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<h3 id="understanding-physics">Understanding physics</h3>
<p>“Understanding Physics” is an introductory physics textbook for
college students, primarily those not intending to pursue science or
engineering careers but also suitable for premedical students. The book,
now in its revised edition, covers both classical and contemporary
non-classical physics topics like relativity theory and quantum
mechanics.</p>
<p>The textbook is divided into two parts: Part One focuses on ‘Matter
and Motion’ while Part Two deals with ‘Fields and Atoms’. The first part
starts with concepts of motion, covering Galileo’s contributions and
Newton’s laws of motion. It then delves into understanding motion
further, culminating in Newton’s unified theory encompassing gravity and
mechanics.</p>
<p>Part Two transitions to electricity, magnetism, and the nature of
atoms. The textbook integrates historical context with physics concepts,
aiming to provide students with an appreciation for how scientific
knowledge evolves over time. It emphasizes the humanistic side of
science, including biographical sketches of key scientists, to foster a
deeper understanding of both content and methodology in scientific
research.</p>
<p>The book is designed without prerequisites beyond high-school
algebra, geometry, and general science, making it accessible for a wide
range of students. It employs narrative explanations rather than
equations where possible, to help students grasp fundamental concepts
and build confidence with physical science techniques.</p>
<p>“Understanding Physics” encourages active learning through hands-on
activities, group discussions, and other interactive methods,
complemented by an Instructor Guide offering suggestions for adapting
the course content according to student backgrounds, educational
settings, time frames, and teaching preferences. The book is accompanied
by an online publisher site with links to related web resources for
instructors and students alike.</p>
<p>The text presents an overview of the historical development of
scientific thought, focusing on the ideas that led to our current
understanding of the physical universe. It begins by emphasizing the
purpose of the course, which is not only to learn about the major
concepts, theories, and laws of physics but also to understand how these
ideas emerged and their impact on society.</p>
<ol type="1">
<li><p>Living Ideas: The course aims to explore significant scientific
ideas, placing them in a historical context. This includes understanding
who proposed these ideas, when they were proposed, and why they were
influential at the time. It also involves appreciating how these ideas
have shaped our current understanding of the physical world.</p></li>
<li><p>Our Place in Time and Space: The text provides a sense of scale
about our position within the universe. We are reminded that our planet
is relatively small, orbiting an average star (the Sun) in an ordinary
galaxy (Milky Way), all located on the outskirts of the known universe.
Despite this, humans have made remarkable progress in understanding and
utilizing scientific principles within just a few centuries, leading to
advancements like airplanes, medical discoveries, and digital
technologies.</p></li>
<li><p>First Things First: The text discusses foundational assumptions
that underpin modern physics, tracing their roots back to ancient Greek
philosophers such as Plato, Aristotle, and Democritus. Plato believed in
mathematical relationships as the permanent first principles behind
natural phenomena, associating these with geometric solids (the Platonic
solids). In contrast, Democritus proposed an atomic hypothesis,
suggesting that all matter consists of tiny, indivisible particles
called atoms moving in empty space.</p></li>
<li><p>Aristotle’s Universe: Aristotle rejected the atomic theory and
instead advocated for relying on sense perceptions and qualitative
properties of bodies. His views dominated scientific thought for
centuries, emphasizing the importance of observational evidence over
abstract mathematical or atomic models.</p></li>
</ol>
<p>These ideas form a foundation upon which subsequent developments in
physics were built. Plato’s and Democritus’ speculations about atoms
laid groundwork for modern atomic theory, while Aristotle’s focus on
qualitative properties influenced later empirical approaches to
scientific investigation. The text encourages readers to appreciate the
intellectual journey that led us from ancient philosophical musings to
our contemporary scientific understanding of the universe.</p>
<p>In this section of the text, the authors discuss Galileo Galilei’s
contributions to understanding motion, particularly his approach to
studying simple moving objects.</p>
<p>Galileo (1564-1642) was an Italian physicist, mathematician, and
philosopher who played a significant role in the Scientific Revolution
of the 17th century. Born during the lifetimes of Michelangelo and
Shakespeare, Galileo initially studied medicine but later switched his
focus to physics after reading classical Greek philosophers like Euclid,
Plato, and Archimedes.</p>
<p>Galileo’s approach to studying motion involved using a smooth,
frictionless surface (like dry ice or a hockey puck on ice) to minimize
complicating factors. He employed photography (using a camera with an
open shutter) to capture the disk in motion and later used a strobe
light to create a series of snapshots, which allowed him to better
observe and measure its position at different times.</p>
<p>By analyzing these measurements, Galileo demonstrated that the moving
object traveled in a straight line, even without any noticeable slowing
down due to friction. This simple observation provided crucial insights
into the nature of motion:</p>
<ol type="1">
<li><p><strong>Position (d) and Time (t):</strong> Galileo used symbols
d for position readings and t for elapsed time from the start of the
experiment, both measured in centimeters (cm) and seconds (s),
respectively.</p></li>
<li><p><strong>Time Intervals (Δt) and Distance Traveled (Δd):</strong>
He introduced the concept of “time intervals” (Δt) between any two time
measurements and “distance traveled” (Δd) between any two position
readings, using the Greek letter delta (Δ) to denote change.</p></li>
<li><p><strong>Calculating Change:</strong> To find the value for Δd or
Δt, Galileo subtracted the initial measurement from the final one:</p>
<ul>
<li>Δd = dfinal - dinitial</li>
<li>Δt = tfinal - tinitial</li>
</ul>
<p>By obtaining these changes (differences), Galileo could analyze and
understand motion more accurately.</p></li>
</ol>
<p>Galileo’s meticulous experiments and mathematical approach to
studying motion were groundbreaking, as they formed the foundation for
modern physics and laid the groundwork for understanding complex motions
involving forces and interactions. This methodical investigation of
simple moving objects, which might seem intuitive today, was a
significant breakthrough in its time and demonstrated that mathematics
could indeed be used to uncover fundamental principles governing the
natural world—a concept championed by Plato centuries earlier.</p>
<p>The text describes how to calculate average speed using the formula
𝑣_av = Δd / Δt, where Δd is the change in position (distance traveled)
and Δt is the change in time.</p>
<p>In the context of a moving object like a disk or runner, you first
identify the beginning and ending values for position (d1 and d2) and
time (t1 and t2). The change in position (Δd) is then calculated as d2 -
d1, while the change in time (Δt) is t2 - t1.</p>
<p>For instance, if a disk’s position changed from 6.0 cm to 19.0 cm
over a time interval of 0.1 s, Δd would be 13.0 cm (19.0 cm - 6.0 cm)
and Δt would be 0.1 s. Using these values in the formula, the average
speed (𝑣_av) during that interval would be 13.0 cm / 0.1 s = 130
cm/s.</p>
<p>When considering different time intervals for the same motion, one
can calculate the average speed for each interval by applying the same
process. If the object maintains a constant (uniform) speed, all these
average speeds will be equal.</p>
<p>The concept of average speed is also connected to the idea of rate or
speed in general, which describes how fast something changes over time.
This could apply to various contexts, not just distance: for example,
the growth rate of a baby or plant. Scientists opted for defining speed
as the ratio of distance traveled (Δd) to time interval (Δt), rather
than the reverse (time per fixed distance).</p>
<p>When dealing with real-world scenarios like sports races or everyday
travel, it’s important to note that the actual motion might not be
uniform. For example, a runner may speed up and slow down during a race.
Graphical representations of such motions—distance vs time graphs—can
provide insight into these variations in speed. The steepness (or slope)
of the graph line at any point represents the average speed during that
interval.</p>
<p>The text also introduces the concept of velocity, which incorporates
both speed and direction, making it a vector quantity. Speed, on the
other hand, is a scalar, representing only magnitude without
direction.</p>
<p>Finally, changes in an object’s speed over time are referred to as
acceleration. To study such variations accurately, instantaneous
measurements of speed (velocity) at specific moments are required, which
can be facilitated by devices like speedometers.</p>
<p>The provided text describes a study of a car’s motion using
instantaneous speed data, and then applies the principles learned to
analyze free fall. Here’s a detailed summary and explanation:</p>
<ol type="1">
<li><p><strong>Car Motion Analysis</strong>: The table presents
instantaneous speeds of a car at different time intervals (t).
Initially, it seems puzzling as speeds fluctuate, but by adding columns
for change in speed (Δv), time interval (Δt), and their ratio (Δv/Δt),
patterns emerge.</p>
<ul>
<li><p>From t=0 to 5 seconds, the car accelerates uniformly. The speed
increases by 8 km/hr each second, indicating an average acceleration of
8 km/hr/s or 8 km/h in each second.</p></li>
<li><p>At t=6 seconds, the speed remains constant (50 km/hr), so Δv = 0
and Δt = 1 second, resulting in a ratio of 0 km/hr/s. This indicates the
car is cruising at a steady speed.</p></li>
<li><p>From t=7 to 10 seconds, the car decelerates uniformly. The speed
drops by 15 km/hr each second (Δv = -15 km/hr), indicating an average
acceleration of -15 km/hr/s or -15 km/h in each second. This is often
called “deceleration” and suggests the driver applied brakes, slowing
down at a constant rate.</p></li>
</ul></li>
<li><p><strong>Graphical Representation</strong>: The speed-time graph
provides a visual representation of this motion:</p>
<ul>
<li>The line starts at 10 km/hr on the vertical axis (y) and rises
steadily to 50 km/hr at t = 5 seconds, indicating positive
acceleration.</li>
<li>From t = 6 to 8 seconds, the line becomes horizontal, showing no
change in speed (constant velocity), meaning the car was cruising.</li>
<li>Finally, the line descends from t = 8 to 10 seconds, signifying
negative acceleration or deceleration as the car slows down.</li>
</ul></li>
<li><p><strong>Free Fall Analysis</strong>: The text then introduces
free fall as another example of accelerated motion. Galileo, a pioneer
in using experiments and mathematics to study physics, conducted studies
on falling objects despite Aristotle’s prevailing views that heavier
objects fall faster due to their greater “earth” element.</p>
<ul>
<li>Galileo proposed that, ignoring air resistance, all objects fall
with the same acceleration regardless of mass (a concept we now
understand as gravitational acceleration).</li>
<li>This insight was initially difficult to accept because creating a
vacuum (to eliminate air resistance) wasn’t possible in his time.
However, later experiments using vacuum pumps confirmed Galileo’s
findings that a feather and a gold coin fall at the same rate in a
near-vacuum environment.</li>
</ul></li>
</ol>
<p>The text emphasizes how understanding changing speeds involves
analyzing instantaneous speeds (or velocities), calculating changes
(Δv), and determining average accelerations (Δv/Δt). It also highlights
Galileo’s groundbreaking approach of using experiments, mathematics, and
neglecting minor factors like air resistance to reveal fundamental
principles of motion.</p>
<p>The provided text discusses Galileo Galilei’s groundbreaking work on
the motion of falling objects, which significantly contributed to the
development of physics. Here’s a detailed summary and explanation:</p>
<ol type="1">
<li><p><strong>Scientific Revolution</strong>: The Scientific Revolution
(approximately 1543-1700) was a period marked by significant
advancements in scientific knowledge, methodology, and understanding of
the natural world, largely challenging Aristotelian cosmology.</p></li>
<li><p><strong>Galileo Galilei</strong>: An Italian physicist,
mathematician, astronomer, and philosopher who played a major role in
the Scientific Revolution. He is known for his improvements to the
telescope and consequent astronomical observations supporting Copernican
heliocentrism.</p></li>
<li><p><strong>Approach to Motion</strong>: Galileo’s approach differed
from Aristotle’s. While Aristotle argued that heavier objects fall
faster than lighter ones (due to their desire to reach their natural
place), Galileo proposed that all objects, regardless of mass, fall at
the same rate in a vacuum, given no air resistance.</p></li>
<li><p><strong>Free Fall</strong>: Free fall refers to motion under the
influence of gravity alone, without any other forces acting upon it. The
term “free” signifies the absence of external influences. Determining if
free fall is uniformly accelerated is challenging due to practical
difficulties in measuring very short time intervals and high
speeds.</p></li>
<li><p><strong>Galileo’s Experiment on Falling Objects</strong>: Galileo
conducted experiments with rolling balls down inclined planes, a method
he used as an indirect test for free fall. He found that the ratio of
distance to time squared (d/t²) was constant for different distances and
times, implying uniform acceleration.</p></li>
<li><p><strong>Definition of Uniform Acceleration</strong>: Galileo
defined uniform acceleration as motion where equal increments of speed
occur over equal intervals of time. This led him to the equation: a = Δv
/ Δt.</p></li>
<li><p><strong>Galileo’s Law of Free Fall</strong>: Based on his
experiments and reasoning, Galileo concluded that all freely falling
objects, regardless of mass, fall with the same acceleration due to
gravity (neglecting air resistance). This is known as Galileo’s law or
rule of free fall: d = 1/2 * a * t².</p></li>
<li><p><strong>Consequences and Legacy</strong>: Although Galileo did
not explain why objects move the way they do, his work laid the
groundwork for mechanics by providing an alternative description to
Aristotle’s cosmology. It paved the way for Newton’s theory of
gravitation, which combined cause (forces) with Galileo’s kinematic
descriptions, forming the basis of classical physics.</p></li>
<li><p><strong>Key Concepts and Formulas</strong>:</p>
<ul>
<li>Speed: Rate of change in distance per unit time.</li>
<li>Velocity: Speed with a direction component.</li>
<li>Uniform Acceleration: Constant rate of change in velocity.</li>
<li>Galileo’s Law of Free Fall (d = 1/2 * a * t²): Applies to objects
falling from rest under constant acceleration due to gravity, neglecting
air resistance.</li>
</ul></li>
</ol>
<p>In essence, Galileo’s work on motion, particularly his law of free
fall, revolutionized our understanding of how objects move and laid
crucial foundations for the development of modern physics and
mechanics.</p>
<p>The geocentric view of the universe, which was widely accepted during
the time of Aristotle, posits that Earth is stationary at the center of
the cosmos, while celestial bodies like the Sun, Moon, stars, and
planets move around it. This perspective stems from the observation that
celestial objects appear to circle overhead in circular paths, leading
early observers to conclude they are centered on Earth.</p>
<p>In this model, the celestial sphere is imagined as a large dome
rotating once every 24 hours around Earth. The celestial equator aligns
with Earth’s equator, and celestial objects like stars are thought to
reside on concentric spheres orbiting above it. Planets, including the
Sun and Moon, move along their own spherical paths (ecliptic) at varying
speeds relative to the stars.</p>
<p>A key feature of this view is the understanding of seasons: The tilt
of Earth’s axis (23.5 degrees) causes the Sun to appear to drift
eastward through the celestial sphere over the course of a year, tracing
out its path called the solar ecliptic. This tilt results in different
angles at which sunlight hits Earth’s surface depending on location and
time of year, creating the changing seasons: spring (vernal equinox),
summer (summer solstice), autumn (autumnal equinox), and winter (winter
solstice).</p>
<p>Despite its widespread acceptance, this geocentric model lacked
quantitative precision; it couldn’t provide a mathematical explanation
for the observed movements of celestial bodies. It was only qualitative
in nature, relying on philosophical arguments rather than precise
calculations. These limitations would later be addressed by the
Copernican heliocentric theory proposed by Nicolaus Copernicus and
others during the Scientific Revolution.</p>
<p>The text discusses two major models of the universe’s structure,
geocentric (Ptolemaic) and heliocentric (Copernican), focusing on their
historical development, key features, and arguments for and against
them.</p>
<ol type="1">
<li><p>Geocentric Model (Ptolemaic): This ancient model posits that the
Earth is stationary at the center of the universe, with all celestial
bodies orbiting around it. It was developed by Claudius Ptolemy in the
2nd century AD to explain various astronomical observations. The model
incorporated complex mechanisms such as epicycles (smaller circles on
which larger circles rotate) and deferents (larger circular orbits) to
account for retrograde motion of planets, where they appear to move
westward in the sky relative to the stars. This was an attempt to
explain celestial motions using perfect circles and uniform
speeds.</p></li>
<li><p>Heliocentric Model (Copernican): Nicolaus Copernicus proposed
this alternative model in the 16th century, placing the Sun at the
center of the universe with Earth and other planets orbiting around it.
This was a radical departure from the geocentric view. The heliocentric
model offered a simpler explanation for retrograde motion: It is an
optical illusion caused by Earth passing the outer planets in their
orbits, giving the appearance of looping motion.</p></li>
</ol>
<p>Arguments for the Heliocentric Model: - Simplicity and Harmony:
Copernicus found beauty in the system’s simplicity. By eliminating
Ptolemy’s epicycles and deferents, the heliocentric model required fewer
mathematical constructs to explain celestial motions. - Symmetry: The
Sun’s central position provided a symmetrical focus for the solar
system, aligning with its role as the source of light, warmth, and life.
Copernicus believed this symmetry indicated the truth behind his model.
- Numerical Harmony: By assuming perfect circles and uniform speeds,
Copernicus discovered that the orbital periods and relative radii of
planets followed a harmonious progression (longer periods corresponding
to larger radii). This alignment was more apparent in his calculations
than in Ptolemy’s geocentric model.</p>
<p>Arguments against the Heliocentric Model: - Common Sense Objections:
The idea of a moving Earth seemed counterintuitive and contradicted
everyday observations. Questions arose about why objects on Earth didn’t
fly off or why there weren’t constant winds due to Earth’s rotation,
issues that would later be addressed with Newtonian mechanics. - Lack of
Definitive Evidence: Unlike the geocentric model, which had been refined
over centuries and could explain most astronomical phenomena, there was
no decisive empirical evidence favoring the heliocentric model
initially.</p>
<p>In essence, the choice between these models initially hinged more on
philosophical preferences (like simplicity and harmony) rather than
concrete observational data. The turning point came with later
advancements in physics, particularly Newton’s laws of motion and
universal gravitation, which provided compelling evidence supporting the
heliocentric view while also offering explanations for phenomena that
had previously seemed puzzling or contradictory to a stationary
Earth.</p>
<p>Johannes Kepler, influenced by Plato’s ideas and his belief that God
used mathematical principles to create the universe, aimed to discover
the “cosmic mystery” behind the solar system. He proposed that the six
visible planets follow precise geometric orbits determined by the five
regular solids (Platonic solids). Kepler began analyzing Tycho Brahe’s
meticulously collected astronomical data with the goal of finding the
perfect geometrical figure representing each planet’s orbit.</p>
<p>Initially, Kepler attempted to fit Mars’ orbit onto a circle –
adhering to Aristotelian physics that held force was necessary for
planets to move along their orbits rather than stay in them. However,
despite 70 attempts over five years, he could not achieve an accurate
enough fit using circles. Eventually, Kepler reluctantly abandoned the
centuries-old commitment to circular orbits and turned his attention to
other geometrical shapes.</p>
<p>After painstaking calculations, Kepler discovered a solution that
described Mars’ orbit more accurately than previous attempts – it was an
ellipse with the Sun at one of its foci (Figure 2.33). This result would
later become known as Kepler’s first law of planetary motion: The
planets orbit the sun on ellipses, with the sun at one focus and nothing
at the other.</p>
<p>Kepler’s discovery of Mars’ elliptical orbit challenged the widely
accepted belief that celestial bodies traveled in perfect circles. This
finding was crucial for understanding planetary motion because it
revealed a more precise representation of their orbits. Kepler’s success
in describing Mars’ path on an ellipse encouraged him to further analyze
Brahe’s data, which led him to two additional fundamental laws of
planetary motion:</p>
<ol type="1">
<li><p>The Law of Ellipses (First Law): The planets orbit the sun on
elliptical paths with the Sun at one focus and nothing at the other.
This law states that a planet moves faster when closer to the Sun,
slowing down as it reaches its farthest point from the Sun.</p></li>
<li><p>The Law of Areas (Second Law): An imaginary line drawn from the
sun to a moving planet sweeps out equal areas in equal amounts of time.
This law implies that planets move faster when closer to the Sun, and
slower when farther away, maintaining a constant rate of area swept by
their orbital path around the Sun.</p></li>
</ol>
<p>These three laws fundamentally changed our understanding of planetary
motion and marked a significant departure from Aristotelian and
Ptolemaic cosmology. Kepler’s work paved the way for Isaac Newton to
develop his theory of universal gravitation, unifying celestial
mechanics under a single, cohesive framework that explained not only
planetary motion but also terrestrial physics.</p>
<p>The text discusses significant advancements in understanding
planetary motion and the celestial sphere, primarily focusing on the
works of Johannes Kepler and Galileo Galilei.</p>
<p><strong>Kepler’s Laws of Planetary Motion:</strong></p>
<ol type="1">
<li><p><strong>First Law (Law of Ellipses):</strong> The orbit of every
planet is an ellipse with the Sun at one focus. This means that not all
planetary orbits are circular, as previously thought.</p></li>
<li><p><strong>Second Law (Law of Equal Areas):</strong> A line joining
a planet and the Sun sweeps out equal areas during equal intervals of
time. In simpler terms, a planet moves faster when it’s closer to the
Sun and slower when it’s farther away. This explains why the speed of a
planet changes throughout its orbit.</p></li>
<li><p><strong>Third Law (Harmonic Law):</strong> The square of the
orbital period of a planet is directly proportional to the cube of the
semi-major axis of its orbit. Mathematically, this can be expressed as
T² ∝ R³, where T is the orbital period and R is the average distance
from the Sun.</p></li>
</ol>
<p>These laws provided a more accurate description of planetary motion
than previous models, including those by Copernicus and Ptolemy, and
laid the groundwork for understanding the dynamics of celestial bodies
in our solar system.</p>
<p><strong>Galileo Galilei’s Observations:</strong></p>
<p>Galileo, a contemporary of Kepler, made several groundbreaking
observations using his telescope:</p>
<ol type="1">
<li><p><strong>Moon:</strong> He discovered that the Moon has a rough
and mountainous surface, contradicting the ancient belief in its perfect
sphericity.</p></li>
<li><p><strong>Stars:</strong> Galileo observed that the Milky Way
consists of countless individual stars, not a single luminous body as
previously thought.</p></li>
<li><p><strong>Sun:</strong> He found dark spots on the Sun’s surface,
indicating its non-perfect nature and further suggesting it could rotate
(a discovery later confirmed).</p></li>
<li><p><strong>Venus:</strong> Galileo observed Venus exhibiting phases
similar to those of the Moon, providing strong evidence for Copernicus’
heliocentric model where Venus orbits the Sun. This observation was
particularly damning to Ptolemy’s geocentric model, which couldn’t
explain these phases.</p></li>
<li><p><strong>Jupiter:</strong> Galileo discovered four of Jupiter’s
moons (now known as the Galilean moons), showing that not all celestial
bodies orbit around Earth but can have satellites of their own—providing
a model for our solar system.</p></li>
</ol>
<p>Galileo’s observations, along with Kepler’s laws, significantly
challenged the established geocentric view and contributed to the
eventual acceptance of the heliocentric model of our solar system.</p>
<p>3.1 Natural Motion:</p>
<p>Natural motion, according to Aristotle’s physics, refers to the
vertical movement of an object towards its “natural place.” For example,
a stone falls straight down through the air and further into water to
reach the earth below, while an air bubble rises upward through water
until it reaches the air above. This motion is considered natural
because it’s the direction in which objects tend to move on their own
without external help.</p>
<p>Galileo challenged this notion by demonstrating that all objects fall
at the same rate regardless of mass, contradicting Aristotle’s belief
that heavier objects fall faster than lighter ones. Galileo showed that,
in the absence of air resistance and friction, all objects fall with
uniform acceleration towards the Earth due to gravity.</p>
<p>3.2 Forces in Equilibrium:</p>
<p>In physics, a force is defined as a push or pull that can make things
move or hold them still. Forces can be balanced (equal but opposite) or
unbalanced (not equal). When forces are balanced, the object remains at
rest or moves with constant velocity; when they’re unbalanced, the
object accelerates in the direction of the net force acting upon it.</p>
<p>An example is two children pulling a toy in opposite directions – if
their forces are equal and opposite, the toy doesn’t move (forces are
balanced), but if one child pulls harder, there’s an unbalanced force
causing motion. This concept can be visualized using arrows representing
the magnitude and direction of each force; when these arrows are added
together, the resultant net force determines whether or not an object
accelerates.</p>
<p>3.3 More about Vectors:</p>
<p>Vectors are quantities that have both magnitude (size) and direction.
They’re used to represent forces in physics, among other things. In a
vector diagram, we use arrows of varying lengths and orientations to
signify different forces’ sizes and directions. To determine the net
force acting on an object, we add up these vectors graphically by
placing them head-to-tail (for addition) or tail-to-tail (for
subtraction). The resulting arrow represents the sum, or net force,
which indicates both its magnitude and direction.</p>
<p>Title: Newton’s Second Law of Motion, Vectors, Mass, and Force</p>
<ol type="1">
<li><strong>Newton’s Second Law of Motion:</strong>
<ul>
<li>This law describes the relationship between a net force (F_net)
acting on an object and its acceleration (a). It states that the
acceleration is directly proportional to the net force and inversely
proportional to the mass (m) of the object, with both quantities being
vector quantities. The mathematical representation of this law is F_net
= ma or a = F_net/m. This means that the greater the net force applied
to an object, the greater its acceleration will be; conversely, the
larger the mass of the object, the smaller its acceleration will be for
a given net force.</li>
</ul></li>
<li><strong>Vectors:</strong>
<ul>
<li>Vectors are quantities characterized by both magnitude (length) and
direction. They can represent physical quantities like forces,
velocities, or displacements. Arrows on paper are used to visualize
vector quantities; the length of an arrow represents the magnitude,
while its orientation indicates the direction.</li>
<li>Vectors can be added using a head-to-tail method (placing vectors
end-to-end) or parallelogram method (completing a parallelogram with the
vectors as adjacent sides and taking the diagonal as the
resultant).</li>
</ul></li>
<li><strong>Measuring Mass and Force:</strong>
<ul>
<li>Mass is an inherent property of an object, representing its
resistance to changes in motion (inertia). It’s measured using a
standard, such as the international kilogram cylinder kept at the
International Bureau of Weights and Measures near Paris.</li>
<li>Force is a push or pull that causes an object’s acceleration. In
everyday life, scales measure weight – the force exerted by gravity on
an object. The newton (N) is defined as the force required to accelerate
1 kg at a rate of 1 m/s² (1 N = 1 kg⋅m/s²).</li>
</ul></li>
<li><strong>Weight and Weightlessness:</strong>
<ul>
<li>Weight is the gravitational force acting on an object, which depends
on both mass and acceleration due to gravity. On Earth’s surface, weight
is approximately 9.8 N per kilogram of mass. Variations in weight occur
across Earth’s surface due to its non-spherical shape and non-uniform
composition.</li>
<li>Weightlessness or apparent weightlessness occurs when an astronaut
or object experiences no net force (e.g., in free fall within Earth’s
gravitational field, during flight on the International Space Station).
Despite feeling “weightless,” the astronaut and objects still possess
mass and are under the influence of gravity; their inertia prevents them
from accelerating without an opposing force.</li>
</ul></li>
<li><strong>Implications of Newton’s Laws:</strong>
<ul>
<li>Newton’s laws provide a fundamental understanding of motion, forces,
and interactions between objects, applicable universally across all
scales – from subatomic particles to galaxies, within the realm of
non-relativistic speeds. They form the basis for classical mechanics and
guide our comprehension of various physical phenomena.</li>
</ul></li>
</ol>
<p>The passage discusses the concept of projectile motion, its history,
and its relation to Galileo’s work.</p>
<ol type="1">
<li><p>Projectile Motion: This is the curved path of an object thrown or
projected into the air, where the horizontal motion is uniform (constant
speed and direction) while the vertical motion changes due to gravity,
resulting in a parabolic trajectory. The motion consists of two
independent components - uniform velocity in the horizontal direction
and changing velocity in the vertical direction due to gravity’s
acceleration.</p></li>
<li><p>Galileo’s Contributions: Galileo was the first to fully
understand projectile motion, deriving key principles from his
experiments with inclined planes. His insights were crucial in resolving
debates about the heliocentric model of the solar system, where critics
argued that a moving Earth would cause dropped objects to land
off-target.</p>
<ul>
<li>Falling Objects on Moving Earth: Galileo argued that a dropped stone
or any other object will continue its initial horizontal velocity while
falling due to gravity. Therefore, regardless of the Earth’s motion
(whether standing still or moving), the object will land at the base
because their horizontal velocities remain equal during the fall. This
demonstrates that the Earth can indeed move without affecting everyday
observations like dropped objects landing on target.</li>
</ul></li>
<li><p>Galilean Relativity: Galileo’s principle of relativity,
summarized in his thought experiment involving a moving ship, states
that the laws of physics are the same whether one is at rest or moving
with constant velocity within an isolated system (like a ship). This
principle forms the foundation for Einstein’s theory of relativity.</p>
<ul>
<li>Thought Experiment: Galileo imagined a person on a moving ship
observing flying animals, falling drops, and jumping. Regardless of
whether the ship is stationary or moving uniformly, all these phenomena
would appear the same—flies fly equally in all directions, drops fall
vertically, jumps cover equal distances in every direction, etc. This
demonstrates that one cannot determine their motion relative to the
Earth’s surface based on such observations alone.</li>
</ul></li>
</ol>
<p>In essence, the passage highlights how Galileo revolutionized our
understanding of motion, particularly projectile motion and the concept
of relativity, which fundamentally changed scientific thought about
Earth’s place in the universe.</p>
<ol type="1">
<li><p><strong>Natural Motion and Newton’s First Law:</strong></p>
<ul>
<li>Natural motion was the belief that heavier objects fall faster than
lighter ones, while violent (forced) motion was any change in velocity
caused by external forces. This seemed reasonable because it aligned
with everyday experiences.</li>
<li>The observation that two objects of different mass fall at the same
rate contradicts natural motion, as it shows that mass doesn’t affect
falling speed under the influence of gravity alone.</li>
</ul></li>
<li><p><strong>Galileo’s Discovery:</strong> Galileo discovered that a
ball rolling frictionlessly on a table maintains a constant speed,
regardless of its mass, until acted upon by an external force. This
observation challenged the concept of natural motion and laid the
groundwork for Newton’s First Law (Law of Inertia).</p></li>
<li><p><strong>Law of Inertia:</strong></p>
<ul>
<li>The law of inertia states that an object at rest tends to stay at
rest, and an object in motion tends to stay in motion with constant
velocity (uniform speed in a straight line) unless acted upon by an
unbalanced force (net force).</li>
</ul></li>
<li><p><strong>Aristotle vs Galileo/Newton:</strong></p>
<ul>
<li>Aristotle would have said that the rollerblader needs to push off
the ground continuously to maintain motion, as objects naturally come to
rest. Galileo and Newton would assert that once the rollerblader is in
motion with a constant velocity, no force is needed to keep them moving
unless acted upon by an external force (like friction or air
resistance).</li>
</ul></li>
<li><p><strong>Forces in Equilibrium:</strong></p>
<ul>
<li>Balanced forces are two or more forces whose vector sum equals zero.
This means their individual effects cancel each other out, resulting in
no acceleration and maintaining the object’s state of rest or uniform
motion.</li>
</ul></li>
</ol>
<p>These study guide questions encourage a deeper understanding of the
concepts presented, focusing on historical context, experimental
observations, and fundamental principles of classical mechanics as
described by Newton’s laws of motion.</p>
<p>Newton’s Principia, published in 1687, is a cornerstone of modern
physics. Written in Latin for an intellectual audience, it presents
Newton’s groundbreaking laws of motion and his universal law of
gravitation. Here’s a detailed explanation:</p>
<ol type="1">
<li><p>Definitions: The book starts with clear definitions of key
physical concepts, including mass (quantity of matter), momentum (mass
times velocity), inertia (resistance to change in motion), and force (a
push or pull upon an object). These definitions establish the framework
for understanding motion and interaction between objects.</p></li>
<li><p>Laws of Motion: Newton introduced three laws of motion, which are
still foundational to classical mechanics:</p>
<ol type="a">
<li><p>First Law (Law of Inertia): An object at rest will stay at rest,
and an object in motion will continue moving at constant velocity unless
acted upon by a net external force. This law effectively describes the
concept of inertia.</p></li>
<li><p>Second Law: The acceleration of an object is directly
proportional to the net force acting on it and inversely proportional to
its mass (F = ma). This equation quantifies how forces cause changes in
motion, making it possible to predict an object’s behavior under various
conditions.</p></li>
<li><p>Third Law: For every action, there is an equal and opposite
reaction. This principle explains that forces always occur in pairs,
with each force causing the other to be equal in magnitude but opposite
in direction.</p></li>
</ol></li>
<li><p>Principles of Addition for Forces and Velocities: These
principles outline how multiple forces combine to produce a net force
(vector addition) and how velocities combine when two objects move
independently (vector addition). This allows scientists to analyze
complex situations involving multiple forces or movements.</p></li>
<li><p>Rules of Reasoning in Philosophy: Newton included four rules,
often called his “method,” which guided scientific investigation:</p>
<ol type="a">
<li><p>Simplicity (or economy): Nature is simple; therefore, theories
should be as straightforward as possible without unnecessary
complexity.</p></li>
<li><p>Unity: The same cause should produce similar effects under
different circumstances. For instance, the force that causes an apple to
fall also governs celestial motion.</p></li>
<li><p>Generalization based on experimentation: Properties observed
within our reach (like mass) are assumed to apply universally until
proven otherwise.</p></li>
<li><p>Acceptance of hypotheses supported by experimental evidence:
Scientists should accept explanations grounded in empirical data, even
if alternative theories exist.</p></li>
</ol></li>
</ol>
<p>Newton’s Principia revolutionized our understanding of motion and
gravity. By synthesizing and formalizing the work of Galileo, Kepler,
and others, Newton laid the groundwork for classical mechanics. His laws
of motion provided a unified framework to analyze motion in various
contexts, from simple everyday situations to complex celestial
phenomena. Moreover, his law of universal gravitation enabled scientists
to understand and predict planetary motions accurately. The Principia’s
influence extended far beyond Newton’s lifetime, shaping the course of
scientific and technological progress for centuries to come.</p>
<p>The text discusses Isaac Newton’s groundbreaking work “Principia
Mathematica,” which presented his theory of universal gravitation. This
theory unified terrestrial and celestial physics under one grand system,
with gravity acting as a universal force governing all bodies in the
solar system.</p>
<ol type="1">
<li><p><strong>Newton’s Synthesis</strong>: Newton’s synthesis combined
the laws of motion (three laws) with Kepler’s three laws of planetary
motion. His first law states that an object remains at rest or moves
uniformly unless acted upon by a net force. The second law relates net
force to acceleration and mass (Fnet = ma). The third law asserts mutual
forces between interacting objects. Kepler’s laws describe planetary
orbits as ellipses, with areas swept out proportional to time, and the
squares of orbital periods proportional to the cubes of their average
distances from the Sun.</p></li>
<li><p><strong>The Inverse-Square Law</strong>: Newton demonstrated that
a central force, directed towards a single point (the Sun), would cause
planets to move in elliptical orbits as per Kepler’s laws. This central
force must follow an inverse-square law, where the strength of the force
decreases proportionally to the square of the distance from the
source.</p></li>
<li><p><strong>Law of Universal Gravitation</strong>: Newton concluded
that a single law of universal gravitation applies to all bodies in the
solar system. He showed that the centripetal acceleration required for
planetary motion, as per Kepler’s laws, matched the Earth’s
gravitational acceleration at its surface. Thus, the force holding the
Moon in orbit (gravitational attraction) is identical to that causing
objects to fall on Earth.</p></li>
<li><p><strong>Mechanism of Gravitational Force</strong>: Newton
proposed that the same gravitational force acting between a planet and
the Sun also operates between other celestial bodies, like moons and
their planets. He rejected ideas such as Descartes’ whirlpool-like fluid
or Kepler’s magnetic model to explain planetary motion, asserting that
gravity alone suffices.</p></li>
<li><p><strong>Newton’s Caution on Hypotheses</strong>: Newton was
cautious about proposing unverifiable hypotheses (like an invisible
“ether” for force transmission), as he recognized the importance of
testable scientific explanations. He famously stated, “Hypotheses non
fingo” (Latin for “I frame no hypotheses”), emphasizing that science
should focus on deducing laws from observable phenomena rather than
inventing untestable mechanisms.</p></li>
<li><p><strong>Quantifying Gravitational Force</strong>: Newton
determined the law’s magnitude by calculating that, for spherical
bodies, gravitational force can be considered as if all mass were
concentrated at their centers. This allowed him to define the distance
(R) between interacting objects’ centers in his universal gravitation
law: F = G(m1m2)/R^2, where G is the gravitational constant.</p></li>
</ol>
<p>Newton’s work fundamentally changed our understanding of physics by
unifying terrestrial and celestial mechanics under one universal law,
paving the way for modern physics and cosmology.</p>
<p>Newton’s Law of Universal Gravitation:</p>
<ol type="1">
<li><p>Formulation: Newton proposed that a single force law could
describe gravitational interactions between any two bodies, regardless
of their size or location in the universe. This law states that the
gravitational force (Fgrav) between two objects is directly proportional
to the product of their masses (m1 and m2) and inversely proportional to
the square of the distance (R) between their centers.</p></li>
<li><p>Mathematical Expression: Using the symbol G for the
proportionality constant, Newton’s law of universal gravitation can be
written as an equation:</p>
<p>Fgrav = G * (m1 * m2) / R^2</p>
<p>Here, G is the gravitational constant, m1 and m2 are the masses of
the two objects, and R is the distance between their centers.</p></li>
<li><p>Constant of Universal Gravitation (G): The value of G was
determined by Henry Cavendish through experiments using a torsion
balance to measure the tiny gravitational forces between lead spheres in
a laboratory setting. Today, we know that G is approximately 6.674 x
10^-11 N(m/kg)^2.</p></li>
<li><p>Implications:</p>
<ul>
<li>Small Forces: The value of G confirms that the gravitational force
between everyday objects is extremely small. For example, two 1 kg
masses separated by a distance of 1 meter experience a gravitational
attraction of only about 6.67 x 10^-11 N.</li>
<li>Acceleration due to Gravity (g): The near-constancy of g on Earth’s
surface can be explained by Newton’s law of universal gravitation. The
acceleration due to gravity is determined by the mass and radius of the
Earth, not the mass of individual objects:</li>
</ul>
<p>g = GM / R^2</p>
<p>Here, G is the gravitational constant, M is the mass of the Earth,
and R is its radius.</p></li>
<li><p>Further Successes: Newton demonstrated that his law could explain
various other phenomena, such as tidal forces and comet orbits.</p>
<ul>
<li>Tides: The tides on Earth result from the gravitational attraction
of the Moon and Sun on the waters of our planet. As the Earth rotates
beneath these celestial bodies, different parts of the oceans experience
varying levels of force, leading to high and low tides.</li>
<li>Comet Orbits: Newton also applied his law to explain the peculiar
motions of comets across the sky, which had previously been considered
enigmatic.</li>
</ul></li>
</ol>
<p>In summary, Newton’s Law of Universal Gravitation is a powerful and
elegant framework that unifies our understanding of gravitational
interactions between all objects in the universe. Its formulation relies
on a single force law involving mass and distance, and it has provided
explanations for various natural phenomena, such as tides and comet
orbits. The law’s successful predictions have firmly established its
validity across scientific disciplines.</p>
<p>Title: Summary and Explanation of Newton’s Laws of Motion and
Universal Gravitation</p>
<ol type="1">
<li><p><strong>Newton’s Laws of Motion</strong>: Isaac Newton formulated
three fundamental laws of motion that govern the behavior of objects
under various conditions. These laws are as follows:</p>
<ul>
<li><p><strong>First Law (Law of Inertia)</strong>: An object at rest
stays at rest, and an object in motion stays in motion with a constant
velocity unless acted upon by an external force. This law introduced the
concept of inertia, which states that an object resists changes to its
state of motion.</p></li>
<li><p><strong>Second Law (F=ma)</strong>: The acceleration of an object
is directly proportional to the net force acting on it and inversely
proportional to its mass. Mathematically expressed as F = ma, where F is
the net force, m is the mass, and a is the acceleration.</p></li>
<li><p><strong>Third Law (Action-Reaction Principle)</strong>: For every
action, there is an equal and opposite reaction. This means that any
force exerted onto another object will result in an equal force being
applied back on the original object, but in the opposite
direction.</p></li>
</ul></li>
<li><p><strong>Universal Gravitation</strong>: Newton’s law of universal
gravitation describes the attractive force between any two objects with
mass. The equation for this force is given by:</p>
<p>Fgrav = (Gm1m2)/R^2</p>
<p>where:</p>
<ul>
<li>Fgrav is the gravitational force between the masses,</li>
<li>G is the gravitational constant,</li>
<li>m1 and m2 are the two masses, and</li>
<li>R is the distance between the centers of these two masses.</li>
</ul></li>
<li><p><strong>Newton’s Synthesis</strong>: This refers to Newton’s
integration of celestial phenomena with terrestrial physics under a
single framework governed by universal laws. His synthesis included
applying his laws of motion and gravitation to explain the behavior of
both planets in the sky and objects on Earth, thus unifying our
understanding of nature.</p></li>
<li><p><strong>Action at a Distance</strong>: This term describes how
two objects interact with each other without any apparent physical
contact or medium between them. In Newton’s theory, gravity is an
example of action at a distance; masses attract one another across empty
space.</p></li>
<li><p><strong>Hypotheses in Science</strong>: Hypotheses are educated
guesses or proposed explanations for natural phenomena that can be
tested and potentially falsified through experimentation or observation.
Newton was known for his emphasis on developing hypotheses grounded in
mathematical equations and testable predictions, distinguishing him from
those who relied solely on ad-hoc explanations.</p></li>
<li><p><strong>Consequences of Newton’s Work</strong>: Newton’s laws of
motion and universal gravitation had profound implications for our
understanding of the physical world:</p>
<ul>
<li>They provided a unified explanation for phenomena ranging from
falling apples to orbiting planets, demonstrating the underlying unity
of natural laws.</li>
<li>These laws allowed for precise predictions about celestial bodies’
movements, leading to advancements in astronomy and navigation.</li>
<li>Newton’s synthesis laid the foundation for classical mechanics,
influencing subsequent scientific developments such as electromagnetism
and relativity theory.</li>
</ul></li>
<li><p><strong>Limitations of Newtonian Physics</strong>: While Newton’s
laws remain highly accurate for most everyday situations and many
astronomical phenomena, they do have limitations:</p>
<ul>
<li>At extremely high speeds or in the presence of immense gravitational
fields (like those near black holes), relativistic effects come into
play, necessitating Einstein’s theory of general relativity.</li>
<li>On the subatomic scale (e.g., atoms and particles), quantum
mechanics is required to describe accurately the behavior of matter and
energy.</li>
</ul></li>
<li><p><strong>Newton’s Impact on Society</strong>: Newton’s work not
only revolutionized physics but also influenced various aspects of
society:</p>
<ul>
<li>His laws facilitated technological advancements, from improved
clock-making to the development of space exploration technology.</li>
<li>The scientific method and empirical approach exemplified by Newton
continue to shape how we understand and interact with the world around
us.</li>
</ul></li>
</ol>
<p>The text discusses the concept of momentum conservation, its
historical development, and its application to collisions. Here’s a
detailed summary:</p>
<ol type="1">
<li><p><strong>Historical Background</strong>: The idea of conserving
mass was first introduced by philosophers like Descartes and Bacon
before Newton. However, it was Antoine Lavoisier who provided the
experimental evidence for mass conservation in chemical reactions during
the 18th century.</p></li>
<li><p><strong>Conservation of Mass</strong>: The law of conservation of
mass states that the total mass remains constant within a closed system
over time. This principle is fundamental to both physics and chemistry,
despite apparent changes in form or composition.</p></li>
<li><p><strong>Collisions and Momentum</strong>: The text introduces the
concept of momentum as the product of an object’s mass and velocity
(mv). It shows that while motion (velocity) isn’t conserved in all
collisions, the total momentum of a system is conserved under specific
conditions.</p></li>
<li><p><strong>Conservation of Momentum</strong>: This principle asserts
that the total momentum of a closed system remains constant before and
after a collision if no net external force acts on it. The law applies
universally across various scenarios, including different types of
forces, friction, varying collision angles, multiple objects, and
dimensions (one-dimensional or two/three-dimensional
collisions).</p></li>
<li><p><strong>Derivation from Newton’s Laws</strong>: The text explains
how the law of conservation of momentum can be derived from Newton’s
second and third laws. By expressing Newton’s second law in terms of
impulse (force × time), one can show that the net force applied to a
system over a certain duration equals the change in its total momentum,
leading directly to the principle of conservation of momentum.</p></li>
<li><p><strong>A Collision in Two Dimensions</strong>: This sidebar
provides an example of analyzing a two-dimensional collision using
vector notation and trigonometry, demonstrating how the law of
conservation of momentum applies even when objects collide at angles
instead of head-on.</p></li>
</ol>
<p>In essence, this section highlights the importance of understanding
and applying the principle of conservation of momentum in various
physical scenarios, emphasizing its universality and applicability
across different fields of science.</p>
<p>The text discusses several key concepts in physics, primarily
focusing on momentum conservation, isolated systems, elastic collisions,
and work.</p>
<ol type="1">
<li><p><strong>Momentum Conservation</strong>: This principle states
that the total momentum of a closed system remains constant unless acted
upon by an external force. The law is demonstrated through a
hypothetical collision between two disks on a frictionless surface.
Despite a 7% difference in measured total momentum before and after the
collision, it’s unclear whether this discrepancy is due to measurement
errors or a genuine violation of momentum conservation.</p></li>
<li><p><strong>Isolated Systems</strong>: These are systems that do not
exchange matter or energy with their surroundings. For momentum
conservation, such systems must also be free from net external forces.
Examples include colliding carts on frictionless tracks or hockey pucks
on ice. While these systems are nearly isolated, minute factors like air
resistance and friction can’t be entirely ignored, necessitating the
inclusion of larger systems for precise calculations.</p></li>
<li><p><strong>Elastic Collisions</strong>: These are collisions where
both momentum and kinetic energy are conserved. The Royal Society’s 1666
demonstration involving swinging balls illustrates this concept.
Christian Huygens later showed that, in addition to momentum
conservation, the total kinetic energy also remains constant in
perfectly elastic collisions. This is expressed mathematically as the
sum of half-mass times velocity squared (1/2mv^2) for the colliding
objects before and after collision being equal.</p></li>
<li><p><strong>Leibniz and Conservation Law</strong>: Gottfried Wilhelm
Leibniz extended conservation principles beyond collisions, proposing
that kinetic energy might be part of a more general, conserved quantity.
His hypothesis paved the way for understanding how motion’s increase in
height by a thrown stone is ‘stored’ rather than lost.</p></li>
<li><p><strong>Work</strong>: In physics, work is defined as the product
of force and displacement in the direction of the force. It measures the
amount of energy transferred when a force moves an object. Work is only
done if there’s displacement; no work occurs if motion is perpendicular
to the applied force or if an object doesn’t move (like pushing against
a stationary wall).</p></li>
<li><p><strong>Work and Kinetic Energy</strong>: Work represents energy
transformation from one form to another. When you exert a constant net
force on an object, causing it to accelerate over a distance d from rest
to speed v, the work done equals half-mass times velocity squared
(1/2mv^2), which is kinetic energy.</p></li>
</ol>
<p>The text concludes by noting that while momentum and kinetic energy
are both conserved in elastic collisions, these laws don’t always apply
universally—kinetic energy isn’t necessarily conserved in all
interactions within an isolated system. Most real-world collisions
aren’t perfectly elastic, resulting in varying degrees of kinetic energy
loss.</p>
<p>The text discusses several key concepts in physics, primarily
focusing on energy conservation and related topics. Here’s a
summary:</p>
<ol type="1">
<li><p><strong>Kinetic Energy (KE)</strong>: The energy of motion is
given by the equation KE = 1/2 mv^2, where m is mass and v is velocity.
This energy can be increased by applying work, which is defined as Force
multiplied by distance in the direction of force.</p></li>
<li><p><strong>Potential Energy (PE)</strong>: Potential energy is
stored energy associated with an object’s position or state. There are
different types of potential energy:</p>
<ul>
<li>Gravitational PE: The higher an object is lifted against gravity,
the greater its gravitational PE.</li>
<li>Elastic PE: This is associated with objects that can be stretched or
compressed, like a spring or rubber band.</li>
</ul></li>
<li><p><strong>Conservation of Energy</strong>: Energy cannot be created
or destroyed but can change from one form to another. For example,
lifting an object against gravity increases its gravitational potential
energy, which can later be converted into kinetic energy when the object
falls.</p></li>
<li><p><strong>Conservation of Mechanical Energy</strong>: In a closed
system (where no external forces are acting), the total mechanical
energy (sum of kinetic and potential energies) remains constant unless
work is done on the system. This principle applies to systems where only
conservative forces (like gravity or elastic forces) are at
play.</p></li>
<li><p><strong>Work</strong>: Work is defined as the product of force
and distance in the direction of the force. No work is done if the
object moves perpendicularly to the applied force, even though a force
might be exerted.</p></li>
<li><p><strong>Isolated Systems</strong>: A closed system is one where
no energy or matter enters or leaves. For conservation laws (mass and
momentum), an isolated system is crucial because it ensures that any
changes in the system are due only to internal processes, not external
influences.</p></li>
<li><p><strong>Collisions</strong>: In elastic collisions (where kinetic
energy is conserved), the total momentum before and after the collision
remains constant. The distribution of momentum between colliding objects
may change, leading to various outcomes like reflection or rebound,