Hey, guys. So, for the next couple of chapters, we're going to start talking about thermodynamics. To start things off, we're going to talk about the most basic fundamental measurement within thermodynamics, which is called temperature. I want to give you an introduction, a brief introduction, on temperature and the different scales and systems that we use in physics. Let's go ahead and check this out here.
What is temperature? Well, we're going to develop a much more precise definition later on, but for now, a basic definition of temperature is it's a measure of how hot or cold something is. We can kind of rely on our everyday experience for this. If you grab an ice cube, that ice cube, relative to you, is probably very cold, whereas if you stick your hand in a pot of boiling water, that, unfortunately, is going to be very painful and feel very hot. These aren't really precise scientific definitions. So, a more useful one is that it's related to the average kinetic energy of the particles that make up an object. Remember that kinetic energy is related to how fast particles are moving. The idea here is that the molecules of water that are locked up inside of an ice cube are vibrating very slowly. They have low temperature, they don't have a lot of kinetic energy, and therefore the particles move relatively slowly. Versus the pot of boiling water, these things are moving around very quickly. So, there's a high temperature, the things feel very hot, so there's lots of kinetic energy and the particles are moving very fast.
We're going to have to do some measurements and calculations with temperature. So, we're actually going to need to know the 3 temperature scales or systems of units that we have in physics, and they're all actually related to arbitrary reference points that have to do with water. These are basically just values that we picked because we could easily reproduce them. These are things like the freezing point or boiling point of water. Basically, any scientist could freeze or boil water, and that's what we chose as our reference points. So, if you live in the United States, you're probably most familiar with the Fahrenheit scale. The Fahrenheit scale has two reference points: the freezing point of water is 32 degrees Fahrenheit and the boiling point is 212 degrees Fahrenheit exactly. Now, there are obviously much colder temperatures. The zero point is going to be somewhere around here, all the way down to the coldest temperature possible. We'll talk about that in just a second here.
Now, the other scale that we use is called the Celsius scale. Basically, if you live anywhere else in the world, you probably use this one. This is sort of like the metric system temperature scale, and the reference points that we use are a little bit more intuitive. Basically, what scientists did is we called the freezing points, the point where ice turns to water and vice versa, the 0 point. This is where 0 degrees Celsius is, and the boiling point, this is actually 100 degrees Celsius. So, what I want to point out is that these measurements mean the exact same thing. So, for instance, 0 degrees Celsius and 32 degrees Fahrenheit both represent the freezing point of water. We're just naming them; we're sort of calling them different numbers. It's kind of how 12 inches is equal to 1 foot. They both represent the same distance just on different number scales. It's the same exact idea here.
The last thing I want to talk about is the Kelvin scale. The Kelvin scale is the one that we're going to use most commonly. It's the one that we're going to plug into all of our equations. We're going to plug in all of our temperatures in Kelvin. Now, Kelvin is a little bit different because it's called an absolute temperature scale. The reason it's called this is that the Kelvin scale actually starts at absolute zero. What do I mean by that? Well, for the Celsius scale, we just chose 0 as the freezing point of water, and in the Fahrenheit scale, 0 was just sort of over here somewhere. It doesn't actually correspond to anything special. But for the Kelvin scale, the absolute zero, the zero point, the starting point is the coldest temperature possible. This is actually what we define as the beginning of the Kelvin scale. It's the coldest possible temperature that you could ever have.
The freezing point in Kelvin is going to be 273.15 Kelvin and the boiling point is going to be 373.15 Kelvin. What I want you to realize is that the difference between these two numbers is 100. The difference between these two numbers is also 100. So, the Kelvin and Celsius scales are actually sort of the same, it's just that one is shifted downwards like this. Whereas this scale over here, the Fahrenheit, these differences are actually 180. So, basically, you can kind of think about it that the scale is a little bit bigger. There are more numbers in between those freezing and boiling points.
We can actually go ahead and convert the coldest temperature possible to Celsius. It's going to be negative 273.15 degrees Celsius, and in Fahrenheit, it's going to be negative 459.67 degrees Fahrenheit. Again, all these measurements mean the same thing. These are all the coldest possible temperatures just in their respective scales. Hopefully, this makes sense. Let me know if you guys have any questions.