as the solutions to the problem. As a quick check we substitute each of these values back into
the original equation, equation 1-10:
24
3 + x =
x + 1
and find that each substitution leads to an identity. (An identity is an equation whose validity is
trivially obvious, such as 6 = 6.)
This chapter does not cover all the non-calculus mathematics you will encounter in this course.
I’ve kept the chapter short so that you will have time to read it all. If you master the concepts in
this chapter (or re-master them if you already mastered them in high school) you will be on your
way to mastering all the non-calculus mathematics you need for this course. Regarding reading
it all: By the time you complete your physics course, you are supposed to have read this book
from cover to cover. Reading physics material that is new to you is supposed to be slow going.
By the word reading in this context, we really mean reading with understanding. Reading a
physics text involves not only reading but taking the time to make sense of diagrams, taking the
time to make sense of mathematical developments, and taking the time to make sense of the
words themselves. It involves rereading. The method I use is to push my way through a chapter
once, all the way through at a novel-reading pace, picking up as much as I can on the way but not
allowing myself to slow down. Then, I really read it. On the second time through I pause and
ponder, study diagrams, and ponder over phrases, looking up words in the dictionary and
working through examples with pencil and paper as I go. I try not to go on to the next paragraph
until I really understand what is being said in the paragraph at hand. That first read, while of
little value all by itself, is of great benefit in answering the question, “Where is the author going
with this?”, while I am carrying out the second read.
9
Chapter 2 Conservation of Mechanical Energy I: Kinetic Energy & Gravitational Potential Energy
2 Conservation of Mechanical Energy I: Kinetic Energy &
Gravitational Potential Energy
Physics professors often assign conservation of energy problems that, in terms of
mathematical complexity, are very easy, to make sure that students can
demonstrate that they know what is going on and can reason through the problem
in a correct manner, without having to spend much time on the mathematics. A
good before-and-after-picture correctly depicting the configuration and state of
motion at each of two well-chosen instants in time is crucial in showing the
appropriate understanding. A presentation of the remainder of the conceptual-
plus-mathematical solution of the problem starting with a statement in equation
form that the energy in the before picture is equal to the energy in the after picture,
continuing through to an analytical solution and, if numerical values are provided,
only after the analytical solution has been arrived at, substituting values with units,
evaluating, and recording the result is almost as important as the picture. The
problem is that, at this stage of the course, students often think that it is the final
answer that matters rather than the communication of the reasoning that leads to
the answer. Furthermore, the chosen problems are often so easy that students can
arrive at the correct final answer without fully understanding or communicating the
reasoning that leads to it. Students are unpleasantly surprised to find that correct
final answers earn little to no credit in the absence of a good correct before-and-
after picture and a well-written remainder of the solution that starts from first
principles, is consistent with the before and after picture, and leads logically, with
no steps omitted, to the correct answer. Note that students who focus on correctly
communicating the entire solution, on their own, on every homework problem they
do, stand a much better chance of successfully doing so on a test than those that
“just try to get the right numerical answer” on homework problems.
Mechanical Energy
Energy is a transferable physical quantity that an object can be said to have. If one transfers
energy to a material particle that is initially at rest, the speed of that particle changes to a value
which is an indicator of how much energy was transferred. Energy has units of joules,
abbreviated J. Energy can’t be measured directly but when energy is transferred to or from an
object, some measurable characteristic (or characteristics) of that object changes (change) such
that, measured values of that characteristic or those characteristics (in combination with one or
more characteristics such as mass that do not change by any measurable amount) can be used to
determine how much energy was transferred. Energy is often categorized according to which
measurable characteristic changes when energy is transferred. In other words, we categorize
energy in accord with the way it reveals itself to us. For instance, when the measurable
characteristic is temperature, we call the energy thermal energy; when the measurable quantity is
speed, we call the energy kinetic energy. While it can be argued that there is only one form or
kind of energy, in the jargon of physics we call the energy that reveals itself one way one kind or
form of energy (such as thermal energy) and the energy that reveals itself another way another
kind or form of energy (such as kinetic energy). In physical processes it often occurs that the
10
Chapter 2 Conservation of Mechanical Energy I: Kinetic Energy & Gravitational Potential Energy
way in which energy is revealing itself changes. When that happens we say that energy is
transformed from one kind of energy to another.
Kinetic Energy is energy of motion. An object at rest has no motion; hence, it has no kinetic
energy. The kinetic energy K of a non-rotating rigid object in motion depends on the mass m and
speed v of the object as follows1:
2
1
K =
v
m
(2-1)
2
The mass m of an object is a measure of the object’s inertia, the object’s inherent tendency to
maintain a constant velocity. The inertia of an object is what makes it hard to get that object
moving. The words “mass” and “inertia” both mean the same thing. Physicists typically use the
word “inertia” when talking about the property in general conceptual terms, and the word “mass”
when they are assigning a value to it, or using it in an equation. Mass has units of kilograms,
abbreviated kg. The speed v has units of meters per second, abbreviated m/s. Check out the
units in equation 2-1:
2
1
K =
v
m
2
On the left we have the kinetic energy which has units of joules. On the right we have the
2
m
product of a mass and the square of a velocity. Thus the units on the right are kg
and we
2
s
2
m
can deduce that a joule is a kg
.
2
s
Potential Energy is energy that depends on the arrangement of matter. Here, we consider one
type of potential energy:
The Gravitational Potential Energy of an object2 near the surface of the earth is the energy
(relative to the gravitational potential energy that the object has when it is at the reference level
about to me mentioned) that the object has because it is "up high" above a reference level such as
the ground, the floor, or a table top. In characterizing the relative gravitational potential energy
of an object it is important to specify what you are using for a reference level. In using the
concept of near-earth gravitational potential energy to solve a physics problem, although you are
free to choose whatever you want to as a reference level, it is important to stick with one and the
same reference level throughout the problem. The relative gravitational potential energy Ug of
1 In classical physics we deal with speeds much smaller than the speed of light c = 3.00×108m/s. The classical
physics expression
1
2
K =
v
m
is an approximation (a fantastic approximation at speeds much smaller than the speed
2
of light—the smaller the better) to the relativistic expression
2
2
2
K = 1
( / 1 −v / c − )
1 mc which is valid for all speeds.
2 We call the potential energy discussed here the gravitational potential energy “of the object.” Actually, it is the
gravitational potential energy of the object-plus-earth system taken as a whole. It would be more accurate to ascribe
the potential energy to the gravitational field of the object and the gravitational field of the earth. In lifting an
object, it is as if you are stretching a weird invisible spring—weird in that it doesn’t pull harder the more you stretch it as an ordinary spring does—and the energy is being stored in that invisible spring. For energy accounting purposes
however, it is easier to ascribe the gravitational potential energy of an object near the surface of the earth, to the
object, and that is what we do in this book. This is similar to calling the gravitational force exerted on an object by the earth’s gravitational field the “weight of the object” as if it were a property of the object, rather than what it
really is, an external influence acting on the object.
11
Chapter 2 Conservation of Mechanical Energy I: Kinetic Energy & Gravitational Potential Energy
an object near the surface of the earth depends on the object's height y above the chosen
reference level, the object's mass m, and the magnitude g of the earth’s gravitational field, which
N
to a good approximation has the same value g = 9 80
.
everywhere near the surface of the
kg
earth, as follows:
g
U = mgy
(2-2)
N
The N in g = 80
.
9
stands for newtons, the unit of force. (Force is an ongoing push or pull.)
kg
Since it is an energy, the units of Ug are joules, and the units on the right side of equation 2-2,
with the height y being in meters, work out to be newtons times meters. Thus a joule must be a
2
m
newton meter, and indeed it is. Just above we showed that a joule is a kg
. If a joule is also
2
s
m
a newton meter then a newton must be a kg
.
2
s
A Special Case of the Conservation of Mechanical Energy
Energy is very useful for making predictions about physical processes because it is never created
or destroyed. To borrow expressions from economics, that means we can use simple
bookkeeping or accounting to make predictions about physical processes. For instance, suppose
we create, for purposes of making such a prediction, an imaginary boundary enclosing part of the
universe. Then any change in the total amount of energy inside the boundary will correspond
exactly to energy transfer through the boundary. If the total energy inside the boundary increases
by ∆E, then exactly that same amount of energy ∆E must have been transferred through the
boundary into the region enclosed by the boundary from outside that region. And if the total
energy inside the boundary decreases by ∆E, then exactly that amount of energy ∆E must have
been transferred through the boundary out of the region enclosed by the boundary from inside
that region. Oddly enough, in keeping book on the energy in such an enclosed part of the
universe, we rarely if ever know or care what the overall total amount of energy is. It is
sufficient to keep track of changes. What can make the accounting difficult is that there are so
many different ways in which energy can manifest itself (what we call the different “forms” of
energy), and there is no simple energy meter that tells us how much energy there is in our
enclosed region. Still, there are processes for which the energy accounting is relatively simple.
For instance, it is relatively simple when there is no (or negligible) transfer of energy into or out
of the part of the universe that is of interest to us, and when there are few forms of energy for
which the amount of energy changes.
The two kinds of energy discussed above (the kinetic energy of a rigid non-rotating object and
gravitational potential energy) are both examples of mechanical energy, to be contrasted with,
for example, thermal energy. Under certain conditions the total mechanical energy of a system
of objects does not change even though the configuration of the objects does. This represents a
special case of the more general principle of the conservation energy. The conditions under
which the total mechanical energy of a system doesn’t change are:
12
Chapter 2 Conservation of Mechanical Energy I: Kinetic Energy & Gravitational Potential Energy
(1) No energy is transferred to or from the surroundings.
(2) No energy is converted to or from other forms of energy (such as thermal energy).
Consider a couple of processes in which the total mechanical energy of a system does not remain
the same:
Case #1
A rock is dropped from shoulder height. It hits the ground and comes to a complete stop.
The "system of objects" in this case is just the rock. As the rock falls, the gravitational potential
energy is continually decreasing. As such, the kinetic energy of the rock must be continually
increasing in order for the total energy to be staying the same. On the collision with the ground,
some of the kinetic energy gained by the rock as it falls through space is transferred to the
ground and the rest is converted to thermal energy and the energy associated with sound.
Neither condition (no transfer and no transformation of energy) required for the total mechanical
energy of the system to remain the same is met; hence, it would be incorrect to write an equation
setting the initial mechanical energy of the rock (upon release) equal to the final mechanical
energy of the rock (after landing).
Can the idea of an unchanging total amount of mechanical energy be used in the case of a falling
object? The answer is yes. The difficulties associated with the previous process occurred upon
collision with the ground. You can use the idea of an unchanging total amount of mechanical
energy to say something about the rock if you end your consideration of the rock before it hits
the ground. For instance, given the height from which it is dropped, you can use the idea of an
unchanging total amount of mechanical energy to determine the speed of the rock at the last
instant before it strikes the ground. The "last instant before" it hits the ground corresponds to the
situation in which the rock has not yet touched the ground but will touch the ground in an
amount of time that is too small to measure and hence can be neglected. It is so close to the
ground that the distance between it and the ground is too small to measure and hence can be
neglected. It is so close to the ground that the additional speed that it would pick up in
continuing to fall to the ground is too small to be measured and hence can be neglected. The
total amount of mechanical energy does not change during this process. It would be correct to
write an equation setting the initial mechanical energy of the rock (upon release) equal to the
final mechanical energy of the rock (at the last instant before collision).
Case #2
A block, in contact with nothing but a sidewalk, slides across the sidewalk.
The total amount of mechanical energy does not remain the same because there is friction
between the block and the sidewalk. In any case involving friction, mechanical energy is
converted into thermal energy; hence, the total amount of mechanical energy after the sliding, is
not equal to the total amount of mechanical energy prior to the sliding.
13
Chapter 2 Conservation of Mechanical Energy I: Kinetic Energy & Gravitational Potential Energy
Applying the Principle of the Conservation of Energy for the Special Case
in which the Mechanical Energy of a System does not Change
In applying the principle of conservation of mechanical energy for the special case in which the
mechanical energy of a system does not change, you write an equation which sets the total
mechanical energy of an object or system objects at one instant in time equal to the total
mechanical energy at another instant in time. Success hangs on the appropriate choice of the two
instants. The principal applies to all pairs of instants of the time interval during which energy is
neither transferred into or out of the system nor transformed into non-mechanical forms. You
characterize the conditions at the first instant by means of a "Before Picture" and the conditions
at the second instant by means of an "After Picture.” In applying the principle of conservation of
mechanical energy for the special case in which the mechanical energy of a system does not
change, you write an equation which sets the total mechanical energy in the Before Picture equal
to the total mechanical energy in the After Picture. (In both cases, the “total” mechanical energy
in question is the amount the system has relative to the mechanical energy it would have if all
objects were at rest at the reference level.) To do so effectively, it is necessary to sketch a
Before Picture and a separate After Picture. After doing so, the first line in one's solution to a
problem involving an unchanging total of mechanical energy always reads
Energy Before = Energy After
(2-3)
We can write this first line more symbolically in several different manners:
E = E or E = E or E = E′
(2-4)
1
2
i
f
The first two versions use subscripts to distinguish between "before picture" and "after picture"
energies and are to be read "E-sub-one equals E-sub-two" and "E-sub-i equals E-sub-f." In the
latter case the symbols i and f stand for initial and final. In the final version, the prime symbol is
added to the E to distinguish "after picture" energy from "before picture" energy. The last
equation is to be read "E equals E-prime." (The prime symbol is sometimes used in mathematics
to distinguish one variable from another and it is sometimes used in mathematics to signify the
derivative with respect to x. It is never used it to signify the derivative in this book.) The
unprimed/prime notation is the notation that will be used in the following example:
14
Chapter 2 Conservation of Mechanical Energy I: Kinetic Energy & Gravitational Potential Energy
Example 2-1: A rock is dropped from a height of 1.6 meters. How fast is the rock
falling just before it hits the ground?
Solution: Choose the "before picture" to correspond to the instant at which the rock is
released, since the conditions at this instant are specified ("dropped" indicates that the rock was
released from rest—its speed is initially zero, the initial height of the rock is given). Choose the
"after picture" to correspond to the last instant before the rock makes contact with the ground
since the question pertains to a condition (speed) at this instant.
BEFORE
AFTER
Rock of
mass m
v = 0
y = 1.6m
Reference Level
v ′ = ?
E
=
E′
0 (since at rest)
0 (since at ground level)
K
+ U
=
K ′
+ U ′
Note that we have omitted
1
2
the subscript g (for
gy
m
=
v
m ′
“gravitational”) from both U
2
and U ′ . When you are
2
v ′
=
2
dealing with only one kind
gy
of potential energy, you
don’t need to use a
v ′
=
2gy
subscript to distinguish it
from other kinds.
v ′
=
2 9
( .80 m /s2 )1.6 m
m
v ′
= 5.6 s
kg ⋅ m
Note that the unit, 1 newton, abbreviated as 1 N, is 1
. Hence, the magnitude of the earth’s
2
s
N
m
near-surface gravitational field g = 9 80
.
can also be expressed as g = 9.80
as we have
kg
2
s
done in the example for purposes of working out the units.
15
Chapter 2 Conservation of Mechanical Energy I: Kinetic Energy & Gravitational Potential Energy
The solution presented in the example provides you with an example of what is required of
students in solving physics problems. In cases where student work is evaluated, it is the solution
which is evaluated, not just the final answer. In the following list, general requirements for
solutions are discussed, with reference to the solution of the example problem:
1. Sketch (the before and after pictures in the example).
Start each solution with a sketch or sketches appropriate to the problem at hand. Use the
sketch to define symbols and, as appropriate, to assign values to symbols. The sketch aids
you in solving the problem and is important in communicating your solution to the reader.
Note that each sketch depicts a configuration at a particular instant in time rather than a
process which extends over a time interval.
2. Write the "Concept Equation" ( E = E′ in the example).
3. Replace quantities in the "Concept Equation" with more specific representations of the same
quantities. Repeat as appropriate.
In the example given, the symbol E representing total mechanical energy in the before picture
is replaced with "what it is,” namely, the sum of the kinetic energy and the potential energy
K + U of the rock in the before picture. On the same line E ′ has been replaced with what it
is, namely, the sum of the kinetic energy and the potential energy K ′ + U ′ in the after picture.
Quantities that are obviously zero have slashes drawn through them and are omitted from
subsequent steps.
This step is repeated in the next line (
2
1
mgy = mv ′ ) in which the gravitational potential
2
energy in the before picture, U, has been replaced with what it is, namely m
gy, and on the
right, the kinetic energy in the after picture has been replaced with what it is, namely,
2
1 mv ′ .
2
The symbol m that appears in this s