Hydrostatic weighing
Hydrostatic weighing, also referred to as "underwater weighing", "hydrostatic body composition analysis", and "hydrodensitometry" is a technique for measuring the density of a living person's body. It is a direct application of Archimedes' principle, that an object displaces its own volume of water. Method. The procedure is based on Archimedes' principle, which states that: "The buoyant force which water exerts on an immersed object is equal to the weight of water that the object displaces." Example 1: If a block of solid stone weighs 3 kilograms on dry land and 2 kilogram when immersed in a tub  of water, then it has displaced 1 kilogram of water. Since 1 liter of water weighs 1 kilogram (at 4 °C), it follows that the volume of the block is 1 liter and the density (mass/volume) of the stone is 3 kilograms/liter. Example 2: Consider a larger block of the same stone material as in Example 1 but with a 1-liter cavity inside of the same amount of stone. The block would still weigh 3 kilograms on dry land (ignoring the weight of air in the cavity) but it would now displace 2 liters of water  so its immersed weight would be only 1 kilogram (at 4 °C). In either of the examples above, the correct density can be calculated by the following equation: Where: Db = Density of the body, Ma = "Mass in air" (i.e. dry weight), Mw = "Mass in water" (i.e. underwater weight), Dw = Density of water (based on water temperature), RV = Residual volume (the unfilled space enclosed by the body- e.g. volume of air in the lungs + respiratory passages after a maximum exhalation). The residual volume in the lungs can add error if not measured directly or  estimated accurately. Residual volume can be measured by gas dilution procedures or estimated from a person's age and height: Residual volume may also be estimated as a proportion of vital capacity (0.24 for men and 0.28 for women). Application. Once body density has been calculated from the data obtained by hydrostatic/underwater weighing, body composition can be estimated. The most commonly used equations for estimating the percent of body fat from density are those of Siri and Brozek et al.: Siri (1956): Fat % = [4.950 /Density - 4.500]×100 Brozek et al. (1963): Fat % = [4.570 /Density - 4.142]×100