Finding the work done by Spiderman

  • Thread starter Thread starter member 731016
  • Start date Start date
  • Tags Tags
    Work Work done
Click For Summary
SUMMARY

The work done by Spiderman while moving is calculated using the formula W = mgr cos θ, where θ is the angle between the displacement vector and the force of gravity. The correct calculation reveals that the angle θ is 120 degrees, leading to a work output of -4.70 kJ. The discussion emphasizes the importance of accurately determining the angle between the displacement and the gravitational force to avoid errors in the work calculation. Participants provided guidance on using diagrams and the relationship between gravitational potential energy and work done by gravity.

PREREQUISITES
  • Understanding of work-energy principles in physics
  • Familiarity with vector mathematics, specifically dot products
  • Knowledge of gravitational potential energy concepts
  • Ability to interpret and create geometric diagrams for problem-solving
NEXT STEPS
  • Study the relationship between work and gravitational potential energy in physics
  • Learn how to accurately use vector diagrams to represent forces and displacements
  • Explore the implications of angles in work calculations, particularly in physics problems
  • Investigate the differences between dot product and cross product in vector mathematics
USEFUL FOR

Students and educators in physics, particularly those focusing on mechanics, as well as anyone interested in understanding work done by forces in real-world scenarios.

  • #91
Callumnc1 said:
Is my proof for θ=90+ϕ geometrically correct?
Yes. The concern with differentials is distracting and the drawings could be done more clearly -- in particular, labelling the angle you are calling ##\theta##. But I agree with the conclusion.

It might make it easier to evaluate the resulting integral if you would write ##\cos ( 90 + \phi )## as ##-\sin \phi##.

Personally, I would have looked at the formula for the projection of a vector normal to a [oriented] surface. That involves ##\sin \theta## where ##\theta## is the angle the vector makes with respect to the surface. In this case, the displacement vector makes an angle of ##- \phi## with respect to a horizontal surface. The projection thus involves ##\sin -\phi = - \sin \phi##.

You can get the dot product of two vectors by taking the projection of one in the direction of the other and multiplying the magnitude of the one by the [signed] magnitude of the projection of the other.

Actually, I would have been sloppy with the sign convention, ignored the orientation of the surface, looked at ##\sin \phi## and then reasoned that the displacement and gravity are pointing generally away from each other and inverted the sign of the resulting path integral.

Actually, I would have recognized a conservative field, reasoned that all path integrals between a particular pair of endpoints across a conservative field will yield the same result and either picked a trivial path or computed the potential difference.

But we can definitely get to work evaluating the integral.
 
  • Like
Likes   Reactions: member 731016
Physics news on Phys.org
  • #92
jbriggs444 said:
Yes. The concern with differentials is distracting and the drawings could be done more clearly -- in particular, labelling the angle you are calling ##\theta##. But I agree with the conclusion.

It might make it easier to evaluate the resulting integral if you would write ##\cos ( 90 + \phi )## as ##-\sin \phi##.

Personally, I would have looked at the formula for the projection of a vector normal to a [oriented] surface. That involves ##\sin \theta## where ##\theta## is the angle the vector makes with respect to the surface. In this case, the displacement vector makes an angle of ##- \phi## with respect to a horizontal surface. The projection thus involves ##\sin -\phi = - \sin \phi##.

You can get the dot product of two vectors by taking the projection of one in the direction of the other and multiplying the magnitude of the one by the [signed] magnitude of the projection of the other.

Actually, I would have been sloppy with the sign convention, ignored the orientation of the surface, looked at ##\sin \phi## and then reasoned that the displacement and gravity are pointing generally away from each other and inverted the sign of the resulting path integral.

Actually, I would have recognized a conservative field, reasoned that all path integrals between a particular pair of endpoints across a conservative field will yield the same result and either picked a trivial path or computed the potential difference.

But we can definitely get to work evaluating the integral.
Thank you so much for your reply @jbriggs444 !

Yeah true, there is a much easier method if I had recognized the conservative field! Sorry, what did you find distracting about my concern with differentials?

Was it the fact that first method I had to make an approximation and the second I did not (due to the choice of triangles)

I will post the integral

Many thanks!
 
  • #93
Here is the integration @jbriggs444 !

##W = -Fr\int_0^{60} \sin\phi d\phi##
##W = mgr\cos60= \frac {mgr}{2}## which is correct!

Many thanks!
 
  • Like
Likes   Reactions: jbriggs444 and Lnewqban
  • #94
Callumnc1 said:
Yeah true, there is a much easier method if I had recognized the conservative field! Sorry, what did you find distracting about my concern with differentials?
Well, a drawing of an isosceles triangle with two right angles is a bit distracting.
 
  • Like
Likes   Reactions: member 731016
  • #95
jbriggs444 said:
Well, a drawing of an isosceles triangle with two right angles is a bit distracting.
Oh true! Thank for letting me know @jbriggs444 !
 

Similar threads

  • · Replies 9 ·
Replies
9
Views
2K
Replies
11
Views
3K
  • · Replies 2 ·
Replies
2
Views
3K
  • · Replies 1 ·
Replies
1
Views
2K
  • · Replies 7 ·
Replies
7
Views
1K
Replies
4
Views
2K
Replies
5
Views
2K
  • · Replies 3 ·
Replies
3
Views
2K
  • · Replies 3 ·
Replies
3
Views
2K
Replies
12
Views
1K