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Physics · Ch 7 — Properties of Matter

Pressure due to fluid column at rest

7.3.2

Pressure due to fluid column at rest

The pressure a mountaineer feels DECREASE with altitude and the pressure a diver feels INCREASE with depth are both examples of HYDROSTATIC PRESSURE -- pressure due to a static fluid. To find how pressure changes with depth below a liquid surface, consider a cylindrical sample of the liquid, cross-sectional area A, with its top face at depth h1h_1 and its bottom face at the greater depth h2h_2 (both measured from the free surface). Let F1=P1AF_1=P_1A be the downward force on the top face and F2=P2AF_2=P_2A the upward force on the bottom face. For the sample to be in equilibrium, the net upward force must balance both the downward force from above AND the weight of the sample itself: F2=F1+mgF_2=F_1+mg. The mass of the sample is m=ρV=ρA(h2−h1)m=\rho V=\rho A(h_2-h_1), so its weight (the gravitational force FGF_G) is ρA(h2−h1)g\rho A(h_2-h_1)g. Substituting and cancelling the common factor A from every term gives P2=P1+ρ(h2−h1)gP_2=P_1+\rho(h_2-h_1)g. Taking level 1 at the free surface itself (so h1=0h_1=0 and P1P_1 equals the atmospheric pressure PaP_a) and level 2 at depth h (so P2=PP_2=P, the pressure being sought) gives the standard result P=Pa+ρghP=P_a+\rho g h: the pressure at depth h is always greater than the pressure at the surface. If the atmospheric contribution is ignored (or the pressure is measured relative to the atmosphere), this simplifies to P=ρghP=\rho g h. Since ρ\rho and g are both fixed for a given liquid, this shows the pressure due to the fluid column depends ONLY on the vertical height h of fluid above the point in question -- never on the cross-sectional area, the total volume, or even the shape of the container. This surprising independence from shape is dramatized by the HYDROSTATIC PARADOX: three vessels of very different shapes -- one narrow and tall, one wide and squat, one irregularly bulging -- connected at the bottom by a common horizontal pipe and filled with the same liquid, all settle to exactly the SAME liquid level, because the liquid at the bottom of each vessel experiences exactly the same pressure regardless of how much liquid t …

Figure 7.10Hydrostatic pressure derivation

What this figure shows. Part (a) shows a cylindrical sample of water of base area A held in equilibrium between two horizontal levels inside a static fluid: an upward force F2 acts on its lower face, a downward force F1 acts on its upper face, and its own weight mg acts downward, with the difference F2 minus F1 exactly balancing the weight of the enclosed water column. Part (b) specialises this to the everyday case where level 1 is taken at the open air-water interface (so its pressure is the atmospheric pressure Pa) and level 2 is taken a depth h below the surface, directly giving the depth-dependent pressure for …

Figure 7.11Illustration of hydrostatic paradox

What this figure shows. Three vessels A, B and C of visibly different shapes -- one narrow and tall, one wide and squat, one an irregular bulging shape -- are connected to a common reservoir at the bottom by a horizontal pipe. When filled with the same liquid, the liquid surface settles to exactly the same height in all three vessels regardless of their very different shapes and the very different total volumes or weights of liquid each one holds, demonstrating that liquid pressure at a given depth depends only on that depth, never on the shape or cross-sectional area of the contai …