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A glider without water ballast is the exact same shape as a glider with water ballast.
Gravity affects them differently though.. |
A RV, (that's a re-entry vehicle, or the bit that goes BANG!) on an ICBM is released in space.
It's merely 'pointed' quite accurately at its target. Not powered. By the time it reaches the ground, it's doing about Mach 10. |
Thank you, Aram.
Good grief! Mass versus drag for the same object is very apparent in weapon development - ballistic co-efficient. It shows up on basic, old bombs that have different times of flight when released from "x" altitude. Fat ones don't fall as fast as "slick" ones. It is true that Mother Earth attracts the falling object at basic gee. Forget very small gravitational forces due to altitude above the "Mother". The point is that F=m*a, and drag is relevant to that equation if in the atmosphere. The falling object is subject to the same "a", but the "F" part has to do with drag, which a function of v^2 and Cd and area of the object. Eventually the drag force equals Mother Earth's force and you have "terminal velocity". A very good science show years ago was called 'Terminal Velocity". It was about determining a falcon's capability to exceed 200 mph. The sky diver could only reach about 120 mph terminal velocity, so the dude trained the bird to follow a bean bag. He would add heavier lead weights to the bean bag, but the bag was the same area when related to the air while going down. He increased the terminal velocity of the bag to over 200 mph, and the doggone bird could keep up. How? Well, the bird changed its area, so the drag decreased/increased according to the equation of Cd* s*1/2*rho*v^2. From personal experience dive-bombing, I can attest to the fact that deploying "dive brakes" kept me from exceeding the aero limits of the plane in a very steep dive. All else equal, then it was the area that was part of the drag equation that kept me from ripping the wings off, heh heh. Don't try this at home. The end of my epistle is that parts of the plane with ottsa area, but relatively low weight will drift in the atmosphere on the way down. The wind will move them away from the point of impact of dense objects of lesser area like engines or fuel pumps or.... They come down slower, so the wind moves them, duhhh? Been a long time since Aero 101, but I think I got most of it right. |
Gums,
It's always a pleasure. Do you use special nails with larger heads, or is all due to lots of practice with the hammer? |
Awblain:
That's reassuring, since there isn't any "variable gravity" until you're worried about altitudes that reach tens or hundreds of km high. |
Originally Posted by ANCPER
(Post 8369758)
What's the world coming to when pilots don't know the basics of physics? Indeed. What you're missing though, is that you are the one who doesn't know the basics of physics. It is astonishing that you continue to insist that you're correct when it has been demonstrated quite thoroughly that you are wrong. And TINSTAAFL, this is directed at you also, as you too seem determined to continue posting your incorrect understanding of this. There have been several very detailed explanation of *why* a more dense object will fall faster through the atmosphere than will less a dense dense object of the same dimensions. Your example of an empty container falling at the same terminal velocity is, quite simply, wrong. It has been repeatedly explained in this thread *why* it is wrong, with detailed discussions of the forces involved. Instead of simply repeating the claim that they fall at the same speed, without offering proof, why don't you *explain* why you think the explanations are incorrect? Serious question? If you wish to be taken seriously, why aren't you explaining your case instead of just contradicting the explanations which have been given? Merely repeating your contradiction makes you appear as John Cleese in Monty Python's argument sketch. Additionally, a number of posters have cited a very compelling example which makes it abundantly obvious that you are wrong, yet, you pretend that you haven't even noticed. Again, consider the example of two balloons, one inflated with air, and one filled to the same dimensions with water, or concrete, or whatever dense material . Drop them both from the same height. They do not fall at the same rate. Everyone realizes this, except, apparently, you. The air filled balloon is identical to the "empty container" you claim will fall at the same rate as one filled with concrete. In fact it *is* by any definition a container (Not technically empty, as it is filled with air, but so too is the "empty" container in your post actually filled with air) So how can an "empty" (air filled) container fall at the same speed as the same container filled with concrete (as you claim) when it is obvious to all that an air filled balloon does not fall at the same rate as one filled with concrete? That, by the way, is not merely a rhetorical question. I actually would like to see your answer. You have a very simple, obvious, very easily understood example that shows without any question that you are wrong, and somehow you rationalize that away. I am truly interested to hear your explanation for how or why you disregard this. If the fact that it the balloon is filled with air is confusing you let's consider a different form of the same example. A feather. No doubt you have seen feathers falling, and noted that they fall rather slowly. Now lets suppose that a jeweler had very carefully crafted a replica of that same feather from gold. The form of the feather is identical on a microscopic level, it is the same dimensions, the same thickness, the shaft is the same dimensions, as are the barbs, and the barbules between them, everything is duplicated to the same dimensions, except that it is made of solid gold instead of ... well whatever it is feathers are made of. With me so far? OK, I think that everyone will agree that the real feather will fall decidedly slower than the gold feather, right? Is that not a pretty conclusive demonstration that , all else being equal, the speed of a falling object through air is *not* independent of it's mass ? If you believe that it is not, explain *why* not. If you can't explain *why* not, than that's likely an indication that you're mistaken. While you are mulling over your explanation of the previous obvious flaws in your claim, you might consider the following: NASA webpage on Terminal Velocity and Wikipedia Article on Terminal velocity Both of these pages contain an equation for calculating an object's terminal velocity (and both pages describe how that equation is derived) the equations are the same equation in slightly different formats. The NASA page puts the equation in a format that can be shown using only ASCI text and no special formatting (such as fractions, radical signs, or greek letters) but mathematically the equations are identical. Now here's the point which demonstrates quite conclusively that you're wrong. Both equations contain a term for mass, which can *only* mean that terminal velocity *is* in fact affected by mass. If terminal velocity was (as you erroneously claim) independent of mass, mass would not be included as a variable in the equation for calculating it. But, it is included, so it must affect the velocity*. Now, I suspect that you're getting ready to say; “ But the NASA equation uses “weight” which is not the same as mass” True, in the context of physics, weight is not the same as mass. In physics, “weight” is the force of gravity on an object. And weight is equal to gravity times mass (g*m ) so where the NASA equation has W, it really means g*m so the first term in parentheses (2 *W) becomes (2*g*m) which you will note is the same as the upper term beneath the radical in the Wikipedia Equation: 2gm The asterisks in the NASA equation denote multiplication, while the multiplication is implied in the Wikipedia equation, so 2*g*m is just a different way of writing: 2gm. Bottom line, the equations are identical, and they both contain mass as a variable. This leaves us with this: Your (fallacious) opinion:
Originally Posted by ANCPER
(Post 8369758)
the only determinate when it comes to how fast an object will fall is the area of the object and therefore the drag(resistance) it will produce, mass does not come into it.
Originally Posted by NASA
Terminal Velocity = sqrt ( (2 * g* mass ) / (Cd * r * A) All the preceding can be summarized neatly in two questions: How do you resolve you claim that mass doesn't affect the velocity of a object falling through air, when a balloon filled with air and a balloon filled with concrete obviously and unquestionably fall at different speeds? If Mass doesn't affect the speed of a falling body, why does NASA, one of the worlds foremost organizations for the study of aerodynamics and ballistics, say that it does? Serious questions. Response expected. Lack of response will indicate a tacit admission of being mistaken. * if anyone is having difficulty following this reasoning, all you have to do is make some simple calculations of terminal velocity using those equations and the same values for all terms, but different values for mass. The calculated terminal velocity will be different. Try it with the following terms to keep it simple: Drag Coefficient (Cd in NASA's equation) = 1 Area(A in NASA's equation) = 1 (square meter) Gravity (g) = 9.8 (meters/sec/sec) Rho ("r" in NASA's equation) = 1.3 (kg per cubic meter sea level standard temp at pressure ) Mass = 1 (kg) Don't worry about the units, just plug the numbers into the equation and see what you come up with. Now do it again, using all the same numbers except you use 10 kg for mass instead of 1kg. Notice that the calculated terminal velocity is different? the point here is that you can't include a quantity in an equation and not have it affect the result. That means the terminal velocity of an object is dependent on mass. QED. |
Oggers,
Look at those variations though, and consider their nature. At constant height above sea level / geoid, they are very modest, requiring days of data from satellite orbit measurements to measure. The differences are typically at the 10 ppm level, and up to about 60 ppm. See GRACE Gravity Model- Gravity Recovery and Climate Experiment Gravity Model for a description of the GRACE mission and its products. GOCE produced more too. If the author is including GRACE maps is his fluttering debris data, then he's missing the wood for the trees. Is he using pressure altitude to start his simulation? If so, then he should have a further think about the "variable gravity" bit and where isobars lie in 3D. |
Originally Posted by AtomKraft
(Post 8370478)
A glider without water ballast is the exact same shape as a glider with water ballast.
Gravity affects them differently though.. |
It would be an important check for the thoughtful reader to work it out first and then check the answers; that way the thoughtful reader might be able to tell whether they'd been thoughtful enough.
It might be easier to consider the flight of a lead zeppelin before adding the complexities of lift. |
A squared:
Originally Posted by ANCPER View Post What's the world coming to when pilots don't know the basics of physics? It is astonishing that you continue to insist that you're correct when it has been demonstrated quite thoroughly that you are wrong. Will some of the numpties posting here please wake up. For an object in freefall at terminal velocity: drag = mass x g. That is not up for debate. 'g' being fixed (notwithstanding the fact it does vary very slightly :rolleyes:) - if you increase the mass you must increase the drag that would result at terminal velocity. And that means an increase in terminal velocity, because the OP is predicated on a fixed shape and hence a fixed coefficient of drag. This result has already been mentioned and proved in other ways in this thread multiple times now. I am bemused - though no longer the least surprised - to see some posters still wading in to contradict this fact with their half baked physics. |
Awblain
Look at those variations though, and consider their nature. there isn't any "variable gravity" until you're worried about altitudes that reach tens or hundreds of km high. If you wish to prove the point you have now shifted to: If the author is including GRACE maps is his fluttering debris data, then he's missing the wood for the trees. Is he using pressure altitude to start his simulation? If so, then he should have a further think about the "variable gravity" bit and where isobars lie in 3D. |
Originally Posted by oggers
(Post 8371580)
This result has already been mentioned and proved in other ways in this thread multiple times now. Comparison of falling spheres. |
Oggers,
You're not entering into a game of semantics, you're missing the point. You get horizontal gravity variations of about 1 part in 100,000. They don't matter. Period. If anyone really sticks them into a model of falling debris, then they're casting doubt upon the quality of other bits in their model. It is possible that the vertical changes in gravity, by about 3 parts in 1000 from 10km up to sea level might have a subtle effect on where heavy dense debris lands, since that slows less and spends less time lower down than lighter debris. |
The video contains a lot if irrelevant and annoying dialog |
Originally Posted by oggers
(Post 8371658)
How dare you. One of those is one of our finest comedians. The other one used to have a show called "Shooting Stars".
|
Awblain:
You're not entering into a game of semantics, you're missing the point. You get horizontal gravity variations of about 1 part in 100,000. They don't matter. Period. there isn't any "variable gravity" until you're worried about altitudes that reach tens or hundreds of km high. |
Oggers,
What is about "1 part in 100,000" that suggest it matters? Drag changes by 1 part in 50,000 would have the same effect. How much is that? It's associated with the same density changes as climbing about 10cm. QED. Perhaps Dr Greaves should worry about density changes from the top to the bottom of the wreckage too? I don't think so, and I assume that in fact Dr Greaves meant something else in his abstract. |
Having read through the paper, the tool is designed to have the ability to deal with very high altitude break ups of re-entering space vehicles where gravitational variation with altitude would have an effect.
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Even then, it's hardly worth the worry.
At 100km, the difference in gravity from sea level is only 3%. If you get have an exosphere density profile correct to 3% then you're already doing well. |
awblain
A question. If you don't believe in variable gravity, what exactly do you think causes tides....? |
There is no relevant, variable gravity.
The tidal force variation at the surface of Earth? 1 part in 10 million. At the Planck scale, gravity's all over the place, but that has no relevance to falling wreckage either. |
I would suggest that anything that can make squillions of tons of water and earth move up and down meters is relevant....
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Interesting indeed, but irrelevant. That headline should be "Well-known gravity variations mapped on much finer scales than before"
If you can measure a difference between free fall times at high and low tide, then you have an aptitude for experiment. You're able to measure 10 parts in a billion. |
Originally Posted by Tourist
(Post 8372107)
I would suggest that anything that can make squillions of tons of water and earth move up and down meters is relevant....
As Awblain said, the amount the effective gravity changes at the earth's surface due to lunar and solar effects is about one ten-millionth of total gravity. Yes, it is sufficient to cause tides. No, it ain't gonna make much difference in how fast an object falls. For an object of say 10 kg, that means it's weight will vary between 98 newtons and 98.000001 newtons. For a falling object, the effects are the difference between and acelelration of 9.8 m/sec/sec and 9.80000001 m/sec/sec. The difference is very small, and orders of magnitude below the noise level for something like predicting falling debris. |
Originally Posted by Tourist
(Post 8372107)
I would suggest that anything that can make squillions of tons of water and earth move up and down meters is relevant....
|
The tidal acceleration moves water about two meters in six hours.
The free fall acceleration moves water two meters in about 0.4 seconds. The force is related to the square of the ratio of those times. That's gives a measure of the low-down scale of tidal forces. If you are in genuine free-fall though (and not the term as bastardized by parachutists), then the presence of tidal forces is the only thing that reveals the presence of gravity. |
Awblain:
I assume that in fact Dr Greaves meant something else in his abstract. a) Clarify in your own mind what you think Dr Greaves meant which is wrong b) Check you have that bit right c) Come back to this forum and detail the errors you have identified in his work. Right now you are obfuscating, shifting position and creating fog. What is about "1 part in 100,000" that suggest it matters? |
In writing an abstract, it would be in Dr Greaves' interest not to make statements that make the whole look wacky. Based upon that choice of words, I would not read his paper.
Looking at it now, it appears that his introducer misquoted him. He includes the term "altitude dependent gravity" in his paper, and while I think this is a bit of a waste of time to consider, it is a viable effect, compared with those of both the geoid and tides. |
awblain
Just admit it, you can't actually find anything wrong with Dr Greaves' model and so you are waffling. And meanwhile That headline should be "Well-known gravity variations mapped on much finer scales than before" "Mount Nevado Huascarán in Peru has the lowest gravitational acceleration, at 9.7639 m/s2, while the highest is at the surface of the Arctic Ocean, at 9.8337 m/s2. These differences mean that in the unlikely event that you found yourself falling from a height of 100 metres at each point, you would hit the surface in Peru about 16 milliseconds later than in the Arctic." 16milliseconds difference in just 100 meters! To my mind that is clearly worth considering if one is developing a model such as Dr Greaves'. However, you say of such variations: They don't matter. Period. If anyone really sticks them into a model of falling debris, then they're casting doubt upon the quality of other bits in their model. Based upon that choice of words, I would not read his paper. |
back to the chase
Seems the robo-moderator is holding/deleting my last post. Prolly 'cause I used a "bad" word.
Anyway, it was about using previous incidents of vehicles coming apart at altitude. So we can look at those to get back to the MAS 370 search and distribution of wreckage. And seems to me that it was that which started this discussion. |
Something further to consider.
If you drop a cat from a height of say 10 feet, it will always fall on it's feet. But if you drop a piece of buttered toast from the same height it will always fall with the buttered side down. So here is the problem, if you tie a piece of buttered toast onto a cat's back and drop it from the same height will the buttered toast land butter down i.e. with the cat upside down, or will the cat land on it's feet i.e with the toast butter side up? :ugh: |
awblain
I only butted in because I was enjoying you try to dig yourself deeper in a hole... However... "The tidal acceleration moves water about two meters in six hours. The free fall acceleration moves water two meters in about 0.4 seconds. The force is related to the square of the ratio of those times. That's gives a measure of the low-down scale of tidal forces." Oh, dear oh dear..... Please tell me that you don't think that is in any way true? |
Please go away with your ignorance about forces, vexatious chappies,
Gravity differences are more complex than you suggest, as it depends where you are, and above what reference level. There is also the rotational/centrifugal/centripetal part to consider. The difference in time between equally spaced gates from above a Peruvian mountain (equatorial bulge plus a mountain under your feet) against the arctic ocean (polar squatting and kms of low-density water) is as extreme as it gets, but the difference in time is very small. The difference in g, by about 0.7% from these spots is only the same as the difference from climbing a few tens of km. Compare the ratios of the distances to the center of the Earth from the North Pole and antiplanic Peru. And tourist, perhaps a remedial course in counting is in order, or am I somehow wrong about the intertidal period and the oceanic tidal range? |
Folks, a delightfully entertaining thread. However, as always, please do keep the excited angst under control ...
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What's this about variable gravity causing tides. That's a bit novel. Can someone explain?
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awblain
You have made about twenty posts since you first took issue with Dr Greaves' paper on trajectory analysis. Still you fail to communicate what errors exist in his model. |
Just read his paper. Oh dear, he has stuffed up on his altitude dependent gravity. Not impressed by his discussions on numerical methods either. But what's this about variable gravity causing the tides again? Perhaps someone can explain ?
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Nothing? How very wise.
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Mr Optimistic
Oh dear, he has stuffed up on his altitude dependent gravity. |
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