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Explanation:
CONCEPT:
EXPLANATION:
The pressure at any point in a fluid at rest is obtained by the Hydrostatic Law which states that the rate of increase of pressure in a vertically downward direction must be equal to the specific weight of the fluid at that point.
\(\frac{{dP}}{{dh}} = \rho g\)
\(\smallint dP = \rho g\smallint dh\)
P = ρgh
For a plane surface of arbitrary shape immersed in a liquid in such a way that the plane of the surface makes an angle θ with the free surface of the liquid:
A = Total area of the inclined surface
h̅ = Depth of centre of gravity of inclined area from the free surface
h* = Distance of centre of pressure from the free surface of the liquid
\({h^*} = \frac{{{I_G}{{\sin }^2}\theta }}{{A\bar h}} + \bar h\)
For vertical plane surface: θ = 90°
\({h^*} = \frac{{{I_G}}}{{A\bar h}} + \bar h\)
A plate immersed vertically:
A plate immersed horizontally:
A double U - tube manometer is connected to two liquid lines A and B. Relevant height and specific gravities of the fluids are shown in the given figure. The pressure difference, in head of water, between fluids at A and B is
Concept:
Hydrostatic Law:
It states that the rate of increase of pressure in a vertical direction is equal to the weight density of the fluid at that point.
\(\frac{{\partial P}}{{\partial Z}} = - pg\;\left[ {Going\;Upward} \right]\)
\(\frac{{\partial P}}{{\partial Z}} = + pg\;\left[ {Going\;Downward} \right]\)
Calculation:
Given:
Converting all into equivalent head form
PA + hA⋅SA – hB⋅S1 + hB⋅S3 – hB SB = PB
PA – PB = hBS1 + hBSB – hASA – hBS3
At base PB = 750 mm of Hg
At top, PA = 600 mm of Hg
∴ Pressure difference = 150 mm of Hg = 150 × 10-3 × 13.6 × 103 × 9.81
(ΔP) = hρg
\( \Rightarrow \;h\; = \;\frac{{{\rm{\Delta }}P}}{{\rho g}}\; = \;\frac{{150 × 13.6 × {{10}^3} × {{10}^{ - 3}} × 9.81}}{{1 × 9.81}}\; = \;2040\;m\)
⇒ Height of mountain = 2040 m
Sensitivity:
Sensitivity is directly proportional to the length of fluid travel for a particular pressure difference.
\(\begin{array}{l} {\left( {Sensitivity} \right)_{U - tube}} \propto \;x\\ {\left( {sensitivity} \right)_{Inclined\;tube}} \propto \frac{x}{{\sin \theta }} \end{array}\)
\(\frac{(Sensitivity)_{Inclined\;tube}}{(Sensitivity)_{U-Tube}}=\frac{1}{\sin \theta}\)
When a body is either wholly or partially immersed in a fluid, a lift is generated due to the net vertical component of hydrostatic pressure forces experienced by the body. This lift is called the buoyant force and the phenomenon is called buoyancy.
The Archimedes principle states that the buoyant force on a submerged body is equal to the weight of the liquid displaced by the body and acts vertically upward through the centroid of the displaced volume.
Thus, the net weight of the submerged body, (the net vertical downward force experienced by it) is reduced from its actual weight by an amount that equals the buoyant force.
FB = ρghA = ρgV
FB = f(Vdisplaced, ρ)
Types of equilibrium
Stable Equilibrium:
Unstable Equilibrium:
Neutral Equilibrium:
Stability of Floating Bodies in Fluid:
When the body undergoes an angular displacement about a horizontal axis, the shape of the immersed volume changes and so the centre of buoyancy moves relative to the body.
Metacentre:
Meta Centre is defined as the point about which a body starts oscillating when the body is tilted by a small angle.
The meta-centre may also be defined as the point at which the line of action of the force of buoyancy will meet the normal axis of the body when the body is given a small angular displacement.
Hence the condition of stable equilibrium for a floating body can be expressed in terms of metacentric height as follows:
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