First, the force itself (being the weight) , we are told by Galileo, does not affect the acceleration of a falling body. — Gampa Dee
So while m (small mass) can indeed affect the force, what good is it in calculating the acceleration if all different masses fall at the same rate? — Gampa Dee
The reason for this is that the mass of a falling object is negligible in relation to the mass of the Earth. — unenlightened
the mass of the Earth cannot probably still be measured to the ton, and if it could, some of the mass would been the air above and exert a negative force. — unenlightened
Different masses accelerate at the same rate towards a reference mass because they also have different inertias, which balances the different forces generated..... — Pantagruel
ndeed it is, but the same condition applies with respect to the relationship between force and inertia. The force is a composite product of the two masses, as is the acceleration. — Pantagruel
...in fact, this is all we need in my opinion to calculate the g acceleration.
However, since the same is said for the second mass, the two accelerations will need to be added, and if the second mass is great or small will make a difference in the overall g, it seems. — Gampa Dee
But also yes, the overall force realized does vary if the mass of the smaller object varies — Pantagruel
Ok. And they have the same acceleration because they have different inertias. How does this not answer that? — Pantagruel
Initial acceleration of an object due to gravity of a primary is mass independent. I mean, F=ma, which if substituted directly into F=GMm/r² gets you A=GM/r², something independent of m altogether.My post is about reconciling gravity with Galileo’s concept of different masses having exactly the same acceleration in freefall; — Gampa Dee
Yep.Initial acceleration of an object due to gravity of a primary is mass independent. I mean, F=ma, which if substituted directly into F=GMm/r² gets you A=GM/r², something independent of m altogether. — noAxioms
Not quite; as noAxiom shows, the mass of the falling object is irrelevant....the mass of a falling object is negligible... — unenlightened
But now if you increase the density of that ball to say the mass of the moon, it will hit the ground in less time, not because its initial coordinate acceleration is any greater, but because it has enough mass to significantly cause the ground to come up and meet it — noAxioms
Initial acceleration of an object due to gravity of a primary is mass independent. I mean, F=ma, which if substituted directly into F=GMm/r² gets you A=GM/r², something independent of m altogether. — noAxioms
No it isn't, since Earth accelerating upward will decrease r more quickly, and since the coordinate acceleration of the dropped mass is a function of that r, it affects the acceleration of the dropped thing. That's the secondary effect I was talking about.but to claim that the increased acceleration due to the earth moving upwards is separated from the downward moving mass, — Gampa Dee
Under Newtonian physics, yes. But we're not adding speeds here, we're computing coordinate acceleration.I don’t quite get. If someone drives towards you at 20 km/hr and you towards him/her at 20 km/hr, the velocity is indeed 40 km/hr relative to the two cars... we add the two velocities
Until r starts changing...As it is written it follows Galileo’s axiom, for it doesn’t matter what you put as the small mass, the acceleration will continue as being (GM/r^2)
Still works, at least under Newtonian physics. Same coordinate acceleration.But then, what do we do for the mass equal to the mass of the moon?
That would be wrong. The acceleration of the moon would not have that component. Earth does. Remember, I was stating that the formula gives acceleration relative to some inertial frame. I think you are trying to use the accelerating frame of Earth when adding them like that. But the force is given by F=GMm/r², and since acceleration is A = F/m, the moon accelerates by the simple formula, not adding the Earth part to it. Either that or F=ma is wrong, which is a denial of some pretty basic laws.It is here that I personally believe that another acceleration needs to be added onto the first.
being A is also = Gm/r^2
Total acceleration of the system is zero by conservation of momentum. So don't add them like that. It would be wrong to do so.... if we add both of them, then we get A = (GM / R^2) + (Gm / r^2)
However , this equation does not agree with Galileo since a change in mass for the small m will indeed change the total acceleration of the system.
In reality, it would take not 3.3 seconds to hit the ground, but probably just a fraction of a second in the dense moon case. You're not going to compute that by just adding the accelerations, which treat both objects as point masses or rigid spheres, which they are not. — noAxioms
Context is needed for that. This seems to come from here:I understand the case for the dense moon would be extreme....would you have a problem with the equation I have written to Pantagruel?
M / 4pi * r ^2 = k g — Gampa Dee
First of all, gravity isn't energy. I have no idea what you might consider the 'gravitational energy' of Earth. Mass divided by 4 π r² gives you, well, I don't know what. It seems vaguely related to area of a circle. You equate this to 'k g', but no idea what 'k' is (kilo?). 'g' is the constant 9.8 m/sec², so you're seemingly equating this function of mass and radius to the constant 9800 m/sec²The way I see it would be that Mass (the earth) gravitational energy will be causing an acceleration g at a certain distance ....the whole sphere at that distance will have the same g...
M / 4pi * r ^2 = k g — Gampa Dee
You seem to be equating g with A. 'g' is a constant magnitude of acceleration (a scalar), so it cannot be smaller or larger. A is a variable, and a vector, not a scalar. A = GM/r², so yes, 'A' becomes quite large if r is small enough. Saying 'g' can be quite large is like saying a meter can be larger if my table is wide enough.Here, if r is small then g can become extremely large.
'mass g' doesn't parse. I don't know what you mean by this. Are you now adding random objects here and there? Then you need to separately compute the acceleration of each and add those accelerations. Newton showed (via shell theorem) that any spherical distribution of mass of radius r can be treated as a point mass by objects outside of r.Any other mass g acceleration would need to be added at every point in space...
First of all, gravity isn't energy. I have no idea what you might consider the 'gravitational energy' of Earth. Mass divided by 4 π r² gives you, well, I don't know what. It seems vaguely related to area of a circle. You equate this to 'k g', but no idea what 'k' is (kilo?). 'g' is the constant 9.8 m/sec², so you're seemingly equating this function of mass and radius to the constant 9800 m/sec² — noAxioms
Here, if r is small then g can become extremely large.
You seem to be equating g with A. 'g' is a constant magnitude of acceleration (a scalar), so it cannot be smaller or larger. A is a variable, and a vector, not a scalar. A = GM/r², so yes, 'A' becomes quite large if r is small enough. Saying 'g' can be quite large is like saying a meter can be larger if my table is wide enough. — noAxioms
Any other mass g acceleration would need to be added at every point in space...
'mass g' doesn't parse. I don't know what you mean by this. Are you now adding random objects here and there? Then you need to separately compute the acceleration of each and add those accelerations. Newton showed (via shell theorem) that any spherical distribution of mass of radius r can be treated as a point mass by objects outside of r. — noAxioms
Sorry, but I kind of came in late to this discussion and I don't know what you're trying to do beyond what is described by these very simple equations. For small objects, they all fall at the same rate, and the only reason the feather falls slower is due to air friction. They brought a feather to the moon to show it falling at the same rate as a rock. PR stunt..,. tax dollars at work. — noAxioms
So the acceleration of the rock in earth's gravitational field is not dependent on the mass of the rock. It is dependent on the distance of the rock from the center of mass of the earth, and on the mass of the earth.
You seem to be asking, what if M were different? — PhilosophyRunner
I have no idea what you might consider the 'gravitational energy' of Earth. Mass divided by 4 π r² gives you, well, I don't know what. It seems vaguely related to area of a circle. — noAxioms
Secondly why would we include the acceleration of the earth caused by the second mass? That is not what we were calculating - we were calculating the acceleration of the rock. If you wanted to calculate the acceleration of the Earth caused by the rock, that is a separate calculation
an hour ago — PhilosophyRunner
If you want to model a system where both bodies are accelerating you will have to use the two-body equations of motion, — PhilosophyRunner
ok; I think we might be going somewhere. When we measure the acceleration of the rock towards the earth, aren't we not measuring, at the same time, the acceleration of the earth towards the rock? How could you know the difference? — Gampa Dee
ok; so, what would be this equation? — Gampa Dee
Very little of Earth is 'at a height above the ground', so by this definition, Earth has negligible gravitational energy. What you are describing is the positive potential energy of a small amount of mass relative to nearby places of lower gravitational potential. It has no requirement that the material be stationary relative to any particular thing.I view gravity as a potential for movement observed as the weight of a body, if the mass is stationary, located at a certain height above the ground — Gampa Dee
The symbol for that is 'a', not 'g'. 'a' is a vector variable acceleration. g is a scalar constant acceleration. Neither are a force. Force is measured in Newtons and uses the symbol F. Try to use standard symbols when discussing such things, as personal preferences only lead to confusion.For me, g is the potential gravitational acceleration given to a “test mass” caused by some other mass (usually a large one), not necessarily the earth; it could be the moon, mars or Jupiter. I was not using the letter “a” because we cannot speak of a force as being the cause.
We've been doing that, but it's actually lowercase. 'A' is used for Area (mathematics) and electrical current (physics). So I'm committing the same offense; :sad:However, if you want me to write down “A”, instead of “g”, then, no problem, noAxiom,, I will use the letter “A”.
Well, I would make A lowercase to fix that problem, and the rest is correct. The acceleration of the moon when it is at radius r is exactly that in Newtonian physics. That does not mean it will hit the ground in 3 1/3 seconds like the 10 kg ball. As I said, a small fraction of a second is more likely.Now, concerning the example of the high density ball pulling the earth towards itself ; How would you write the equation, if A = GM/r² is the acceleration caused by the earth?
I'm assuming that the dense super-mass is rigid, so yes, the acceleration applies to every point in the moon-ball. I am not assuming Earth is sufficiently rigid to not deform under the ungodly tidal stress the ball would apply to it. The sidewalk slab 60 meters below will be yanked up without waiting for Earth to catch up with it.Any other mass g acceleration would need to be added at every point in space
Acceleration is absolute, not relative, so adding them seems to result in a fairly meaningless value. I suppose you can use it to compute the rate of change in distance between the two objects, only in a 1-dimensional case, but that rate isn't acceleration. For instance, if an apple detaches from a tree and the distance between me and it decreases at 9.8 m/sec², that in no way suggests that I am accelerating at that rate, and in fact I'm accelerating (coordinate acceleration, not proper acceleration) away from it a little bit.Now you mentioned that when adding masses we also need to “add” accelerations... this is all that I am saying in this post.
But there is an equation for each object, each dependent on only that mass, and not on the mass of the thing accelerating towards it.The Newtonian gravitational equation, identifying two masses, has only one acceleration , the one caused by the earth.
OK, but the surface area seems to be a needless complication. We know the acceleration as a=GM/r². Where the surface is is irrelevant so long as it is below r.4 π r², being the surface area of a sphere, would be dependent to the surface Acceleration — Gampa Dee
That would not work. A grapefruit has a similar area, but far less gravitational acceleration at its surface. So acceleration is not a function of just area.While, this is not directly the density of mass, it seems to identify a mass having a certain spherical area as having a certain gravitational surface acceleration..
As P-R points out, the coordinate acceleration described by Newton's equations is relative to any inertial coordinate system, and the equations don't work when used with a non-inertial coordinate system such as an accelerating or rotating one (Earth is both).ok; I think we might be going somewhere. When we measure the acceleration of the rock towards the earth, aren't we not measuring, at the same time, the acceleration of the earth towards the rock? How could you know the difference? — Gampa Dee
I suppose you can use it to compute the rate of change in distance between the two objects, but that rate isn't acceleration. — noAxioms
The symbol for that is 'a', not 'g'. 'a' is a vector variable acceleration. g is a scalar constant acceleration. Neither are a force. Force is measured in Newtons and uses the symbol F. Try to use standard symbols when discussing such things, as personal preferences only lead to confusion. — noAxioms
:(
— noAxioms
The acceleration of the moon when it is at radius r is exactly that in Newtonian physics. That does not mean it will hit the ground in 3 1/3 seconds like the 10 kg ball. As I said, a small fraction of a second is more likely. — noAxioms
I'm assuming that the dense super-mass is rigid, so yes, the acceleration applies to every point in the moon-ball. I am not assuming Earth is sufficiently rigid to not deform under the ungodly tidal stress the ball would apply to it. The sidewalk slab 60 meters below will be yanked up without waiting for Earth to catch up with it. — noAxioms
:)
— noAxioms
Acceleration is absolute, not relative, so adding them seems to result in a fairly meaningless value — noAxioms
I suppose you can use it to compute the rate of change in distance between the two objects, only in a 1-dimensional case, but that rate isn't acceleration. For instance, if an apple detaches from a tree and the distance between me and it decreases at 9.8 m/sec², that in no way suggests that I am accelerating at that rate, and in fact I'm accelerating (coordinate acceleration, not proper acceleration) away from it a little bit. — noAxioms
The Newtonian gravitational equation, identifying two masses, has only one acceleration , the one caused by the earth.
But there is an equation for each object, each dependent on only that mass, and not on the mass of the thing accelerating towards it. — noAxioms
ok; I think we might be going somewhere. When we measure the acceleration of the rock towards the earth, aren't we not measuring, at the same time, the acceleration of the earth towards the rock? How could you know the difference?
— Gampa Dee
As P-R points out, the coordinate acceleration described by Newton's equations is relative to any inertial coordinate system, and the equations don't work when used with a non-inertial coordinate system such as an accelerating or rotating one (Earth is both).
Mind you, plenty of books treat things like the Earth-moon system in isolation, which is to reference an accelerating coordinate system. It works to an extent, but adds confusion. For instance, few are aware that the moon always accelerates towards the sun since the sun exerts more force on it that does Earth. That means that when the moon is between the two (solar eclipse), the moon is accelerating directly away from Earth.
From the accelerating frame of Earth, the moon seems to maintain a fairly constant distance that isn't much a function of which direction the sun is. Yes the orbit of the moon (like any orbit) is eccentric to a degree, but that again isn't due to the sun. — noAxioms
Yes, that's the physics definition. Never confuse it with the common language definition which is the 'rate of increase in speed'.If we identify acceleration as simply a change in the rate of velocity, — Gampa Dee
It's not that it's simpler. Adding the equations only produces a useful result if there is no motion except along one axis. So for instance, under Newtonian mechanics, the ISS is continuously accelerating (coordinate acceleration) towards Earth at about 8.7 m/s² and yet its distance from Earth is roughly fixed, and its speed relative to Earth is also roughly fixed. This is because it is not a 1d case. The ISS has motion in a direction other than just the axis between it and Earth.I suppose you can use [the two added equations] to compute the rate of change in distance between the two objects, only in a 1-dimensional case, but that rate isn't acceleration.
— noAxioms
I do agree that the 1 dimensional is much simpler.
No. Under Newtonian mechanics, relative to any inertial coordinate system, it is the apple and only the apple that is accelerating.As for the acceleration of the apple at that rate relative to you, if we identify acceleration as simply a change in the rate of velocity, then, I would say that it’s only a relative situation to claim yourself as the one who is accelerating.
That's what the accelerometer does. Multiply what it says by your mass and you get your weight, which is why one is weightless on the ISS.and you feel the force to say so
Thank you PhilosophyRunner
For example see: https://orbital-mechanics.space/the-n-body-problem/two-body-inertial-motion.html
— PhilosophyRunner — Gampa Dee
So, now we have 2 accelerations; one is negative, the other positive. What do we do at this point?
If we have two cars having velocities of v1 and –v2(since it is going towards v1), relative to the road, what will the observers within the car measure the relative velocity between themselves?
It’s not going to be v1 – v2, but v1 + v2....I see the same problem for the two accelerations. — Gampa Dee
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