The method of hydrostatic weighing allows us to determine the average density () of a any object without any need for a volume (V) measurement by measuring only its weight () and apparent weight, also known as under water weight (). To see how we arrive at this useful result, follow the steps in the derivation at the end of this chapter.

(1)  

The previous equation is very similar to the body density equation used for hydrostatic weighing, but you will notice a slight difference. The previous equation determines the average density of the object including any hollow parts containing trapped air, but the body density equation is designed to determine the average density of body tissues only, not including trapped air. Therefore, the body density equation is modified to account for a volume of air trapped inside the body, known as the residual volume (RV).  Also different standard symbols are used to designate  body density, apparent weight, and water density.

^[1]

Specific Gravity

The ratio of the density of a substance to that of water is known as the specific gravity. Specific gravity can be determined by hydrostatic weighing. If we simply divide both sides of our density equation by the density of water we will have a formula for the specific gravity with weight and apparent weight as input:

(2)  

Hydrostatic Weighing Equation Derivation

We arrived at equation (1) by starting with the definition of density as mass divided by its volume:

We can find the mass of an object if we divide its weight by g:

Inserting that result for mass into the density equation we have:

For a completely submerged object the volume of water displaced is equal to the volume of the object, so we can replace with .

Using the definition of density again, we can replace the volume of water displaced with the displaced water mass () divided by water density ().

We can look up the density of water, but it depends on the water temperature, which is why its important to measure the water temperature when hydrostatic weighing. Notice that we happen to have the mass of displaced water multiplied by g in the previous equation. That is exactly how we calculate the weight of the displaced water (), so we can make that substitution:

Archimedes' Principle which tells us that the  buoyant  force pushing upward on objects in a fluid is equal to the weight displaced fluid. Therefore we can replace with .

We have learned that the difference between an object’s weight () and apparent weight () tells us the size of the buoyant force (), as long as the body is in static equilibrium (holding still):

Making that replacement in our density equation we have:

We now have an equation that allows us to calculate the density of an object by measuring only its weight and apparent weight, as long as we know the density of the fluid we are using.