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04-BS-7 · May 2014

Question 2 of 13: Manometer Fluid Identification

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

04-BS-7 Mechanics of Fluids — National Examinations, May 2014. Three (3) hours, closed book. Section A: Calculative (9 questions, do 7); Section B: Analytical/Graphical (4 questions, do 3). Ten questions constitute a complete paper (50 marks). Every printed question is solved below, including the two "extra" questions in each Section beyond the minimum required.

Reference texts: White, Fluid Mechanics, 8th ed. (fluid statics & capillarity Ch.2; Bernoulli/energy equation Ch.3; pipe friction & the Moody chart Ch.6; drag on immersed bodies Ch.7; buoyancy Ch.2; momentum & jet propulsion Ch.3).

Question 2 — Manometer Fluid Identification (5 marks)

Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.

Given. All pressures absolute; atmospheric p0 = 100 kPa; SGwater=1.00, SGglycerine=1.26, SGmercury=13.56 (General Reference Information, p.12). Column heights and end pressures as marked on the attachment (85, 110, 108, 150, 200, 160 kPa; 1530, 810, 815, 1000, 300, 260 mm).

Find. The fluid (air, water, glycerine or mercury) in every section of all four manometers, written into the label spaces.

WATERGLYCERINEAIRWATERMERCURYAIRAIRWATERWATERMERCURY
Fig. Q2 — the page-8 attachment with the answer written into each of the ten label spaces (dashed leader lines). Note the trap the question warns about: the bulbs and legs of the lower-left manometer are hatched like the water elsewhere, but the pressure balance shows they hold AIR.

Approach. For a static fluid column of height h connecting two points of known pressure, ρ = Δp/(gh); match the computed density to the given specific gravities (using the shading change noted in the instructions to confirm where one fluid ends and the next begins).

  1. Column 1 (1530 mm, 85 kPa bulb to the open/atmospheric leg). $$\rho_1 = \frac{{|100,000-85,000|}}{{9.81\times1.530}} = \frac{{15,000}}{{15.01}} = 999\text{{ kg/m}}^3 \Rightarrow \boxed{{\text{{WATER}}}}\ (SG\approx1.00)$$
  2. Column 2 (810 mm, atmosphere to 110 kPa bulb). $$\rho_2 = \frac{{|110,000-100,000|}}{{9.81\times0.810}} = \frac{{10,000}}{{7.946}} = 1259\text{{ kg/m}}^3 \Rightarrow \boxed{{\text{{GLYCERINE}}}}\ (SG=1.26,\text{{ exact match}})$$
  3. Column 3 (815 mm, atmosphere to 108 kPa bulb). $$\rho_3 = \frac{{|108,000-100,000|}}{{9.81\times0.815}} = \frac{{8,000}}{{7.995}} = 1001\text{{ kg/m}}^3 \Rightarrow \boxed{{\text{{WATER}}}}$$
  4. Air spaces in the upper manometers. The unshaded crown of the 810 mm (glycerine) manometer and the unshaded inverted U above the 815 mm column, running across to the flared open end, hold AIR at atmospheric pressure. That is why the free surfaces of columns 2 and 3 sit at p0 = 100 kPa; air's weight over these heights is negligible.
  5. Lower-right manometer (108 kPa bulb → 150 kPa bulb, 260 mm deflection). The 108 kPa bulb is the same water-filled bulb as column 3, so the long leg that drops from it (the 1000 mm level difference to the 150 kPa bulb) is water. If the leg rising to the 150 kPa bulb is also water, the loop closes with mercury in the bottom of the U: $$p_{150} = 108 + \frac{1000\times9.81\times1.000}{1000} + \frac{(13{,}560-1000)\times9.81\times0.260}{1000} = 108 + 9.81 + 32.04 = 149.85\text{ kPa} \approx 150\text{ kPa}$$ Water in both upper legs closes to 0.1%. Glycerine would give 151.7 kPa, and air over the mercury would give 142.6 kPa. So the answer is WATER (both legs and the 150 kPa bulb) over MERCURY (the dark bottom of the U).
  6. Lower-left manometer (200 kPa and 160 kPa bulbs at the same level, 300 mm deflection). Take a fluid of density ρ above the mercury on both sides. Because the bulbs are level, the 40 kPa difference must equal (ρHg − ρ)g(0.300): $$\rho = 13{,}560 - \frac{200{,}000-160{,}000}{9.81\times0.300} = 13{,}560 - 13{,}592 \approx 0\ \text{kg/m}^3 \Rightarrow \boxed{\text{AIR}}$$ Check: 300 mm of mercury alone gives 13,560×9.81×0.300 = 39.9 kPa ≈ 40 kPa. Water above the mercury would give only (13,560 − 1000)×9.81×0.300 = 37.0 kPa. So the hatched bulbs and legs here are AIR over MERCURY (dark), even though they are shaded like the water elsewhere. This is exactly the trap the note "similar shading does not necessarily mean the same fluid" warns about.
Section (label space)EvidenceFluid
85 kPa manometer, 1530 mm columnρ = 999 kg/m³Water
110 kPa manometer, 810 mm columnρ = 1259 kg/m³Glycerine
Crown of the 810 mm manometer (unshaded)open to atmosphereAir
108 kPa manometer, 815 mm columnρ = 1001 kg/m³Water
Inverted U above the 815 mm column (unshaded)open to atmosphereAir
Leg from the 108 kPa bulb, and the 150 kPa bulb/legloop closes at 149.85 vs 150 kPaWater
Bottom of the 260 mm Udark; closes the loop aboveMercury
200 kPa and 160 kPa bulbs and legsρ ≈ 0 from the 40 kPa balanceAir
Bottom of the 300 mm U13,560×9.81×0.3 = 39.9 kPaMercury
Assumption: the 1530, 810 and 815 mm columns are each measured from the bulb level to the free surface in the open leg, which is at p0 = 100 kPa. The 1000 mm dimension is taken between the 108 kPa and 150 kPa bulb levels. With these readings, every section closes numerically against the reference SGs.