In this section we will explore Archimedes principle which relates an upward force acting on an object that is fully or partially submerged within a fluid to the weight of the fluid that the object displaces. We will also build upon our understanding of density, pressure, and hydrostatics to quantify the buoyant force.
Lecture 2 | Hydraulics, Buoyancy
Fluid Statics
Lecture 2 | Hydraulics, Buoyancy
Fluid Statics
Do you ever woder why you don't sink to the bottom of the pool or ocean? Check out this OpenStax concept trailer to find out.
Pre-lecture Study Resources
Watch the pre-lecture videos and read through the OpenStax text before doing the pre-lecture homework or attending class.
Fluid Statics | Hydraulics Pressure and Buoyancy
Hydraulics
Consider the analysis we did in the "pressure at a depth" section. If the pressure $P_0$ above the surface of the water increases by some amount $\Delta P$ so that the new pressure above the surface is now $P^{'}_{0} = P_0 + \Delta P$, then the pressure at all locations within the fluid also increase by the same amount $\Delta P$. Thus the pressure at the bottom of the volume element would be $P_1 + \Delta P = P_0 + \rho_{f} \, g \, d + \Delta P$.
Hydraulic brakes and lifts generally work by applying a force over an area at one location which increases the pressure at that location along with all other locations in the system. Thus hydraulics are an interesting application of Pascal's law. Below is a figure illustrating a simplified hydraulic lift.
Required Videos
OpenStax Section 11.7 | Archimedes' Principle (Buoyancy)
