This problem is a beautiful symphony of fluid dynamics and thermodynamics. We are tasked with analyzing an ideal gas flowing steadily through a heat-insulated chimney. To conquer this, we must weave together mass conservation, adiabatic processes, the ideal gas law, and the Steady Flow Energy Equation (SFEE).
The Inlet Dynamics
Let's start at the bottom of the chimney. We are given a steady mass flow rate α=0.8 kg/s. Since the flow is steady, this mass flow rate must be conserved throughout the chimney. At the lower end, the mass flow rate is the product of density, cross-sectional area, and velocity:
By rearranging this, we can easily find the inlet velocity v1:
v1=ρ1A1α=0.2×0.10.8=40 m/s
The Adiabatic Journey
As the gas rises, it expands. Because the chimney is perfectly heat-insulated, this expansion is strictly adiabatic. For an ideal gas undergoing an adiabatic process, the relationship between pressure and temperature is governed by:
We can set up a ratio between the upper and lower ends:
Given that the ratio of specific heats γ=2, the exponent becomes 1−22=−2. Plugging in our known temperatures (T1=300 K, T2=150 K) and the initial pressure (P1=600 Pa):
P2=600×(150300)−2=600×(2)−2=4600=150 Pa
Finding the New Density
With the new pressure and temperature in hand, we can determine the density at the top using the Ideal Gas Equation, P=MρRT. This tells us that density is directly proportional to pressure and inversely proportional to temperature:
ρ1ρ2=(P1P2)(T2T1)
Substituting our values:
ρ2=0.2×(600150)×(150300)=0.2×41×2=0.1 kg/m3
Now, armed with the top density ρ2, we return to our trusty mass conservation principle to find the exit velocity v2:
v2=ρ2A2α=0.1×0.40.8=20 m/s
The Master Equation
SFEE
Here is where the magic happens. To find the height of the chimney, we must apply the Steady Flow Energy Equation (SFEE). For an adiabatic flow with no external shaft work, the total energy per unit mass is conserved. This means the sum of specific enthalpy (h), kinetic energy, and potential energy remains constant:
h1+2v12+gz1=h2+2v22+gz2
Rearranging to solve for the height difference h=z2−z1:
For an ideal gas, the change in specific enthalpy is h2−h1=cp(T2−T1). Using the relation cp=M(γ−1)γR and the ideal gas law ρP=MRT, we can express the enthalpy change purely in terms of pressure and density:
h2−h1=γ−1γ(ρ2P2−ρ1P1)
Since γ=2, the coefficient γ−1γ simplifies beautifully to 2. Therefore:
h1−h2=2(ρ1P1−ρ2P2)
The Final Calculation
Let's substitute this back into our energy equation:
2(ρ1P1−ρ2P2)=2v22−v12+gh
Now, we carefully plug in every value we've painstakingly calculated:
2(0.2600)−2(0.1150)=2202−402+10h
2(3000)−2(1500)=2400−1600+10h
3000=−600+10h⟹10h=3600⟹h=360 m
Reviewing the options, we see that only the velocities match our derived results. The correct statement is indeed (B).