Conservation of Energy and calculating potential energy?

In summary, the rock slides down a hillside and has a coefficient of kinetic friction of 0.25. The gravitational potential energy of the rock-earth system is just 9.2 x 10^5J before the rock slides.
  • #1
suspenc3
402
0
during a rockslide a 520kg rock slides from rest down a hillside that is 500m long and 300m high. The coeeficient of kinetic friction is 0.25. If the gravitational potential energy [tex]U[/tex] of the rock-earth system is zero at the bottom of the hill, what is the value of [tex]U[/tex] just beofre it slides?

I know this is wrong, but I tried:

[tex]U_g = mghcos \Theta[/tex]
[tex]U_g = 9.2 x 10^5J[/tex]

What do I do?
 
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  • #2
This is a good question. There is too much information given in the problem. Specifically, neither the length of the hillside nor the coefficient of friction are important. The gravitational potential energy is just U = mgh. The statement about U = 0 at the bottom of the hill just establishes that h = 0 at the bottom of the hill (since m and g are never 0).

The important part is: do you understand why the friction and length are unimportant in this question?

-Dale
 
Last edited:
  • #3
well friction wouldn't matter because it only has to do with thermal energy?

but there are more parts to the question, that is why a lot of the info seems useless.

Why doesn't the angle come into play when calculating potential energy?
 
  • #4
suspenc3 said:
well friction wouldn't matter because it only has to do with thermal energy?
but there are more parts to the question, that is why a lot of the info seems useless.
Why doesn't the angle come into play when calculating potential energy?

Potential energy is the energy a mass has at rest, potentially it could fall and turn that energy into kinetic energy. change in U is = change in K [conservation of energy] U doesn't even care about any angles because there is no angle involved with a rock sitting in one place.
 
  • #5
That and also gravity is a conservative field. Meaning that the path you take (the angle) is irrelevant, only the change in the potential is important.

Suspenc3, you hit the key idea about the friction. Basically, if it were frictionless than all of the PE at the top would go into KE at the bottom. With the friction some of the PE will go to heat and some will go to KE, but the initial PE is still the same.

-Dale
 
  • #6
Ya..Other information are irrelevent.
You can simply use [tex] mgh [/tex] to find the change in GPE, then add it to zero.. U shld get an answer.
 

1. What is the law of conservation of energy?

The law of conservation of energy states that energy can neither be created nor destroyed, but can only be transformed from one form to another. This means that the total amount of energy in a closed system remains constant over time.

2. How do you calculate potential energy?

Potential energy is calculated by multiplying the mass of an object by the acceleration due to gravity (9.8 m/s^2) and the height of the object above a reference point. The formula is PE = mgh, where m is mass, g is acceleration due to gravity, and h is height.

3. What are some examples of potential energy?

Some examples of potential energy include a book sitting on a shelf, a stretched spring, a roller coaster at the top of a hill, and a drawn bow and arrow.

4. How does conservation of energy apply to everyday life?

Conservation of energy applies to everyday life in many ways, such as when we use electricity, drive a car, or lift an object. In all of these situations, energy is transformed from one form to another, but the total amount remains constant. This concept also plays a role in renewable energy sources and energy efficiency efforts.

5. Can energy be lost or wasted?

Energy cannot be lost or wasted, but it can be converted into forms that are not useful to us. For example, when we burn fossil fuels, some of the energy is lost as heat and cannot be used to power a car or generate electricity. However, this energy is not truly lost, as it is still present in the universe in some form.

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