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 10: Satellite Example Continued

Lecture 14, Part 10: Satellite Example Continued

https://youtu.be/B77rjaRLzTo

PHYS 1101: Lecture Fourteen, Part Ten

Okay. Back to our problem now. Once we’re away from the surface of the planet Earth, we’ve got to go back to that more general equation. We have to use that FG is actually this universal constant times the mass, in this problem, of Mars, times the mass of the satellite, I’ll call it Msat, divided by r squared. What’s r again? This has to be the separation or the distance between the centers of these two masses.

The distance between these two centers is going to be from the center of Mars, the radius of Mars plus the altitude. That’s r. That also happens to be the radius of our circular orbit.

Okay, so we’ve thought about a for this object, the satellite. It points to the center. We’ve thought now about the magnitude of the force that’s responsible for this a. We’re ready to do our list of knowns. Let’s start that with the radius, as I just said, has to be the radius of Mars plus the altitude. Right? That’s sum of these two pieces gets me the total radius.

As an aside, that’s common in a satellite problem that you’re told an altitude above the planet’s surface. And to get the proper r, you’ve got to add the radius of that planet. So I have a radius of 3397 times 10 to the 3rd meters, and I have to add the altitude, which is 488 times 10 to the 3rd meters. That combination turns out to be 3885 times 10 to the 3rd meters. Okay, there’s my r.

What other facts do I know? It looks like only the mass of Mars. That’s, like that planet Earth, is big. 6.4 times 10 to the 23rd kilograms, according to the problem.

What variable do I want? They asked for the orbital period of the satellite, okay? I’ve got to pick a variable. What variable or symbol were we using to represent that? That period, the time to go around once, I’m going to use a fancy T to represent. That’s the variable I’ve got to focus on. Now I’m ready to start with my second law equations and customize them. Work with them until I can arrive at a value for T.

Here’s my picture again. I’m going to add a coordinate system here. I only have vertical forces. I’m going to go ahead and call the y-axis positive downward, just so I can make all of my vectors positive. So I’m working with Ay is equal to the sum of the y forces divided by the mass of this object, the satellite. Okay, Ay I know is not 0. As usual I’m going to make the substitution that the magnitude is the speed squared divided by r. That’s positive. It’s downward. That’s equal to all of my y forces. I only have one.

I’m substituting that in, and then I still have the mass of the satellite in the denominator. Okay, well let’s keep peeling this away. Let me work on the right side for awhile. I don’t yet see T, the period, in my equation. I have v’s and things. V, for example, which I don’t have a value for. I’ve got to keep modifying this equation. I keep working it until I get to the thing I want. Well, I know I can substitute in here for the gravitational force.

I know that’s the universal constant times the mass of Mars, mass of the satellite divided by r squared. Let’s make that substitution just into the right side there. Notice I have to be careful, and I’m substituting that in for the numerator on the right side. In other words, this is all of this. I still have to divide by m of the satellite. But notice or recall that this denominator effectively is in this denominator. So this variable cancels with that variable.

Okay, now I end up with v squared over r is equal to G. Mass of Mars divided by r squared. And let’s see. I can simplify here a little bit. I see a lot of r’s that are the same variable. I multiply both sides by 1r just to simplify that a bit. It’s looking pretty good. I have a number for the mass of Mars. I know the value for G. I know the value for r. I don’t this, and I don’t know the period. But you know what? If I go back to those kinematic relationships for circular motion, I remember that the speed is related to the circumference of the circular path divided by the time to go around once, the period.

This is an excellent substitution to make because I know the radius and I now then have the variable I need to solve for. So let’s substitute this in. Okay, so I’m again going back to my main starting equation, Newton’s second law, and I’m massaging it some more. For v, I’m going to plug in 2 pi r over the period, but notice I have to square that to make that substitution correct. I’m substituting in for this, and on the right I have G, mass of Mars, divided by r.

Now I’m in great shape. I have the variable that I want, and I know the values of everything else. I just have to do some algebra. I’m going to multiply both sides by the period squared just to get the period out of the denominator. And now I’m going to move all of this over to the other side, which means multiplying by the inverse of that. And this then has been moved to the other side.

What do I have now? I’m going to switch the order here and write that I end up with T squared is equal to the product of all of this stuff. What do I have left? 2 pi r squared, but that’s another factor of r, so I’m going to write 2 pi squared times r cubed, then I have to divide that by G times the mass of Mars. All this stuff now will be equal to the period directly if I simply take the square root. So the period should be given by… It’s kind of a complicated equation, but it’s nonetheless, if we’ve not made any algebra mistakes, it should give us the right answer.

I have to take 4 times pi squared. I have to multiply by the radius of the circular orbit cubed. That’s 3,885 times 10 to the third meters cubed because I do have to work in SI units. I have to do that conversion of kilometers to meters. Then I have to divide by this universal constant G and divide by the mass of Mars, 6.4 times 10 to the 23rd kilograms.

Okay, here’s a word of caution. When you start doing satellite problems, you’re going to end up working with very large and very small numbers. To input these into your calculator, you need to use the ee button, or it might look slightly different to you. It might say times 10 to the x or something. Do not use the e to the x button. So e to the x, don’t use that. That’s not what you want when you enter these large and small numbers. You don’t want to type in all these zeroes.

Okay, so you just have to take your time, multiply it out carefully. Be sure, for example, that you cube this whole number, etc. When I plugged that into my calculator, I ended up with a period of 7,360 seconds and there’s 3,600 seconds in an hour. So when I convert that I get just a little over two hours. Takes a long time for the satellite to get around once. Okay, that brings us to the end of Lecture 15. I’m sorry. Okay, that brings us to the end of Lecture 14.

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