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8.2 Unsteady-State Mass Balances

Key Takeaways

  • Unsteady-state mass balances retain the time-dependent accumulation term, dm/dt = sum(m_in) - sum(m_out), which must be integrated over a defined time interval.

  • When modeling liquid volume changes in a vessel, the rate of change of liquid height is governed by the volumetric balance A dh/dt = F_in - F_out, assuming constant fluid density.

  • Gravity-draining or leaking tanks follow Torricelli's law, where the outlet flow rate varies with the square root of the liquid height (F_out = C_d * A_o * sqrt(2g*h)), leading to a non-linear first-order differential equation.

  • In well-mixed dilution vessels (dynamic concentration modeling), both mass and species balances must be solved simultaneously using separation of variables or integrating factors.

  • For variable-volume systems (e.g., where inlet and outlet volumetric flow rates differ), the volume term inside the differential d(VC)/dt must be expanded as V dC/dt + C dV/dt.

Last updated: July 2026

The Nature of Transient Systems

In contrast to steady-state operations, unsteady-state (or transient) systems exhibit process variables that change with time. Transient conditions are typical in batch processes, during startup and shutdown sequences, and when responding to process upsets or setpoint changes. For transient systems, the accumulation term in the general material balance equation cannot be neglected, meaning the rate of accumulation of mass within the system boundary is equal to the net rate of mass entering and leaving the system plus generation minus consumption. For a non-reactive system, this transient mass balance is written as:

dmsysdt=∑m˙in−∑m˙out\frac{dm_{sys}}{dt} = \sum \dot{m}_{in} - \sum \dot{m}_{out}

where msysm_{sys} is the total mass within the system boundary at any time tt, and m˙in\dot{m}_{in} and m˙out\dot{m}_{out} are the mass flow rates entering and leaving the system, respectively. If the system contains multiple components, a transient balance must be written for each individual species. For a component ii with mass fraction wiw_i, the transient species balance is:

d(msyswi)dt=∑m˙inwi,in−∑m˙outwi,out\frac{d(m_{sys} w_i)}{dt} = \sum \dot{m}_{in} w_{i,in} - \sum \dot{m}_{out} w_{i,out}

To solve unsteady-state material balances, you must formulate the differential equation, separate the variables, and integrate over the specified time interval using the initial conditions of the system.

Liquid Level in Draining and Leaking Tanks

A classic FE Chemical exam problem involves modeling the liquid level in a storage vessel as it fills, drains, or leaks. Consider a tank with a constant cross-sectional area AA containing a liquid of constant density ρ\rho. The volume of liquid in the tank is V(t)=Ah(t)V(t) = A h(t), where h(t)h(t) is the liquid height. The mass of liquid is msys=ρAhm_{sys} = \rho A h.

Substituting this into the transient mass balance gives:

d(ρAh)dt=ρFin−ρFout\frac{d(\rho A h)}{dt} = \rho F_{in} - \rho F_{out}

where FinF_{in} and FoutF_{out} are the volumetric flow rates entering and leaving the tank, respectively. Since density ρ\rho and area AA are constant, we can simplify this to a volumetric balance:

Adhdt=Fin−FoutA \frac{dh}{dt} = F_{in} - F_{out}

If the tank is draining under the force of gravity through a leak or an orifice at the bottom, the outlet velocity is described by Torricelli's Law, which is derived from the Bernoulli equation. The outlet volumetric flow rate FoutF_{out} is:

Fout=CdAo2ghF_{out} = C_d A_o \sqrt{2gh}

where CdC_d is the discharge coefficient (typically between 0.60 and 0.98), AoA_o is the cross-sectional area of the orifice, and gg is the acceleration due to gravity. The governing differential equation for the liquid height becomes:

Adhdt=Fin−CdAo2ghA \frac{dh}{dt} = F_{in} - C_d A_o \sqrt{2gh}

This is a non-linear first-order ordinary differential equation. If there is no inlet flow (Fin=0F_{in} = 0), the equation is separable and can be integrated directly to find the time required to drain the tank from an initial height h0h_0 to a final height hfh_f:

∫h0hfdhh=−CdAo2gA∫0tdt\int_{h_0}^{h_f} \frac{dh}{\sqrt{h}} = -\frac{C_d A_o \sqrt{2g}}{A} \int_0^t dt 2(hf−h0)=−CdAo2gAt2(\sqrt{h_f} - \sqrt{h_0}) = -\frac{C_d A_o \sqrt{2g}}{A} t

Rearranging this expression allows you to calculate the elapsed time tt:

t=2ACdAo2g(h0−hf)t = \frac{2A}{C_d A_o \sqrt{2g}} (\sqrt{h_0} - \sqrt{h_f})

Concentration Dynamics in Well-Mixed Dilution Vessels

Another high-yield transient problem is the dilution or mixing tank. Consider a well-mixed vessel of constant volume VV containing a solute of concentration C(t)C(t). A liquid stream enters the vessel at a volumetric flow rate FF and solute concentration CinC_{in}, and an outlet stream leaves at the same flow rate FF to maintain constant volume (Fin=Fout=FF_{in} = F_{out} = F).

Because the vessel is well-mixed, the solute concentration in the outlet stream is equal to the concentration inside the tank (Cout=CC_{out} = C). The species balance for the solute is:

d(VC)dt=FCin−FC\frac{d(V C)}{dt} = F C_{in} - F C

Since VV is constant, this simplifies to:

VdCdt=F(Cin−C)  ⟹  dCdt+FVC=FVCinV \frac{dC}{dt} = F (C_{in} - C) \implies \frac{dC}{dt} + \frac{F}{V} C = \frac{F}{V} C_{in}

This is a first-order linear ordinary differential equation. Defining the residence time or space time as τ=V/F\tau = V/F, we can write:

dCdt+1τC=1τCin\frac{dC}{dt} + \frac{1}{\tau} C = \frac{1}{\tau} C_{in}

Integrating this equation from an initial concentration C(0)=C0C(0) = C_0 yields the concentration as a function of time:

C(t)=Cin+(C0−Cin)e−t/τC(t) = C_{in} + (C_0 - C_{in}) e^{-t/\tau}

This equation shows that as t→∞t \to \infty, the concentration exponentially approaches the inlet concentration CinC_{in}. The quantity e−t/τe^{-t/\tau} represents the fraction of the initial fluid remaining in the vessel at time tt.

For systems where the inlet and outlet flow rates are different (Fin≠FoutF_{in} \neq F_{out}), the volume is also a function of time: V(t)=V0+(Fin−Fout)tV(t) = V_0 + (F_{in} - F_{out})t. In this case, the product rule must be used to expand the accumulation term:

d(VC)dt=VdCdt+CdVdt=FinCin−FoutC\frac{d(V C)}{dt} = V \frac{dC}{dt} + C \frac{dV}{dt} = F_{in} C_{in} - F_{out} C

Substitute dVdt=Fin−Fout\frac{dV}{dt} = F_{in} - F_{out} into the equation and rearrange to isolate dCdt\frac{dC}{dt}:

VdCdt+C(Fin−Fout)=FinCin−FoutC  ⟹  V(t)dCdt=Fin(Cin−C)V \frac{dC}{dt} + C(F_{in} - F_{out}) = F_{in} C_{in} - F_{out} C \implies V(t) \frac{dC}{dt} = F_{in}(C_{in} - C)

This must be solved by separating variables and integrating using the time-dependent volume function V(t)V(t).

The table below compares the concentration dynamics equations for constant-volume and variable-volume well-mixed vessels:

ParameterConstant-Volume VesselVariable-Volume Vessel
Volume V(t)V(t)Constant (V=V0V = V_0)Time-dependent (V(t)=V0+(Fin−Fout)tV(t) = V_0 + (F_{in} - F_{out})t)
Species BalanceVdCdt=F(Cin−C)V \frac{dC}{dt} = F(C_{in} - C)VdCdt=Fin(Cin−C)V \frac{dC}{dt} = F_{in}(C_{in} - C)
Solute ConcentrationC(t)=Cin+(C0−Cin)e−t/τC(t) = C_{in} + (C_0 - C_{in}) e^{-t/\tau}Solved by separating variables with V(t)V(t)

Worked Example: Emptying a Leaking Storage Tank

A cylindrical storage tank with a diameter of 2.0 m2.0 \text{ m} (cross-sectional area A=3.1416 m2A = 3.1416 \text{ m}^2) is initially filled with water to a height of 4.0 m4.0 \text{ m}. A drain hole with a diameter of 0.05 m0.05 \text{ m} (Ao=0.001963 m2A_o = 0.001963 \text{ m}^2) at the bottom of the tank is opened. Assuming the discharge coefficient is Cd=0.60C_d = 0.60 and the acceleration due to gravity is g=9.81 m/s2g = 9.81 \text{ m/s}^2, calculate the time (in minutes) required for the water level to drop from 4.0 m4.0 \text{ m} to 1.0 m1.0 \text{ m}.

Solution:

We start with the derived integration formula for a draining tank with no inlet flow:

t=2ACdAo2g(h0−hf)t = \frac{2A}{C_d A_o \sqrt{2g}} (\sqrt{h_0} - \sqrt{h_f})

First, calculate the constant coefficient:

Coefficient=2(3.1416)(0.60)(0.001963)2(9.81)=6.2832(0.001178)(4.4294)=6.28320.005218=1,204.1 s/m1/2\text{Coefficient} = \frac{2(3.1416)}{(0.60)(0.001963) \sqrt{2(9.81)}} = \frac{6.2832}{(0.001178) (4.4294)} = \frac{6.2832}{0.005218} = 1,204.1 \text{ s/m}^{1/2}

Next, substitute the initial and final heights:

h0−hf=4.0−1.0=2.0−1.0=1.0 m1/2\sqrt{h_0} - \sqrt{h_f} = \sqrt{4.0} - \sqrt{1.0} = 2.0 - 1.0 = 1.0 \text{ m}^{1/2}

Multiply the coefficient by the height difference:

t=1,204.1 s/m1/2×1.0 m1/2=1,204.1 secondst = 1,204.1 \text{ s/m}^{1/2} \times 1.0 \text{ m}^{1/2} = 1,204.1 \text{ seconds}

Convert the time into minutes:

t=1,204.1 seconds60 seconds/minute=20.1 minutest = \frac{1,204.1 \text{ seconds}}{60 \text{ seconds/minute}} = 20.1 \text{ minutes}

Therefore, it will take approximately 20.120.1 minutes for the liquid level in the tank to drop from 4.0 m4.0 \text{ m} to 1.0 m1.0 \text{ m}.

Test Your Knowledge

A flat-bottomed cylindrical tank has a diameter of 4.0 m (area A = 12.57 m^2) and is initially filled with water to a height of 9.0 m. Water leaks from a circular hole at the bottom of the tank. If it takes 30.0 minutes for the liquid level to drop to 4.0 m, what is the value of the drainage constant K = (C_d * A_o * sqrt(2g)) / A in units of s^-1/2?

A

0.00056 s^-1/2

B

0.00083 s^-1/2

C

0.00222 s^-1/2

D

0.00111 s^-1/2

Test Your Knowledge

A well-mixed storage vessel with a constant liquid volume of 10.0 m^3 initially contains pure water. At t = 0, a brine stream containing 2.0 kg/m^3 of salt enters the vessel at a volumetric flow rate of 0.50 m^3/min, and an outlet stream leaves the vessel at the same flow rate. What is the salt concentration in the vessel after 20.0 minutes?

A

1.26 kg/m^3

B

0.74 kg/m^3

C

2.00 kg/m^3

D

1.00 kg/m^3

Test Your Knowledge

In a transient system where a well-mixed tank is being filled, water enters the tank at a volumetric flow rate F_in = 5.0 L/min containing solute at C_in = 1.0 mol/L. Water is pumped out at F_out = 3.0 L/min. If the initial volume of liquid in the tank is V_0 = 10.0 L and the initial concentration is C_0 = 0.50 mol/L, what is the differential equation describing the solute concentration C(t)?

A

dC/dt = (1.0 - C) / (10 + 2t)

B

dC/dt = (5.0 - 3.0*C) / (10 + 2t)

C

dC/dt = 5.0 * (1.0 - C) / (10 + 2t)

D

dC/dt = 5.0 * (1.0 - C) / 10

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