Q.Torricelli's barometer used mercury. Pascal duplicated it using French wine of density 984 kg m−3. Determine the height of the wine column for normal atmospheric pressure.
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Hydrostatic Pressure Balance
Imagine you're standing at the bottom of a swimming pool. You feel pressure on your ears — and the deeper you go, the more intense that pressure becomes. Now think about a column of water above you: every kilogram of that water is being pulled down by gravity. That weight has to be supported by the water below it. The deeper you go, the more water is stacked above you, so the greater the weight pressing down.
That's the core intuition: pressure in a fluid at rest increases with depth because the fluid above has to be supported by the fluid below.
The Precise Statement
Hydrostatic pressure balance is the condition that holds for any fluid at rest in a uniform gravitational field. It says:
Pbelow=Pabove+ρgh
where:
- Pbelow is the pressure at a lower point,
- Pabove is the pressure at a higher point,
- ρ is the density of the fluid (assumed constant),
- g is the acceleration due to gravity,
- h is the vertical depth between the two points.
Equivalently, the pressure gradient in the vertical direction is:
dzdP=−ρg
where z increases upward. The minus sign tells you pressure decreases as you go up.
Why This Makes Sense
Take a thin horizontal slab of fluid of area A, thickness dz, at some depth. Its weight is dW=ρgAdz. For the slab to be in equilibrium (not accelerating), the net upward force from pressure must exactly balance this weight.
The upward force on the slab's bottom face is P(z)A, and the downward force on its top face is P(z+dz)A. The net upward force is:
P(z)A−P(z+dz)A=−dzdPAdz
Setting this equal to the weight ρgAdz gives:
−dzdP=ρg
which is exactly the differential form above.
This balance assumes the fluid is static — no flow, no acceleration. If the fluid moves, additional terms (like viscous forces or inertial effects) appear.
Key Implications
-
Pressure depends only on depth, not on the shape of the container. A tall thin tube and a wide shallow tank give the same pressure at the same depth — because only the vertical height of fluid above matters.
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Pressure is the same at all points on the same horizontal level. If you move sideways at constant depth, ρgh doesn't change, so P doesn't change.
-
Gases are compressible, so ρ is not constant. For air, the density changes with pressure itself, leading to an exponential decrease — but the same principle applies locally.
A Common Mistake …
Concept: Atmospheric pressure at sea level supports a liquid column whose weight per unit area equals that pressure; the height depends inversely on the liquid's density.
In a barometer, atmospheric pressure P0 balances the hydrostatic pressure of the liquid column:
P0=ρgh
where ρ is the liquid density, g=9.8 m s−2, and h is the column height. Normal atmospheric pressure is P0=1.013×105 Pa.
Rearranging for height:
h=ρgP0=984×9.81.013×105=9643.21.013×105≈10.5 m …
A barometer measures atmospheric pressure by balancing it against a column of liquid; since wine is much less dense than mercury, it requires a proportionally taller column. For standard atmospheric pressure, the wine column reaches 10.5 m.
Why liquids of different densities give different column heights
A barometer works on a beautifully simple principle: atmospheric pressure at the base supports a column of liquid in an evacuated tube. The pressure at the bottom must equal the weight per unit area of the liquid column above it.
For any liquid in hydrostatic equilibrium, the pressure exerted by a column of height h is
P=ρgh
where ρ is the liquid's density and g is gravitational acceleration. Since atmospheric pressure Patm is fixed (at a given location and time), a denser liquid like mercury needs a shorter column to produce the same pressure, while a lighter liquid like wine needs a much taller one.
Mercury's fame in barometry comes from its high density (13,600 kg m−3), which keeps the instrument compact at about 76 cm. Wine, being roughly 14 times less dense, will require a column about 14 times taller.
Step-by-step calculation
1. Identify the known quantities
- Standard atmospheric pressure: Patm=101,325 Pa (or 1.01325×105 Pa)
- Density of French wine: ρwine=984 kg m−3
- Gravitational acceleration: g=9.8 m s−2 (or 9.81 m s−2 for higher precision)
2. Apply the hydrostatic pressure formula
The atmospheric pressure must balance the pressure from the wine column:
Patm=ρwine⋅g⋅h
3. Solve for the height h
Rearranging for h:
h=ρwine⋅gPatm
4. Substitute the numerical values
Using g=9.8 m s−2:
h=984×9.8101,325=9,643.2101,325≈10.51 m
If we use g=9.81 m s−2 for slightly better accuracy: …
Barometer balance: P0=rhogh. h=P0/(rhog)=1.013e5/(9849.8)~=10.5 m for wine ( …
Showing the 12 most recent of 21 on this concept.
- AP EAPCET 2026Set eng-2026-05-12-FN1 markMCQQ.An iceberg floats on sea water of density ρ=1.03×103 kgm−3. The percentage of total volume of ice above the surface of water is about (Density of ice σ=0.92×103 kgm−3) (A) 10.7% (B) 12.5% (C) 9.8% (D) 11.3%
›Reveal solutionSolution
Floating equilibrium requires the weight of the iceberg to equal the buoyant force from the displaced seawater — this directly gives the submerged fraction as the density ratio, and the rest is the visible fraction above water. Answer: (A) 10.7%.
Concept and Intuition
When an object floats, it displaces just enough fluid so the buoyant force (weight of displaced fluid) equals its own weight. If V is the iceberg's total volume and Vsub the submerged part, then:
σVg=ρVsubg⇒VVsub=ρσ.
Since ice is less dense than seawater, this ratio is less than 1 — most of an iceberg is submerged (the famous "tip of the iceberg" only shows the small fraction above water).
Step-by-Step Solution
- Submerged fraction: VVsub=ρσ=1.03×1030.92×103=1.030.92=0.8932. …
- AP EAPCET 2026Set eng-2026-05-13-AN1 markMCQQ.When a body floats in water and another liquid separately, it floats with one third of its volume outside water and 43 of its volume outside another liquid. The density of the liquid is (A) 9.4 gcc−1 (B) 4 gcc−1 (C) 38 gcc−1 (D) 83 gcc−1
›Reveal solutionSolution
This tests the law of flotation (weight of body = weight of displaced liquid). Using the fraction submerged in each liquid gives the body's density from water, then the unknown liquid's density from the second condition.
Concept and Intuition
When a body floats in equilibrium, its weight equals the weight of the liquid it displaces (Archimedes' principle applied to flotation): ρbVg=ρliquidVsubg, i.e. ρbV=ρliquidVsub. If a fraction f of the volume is outside the liquid, then the submerged fraction is (1−f), and
ρb=(1−f)ρliquid.
Applying this once with water (whose density we know, 1 g/cc) pins down ρb. Applying it a second time with the unknown liquid, now that ρb is known, gives the unknown liquid's density.
Step-by-Step Solution
- In water: fraction outside =1/3, so submerged fraction =2/3.
ρb=32×ρwater=32×1=32 g/cc.
- In the other liquid: fraction outside =3/4, so submerged fraction =1/4.
ρb=41×ρL.
- Equate the two expressions for ρb (same body, same mass/volume): …
- AP EAPCET 2026Set eng-2026-05-15-AN1 markMCQQ.A vessel contains oil of density 0.8 gcm−3 over mercury of density 13.6 gcm−3. A homogenous sphere floats with half of its volume immersed in mercury and the other half in oil. Then the density of the material of the sphere is (A) 3.3 gcm−3 (B) 6.4 gcm−3 (C) 7.2 gcm−3 (D) 12.8 gcm−3
›Reveal solutionSolution
Tests Archimedes' principle for a body floating at the interface of two immiscible liquids. Each half of the sphere's volume displaces one liquid, and equilibrium gives ρsphere=7.2 g/cm3, the simple average of the two liquid densities (since the two immersed volumes are equal).
Concept and Intuition
When a solid floats in equilibrium (whether fully or partly submerged, or split between two liquids), Newton's first law for the floating body requires the net upward buoyant force to exactly balance its weight. Here the sphere straddles the oil-mercury interface with exactly half its volume in each liquid. Each half displaces its own liquid and contributes its own buoyant force — we simply add the two buoyant contributions and set the sum equal to the total weight of the sphere.
Step-by-Step Solution
- Let the sphere have total volume V and density ρs. Its weight is ρsVg.
- Half the volume (V/2) is immersed in oil (density 0.8 g/cm3), contributing buoyant force ρoil⋅2V⋅g.
- The other half (V/2) is immersed in mercury (density 13.6 g/cm3), contributing buoyant force ρHg⋅2V⋅g.
- Equilibrium (floating, net force zero): …
- AP EAPCET 2025Set eng-2025-05-22-FN1 markMCQQ.In a hydraulic lift, if the radius of the smaller piston is 5 cm, and the radius of the larger piston is 50 cm, then the weight that the larger piston can support when a force of 250 N is applied to the smaller piston is (A) 50 kN (B) 100 kN (C) 40 kN (D) 25 kN
›Reveal solutionSolution
Hydraulic lift multiplies force by the ratio of piston areas (radius squared); the larger piston supports 25 kN.
Concept and Intuition
Pascal's law says pressure applied to an enclosed incompressible fluid is transmitted undiminished in all directions. Since pressure =F/A must be equal on both pistons, a small force on a small piston produces a large force on a large piston — the mechanical advantage is the ratio of the piston areas, i.e. the square of the radius ratio.
Step-by-Step Solution
- Pascal's law: A1F1=A2F2, with A∝r2.
- F2=F1(r1r2)2=250×(550)2. …
- AP EAPCET 2024Set ap-2024-05-17-FN1 markMCQQ.A U-tube is partially filled with water. Oil which does not mix with water is next poured into one-side of U-tube until entire water rises by 25 cm on the other side. If the density of oil is 0.8 gcm−3, the oil level will stand higher than the water level by (A) 6.25 cm (B) 12.50 cm (C) 31.75 cm (D) 63.50 cm
›Reveal solutionSolution
This tests pressure balance in a U-tube with two immiscible liquids; the answer is (B) 12.50 cm.
Concept and Intuition
When oil is poured into one arm of a U-tube containing water, it cannot mix, so it floats as a layer on top of the water in that arm and pushes the water down. Because the tube has the same cross-section throughout, the volume of water pushed down in the oil arm must reappear as a rise in the plain-water arm — so the drop of the oil–water interface equals the rise of the water surface in the other arm. Once the system is in equilibrium, the pressure at any given horizontal level, measured through connected fluid, must be equal on both arms. This is the standard "connected liquids" pressure-balance idea.
Step-by-Step Solution
- Let the original common water level (before oil was added) be the datum, height 0.
- Water rises by h=25 cm on the plain-water arm ⇒ its free surface is at +h=+25 cm.
- By volume conservation (equal areas), the oil–water interface in the oil arm falls by the same amount, to −h=−25 cm.
- Take the horizontal level of this interface (−h) as the reference for pressure balance.
- Via the plain-water arm: the pressure at this level equals atmospheric pressure plus the pressure of the water column from −h up to the free surface at +h, i.e. a column of height 2h=50 cm of water: P=Patm+ρwaterg(2h).
- Via the oil arm: the pressure at the same level equals atmospheric plus the oil column above it, of height H (unknown, up to the oil's free surface): P=Patm+ρoilgH. …
- AP EAPCET 2024Set eng-2024-05-22-AN1 markMCQQ.Two cylindrical vessels A and B of different areas of cross-section kept on same horizontal plane are filled with water to the same height. If the volume of water in vessel A is 3 times the volume of water in vessel B, then the ratio of the pressures at the bottom of the vessels A and B is (A) 1 : 1 (B) 1 : 3 (C) 1 : 9 (D) 1 : 6
›Reveal solutionSolution
This tests whether you know that hydrostatic pressure depends only on depth, not on the shape/volume of the container.
Concept and Intuition
The pressure at the bottom of a liquid column comes purely from the weight of the liquid sitting directly above a unit area, which is captured by P=ρgh. This formula has no term for cross-sectional area or total volume — it is the classic "hydrostatic paradox": a wide short vessel and a narrow tall vessel filled to the same height exert the same pressure at the bottom, even though they hold very different volumes of liquid, because the extra volume in the wide vessel is exactly compensated by the extra area over which that weight is spread.
Step-by-Step Solution
- Let vessel A have base area A1 and vessel B have base area A2, both filled to the same height h.
- Volume in A: VA=A1h. Volume in B: VB=A2h. Given VA=3VB⇒A1=3A2 — this tells us about the areas, not the pressures. …
- AP EAPCET 2023Set ap-2023-05-22-FN1 markMCQQ.A liquid of density 800 kgm−3 is used instead of mercury, in the Torricelli barometer. The height of the liquid column is (Density of mercury =13.6×103 kgm−3 and atmospheric pressure = 76 cm of Hg) (A) 13.2 m (B) 12.9 m (C) 13.6 m (D) 800 m
›Reveal solutionSolution
A Torricelli barometer works because the atmospheric pressure balances the weight of a liquid column with a vacuum above it; replacing mercury with a lighter liquid makes the column proportionally taller.
Concept and Intuition
In a barometer, the space above the liquid in the closed tube is (nearly) vacuum, so the pressure at the base of the column, ρgh, must equal the atmospheric pressure pressing on the open reservoir. This balance condition is independent of which liquid is used — only ρh must stay the same (since g and Patm are fixed). A less dense liquid therefore needs a taller column to produce the same pressure.
Step-by-Step Solution
- For mercury: Patm=ρHgghHg, with hHg=76 cm=0.76 m and ρHg=13.6×103 kgm−3.
- For the new liquid: Patm=ρliqghliq, with ρliq=800 kgm−3. …
- AP EAPCET 2023Set eng-2023-05-15-AN1 markMCQQ.The gauge pressure at a depth of 50 m in a sea is (Density of sea water is 1025 kg m−3 and g = 10 ms−2) (A) 1025 Pa (B) 512500 Pa (C) 20000 Pa (D) 15000 Pa
›Reveal solutionSolution
Direct substitution into P=ρgh gives the gauge pressure at the given depth: 512500 Pa.
Concept and Intuition
Gauge pressure (pressure in excess of atmospheric) at a depth h in a fluid of density ρ is P=ρgh, arising from the weight of the fluid column above that point.
Step-by-Step Solution
- Given: ρ=1025kg m−3, g=10ms−2, h=50m.
- P=ρgh=1025×10×50.
- Compute: 1025×10=10250; 10250×50=512500Pa.
Common Mistakes …
- AP EAPCET 2023Set eng-2023-05-16-FN1 markMCQQ.A tank of oil has height of 4 m and density of 850 kgm−3. The gauge pressure at the bottom of the tank is (1 atm = 105 Pa, Acceleration due to gravity = 10 ms−2) (A) 34 kPa (B) 384 kPa (C) 284 kPa (D) 200 kPa
›Reveal solutionSolution
This tests the direct hydrostatic pressure formula P=ρgh, giving gauge pressure (pressure in excess of atmospheric) at the base of a liquid column.
Concept and Intuition
Gauge pressure is the pressure due to the fluid column alone, excluding atmospheric pressure (which acts equally on any exposed surface and is usually already "zeroed out" by the measuring instrument). For a fluid of density ρ at depth h, this is simply ρgh — it does not depend on the shape or cross-section of the tank, only on the vertical height of fluid above the point.
Step-by-Step Solution
- Given: height of oil column h=4 m, density ρ=850 kgm−3, g=10 ms−2.
- Gauge pressure at the bottom: Pgauge=ρgh=850×10×4.
- 850×10=8500; 8500×4=34,000 Pa.
- Convert to kPa: 34,000 Pa=34 kPa. …
- AP EAPCET 2023Set eng-2023-05-18-FN1 markMCQQ.A swimming pool has depth of 3 meters. The pressure at the bottom of the pool due to water alone is (Density of water is 1000 kgm−3, Acceleration due to gravity = 10 ms−2) (A) 104 Pa (B) 3×103 Pa (C) 29×103 Pa (D) 30×103 Pa
›Reveal solutionSolution
The hydrostatic pressure due to water alone at depth h is ρgh, giving 30×103 Pa.
Concept and Intuition
The pressure at a depth h in a static fluid (due to the fluid column alone, ignoring atmospheric pressure which the question explicitly excludes by saying "due to water alone") is P=ρgh.
Step-by-Step Solution
- ρ=1000 kgm−3, g=10 ms−2, h=3 m. …
- AP EAPCET 2022Set ap-2022-07-11-FN1 markMCQQ.A container is filled to a height of 20 cm with water. A 30 cm thick layer of oil with specific gravity 0.8 floats on the top of water. If the density of water is 1000 kgm−3 and atmospheric pressure is 1×105 Pa, then the total pressure at the bottom of the container is (Acceleration due to gravity =10 ms−2) (A) 1.044×105 Pa (B) 1.24×105 Pa (C) 1.062×105 Pa (D) 1.15×105 Pa
›Reveal solutionSolution
Total pressure at the bottom is the atmospheric pressure plus the weight-per-area contributions of each fluid layer stacked above: P=Patm+ρoilghoil+ρwaterghwater=1.044×105 Pa.
Concept and Intuition
Pressure in a fluid at rest increases with depth due to the weight of fluid above. When layers of different fluids are stacked, the total pressure at the bottom is simply the sum of the atmospheric pressure at the top surface plus each layer's own ρgh contribution (heavier/lighter fluids each contribute according to their own density and thickness).
Step-by-Step Solution
- Oil layer: density =0.8×1000=800 kgm−3, thickness hoil=0.30 m. Contribution: ρoilghoil=800×10×0.30=2400 Pa.
- Water layer: density =1000 kgm−3, thickness hwater=0.20 m. …
- AP EAPCET 2022Set ap-2022-07-12-FN1 markMCQQ.An object hangs from a spring balance. The balance shows 40 N when the object is in air, 30 N when the object is immersed in water, and 34 N when the object is immersed in another liquid. If the density of water is 1000 kgm−3, then the density of liquid is (Acceleration due to gravity = 10 ms−2) (A) 500 kgm−3 (B) 800 kgm−3 (C) 750 kgm−3 (D) 600 kgm−3
›Reveal solutionSolution
The loss of apparent weight in each fluid equals the buoyant force ρfluidVg; comparing the two losses (with the same V and g) gives the unknown liquid's density directly. Answer: 600 kgm−3.
Concept and Intuition
Archimedes' principle says the apparent weight loss when submerged equals the weight of fluid displaced, ρfluidVg, where V is the object's volume (same in both fluids). Taking the ratio of weight losses in water and in the unknown liquid eliminates the unknown V, leaving a simple density ratio.
Step-by-Step Solution
- Weight in air: 40N (true weight of the object).
- Weight in water: 30N, so buoyant force in water =40−30=10N =ρwVg.
- Weight in liquid: 34N, so buoyant force in liquid =40−34=6N =ρLVg. …
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