# 31 Apparent Weight

The method of allows us to determine the average ( ) of an object without the need for a measurement, which can be difficult for large, odd objects like the human body. Instead, we measure only the object’s weight ( ) and  apparent weight when submerged ( ) and enter them into the equation below to calculate the density. To see how we arrive at this useful result, we first need to understand how the apparent weight is related to the buoyant force, and also how the buoyant force works.

(1) # Apparent Weight

When an object is held still under water it appears to weigh less than it does in air because the is helping to hold it up (balance its ). For this reason, the reduced force you need to apply to hold the object is known as the . When a scale is used to weigh an object submerged in water the scale will read the apparent weight. When performing for body composition measurement the apparent weight is often called the ( ).

# Static Equilibrium

When weighing under water we know the must be equal to the difference in magnitude between the and because the object remains still, which is a state known as . For an object to be in static equilibrium, all of the forces on it must be balanced so that there is no . For the case of under water weighing, the buoyant force plus the force provided by the scale must perfectly balance the weight of the object, as long as the object is holding still. We can use arrows to represent the forces on an object and visualize how they are balanced or unbalanced. This type of diagram is known as a (FBD). The direction of arrows shows the direction of the forces and the arrow lengths shows the size () of the force. In this case we call the arrows and say the forces they represent are vector quantities. Free body diagram of an object hanging from a scale, submerged in water. The length of the weight arrow is equal to the combined lengths of the force supplied by the scale and the buoyant force. A scale will read the weight that it must supply, therefore it will read an apparent weight for submerged objects that is less than the actual weight.

We learned in the last chapter that scales measure the force that they are supplying to other objects. When the is also helping, the scale must supply less force to counteract the and maintain . Therefore the scale will provide a reading that is less than the actual weight. As we see from the diagram above, the magnitudes of the force supplied by scale and buoyant force must balance the magnitude of the actual weight. In other words, we can calculate the buoyant force ( ) as the difference between the magnitudes of weight ( ) and apparent ( ) weight read from the hanging scale. Notice that if the object tended to float rather than sink, then the scale would need to pull downward to hold it in place. In that case the buoyant force would balance both the apparent force supplied by the scale and the actual weight so we could find the buoyant force as:  