danielakkerma
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Greetings!
I've recently embarked upon an attempt to compute the various aspects of (rather) simple Newtonian motion on the surface of a parabola, encompassing alternating conditions(such as friction, intial conditions, etc).
I start with a trivial parabolic representation of:
y(t)=ax(t)^2
Therefore, as illustrated in the first diagram appended(though roughly), the forces at play are detailed there.
Thence, I had acquired the following equations of motion:
<br /> Ncos(\alpha)+fsin(\alpha)-mg=m\ddot{y}<br />
<br /> Nsin(\alpha)-fcos(\alpha)=-m\ddot{x}<br />
\alpha = tg^{-1}(2ax)<br />
<br /> f = \mu N <br />
<br /> \frac{dy}{dx} = 2ax = tg(\alpha)<br />
(where mu is taken as the friction constant).
Of course, one must first differentiate y, which yields:
<br /> \frac{d^2y}{dt^2} = 2a(\dot{x}^2+x\ddot{x})<br />
Finally, assembling all these together grants us:
<br /> (2a(\dot{x}^2+x\ddot{x})+g)\frac{(sin(\alpha)-\mu cos(\alpha))}{(\mu sin(\alpha)+cos(\alpha))}=-\ddot{x}<br />
Analytically, this differential equation is of course insoluble; But, numerically, it can very well be evaluated. So, intuitively, I fed it to an excellent numerical processor("Mathematica"), expecting to see some physically sound results. But "Lo' and behold", to my dismay and horror, when the product of all these efforts had been but venial.
You'll find two charts demonstrating my perplexity; Both depict a manipulated and interchanged \mu.
But as you can see, for different(or any!, excepting 0) values of that constant(mu) the amplitude of the oscillations(which should be present) does not change! one would've thought, that under the constraints of energy loss, there would be no gains to accommodate such a behavior, and I am left, as a result really puzzled.
In any case, I leave it to you, with gratitude for your time and attention,
What have I done wrong?
Thankful,
Beholden,
Daniel Akkerman
I've recently embarked upon an attempt to compute the various aspects of (rather) simple Newtonian motion on the surface of a parabola, encompassing alternating conditions(such as friction, intial conditions, etc).
I start with a trivial parabolic representation of:
y(t)=ax(t)^2
Therefore, as illustrated in the first diagram appended(though roughly), the forces at play are detailed there.
Thence, I had acquired the following equations of motion:
<br /> Ncos(\alpha)+fsin(\alpha)-mg=m\ddot{y}<br />
<br /> Nsin(\alpha)-fcos(\alpha)=-m\ddot{x}<br />
\alpha = tg^{-1}(2ax)<br />
<br /> f = \mu N <br />
<br /> \frac{dy}{dx} = 2ax = tg(\alpha)<br />
(where mu is taken as the friction constant).
Of course, one must first differentiate y, which yields:
<br /> \frac{d^2y}{dt^2} = 2a(\dot{x}^2+x\ddot{x})<br />
Finally, assembling all these together grants us:
<br /> (2a(\dot{x}^2+x\ddot{x})+g)\frac{(sin(\alpha)-\mu cos(\alpha))}{(\mu sin(\alpha)+cos(\alpha))}=-\ddot{x}<br />
Analytically, this differential equation is of course insoluble; But, numerically, it can very well be evaluated. So, intuitively, I fed it to an excellent numerical processor("Mathematica"), expecting to see some physically sound results. But "Lo' and behold", to my dismay and horror, when the product of all these efforts had been but venial.
You'll find two charts demonstrating my perplexity; Both depict a manipulated and interchanged \mu.
But as you can see, for different(or any!, excepting 0) values of that constant(mu) the amplitude of the oscillations(which should be present) does not change! one would've thought, that under the constraints of energy loss, there would be no gains to accommodate such a behavior, and I am left, as a result really puzzled.
In any case, I leave it to you, with gratitude for your time and attention,
What have I done wrong?
Thankful,
Beholden,
Daniel Akkerman
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