# Pressure

Pressure is the key physical factor in diving. The basic understanding is essential, as the term pressure appears in all sub-areas of diving.

From a physical point of view, pressure is a force related to the area it is acting on. In diving, the pressure is measured in bar.

From a physical point of view, pressure is the amount of force applied at right angles to the surface of an object per unit area. The higher the force, the higher is also the pressure. On the surface, we are constantly exposed to the surrounding air at a pressure of 1 bar at sea level. This pressure is caused by the weight of the atmosphere. Since water is significantly denser and therefore heavier than air, the pressure we are exposed to in water increases drastically with depth.

While diving you do not need to worry about being crushed and being hurt by the pressure you are exposed to. You will only feel the pressure on your ears, which is why it is important to equalize frequently while descending. Since you are breathing compressed air and your lungs, therefore, equalizing automatically, one of the most important rules in diving is to never hold your breath.

## Basic knowledge for Open Water Diver* (OWD*)

In diving, pressure is usually measured in the unit bar. A pressure of 1 bar prevails at about sea level on the water surface.

### Ambient pressure

The ambient pressure is caused by the weight of the surrounding medium an object is exposed to. As divers we are exposed to air on the surface and to water while diving. Water has a much higher density than air. Therefore, the ambient pressure under water rises drastically with the depth. The water pressure increases by 1 bar every 10 m of depth. In addition, there is the atmospheric pressure on the water surface. This means, for example, that you are exposed to an ambient pressure of 2 bar in the sea at 10 m depth: 1 bar water pressure plus 1 bar atmospheric pressure.

Ambient pressure at different water depths
Depth Water
pressure
Atmospheric
pressure
Ambient
pressure
0 m 0 bar 1 bar 1 bar
10 m 1 bar 1 bar 2 bar
20 m 2 bar 1 bar 3 bar
30 m 3 bar 1 bar 4 bar
40 m 4 bar 1 bar 5 bar

### Gas pressure

The pressure of a gas is caused by the smallest building block of the gas, it's molecules or atoms. These particles are permanently moving. Their speed is depending on the gas temperature and density. During these movements they collide with each other and the walls of its container, e. g. the cylinder.

You can imagine it as if you hold up a table top and your dive partner throws tennis balls against it. If he or she throws enough balls at the same time, you will find that you have to push yourself against the plate with strong force not to be pushed backwards. This force acting on the plate with a defined surface area is called pressure. The more balls hit the surface at the same time, the greater the force and the pressure. Exactly the same happens in your compressed air cylinder – but on a smaller scale: The particles are much smaller and exercise a very small force, but it holds a very high amount of gas molecules.

More particles in the same size container (volume) produce a higher pressure. So you can easily imagine what it means that your dive tank is holding compressed air with 200 bar pressure: The empty tank would have the same pressure as the surrounding area. Ambient pressure at sea level is 1 bar. A filled tank holds 200 times this pressure. This relationship is described by the Boyle-Mariotte law.

## Knowledge for experts (DM***)

### Definition of pressure

The pressure $p$ is generally considered as a force $F$ which acts on a defined surface with the area $A$.

$p = \frac{F}{A}$

The greater the force, the higher the pressure. If the same force spreads over a larger area, the pressure is correspondingly lower.

Just try to stand on your tow tips for a while. Your weight respectively the force is acting on a much smaller area as if you would standing as usually on your whole foot. Got the point?

### Hydrostatic pressure

Hydrostatic pressure is the pressure that is exerted by a fluid, i. e. a fluid or a gas, at equilibrium at a given point within the fluid, due to the force of gravity. Hydrostatic pressure increases in proportion to depth measured from the surface because of the increasing weight of fluid exerting downward force from above. The force $F$ is determined by the objects mass $m$ and its acceleration due to gravity $g$.

$F = m \cdot g$ Force $F$ acting on the ground of a column of fluid with height $t$ due to the hydrostatic pressure.

On an imaginary surface with the area $A$ in depth $t$ acts a column of fluid with the volume $V$. Assuming that, as in the case of water, the fluid is not compressible and its density $\rho_{\text{f}}$ is constant, then the pressure $p$ in the depth $t$ is:

$p = \frac{m \cdot g}{A} = \frac{g \cdot \rho_{\text{f}} \cdot V}{A}$

The volume of the fluid column is $A \cdot t$:

$p = \frac{g \cdot \rho_{\text{f}} \cdot A \cdot t}{A} = g \cdot \rho_{\text{f}} \cdot t$

The hydrostatic pressure is dependent of the density of the fluid $\rho_{\text{f}}$ and the depth $t$.

To calculate the hydrostatic pressure of water, e. g. the water pressure in dependency of the depth, we assume the gravitational acceleration $g$ to 9.81 m/s2 and set the density $\rho_{\text{f}}$ to 1 kg/dm3 for fresh water. Then the water pressure $p$ in depth $t$ is:

$p = 0,0981 \ \frac{\text{bar}}{\text{m}} \cdot t$

Since salt water has a slightly higher density than fresh water, the pressure increase in salt water is slightly higher. In both cases, however, it roughly corresponds to the approximate calculation used in scuba diving that the water or ambient pressure increases by 1 bar per 10 m of water depth.

### Atmospheric pressure

Height above
sea level
atmospheric
pressure
0 m 1.01 bar
500 m 0.95 bar
1000 m 0.89 bar
2000 m 0.78 bar
3000 m 0.69 bar
4000 m 0.61 bar
5000 m 0.53 bar
6000 m 0.47 bar

In order to determine the pressure relevant for the decompression calculation, we need the ambient pressure acting on our body. That means we have to add to the water pressure the atmospheric pressure from the surface.

The air in the earth's atmosphere also generates a hydrostatic pressure as gas, which, like the water pressure, depends on the height of the air layer above. This again depends on the altitude we are in. However, since air is compressible and its density therefore depends on both pressure and temperature, the calculation is much more complex than with water pressure.

It can be assumed that the atmospheric pressure at sea level is 1 bar and drops by 0.1 bar per 1000 m to 2000 m above sea level. At higher altitudes and for more accurate calculations, the atmospheric pressure can be taken from the adjacent table depending on the altitude. The table does not take into account the weather conditions.