In this chapter, we will switch to using energy to solve physical problems instead of Newton’s laws and momentum. We will review the concepts of work, kinetic energy, and potential energy, and we will introduce conservative forces.
where Δr represents the displacement between two points, r1 and r2. Alternatively, the vector dot product can be solved following F⋅Δr=FΔrcosθ, where θ is the angle between the two vectors.
If F and dr are parallel (θ = 0), then the force is acting in the same direction as the displacement and the force does maximum positive work. If the force is perpendicular to the displacement (θ=2π), then the force does zero work. That is, the force is not responsible for the displacement and contributed no work to that displacement. If the force
is antiparallel to the displacement (θ=π), then the force does maximum negative work (the force acts to counter the motion as much as it can).
Work is a scalar quantity. It has magnitude but no direction. Since work is calculated by a vector dot product between force and displacement, only the component of the force that is along the displacement vector matters for the work calculation. Thus, solving problems with energy can make the math much easier if you select the right coordinate system (e.g., Cartesian versus polar coordinates) when defining your force and displacement.
Now, torque is a vector quantity given by τ=r×F . But work is a scalar quantity and the work done on a particle to move it from one position to another applies only to the component of the force in the direction of motion. If a force is perpendicular to the direction of motion, that force does no work. And if a force is parallel to the direction of motion, it does maximum work.
So if the path length in the direction of the force is ds=rdθ, then we can say that the work done by the force is:
dW=Fsds=⇒Fs is the component parallel to the path s
Integrating both sides will give you the same answer as the linear case: W(θ1→θ2)=ΔK. So the work-kinetic energy theorem applies for both translation and rotation movement. The kinetic energy equations are slightly different, however.
The work-kinetic energy theorem applies to all inertial frames (constant velocity) whether they are moving or stationary. So the change in work is the same within a stationary (S) frame or in a moving frame S′ (e.g., the centre-of-mass frame such as in Chapter 6).
Figure 8.1 show a particle starting from rest and moving under a constant force F in a laboratory. This particle will have a constant acceleration a due to this force. The work done to move this particle from point x1 to x2 in the laboratory frame (S) is simply WS=FΔx=ΔK because all the motion is in 1-D.
Figure 8.1:The motion of a particle in two different inertial frames. The lab frame S is stationary (red) and the second frame S′ is moving at a constant velocity u relative to the lab frame. A particle moves under a constant force F with an acceleration a in the lab frame. The work done to move that particle from points x1 to x2 in the lab frame is equal to the work done to move the particle in the moving inertial frame.
Now, consider what an observer in a moving frame, S′ would measure for the work done by that force. Here, S′ is moving at a constant velocity and is also an inertial frame. Because S′ is moving at a constant velocity, the observer in S′ would find the same acceleration as the observer in S (e.g., dtd(v+v0)=dtdv ). As a result, both the acceleration and force are unchanged in the moving frame. So
If the force is constant (given in the question), then the work in the moving frame is WS′=FΔxS′, where ΔxS′ is the displacement in the moving frame. Note that since the motion still takes place in 1-D we can drop vectors (if there are more dimensions, you just need to break up the movement by each coordinate).
For the displacement, ΔxS′, we need to know how far the particle travels in time Δt. For a system with constant acceleration (see Chapters 1 and 2), the displacement Δx=21at2+vit, where vi is the initial velocity of the system. While the particle is initially at rest in the stationary frame, from the perspective of the moving frame, the particle does not start stationary. The moving frame has a velocity of −u^ relative to the lab frame. That means that the moving frame would see the particle as having an initial speed of u^. So we can say that vi=u and the displacement is:
where Kf is the final kinetic energy and Ki in the initial kinetic energy.
So while the values of W and K as measured in the two frames (stationary and moving) may be different, the requirement that ΔW=ΔK holds in both frames. Again, this is only the case for inertial frames. In non-inertial frames (e.g., rotating or accelerating frames), the net force will include fictitious forces due to the non-inertial frame and the measured accelerations would be different (see Chapters 4 and 5).
Near the Earth’s surface, we often describe the gravitational force as Fg=mg, where g is a constant vector that points down vertically and has a constant magnitude.
Consider the case where the position of a heavy box of mass m changes y1 to y2 in vertical height and that both positions y2 and y1 are near the Earth’s surface. Work is done by gravity as the box moves by this displacement. The vector describing the displacement of
the box is Δy=(y2−y1)^ , whereas the gravitational force is Fg=−mg^ , which is constant. Taking the equation for work with a constant force, the work is:
Remember, this is the work done by gravity. So if a box is lifted upward (y2>y1), gravity acts against the displacement and W<0. If the box is lowered (y2<y1), gravity acts with (helps) the displacement and W>0. And if y2=y1 then W = 0 (no work is done by gravity).
where G is the gravitational constant of 6.67×10−11 N m2kg−2,M is the mass of the object producing the gravitational field, m is the mass of an object being accelerated in the gravitational field, and r is the distance between the centers of the two objects. Thus, the true form for the acceleration due to gravity is given by:
Note that the acceleration due to gravity always points toward the centre of the source of the gravitational field (points radially inward).
The force of gravity is a radial force with no azimuthal (angle) dependence. That means that any point that has the same radial distance (∣r∣) will have the same magnitude of gravity ∣g∣. We often describe gravity as a gravitational field, a sphere of influence where any object with a mass m will be subjected to a gravitational force. The magnitude of the gravitational field changes as a function of radial distance. For example, Figure 8.2 shows a cartoon of the Earth with two different vectors, r1 and r2. Their magnitudes of gravitational acceleration are:
Figure 8.2:A cartoon of the Earth with two different vectors, r1 and r2. Each vector also has a circle with corresponding radii of r1 and r2. Every point on the r1 circle will have the same gravitational field magnitude and similarly, every point on the r2 circle will have the same gravitational field magnitude.
Since r2>r1,∣g1∣>∣g2∣. But any point on a sphere with radius r1 around the Earth will have the same magnitude of acceleration due to gravity (e.g., the circles in Figure 8.2), and likewise for all the points on a sphere with radius r2. You can think of gravity as a sphere of influence, where any point that has the same distance from the centre of the Earth has the same magnitude of ∣g∣.
Note that the direction of gravity will be different depending on where you are, because the force always points inward toward the centre of the Earth (in its true form, gravity is not vertical, but radial). For very small distances and positions near the Earth’s surface, you can still assume a vertical direction and constant magnitude for a frame at that surface.
What is the work done by gravity using this general equation?
Well, consider going from r1 to r2 as shown in Figure 8.2.
Note that if r2>r1,W<0 as we would expect (e.g., you are doing work against gravity to move an object further away). You may recognize −rGMm as the gravitational potential energy. We will discuss potential energies in more detail in Section 8.6.
The gravitational force follows an inverse square ( r21) law. So at very large distances from the source of the gravitational field, the gravitational force goes to zero and the work necessary to move a particle also goes to zero (if there is no force, there is no work).
Consider an object that is on the surface of Earth and is launched so that it reaches a very large distance away (assume infinity). Due to Earth’s gravitational field, the object will feel a force that opposes its motion to leave. Gravity will be doing negative work and the kinetic energy of the object will decrease. What speed is needed for this object tojust reach infinity? Assume Earth’s atmosphere does not affect its motion.
To solve this problem, we will use the work-kinetic energy theorem (Equation (8.3)).
We just solved for the work to move an object between two radii in a gravitational field. We start with Earth’s surface (r1=RE) and we end very far away (r2=∞). That means that:
where RE is the radius of the Earth, ME is the mass of the Earth, and m is the mass of our object being moved. For kinetic energy, v2 = 0 because the object just reaches infinity. As such:
Equation 8.9 describes the escape velocity and for Earth, which is roughly 11 km s−1. The escape velocity is the minimum speed for rockets and satellites to leave Earth’s surface and travel great distances away.
Note that an object starting from rest at a great distance from the Earth will hit the Earth at a speed equivalent to the escape velocity. This converse situation is true because gravity is a conservative force, which we will discuss in the next section.
Conservative forces are a class of forces that depend only on position. These forces are also ones where energy is conserved. Common examples of conservative forces are gravity, the spring force, and the electric force. Conservative forces must meet the following criteria:
A conservative force does no total work on an object during a round trip.
The work done by a conservative force is independent of the path taken between two points.
If you add those two segments, you indeed get W = 0. This is true for any number of stops in the closed loop. As long as your starting and final positions are the same, you will get W = 0 for a conservative force.
The second requirement states that the total work done to move an object between two points only depends on the initial and final positions. How you get from point one to point two doesn’t matter. Figure 8.3 shows two paths that connect points r1 and r2. The work done by a conservative force will be the same no matter the path chosen.
Figure 8.3:Comparison of two paths between points r1 and r2. For a conservative force, the work done to go from r1 to r2 is the same for both paths, even though the paths are very different.
And of course, if you go from r1 to r2 and then from r2 back to r1, the total work is zero (first criterion) no matter which path you take in either case (e.g., Path I from r1 to r2 and then Path II from r2 back to r1).
Note that forces like friction are not conservative forces. First, friction doesn’t depend on position. Second, friction removes energy from a system. Third, the work done by friction in a closed loop is not zero. For example, consider a hockey puck moving in a circle of radius R on a rough horizontal surface that has friction. The friction force on the hockey puck is f=μKmgθ^ , and the puck moves so that it is always antiparallel (180∘) to the displacement. So Wf=−fΔd=−μKmg(2πR) for a closed loop. Thus, Wf= 0.
Note that ∇×F is a vector cross product called the curl of the vector F . The ∇ symbol is a vector differential operator sometimes called the del or nabla operator. In Cartesian coordinates, it has the form of:
where ∂ indicates the partial derivative. For partial derivatives, you ignore any other variable. For example, ∂x∂f(y) = 0 because x is not present in the function (you treat y as a constant for a partial derivative with respect to x). For ∇ in other coordinate systems, see Appendix A.5.
The curl of A (in Cartesian coordinates) is then given by the following matrix.
Potential energy is associated with conservative forces only. Consider a heavy box. If you lift that box upward, the work done by gravity is negative (gravity opposes the motion), but you increase the potential energy of the box because work is being done against gravity (W<0). If you lower that box or let go, then gravity is doing positive work on the box (W>0) and it will have a decrease in potential energy.
Let’s look at the gravitational potential energy between positions r1 and r2.
In general, the gravitational potential energy is measured between two points. It is a relative energy. You will want to set a convenient reference point. For example, we can set r1=∞, where there would be no contribution from the force, such that:
Once again, we want to set a convenient initial value like x1 = 0 (the equilibrium position), so that the potential energy of a spring is simply U=21kx2 relative to that point.
The work-kinetic energy theorem states that ΔW=ΔK. That is, the total work on a system by a force is equal to the change in the kinetic energy. The total work is the sum of work by conservative forces (ΔWcon) and the work by non-conservative forces (ΔWnc):
In the absence of non-conservative forces (e.g., if all forces acting on a system are conservative), then ΔWnc = 0 and ΔE = 0 such that we get Δ(K+U) = 0 or K+U = constant. This is the conservation of energy. When energy is conserved, ΔK=−ΔU or the change in kinetic energy directly corresponds to a change in potential energy. If kinetic energy increases, then potential energy decreases and vice versa.
Note for the above we are assuming that U is twice continuously differentiable. If U can be differentiated twice, then its partial derivatives are independent of the order and all terms cancel (e.g, ∂y∂z∂2U=∂z∂y∂2U).
For a potential, U, there can be points where −∇U=F = 0. Mathematically, these points are located where the derivative of the potential is zero and correspond to points of local maxima or local minima. Figure 8.5) shows a sketch of a potential with a local maximum and local minimum. These locations are also known as equilibrium points or saddle points.
Figure 8.5:Example potential with a local maximum and local minimum.
A local minimum is a stable equilibrium point. At the minimum, if a particle is slightly perturbed, it wouldn’t really go anywhere. The particle will feel a force that just brings it back to the minimum saddle point. Recall that the force is the negative derivative of the potential, so if you perturb the particle to a lower x value, the potential has a negative slope and the force will be positive back toward the saddle point. And if you perturb the particle to a higher x value, the potential has a positive slope and the force will be negative back toward the saddle point. So for a small shift in position, your particle more or less stays at the saddle point.
At the local maximum saddle point, however, a slight perturbation will have a huge effect on the particle’s motion. If you slightly perturb the particle to a lower x value, the potential has a positive slope so the force will be negative toward even more negative x values. (Similar case if you perturb the particle to a higher x value). So a slight perturbation at the maximum of a potential will cause the system to be unstable and move away from that position.