Hello! Welcome back to our journey into thermodynamics.
In our last lesson, we tackled the visible, mechanical forms of energy: kinetic energy (the energy of motion) and potential energy (the stored energy of position). We saw how doing work on a system—like a gas in a cylinder—transfers energy to it. You'll recall the crucial formula for the work done by a gas: . This equation has a big 'P' in it for pressure, which we've so far just taken for granted.
Today, we're going to put that 'P' under the microscope. What is pressure, really? Where does it come from? How do we measure it in the real world? This is a fundamental step in being able to describe the state of any substance we want to study.
Our learning outcome for this lesson is to explain pressure from a molecular perspective and solve problems involving absolute, gauge, and vacuum pressures.
Here’s how we'll break it down:
- Pressure from the Ground Up: We'll visualize what pressure is at the level of individual molecules.
- The Different "Flavors" of Pressure: We'll untangle the terms you hear in the real world—absolute, gauge, and vacuum—and see how they all relate.
- Putting it to Practice: We'll work through some practical problems, like figuring out the true pressure in your car tires.
Let's dive in and get a feel for what pressure is all about.
What is Pressure? A Molecular Story
At its simplest, pressure is defined as force applied over an area.
Where is pressure, is force, and is area.
This explains why a sharp knife cuts better than a dull one. The force from your hand is the same, but the tiny area of the sharp edge concentrates that force into a very high pressure, allowing it to slice through a tomato. A dull knife spreads the same force over a larger area, resulting in lower pressure that just squishes the tomato.
But in thermodynamics, we're usually dealing with fluids—liquids and gases. Where does the force come from in a tank of air or a pot of water? It comes from the frantic, non-stop motion of trillions upon trillions of molecules.
To build our intuition, let's watch a couple of short video clips.
Absolute Pressure, Gauge Pressure, Atmospheric Pressure & Vacuum Pressure: Definition & Calculation
First, this video from MechStudies will give us a simple analogy for pressure and then show what's happening inside a container of gas.
Watch from 0:22 to 2:56. The first part uses the pin analogy to separate the ideas of force and pressure. The second part visualizes how gas molecules colliding with container walls create what we measure as gas pressure.
As you saw, a gas isn't a static, calm substance. It's a chaotic collection of particles, each with its own velocity, zipping around and bouncing off everything they hit.

According to the Kinetic Molecular Theory of Gases, this chaotic motion is the very source of pressure. Here's the story:
- Constant Motion: Gas particles are in continuous, random, straight-line motion.
- Collisions: They constantly collide with each other and, crucially, with the walls of their container.
- Force Transfer: Each time a particle hits a wall and bounces off, it exerts a tiny push, or force, on that wall.
- Collective Effect: A single collision is insignificant. But billions of particles hitting the wall every second add up to a steady, measurable force.
- Pressure: This total, averaged-out force, spread over the area of the wall, is what we perceive and measure as pressure.
So, when you feel the pressure in a bicycle tire, you're literally feeling the collective impact of countless air molecules hammering against the inner surface of the tire.
To reinforce this, let's hear another excellent explanation.
Kinetic Molecular Theory and its Postulates
Professor Dave Explains gives a very clear and concise breakdown of the key ideas (postulates) of the Kinetic Molecular Theory. This clip focuses on how molecular motion directly causes pressure.
Please watch from 0:56 to 3:30. Pay close attention to how he connects the number of particles and their speed to the resulting pressure.
From these ideas, physicists derived a powerful equation that connects the microscopic world of molecules to the macroscopic world we measure.
CHAPTER 8.1: KINETIC THEORY OF GASES
This document, 'Kinetic Theory of Gases,' formalizes what we just saw. You don't need to follow every step of the derivation, but seeing the final result is powerful.
Skim through the section 'D. Pressure, Temperature, and RMS Speed of an Ideal Gas,' specifically focusing on the part titled 'Pressure Exerted by a Gas.' Notice the conclusion they reach in Equation (1): PV = (1/3)Nmv².
The equation is profound. It tells us that the pressure () in a container of volume () is directly related to the number of molecules (), their mass (), and how fast they're moving on average (). More molecules or faster molecules mean more collisions, and thus higher pressure.
The Sea of Air Around Us: Atmospheric Pressure
This idea of molecular collisions doesn't just apply to gases in containers. We are living at the bottom of a giant "ocean" of air called the atmosphere. The air molecules that make up this ocean—nitrogen, oxygen, etc.—are all in motion and have weight. The pressure exerted by the weight of all the air above you is called atmospheric pressure, .
Think of it as the pressure from the column of air stretching from your head all the way to the edge of space. This is why atmospheric pressure is highest at sea level (the bottom of the air ocean) and gets lower as you go up a mountain (less air above you).
At sea level, the standard atmospheric pressure is defined as:
- 101,325 Pascals (Pa), or 101.325 kilopascals (kPa)
- 14.696 pounds per square inch (psi)
- 1 atmosphere (atm)
This is our everyday reference point.
Absolute, Gauge, and Vacuum Pressure: What's the Reference?
This is where things can get confusing, but it's simple once you grasp the central idea: pressure is always measured relative to a reference point. There are two main reference points we use.
- Absolute Zero Pressure: This is a perfect vacuum. A space with absolutely no molecules and therefore zero pressure. This is the true, ultimate zero.
- Local Atmospheric Pressure: The pressure of the air currently around you. This is a convenient reference, but it changes with weather and altitude.
This leads to our three key definitions:
- Absolute Pressure (): Measured relative to a perfect vacuum. This is the true total pressure. It can never be a negative number.
- Gauge Pressure (): Measured relative to the local atmospheric pressure. This is what most pressure gauges, like a tire gauge, read. It measures how much above (or below) atmospheric pressure a system is.
- Vacuum Pressure (): A pressure that is below atmospheric pressure. It's essentially a negative gauge pressure. When you suck on a straw, you are creating a vacuum pressure inside the straw.
The relationship between them is simple arithmetic:
For pressures above atmospheric:
Your tire's true pressure is the gauge reading PLUS the atmospheric pressure pushing on the outside of the tire.
For pressures below atmospheric:
The true pressure in a vacuum chamber is the atmospheric pressure MINUS how much vacuum you've pulled.
Let's watch a final video that puts all of this together with clear graphics and examples.
Absolute Pressure, Gauge Pressure, Atmospheric Pressure & Vacuum Pressure: Definition & Calculation
This video from MechStudies is the perfect summary. It visually explains the differences between gauge, absolute, and vacuum pressure and walks through the formulas we just discussed.
Watch from 5:38 until the end (11:54). He covers gauge pressure (using a tire gauge example), absolute pressure, the key formulas, and vacuum pressure. Pay close attention to the animated graphs that show how the pressures relate.
Quick Recap
Alright, let's pause. We've defined pressure from a molecular viewpoint and distinguished between the three ways we measure it.
- Pressure = Force from molecular collisions per unit area.
- Absolute Pressure = True pressure, measured from a perfect vacuum (zero molecules).
- Gauge Pressure = Pressure relative to the atmosphere. What most gauges read.
- Vacuum Pressure = Pressure below atmosphere.
The key formula to remember is: Absolute = Atmospheric + Gauge.
Now, let's make this concrete with some problems.
Let's Practice: Problems and Questions
Time to put on your engineering hat. We'll use a standard atmospheric pressure of 101.3 kPa or 14.7 psi for these problems.
Worked Problems
Problem 1: Tire Pressure
A car tire pressure gauge reads 35 psi on a standard day at sea level. What is the absolute pressure inside the tire in psi and in kPa?
Solution:
-
Identify what you have:
- Gauge Pressure () = 35 psi
- Atmospheric Pressure () = 14.7 psi
-
Find the absolute pressure in psi:
The true pressure in the tire is nearly 50 psi.
-
Convert to kPa: We know . We can create a conversion factor.
Problem 2: Pressure Cooker
A pressure cooker operates with an internal absolute pressure of 225 kPa. If the local atmospheric pressure is 100 kPa, what is the gauge pressure inside the cooker?
Solution:
-
Identify what you have:
- Absolute Pressure () = 225 kPa
- Atmospheric Pressure () = 100 kPa
-
Find the gauge pressure: Rearrange the main formula.
A pressure gauge on this cooker would read 125 kPa.
Problem 3: Vacuum Chamber
A vacuum pump reduces the pressure in a tank down to an absolute pressure of 10 kPa. What is the vacuum pressure in the tank, assuming the surrounding atmosphere is at 101.3 kPa?
Solution:
-
Identify what you have:
- Absolute Pressure () = 10 kPa
- Atmospheric Pressure () = 101.3 kPa
-
Find the vacuum pressure: Rearrange the second formula.
This means the pressure has been reduced by 91.3 kPa below atmospheric.
Conceptual Questions
Test your understanding!
Question 1: Why can gauge pressure be negative (a vacuum), but absolute pressure can never be negative?
Show answer
Gauge pressure is a comparison to atmospheric pressure. If the pressure is lower than atmospheric, the difference is negative. Absolute pressure is measured from a perfect vacuum, which is the ultimate zero point (no molecules, no motion, no pressure). You cannot have less pressure than zero pressure, just as you can't have negative mass or negative volume.
Test your understanding!
Question 2: You inflate your car tire to 35 psi in Denver, Colorado, where the atmospheric pressure is lower (around 12.2 psi). You then drive to sea level (where psi). If the tire's volume and temperature haven't changed, will your tire pressure gauge read higher, lower, or still 35 psi?
Show answer
The gauge will read higher. Let's analyze it.
-
In Denver: . This is the true pressure inside the tire, which doesn't change (assuming constant T and V).
-
At Sea Level: The absolute pressure is still 47.2 psi. But now the atmosphere is pushing back with 14.7 psi. The new gauge reading will be:
.
Whoops, my intuition was wrong! Let's re-read the question. You inflate it to 35 psi in Denver. So that's the starting point. The absolute pressure is 47.2 psi. When you drive to sea level, the absolute pressure inside the tire is still 47.2 psi. The gauge now reads psi. The question asks if the gauge will read higher, lower or the same. It will read lower. This is a great example of how important it is to keep absolute and gauge pressures straight! The external atmospheric pressure assists the tire pressure less at sea level. No, wait. The higher external pressure at sea level pushes in on the tire more, so the difference that the gauge measures is smaller. Let's redo the logic. -
In Denver: Gauge reads 35 psi. Absolute pressure is psi.
-
At Sea Level: The absolute pressure inside the tire is still 47.2 psi (since no air was added/removed). The new gauge reading is the difference between this absolute internal pressure and the new external atmospheric pressure.
New Gauge Reading = psi.
The gauge reading will be lower. The higher outside pressure "squeezes" the tire more, reducing the pressure difference that the gauge measures.
Test your understanding!
Question 3: When a weather forecaster says a "high-pressure system" is bringing sunny weather, are they talking about absolute or gauge pressure?
Show answer
They are talking about absolute pressure. Specifically, they are referring to the local barometric (atmospheric) pressure. A "high pressure" system means the absolute atmospheric pressure is higher than average (e.g., 103 kPa instead of 101.3 kPa). If they used gauge pressure, the reading for the atmosphere would always be zero by definition, which would make for a very boring weather report!
Lesson Summary
Excellent work today. We've demystified one of the most fundamental properties in thermodynamics. It's not just a number in an equation; it's the physical result of a microscopic storm of particles.
Here are the key takeaways:
- Pressure is the macroscopic effect of microscopic molecular collisions.
- The pressure we live in is called atmospheric pressure, created by the weight of the air above us.
- Absolute pressure is the true pressure measured from a perfect vacuum (the ultimate zero).
- Gauge pressure is what most gauges read, and it's the pressure relative to the local atmosphere.
- The simple but critical formula connects them: .
Preview of the Next Lesson
We now have one of the two key properties needed to describe the state of a gas: pressure. What's the other? You've probably guessed it: temperature.
In our next lesson, we will explore what temperature really is from a molecular perspective. We'll see that it's a close cousin of pressure, as it also relates to the motion of molecules. This will lead us to the Zeroth Law of Thermodynamics, the different temperature scales (Celsius, Kelvin, etc.), and the crucial concept of absolute zero temperature. See you then