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 14 » Lecture 14, Part 09: The Universal Law of Gravitation

Lecture 14, Part 09: The Universal Law of Gravitation

https://youtu.be/8P-YMHFjHL8

PHYS 1101: Lecture Fourteen, Part Nine

Okay. Newton was the one that worked this out. He arrived at what’s called the Universal Law of Gravitation. Here’s what’s behind the scene, or what’s at the heart of the force due to gravity. All objects that have mass exert gravitational force on each other. The mere fact that they have mass means that there is this interaction between them, this gravitational force.

The situation, though, is that it’s very, very weak. It depends on how much mass each of these two objects have. For typical day-to-day objects, like a television and a laptop, the masses are small. This gravitational force is small because these masses are small. So, you don’t notice this at all. The only time it’s significant is when one of these masses is really big.

Here’s the mathematical equation for the force due to gravity, this Universal Law of Gravitation. The force due to gravity will always have a magnitude that is a constant capital G. It has a value of 6.67 times 10 to the minus 11. Newtons, meters squared, per kilograms squared. It always, universally, has this value.

To that constant, I have to multiply a few factors. I have to look at the product of the two masses that are exerting this gravitational force, and it’s an action/reaction pair. Each of these two masses feels the same size force. They’re equal, opposite direction. I have to include both of these masses, and then I have to divide by the separation of the two. The closer the two masses are, the bigger the gravitational force will be.

Here’s a cartoon to help you visualize what these variables represent. I’ve got two objects, mass 1 and mass 2. Any two objects with any size mass exert a gravitational pull on each other. These two forces are equal and opposite, equal magnitude, opposite direction. m2 feels a pull to the center of m1. m1, as the object, feels a force on it that pulls it to the center of m2. The magnitude of these forces are calculated by the relationship shown right there. Got to multiply G times each mass times r squared. Okay.

Before we apply that to our problem, see if we’ve got enough to calculate the size of fG for the satellite. Let me show you a couple of things. First important point, this gravitational force is only significant if either one or both of these masses is huge, like a planet. That’s why we never include the gravitational force of the trunk of Sarah’s car on the box. There is a gravitational force attraction between the two. There’s also one on the box from Sarah and from all the other mass around her. All of those forces are incredibly small compared to the normal force of the trunk and the weight, the gravitational pull from the Earth.

Okay. So, here’s how we’ve been using this long range gravitational force. Let me point that out. I got a snapshot here of the planet Earth, large mass, and here I am. Looks like Angela is in Africa somewhere, West Africa. Mass of Angela. So, I’m thinking of me as being the object. How large is this force, gravitational force, from the planet Earth? Let’s apply this now general Universal Law of Gravitation to me, and let’s see how it compares to what we’ve been doing for the force due to gravity.

Well, let’s start with… Here’s Angela. What forces are on her? I know there’s the gravitational force from the Earth, and then the surface of the Earth is countering that. So, my normal force is equal and opposite, and it’s balancing me, which is why I’m in equilibrium. I’m just sitting there. We’re going to start this analysis with asking how big is this gravitational force, and let’s start with the Universal Law and see where it leads us.

Newton says that, in general, a gravitational force can be calculated as this constant capital G times the mass of one object, the Earth. Then, times the mass of the object that you care about, that this force is being exerted on. This is the mass of Angela. So, I’m thinking of Angela as the object.

Then, I have to divide by the radius. I’m sorry, the distance between my center and the Earth’s center, and I have to square that.

What would this radius be? Well, I’m, of course, dramatically exaggerated here. I’m actually so small, in reality, on the scale, you wouldn’t see me. This distance between my center and the center of the Earth, effectively, is just the radius of the Earth.

So, this r… I’m going to make it more clear. The separation between these two masses really is just the radius of the Earth. So, what are the numbers for the planet Earth to plug into this? Remember, G was 6.67 times 10 to the minus 11. Newtons, kilogram. Sorry. Newtons, meters squared, per kilogram squared.

I just went to the tables that are in the front of your book. They’re also on your equation sheet pages. To get some other constants here… The mass of the Earth is, of course, huge. 5.98 times 10 to the 24 kilograms. The radius of the Earth is 6.38 times 10 to the 6th meters. So then, we have the numbers for all of these terms, except I’m not going to tell you what my mass is.

Let’s just plug in these numbers and see what we get. If you do that, G, this value, I have to multiply by this mass. I have to divide by the radius of the Earth squared. You end up with 9.8 meters per second squared. That’s the equivalent to everything in yellow.

This is y. This is what, you’ll notice, we’ve been using for the weight. It’s the mass of the object on the surface of the earth, e.g. me, times G, m times G. This is what’s called the surface gravity and has a value of a little g.

We use this for every object, multiplying only by its unique mass, because every object on the surface of the Earth will have the same values for these other terms. If you’re on the surface Earth, this number is the same for every mass. Every mass is going to be much smaller than the Earth itself. So, the radius would basically be the radius of the Earth. That’s why we take this shortcut. We’ve been using… Force due to gravity is always m times little g.

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