Phys1101 - Introductory Physics 1
Phys1101 - Introductory Physics 1
College of Liberal Arts & Sciences

  • Introduction
  • Lecture 01
  • Lecture 02
    • Lecture 2, Part 1: Announcements
    • Lecture 2, Part 2: Units
    • Lecture 2, Part 3: Vector Introduction
    • Lecture 2, Part 4: Adding Vectors Graphically
    • Lecture 2, Part 5: Vector Addition Examples
    • Lecture 2, Part 6: Vector Component Introduction
    • Lecture 2, Part 7: Trigonometry
  • Lecture 03
    • Lecture 3, Part 1: Introduction
    • Lecture 3, Part 2: Where Were We
    • Lecture 3, Part 3: Vector Components in Detail
    • Lecture 3, Part 4: Scalar Component Description
    • Lecture 3, Part 5: Example of Finding Scalar Components
    • Lecture 3, Part 6: Scalar Component Addition
    • Lecture 3, Part 7: Scalar Addition Example
    • Lecture 3, Part 8: Motion Diagrams
  • Lecture 04
    • Lecture 4, Part 1: Introduction
    • Lecture 4, Part 2: Where Were We
    • Lecture 4, Part 3: Location Location Location …
    • Lecture 4, Part 4: How Fast ??? What Direction ???
    • Lecture 4, Part 5: Speeding Up? Slowing Down?
    • Lecture 4, Part 6: What Happens at a Turning Point?
  • Lecture 05
    • Lecture 5, Part 01: Introduction
    • Lecture 5, Part 02: Where Were We
    • Lecture 5, Part 03: Big Picture:  1D Kinematics
    • Lecture 5, Part 04: Kinematic Problem Solving Steps
    • Lecture 5, Part 05: Example 1
    • Lecture 5, Part 06: Example 2
    • Lecture 5, Part 07: Example 3
    • Lecture 5, Part 08: Free Fall
    • Lecture 5, Part 09: Free Fall and Kinematic Equations
    • Lecture 5, Part 10: Example 4
    • Lecture 5, Part 11: Example 5
  • Lecture 06
    • Lecture 6, Part 1: Introduction
    • Lecture 6, Part 2: Where Were We
    • Lecture 6, Part 3: Reading Quiz
    • Lecture 6, Part 4: Graph Basics
    • Lecture 6, Part 5: Practice Makes Perfect…
    • Lecture 6, Part 6: The Tangent Line
  • Lecture 07
    • Lecture 7, Part 1: Introduction
    • Lecture 7, Part 2: Where Were We
    • Lecture 7, Part 3: 2D Motion Diagrams
    • Lecture 7, Part 4: Trajectories
    • Lecture 7, Part 5: Why Work With Components…
    • Lecture 7, Part 6: Key Vectors in 2D
    • Lecture 7, Part 7: Watching 2D Motion
    • Lecture 7, Part 8: Dropping Versus Firing…
  • Lecture 08
    • Lecture 8, Part 1: Introduction
    • Lecture 8, Part 2: Where Were We
    • Lecture 8, Part 3: 2D Kinematic Problems:  The Big Picture
    • Lecture 8, Part 4: 2D Kinematic Problem Solving Steps
    • Lecture 8, Part 5: Example – Part a
    • Lecture 8, Part 6: Example – Part b
    • Lecture 8, Part 7: Your Turn
  • Lecture 09
    • Lecture 9, Part 1: Introduction
    • Lecture 9, Part 2: Where Were We
    • Lecture 9, Part 3: What is Special About Projectile Motion?
    • Lecture 9, Part 4: Example Part a
    • Lecture 9, Part 5: Example Part b
    • Lecture 9, Part 6: Example Part c
    • Lecture 9, Part 7: Your Turn
  • Lecture 10
    • Lecture 10, Part 1: Introduction
    • Lecture 10, Part 2: Where Were We
    • Lecture 10, Part 3: Dynamics:  Why Does Velocity Change?
    • Lecture 10, Part 4: Physical Interpretation of Newton’s Laws
    • Lecture 10, Part 5: What is a Force?
    • Lecture 10, Part 6: Mathematics of Newton’s 2nd Law
  • Lecture 11
    • Lecture 11, Part 1: Introduction
    • Lecture 11, Part 2: Where Were We
    • Lecture 11, Part 3: Free Body Diagram and Vector Nature of Newton’s 2nd Law
    • Lecture 11, Part 4: Common Forces:  Weight
    • Lecture 11, Part 5: Common Forces:  Tension
    • Lecture 11, Part 6: Common Forces:  Normal Force
    • Lecture 11, Part 7: Common Forces:  Friction
    • Lecture 11, Part 8: Problem Solving Steps
    • Lecture 11, Part 9: Example
  • Lecture 12
    • Lecture 12, Part 1: Introduction
    • Lecture 12, Part 2: Where Were We
    • Lecture 12, Part 3: Example 1
    • Lecture 12, Part 4: Example 2
    • Lecture 12, Part 5: Example 3
  • Lecture 13
    • Lecture 13, Part 1: Introduction and Where Were We?
    • Lecture 13, Part 2: Why/When Do We Need Newton’s Third Law?
    • Lecture 13, Part 3: Newton’s 3rd Law
    • Lecture 13, Part 4: Changes To Our Problem-Solving Steps
    • Lecture 13, Part 5: Example 1
    • Lecture 13, Part 6: Ropes and Pulleys
    • Lecture 13, Part 7: Example 2
    • Lecture 13, Part 8: Your Turn
  • Lecture 14
    • Lecture 14, Part 01: Introduction
    • Lecture 14, Part 02: Where Were We ?
    • Lecture 14, Part 03: Uniform Circular Motion:  What You Need To Know
    • Lecture 14, Part 04: Example 1
    • Lecture 14, Part 05: Example 2
    • Lecture 14, Part 06: Example 3
    • Lecture 14, Part 07: Optional Roller Coaster Example
    • Lecture 14, Part 08: Satellite Example
    • Lecture 14, Part 09: The Universal Law of Gravitation
    • Lecture 14, Part 10: Satellite Example Continued
  • Lecture 15
    • Lecture 15, Part 1: Introduction and Where Were We?
    • Lecture 15, Part 2: Energy Conservation:  The Basics
    • Lecture 15, Part 3: How Do You Calculate the Net Work?
    • Lecture 15, Part 4: New Problem Solving Steps
    • Lecture 15, Part 5: Example 1
    • Lecture 15, Part 6: Example 2
    • Lecture 15, Part 7: Last Example
    • Lecture 15, Part 8: Final Quiz Questions…
  • Lecture 16
    • Lecture 16, Part 1: Introduction and Where Were We?
    • Lecture 16, Part 2: Defining Our New “Energy Conservation Starting Equation”
    • Lecture 16, Part 3: Defining Mechanical Energy
    • Lecture 16, Part 4: New Problem Solving Steps
    • Lecture 16, Part 5: First Example
    • Lecture 16, Part 6: Second Example
    • Lecture 16, Part 7: Last Example
    • Lecture 16, Part 8: Redo Example From Last Lecture
  • Lecture 17
    • Lecture 17, Part 1: Lecture
  • Lecture 18
    • Lecture 18, Part 1: Introduction and Where Were We?
    • Lecture 18, Part 2: Momentum Change of a Single Object
    • Lecture 18, Part 3: Conservation of Momentum
  • Lecture 19
    • Lecture 19, Part 1: Introduction and Where Were We?
    • Lecture 19, Part 2: Let’s Start With Another Example
    • Lecture 19, Part 3: Elastic Collisions
    • Lecture 19, Part 4: Remaining Quiz Questions
  • Lecture 20
    • Lecture 20, Part 1: Introduction and Where Were We?
    • Lecture 20, Part 2: Rotational Kinematics:  The Basics
    • Lecture 20, Part 3: Examples
  • Lecture 21
    • Lecture 21, Part 1: Introduction and Where Were We?
    • Lecture 21, Part 2: Describing Motion ALONG the Circular Path…
    • Lecture 21, Part 3: Examples
    • Lecture 21, Part 4: Rolling Motion
  • Lecture 22
    • Lecture 22, Part 1: Introduction and Where Were We?
    • Lecture 22, Part 2: A Net Torque Causes Angular Acceleration
    • Lecture 22, Part 3: Torque Example
    • Lecture 22, Part 4: Equilibrium Example
    • Lecture 22, Part 5: Moment of Inertia
    • Lecture 22, Part 6: Non-Equilibrium Example
    • Lecture 22, Part 7: Another Example
  • Lecture 23
    • Lecture 23, Part 1: Introduction and Where Were We?
    • Lecture 23, Part 2: The Basics of Oscillatory Motion
    • Lecture 23, Part 3: Hooke’s Law
    • Lecture 23, Part 4: Kinematics of Simple Harmonic Motion
    • Lecture 23, Part 5: Example
  • Lecture 24
    • Lecture 24, Part 1: Lecture
  • Lecture 25
    • Lecture 25, Part 1: Introduction
    • Lecture 25, Part 2: The Basics of Wave Motion
    • Lecture 25, Part 3: Motion of a Particle on a Wave
    • Lecture 25, Part 4:  Motion of The Wave Crest
    • Lecture 25, Part 5: Examples
Lecture 15 » Lecture 15, Part 1: Introduction and Where Were We?

Lecture 15, Part 1: Introduction and Where Were We?

https://youtu.be/TxCBPP0aBeE

PHYS 1101: Lecture Fifteen, Part One

Welcome to lecture 15. We’re finished with Newton’s Second Law now as our primary tool for solving problems and we’re onto a whole new concept. This notion has to do with energy conservation. So again, we’re going to be focused on a single object, and we’re going to be asking, now, what’s the energy of that object and how does that energy change. That consideration is going to allow us to determine a lot of things about the motion.

At the heart of this new tool is, again, always a fundamental starting equation. For energy conservation, that equation is what we call the net work. This ends up being the net energy that’s added to this object. Whatever gets added or taken away from this object has to balance, or be equivalent to, the change in the kinetic energy of this object. Kinetic energy is nothing more than a measure of how much energy something has simply because it has mass and it has speed.

This is the very basic starting equation. In lecture 16, I’m going to introduce you to a slight variation of that equation, which is just a little easier to work with. It doesn’t look easier at first glance, but in the end, it is.

So, let’s get started with the lecture by going over a couple of quiz questions about previous material. The first one is a typical brain teaser, if you will, that people run into. This has to do with Newton’s Third Law. And the idea is that if you’re told that the force on the carriage, according to Newton’s law, is equal and opposite to the force on the horse, then how can the horse pull a carriage at all? Which of the choices, there, do you think best describes what has to be happening? Is this a contradiction of Newton’s Third Law? Plus 8 points if you get it correct.

Quiz question 2 goes back and has you looking a little more closely at uniform circular motion. You have four scenarios here below where the mass of the object changes between these scenarios. The radius, as shown, is different. All, in all cases, though, they’re going around the circle with the same speed. So, notice the v is the same for all 4 of these scenarios.

You need to rank, in order from largest to smallest, the tension in the line. So, this rope is attached to this ball that’s moving in this uniform circular motion. So you need to focus on the equation that relates the tension to the speed, the radius, and the mass.

We derived this in the previous lecture. Go back and have a look at that equation. Or, derive it again for yourself. Solve for what the tension has to be by starting with Newton’s Second Law. ay, for example, is equal to some of the forces in y over m. This is what you would use if you want to consider the snapshot of the ball, say, in this orientation at that instant. Set up this equation, derive what the tension has to be, and then see how it compares to these 4 scenarios.

Here’s a quick overview for you of last lecture, the key points. The new thing we learned about in lecture 14 was this idea of uniform circular motion. The uniform means my speed has to be constant for this object as it goes around in a circle. And circular motion, that’s straightforward.

There were some key relationships, or equations, that had to be true if something is undergoing this very special case of motion. One was that the acceleration is never 0. The acceleration vector always has to point to the center of the circle. And the size of it depends on the speed and the radius of that circle. In fact, it’s the speed squared divided by the radius.

We also then learned that the speed is not completely independent either. It depends on the circumference of the circle and the time that it takes to go around once. Speed is distance divided by time. So this is a new variable for us, this fancy capital t, and it has units of time. It’s going to represent the time to complete one cycle.

For uniform circular motion, our starting place is still Newton’s Second Law. This is just a special case of that. The key concepts to apply Newton’s Second Law, or the tricks to it, are that you have to pick a snapshot in time to apply the law because you have to have a clear picture of what the direction of a is at that instant and the direction of the net force. So you have to have a clear picture in your mind where it is when, when you want to solve Newton’s law. And that’s usually clearly spelled out for you in the problem. It will say at the bottom, at the right, etc.

And often, too, we notice that drawing the free body diagram to focus on the forces and see if it’s consistent with the a,  that that usually works best if you imagine a side view of this motion. So not a top view like you see, but you imagine looking from the side. That’s why I always drew the  kind of this oval trajectory, trying to get you to picture the side view and then what the forces would be.

In the context of uniform circular motion, we looked at satellites orbiting planets, the moon orbiting the Earth, for example. And for cases like that, these objects are undergoing uniform circular motion, a very simple example of that. The only force that’s on these satellites is going to be the gravitational pull caused by the large mass of the planet that this satellite is orbiting. The direction of that force is always to the center of the other mass, and the magnitude is given by this expression. In other words, the force due to gravity, which we’ve called w, has, of course, magnitude and direction.

On the magnitude side, we can continue to use the mass of the object times our 9.8 meters per second squared as long as we’re at the surface of the Earth. But once we get away from the surface of the Earth, say, a satellite, the moon, it’s far away or it’s a satellite, something that’s around or next to a different planet, we need to go to this more general equation for gravitational force.

This equation says that the size of the force due to gravity is actually equal to, very generally, a universal constant that has this value. I then need to multiply by 2 masses. The first mass is the mass of the agent. So if you’re focused on the satellite as the object, the agent causing this gravitational force is this big mass, the planet that the satellite is orbiting around. I need the mass of that planet. Then, I need to multiply by the mass of the object. And then, I need to divide that by r2, where r is the distance between the centers of these 2 objects.

In the case of a satellite orbiting, that distance will be the radius of the orbit, if you can see that from the drawing. This is the same distance r from the center of the two masses and then from the center of circle out to the path, the circular path.

Okay, the force due to the gravity, if you’re at the surface of the Earth, it just appears to us to be straight down and more generally said the force due to gravity always points to the center of the opposite mass. And so for a small object here on the surface of the planet, that’s always going to look like straight down to us.

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