics of Cycling II, or Why I am Awesome on the Downhill
https://www.analyticcycling.com/DiffE...lope_Page.html
Another blog has a graph that clearly shows the square root dependence, though it wrongly gives the equation for terminal velocity as linear with slope (a typo I assume)
The Penultimates Cycling Team: The Physics of Cycling II, or Why I am Awesome on the Downhill
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But, this particular example is incorrect. Take a 10 mile long descent. You can reach a terminal velocity in about a mile. You can brake 10 times to zero. Or just once at the bottom. Letting the wind do all the braking.
Similar example is holding the speed below a safe threshold. Whichever that particular speed was - depending on road, skill etc. The faster you let the bike go, the more work is done by the wind, less with the brakes.
Similar example is holding the speed below a safe threshold. Whichever that particular speed was - depending on road, skill etc. The faster you let the bike go, the more work is done by the wind, less with the brakes.
True, partly. If let the bike go faster and you have the nerve to go around corners faster, you will brake less. But if you have to slow or stop, the faster you go the more you will have to brake and the more heat you will generate. Again, aerodynamic drag will handle a portion of the speed control but it may not be enough of a portion to keep you from running off the road if you are coming into a corner too hot. Nor will it be enough if you have to stop completely.
It's a matter of magnitude and how much you consider to be "much higher". Sure, aerodynamic drag reduces the amount of time you have to use your brakes and the amount of heat generated. But I simply disagree with you as to how much that is. If you are in a tuck and squeezing every last mph out of a downhill...say doing 80 mph down a hill..., sitting up suddenly and increasing the drag isn't going to suddenly scrub half the speed off. I doubt that it will scrub a quarter of the speed off and it's going to take a long time to do even that.
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The problem here is that you are attributing too much braking power to the wind. Yes, it has an effect. But the magnitude just isn't that great. I'm not talking about braking 10 times to a full stop on some 10 mile long descent but only controlling your speed to some speed the rider feels save with. Simply put, the wind will not do all the braking. It will do some of it, of course. And, if you have a long enough run-out at the bottom of the hill, you might have time to let the wind do all the braking but in the real world where you don't have long run-outs and 10 mile long descents include curves, your brakes will have to handle the job.
#85
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It's a matter of magnitude and how much you consider to be "much higher". Sure, aerodynamic drag reduces the amount of time you have to use your brakes and the amount of heat generated. But I simply disagree with you as to how much that is. If you are in a tuck and squeezing every last mph out of a downhill...say doing 80 mph down a hill..., sitting up suddenly and increasing the drag isn't going to suddenly scrub half the speed off. I doubt that it will scrub a quarter of the speed off and it's going to take a long time to do even that.
Getting back to your point about kinetic energy. Starting at the top of the hill.
We'll assume 6% grade, 100m elevation, 100 kg (rider + bike). At the top of the hill, the rider has 98 kJ of potential energy.
If the rider applies, no brakes and simply coasts hitting a terminal velocity of 60.4 km/h.(Bicycle Speed (Velocity) And Power Calculator, [drops, 90kg rider, 10kg bike, 0W, 0 wind]
At the bottom of the hill, the rider has a kinetic energy of 14.1 kJ.
That means that the aerodynamic drag has dissipated the equivalent of 84 kJ of energy. Which is far more than the brakes would have to do to stop the rider at the bottom. If you don't like the calculated value for terminal velocity choose a different one, it doesn't really matter. Any realistic terminal velocity will result in the majority of the energy being dissipated by aero drag.
In the situation I just pointed, if the rider's potential energy were converted into kinetic energy, the rider would reach the bottom of the hill at 160 kph (~100 mph). Clearly, that's absurd, since no rider gets going that fast.
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Wheel stress and braking force?
Wheel stress and braking force
The original post referred to spoke breakage, but mechanical stress has not been given much attention in this thread. It is tempting to suppose that braking on a steep descent stresses the wheels, but this may wrong. Theoretically, under admittedly drastic simplifying assumptions, *steady* braking to maintain a target downhill speed produces no wheel stress, and stresses on the wheel are actually reduced on a steep fast descent.
Suppose first for simplicity that the rim is absolutely rigid. The effect of gravity is then to decenter the circular rim slightly relative to the dropout, and the pattern of tension in the spokes follows from that. If you are parked by applying rim brakes on a downhill grade, both the downhill component of the gravitational force and the orthogonal ‘into the ground’ component are cancelled by an uphill braking force applied to the rim (that is divided equally between the brake pad contact patch and the tire contact patch). So the decentering force and the resulting spoke tensions are all the same as with no brakes on the flat. With slow downhill progress, the pattern of spoke tensions moves around the wheel without changing otherwise, and this happens in the same way whether the descent is gradual or steep.
On a fast descent, the uphill braking force is handed over in part to air resistance, and is not (fully) applied to the rim. The ‘into the ground’ force is reduced by the cosine of the angle of descent. So the variation in spoke tension is slightly reduced accordingly (until in the limit of vertical free fall, spoke tension becomes uniform).
If we relax the rigidity assumption, it’s clear that subtle flattening of the rim near the contact patch reduces the tension of just a few spokes there, with only a slight compensatory increase of tension at the top and sides (see for instance, Jobst Brandt). That effect survives on downhills, with the cosine reduction alleviating it slightly. The tangential braking forces applied to the rim will not cause deformation, so they add no stress to what is captured in the rigid rim model.
This analysis suggests that risks to the wheel from heavy braking on steep descents are not mechanical but thermal (like the blowout risk).
The original post referred to spoke breakage, but mechanical stress has not been given much attention in this thread. It is tempting to suppose that braking on a steep descent stresses the wheels, but this may wrong. Theoretically, under admittedly drastic simplifying assumptions, *steady* braking to maintain a target downhill speed produces no wheel stress, and stresses on the wheel are actually reduced on a steep fast descent.
Suppose first for simplicity that the rim is absolutely rigid. The effect of gravity is then to decenter the circular rim slightly relative to the dropout, and the pattern of tension in the spokes follows from that. If you are parked by applying rim brakes on a downhill grade, both the downhill component of the gravitational force and the orthogonal ‘into the ground’ component are cancelled by an uphill braking force applied to the rim (that is divided equally between the brake pad contact patch and the tire contact patch). So the decentering force and the resulting spoke tensions are all the same as with no brakes on the flat. With slow downhill progress, the pattern of spoke tensions moves around the wheel without changing otherwise, and this happens in the same way whether the descent is gradual or steep.
On a fast descent, the uphill braking force is handed over in part to air resistance, and is not (fully) applied to the rim. The ‘into the ground’ force is reduced by the cosine of the angle of descent. So the variation in spoke tension is slightly reduced accordingly (until in the limit of vertical free fall, spoke tension becomes uniform).
If we relax the rigidity assumption, it’s clear that subtle flattening of the rim near the contact patch reduces the tension of just a few spokes there, with only a slight compensatory increase of tension at the top and sides (see for instance, Jobst Brandt). That effect survives on downhills, with the cosine reduction alleviating it slightly. The tangential braking forces applied to the rim will not cause deformation, so they add no stress to what is captured in the rigid rim model.
This analysis suggests that risks to the wheel from heavy braking on steep descents are not mechanical but thermal (like the blowout risk).
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It's a matter of magnitude and how much you consider to be "much higher". Sure, aerodynamic drag reduces the amount of time you have to use your brakes and the amount of heat generated. But I simply disagree with you as to how much that is. If you are in a tuck and squeezing every last mph out of a downhill...say doing 80 mph down a hill..., sitting up suddenly and increasing the drag isn't going to suddenly scrub half the speed off. I doubt that it will scrub a quarter of the speed off and it's going to take a long time to do even that.
Slowing down from a terminal velocity of 80kph is not going to cause aluminum rims to overheat since there isn't enough energy available. Dragging your brakes for 10 min to limit your speed to 50kph will inject a lot of heat into your rims.
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Wheel stress and braking force
The original post referred to spoke breakage, but mechanical stress has not been given much attention in this thread. It is tempting to suppose that braking on a steep descent stresses the wheels, but this may wrong. Theoretically, under admittedly drastic simplifying assumptions, *steady* braking to maintain a target downhill speed produces no wheel stress, and stresses on the wheel are actually reduced on a steep fast descent.
Suppose first for simplicity that the rim is absolutely rigid. The effect of gravity is then to decenter the circular rim slightly relative to the dropout, and the pattern of tension in the spokes follows from that. If you are parked by applying rim brakes on a downhill grade, both the downhill component of the gravitational force and the orthogonal ‘into the ground’ component are cancelled by an uphill braking force applied to the rim (that is divided equally between the brake pad contact patch and the tire contact patch). So the decentering force and the resulting spoke tensions are all the same as with no brakes on the flat. With slow downhill progress, the pattern of spoke tensions moves around the wheel without changing otherwise, and this happens in the same way whether the descent is gradual or steep.
On a fast descent, the uphill braking force is handed over in part to air resistance, and is not (fully) applied to the rim. The ‘into the ground’ force is reduced by the cosine of the angle of descent. So the variation in spoke tension is slightly reduced accordingly (until in the limit of vertical free fall, spoke tension becomes uniform).
If we relax the rigidity assumption, it’s clear that subtle flattening of the rim near the contact patch reduces the tension of just a few spokes there, with only a slight compensatory increase of tension at the top and sides (see for instance, Jobst Brandt). That effect survives on downhills, with the cosine reduction alleviating it slightly. The tangential braking forces applied to the rim will not cause deformation, so they add no stress to what is captured in the rigid rim model.
This analysis suggests that risks to the wheel from heavy braking on steep descents are not mechanical but thermal (like the blowout risk).
The original post referred to spoke breakage, but mechanical stress has not been given much attention in this thread. It is tempting to suppose that braking on a steep descent stresses the wheels, but this may wrong. Theoretically, under admittedly drastic simplifying assumptions, *steady* braking to maintain a target downhill speed produces no wheel stress, and stresses on the wheel are actually reduced on a steep fast descent.
Suppose first for simplicity that the rim is absolutely rigid. The effect of gravity is then to decenter the circular rim slightly relative to the dropout, and the pattern of tension in the spokes follows from that. If you are parked by applying rim brakes on a downhill grade, both the downhill component of the gravitational force and the orthogonal ‘into the ground’ component are cancelled by an uphill braking force applied to the rim (that is divided equally between the brake pad contact patch and the tire contact patch). So the decentering force and the resulting spoke tensions are all the same as with no brakes on the flat. With slow downhill progress, the pattern of spoke tensions moves around the wheel without changing otherwise, and this happens in the same way whether the descent is gradual or steep.
On a fast descent, the uphill braking force is handed over in part to air resistance, and is not (fully) applied to the rim. The ‘into the ground’ force is reduced by the cosine of the angle of descent. So the variation in spoke tension is slightly reduced accordingly (until in the limit of vertical free fall, spoke tension becomes uniform).
If we relax the rigidity assumption, it’s clear that subtle flattening of the rim near the contact patch reduces the tension of just a few spokes there, with only a slight compensatory increase of tension at the top and sides (see for instance, Jobst Brandt). That effect survives on downhills, with the cosine reduction alleviating it slightly. The tangential braking forces applied to the rim will not cause deformation, so they add no stress to what is captured in the rigid rim model.
This analysis suggests that risks to the wheel from heavy braking on steep descents are not mechanical but thermal (like the blowout risk).
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But I also know that the faster the bike goes, the more heat will be generated when I inevitably have to use the brakes. Dragging the brakes all the way down the hill is worse for overheating the rims but that's because riders who do this are never allowing the brake system to lose the heat that's being put into the system. It's not because they are putting more heat into the system, only that they are keeping what heat the generate at the rim.
Going faster doesn't put less heat into the rims when the brakes are used. The amount of heat put into the system is proportional to the square of the speed of the bike and rider. It's still possible to overheat the system by going faster if you have to use the brakes.
I agree the aero drag will not help in stopping you but that's not the point. The idea of letting your speed rise is you don't need to use your brakes until you need to slow down for a corner. The majority of time you won't be on your brakes at all and you'll either be at terminal velocity or accelerating to terminal velocity.
Think of it this way: if you were traveling at 80kph and had to brake to 50 kph and keep the speed there for some reason would the brake system be cooler than if you kept the brakes on for 10 minutes to keep the bike at 50 kph down the same hill?
Pulse braking...i.e. getting short intense braking followed by coasting...works not because it generates less heat but because you are allowing the system to radiate the heat away during those coasting periods. The amount of heat generated is the same or even higher but the rider is managing the heat better.
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#90
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Yes, by a very large margin.
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To summarize the two scenarios for a descent down a 12.7% hill:
A) Ride your brakes and limit your speed to 50kph => dissipate 560,000J of heat over 10 min
B) Coast at an 80kph terminal velocity and slow from 80 to 50kph at the end => 13,500J into the rims.
While you're pouring 900+W into your rims for 10min they will reach an equilibrium temperature but it's going to be fairly high. A bike rim is not an ideal shape for an effective heat sink.
Pulse braking...i.e. getting short intense braking followed by coasting...works not because it generates less heat but because you are allowing the system to radiate the heat away during those coasting periods. The amount of heat generated is the same or even higher but the rider is managing the heat better.
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In #50 I suggested a different reason why intermittent braking can be helpful: for a given net propulsive energy, average speed is greatest--or total descent time is least—when the speed is constant. So you can increase descent time--which is also the time that the rim has to cool down--by braking strongly and infrequently rather than dissipating the same amount of energy in steady braking. But this benefit is small unless you drastically reduce your speed each time, and then coast back slowly to your chosen max speed. If the braking pulses are breif and come often enough that speed is almost constant, the benefit is negligible.
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That's only if you don't have to use the brakes for some reason. I'll agree that using the wind to help control speed is a wise thing to do. I practice that myself. I let the bike go as fast as it wants to...and often push it to go faster...then use the brakes quickly and only as much as necessary.
But I also know that the faster the bike goes, the more heat will be generated when I inevitably have to use the brakes. Dragging the brakes all the way down the hill is worse for overheating the rims but that's because riders who do this are never allowing the brake system to lose the heat that's being put into the system. It's not because they are putting more heat into the system, only that they are keeping what heat the generate at the rim.
Going faster doesn't put less heat into the rims when the brakes are used. The amount of heat put into the system is proportional to the square of the speed of the bike and rider. It's still possible to overheat the system by going faster if you have to use the brakes.
But I also know that the faster the bike goes, the more heat will be generated when I inevitably have to use the brakes. Dragging the brakes all the way down the hill is worse for overheating the rims but that's because riders who do this are never allowing the brake system to lose the heat that's being put into the system. It's not because they are putting more heat into the system, only that they are keeping what heat the generate at the rim.
Going faster doesn't put less heat into the rims when the brakes are used. The amount of heat put into the system is proportional to the square of the speed of the bike and rider. It's still possible to overheat the system by going faster if you have to use the brakes.
Using wind to slow the rider down keeps the brakes doing total work - lower, as well as shorter total braking time. As well as more cooling time. So I think it's a better option for keeping them cooler.
There might be a flaw in my logic. The fact you're the only member disagreeing with the theory, doesn't automatically mean you're wrong. We could all be missing something. I really respect your posts and knowledge, but fail to see your point of view on this topic as a correct one. Still doesn't mean I'm right. The only way to be 100% sure is to borrow a speedometer and a laser thermomether and do a test on a local hill.
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Other than the fact that 18 mph is an extremely slow speed for a 6% grade, I fail to see how it's the "worst possible speed".
If you are using rubber rim strips, maybe. But the increase in air pressure from heating has less of an effect than most people think. If you have a tire at 100 psi at 70°F and you raise the temperature to 270°F, the pressure rises 37psi. That might be enough to push into a rubber rim strip but if you use a fabric rim strip...which you should...it won't be a problem.
If you are using rubber rim strips, maybe. But the increase in air pressure from heating has less of an effect than most people think. If you have a tire at 100 psi at 70°F and you raise the temperature to 270°F, the pressure rises 37psi. That might be enough to push into a rubber rim strip but if you use a fabric rim strip...which you should...it won't be a problem.