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The sum force acting on the object, then, is equal to the difference between the weight of the object ('down' force) and the weight of displaced liquid ('up' force). Equilibrium, or neutral buoyancy, is achieved when these two weights (and thus forces) are equal.
This means the sum of the forces in a given direction must be opposed by an equal sum of forces in the opposite direction. This force balance is called a hydrostatic equilibrium. The fluid can be split into a large number of cuboid volume elements; by considering a single element, the action of the fluid can be derived.
Heath called it "a veritable tour de force which must be read in full to be appreciated." [ 5 ] The book contains a detailed investigation of the stable equilibrium positions of floating right paraboloids of various shapes and relative densities when floating in a fluid of greater specific gravity, according to geometric and hydrostatic variations.
This vertical force is termed buoyancy or buoyant force and is equal in magnitude, but opposite in direction, to the weight of the displaced fluid. Mathematically, = where ρ is the density of the fluid, g is the acceleration due to gravity, and V is the volume of fluid directly above the curved surface. [8]
Buoyancy (/ ˈ b ɔɪ ən s i, ˈ b uː j ən s i /), [1] [2] or upthrust is a net upward force exerted by a fluid that opposes the weight of a partially or fully immersed object. In a column of fluid, pressure increases with depth as a result of the weight of the overlying fluid.
Consequently, the object is in a state of static mechanical equilibrium. In classical mechanics, a particle is in mechanical equilibrium if the net force on that particle is zero. [1]: 39 By extension, a physical system made up of many parts is in mechanical equilibrium if the net force on each of its individual parts is zero. [1]: 45–46 [2]
g is the acceleration due to gravity and is equal to 980 cm/s 2 or 9.8 m/s 2; ρ is the density of the liquid in grams per cubic centimeter or kilograms per cubic meter; Illustration of how lower contact angle leads to reduction of puddle depth
For a water-filled glass tube in air at sea level: γ = 0.0728 J/m 2 at 20 °C; θ = 20° (0.35 rad) ρ = 1000 kg/m 3; g = 9.8 m/s 2; and so the height of the water column is given by: . Thus for a 2 mm wide (1 mm radius) tube, the water would rise 14 mm.