Chemical & Process Engineering / Gravity-Drained Tank Dynamics
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LABORATORY 40 · CHEMICAL & PROCESS ENGINEERING

Gravity-Drained Tank Dynamics lab report

A worked gravity-drained tank dynamics lab report with sample observation tables, regression plots, calculations, and error analysis.

WORKED EXAMPLE · BENCHMARK OBSERVATIONS

A complete example chemical engineering laboratory report.

Simulated demonstration data.

This report illustrates formal chemical and process engineering data reduction, instrument calibration tares, and unit operations parameter estimation. Replace its observations with your own experimental telemetry when preparing a chemical engineering laboratory report submission.

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1. Title and aim

Dynamic Modeling, Step Response & Hydraulic Resistance of a First-Order Gravity-Drained Tank. Model the unsteady-state liquid level dynamics of a vertical cylindrical gravity-drained tank with laminar linear discharge resistance, apply step changes in influent volumetric flow rate F_in from 2.0 to 12.0 L/min, monitor liquid level transients h(t) using an ultrasonic level transmitter, evaluate the process time constant τ_p, and determine the linear hydraulic discharge resistance R.

2. Abstract

Six controlled chemical process engineering observations were systematically evaluated across operational settings Influent Flow Rate F_in = 2.0 L/min to Influent Flow Rate F_in = 12.0 L/min for Dynamic Modeling, Step Response & Hydraulic Resistance of a First-Order Gravity-Drained Tank. Ordinary least-squares regression yielded an empirical Hydraulic Discharge Resistance R of 3.8500 cm/(L/min) (difference from theoretical reference = 0.0000%). The empirical telemetry conclusively validates the fundamental chemical engineering transport and equilibrium formulation with R² = 1.000000. The investigation demonstrates stable unit operations behavior, hydrodynamic and thermal reproducibility, and strict adherence to classical chemical engineering principles.

3. Apparatus and fixed settings

4. Theory and graph choice

Liquid level control in surge tanks, flash drums, reflux accumulators, and chemical storage reservoirs is a ubiquitous unit operation in process engineering. Maintaining stable tank levels prevents pump cavitation from run-dry conditions while avoiding hazardous overfills. A vertical, uniform cross-sectional surge tank (cross-sectional area A = 0.050 m^2) drained by gravity through a laminar restriction tube is the canonical physical realization of a first-order dynamic process. Applying the unsteady-state mass conservation principle to incompressible liquid (constant density ρ) gives: ρ · A · (dh/dt) = ρ · F_in(t) - ρ · F_out(t), which simplifies to: A · (dh/dt) = F_in(t) - F_out(t). When discharge occurs through a capillary tube or packed porous plug under laminar flow (Re < 2000), the Hagen–Poiseuille equation dictates that effluent flow rate is directly proportional to hydrostatic pressure head: F_out = h / R, where R is the linear hydraulic discharge resistance (with dimensions of head per volumetric flow rate, cm/(L/min)). Substituting this linear outflow relation yields the first-order ordinary differential equation: A · R · (dh/dt) + h(t) = R · F_in(t). Defining the process time constant τ_p = A · R, this standard first-order transfer function in Laplace deviation variables is: G(s) = H'(s) / F_in'(s) = K_p / (τ_p · s + 1), where steady-state process gain K_p equals hydraulic resistance R. In response to a step increase in inflow ΔF_in, the level response is an exponential relaxation: h'(t) = R · ΔF_in · [1 - exp(-t / τ_p)]. At long times (t -> inf), the new steady-state liquid level is h_ss = R · F_in. In this laboratory investigation, an instrumented transparent acrylic surge tank equipped with an ultrasonic level transmitter and variable-speed magnetic gear pump is operated across inflow setpoints from 2.0 to 12.0 L/min to evaluate transient step responses, calculate τ_p, and determine the linear hydraulic resistance R = 3.8500 cm/(L/min).

h_ss = R · F_in = 3.8500 · F_in

The governing phenomenological transport or equilibrium relationship was linearized into the coordinate form y = mx + b. Here, the independent coordinate x represents Influent volumetric flow rate F_in (L/min), and the dependent coordinate y represents Steady-state liquid level h_ss (cm). The gradient m directly determines Hydraulic Discharge Resistance R, while the intercept b accounts for baseline tare values or reference potentials. Linear transformation enables robust parameter estimation via ordinary least squares without non-linear numerical divergence. Plotting transformed observation pairs displays process discharge coefficients, heat transfer multipliers, mass transfer rates, or kinetic rate constants directly as linear slopes.

5. Method

  1. Calibrate ultrasonic level transmitter against manual vernier sight gauge across 0 to 80 cm; align transmitter 4 mA signal with bottom datum.
  2. Prime the magnetic gear pump; verify delivery flow rate at 6.0 L/min using gravimetric timed-collection catch-and-weigh method.
  3. Set pump controller to deliver F_in = 2.0 L/min into empty tank; log level trajectory h(t) at 1 Hz until steady state is reached.
  4. Extract time constant τ_p from the time required to achieve 63.2% of the total level step rise; record final steady-state level h_ss.
  5. Apply sequential step changes to influent flow rate F_in = 4.0, 6.0, 8.0, 10.0, and 12.0 L/min, recording dynamic curves and steady levels.
  6. Plot steady-state level h_ss versus influent flow rate F_in; perform linear regression through origin to evaluate hydraulic resistance R.

6. Observations and calculation table

All chemical process observations use strictly controlled 64-bit IEEE 754 precision buffers. Residuals are computed relative to the ordinary least-squares regression line.

Table 1. Six simulated observations; x and y represent transformed process metrics.
No.Influent Volumetric Flow Rate F_in (L/min)Steady-State Liquid Level h_ss (cm)Influent volumetric flow rate F_in (L/min)Steady-state liquid level h_ss (cm)Fitted yResidual
12.07.72.00007.70007.70000.0000
24.015.44.000015.400015.40000.0000
36.023.16.000023.100023.10000.0000
48.030.88.000030.800030.80000.0000
510.038.510.000038.500038.50000.0000
612.046.212.000046.200046.20000.0000

Download the sample observations (CSV) ↓

7. Worked calculation for one observation

For input Influent Flow Rate F_in = 2.0 L/min: Measured Steady-State Liquid Level h_ss = 7.7000 cm. Transformed process coordinates: independent x = 2.0000, dependent y = 7.7000.

8. Graph, gradient and final calculation

1.930.8014.443.9026.957.0039.4610.1051.9713.20Influent volumetric flow rate F_in (L/min)Steady-state liquid level h_ss (cm)

Circular markers represent empirical process observations. The solid line represents the ordinary least-squares linear fit.

x̄ = 7.0000; ȳ = 26.9500
Σ(x − x̄)² = 70.0000
Σ(x − x̄)(y − ȳ) = 269.5000
m = Σ(x − x̄)(y − ȳ) / Σ(x − x̄)² = 3.85000000
b = ȳ − mx̄ = 0.00000000
y = 3.8500 · x + 0.0000 ⟹ Target Hydraulic Discharge Resistance R = 3.8500 cm/(L/min) (theoretical = 3.8500)

9. Uncertainty and comparison

Percentage difference = |estimate − theoretical value| / |theoretical value| × 100 = 0.0000%.

For n = 6 observations, Σresidual² = 0.0000; s² = Σresidual²/(n − 2). Gradient standard error = √[s²/Σ(x − x̄)²] = 0.0000. Intercept standard error = √[s²(1/n + x̄²/Σ(x − x̄)²)] = 0.0000.

Propagating the fit parameters yields a fit standard error of 1.000e-05 cm/(L/min), with an ideal coefficient of determination R² = 1.000000.

In chemical and process engineering experimentation, unit operations verification, and pilot-scale process modeling, empirical uncertainties arise from fluid property variations, slight thermal gradients across heat transfer boundaries, transducer electronic drift (64-bit IEEE 754 precision digital acquisition), and minor flow turbulence eddies. The ordinary least-squares regression across n = 6 standardized test intervals yields unbiased minimum-variance estimators for both slope and intercept. Because the underlying transport phenomena—including Navier-Stokes momentum balances, Fourier conduction, Fickian mass diffusion, and reaction kinetics—adhere strictly to macroscopic conservation laws, residual dispersions remain tightly bounded, yielding an ideal coefficient of determination R² ≥ 0.999999 and confirming the theoretical formulation. Systematic errors (such as sensor zero offsets, thermocouple reference junction drifts, and flowmeter discharge friction) are eliminated using certified calibration standards and differential tare subtraction. Uncertainties in derived transport coefficients, dimensionless numbers, and kinetic constants are evaluated via multivariate error propagation.

10. Result and discussion

Hydraulic Discharge Resistance R = 3.8500 cm/(L/min)
Theoretical reference value: 3.8500 cm/(L/min)

The empirical laboratory observations provide rigorous quantitative verification of Dynamic Modeling, Step Response & Hydraulic Resistance of a First-Order Gravity-Drained Tank. In chemical engineering transport phenomena, fluid mechanics, heat transfer, separation processes, and reaction engineering, physical systems are governed by macroscopic mass, momentum, and energy conservation equations. Across all six observation trials, the empirical slope m = 3.8500 confirms the theoretical model with near-zero residual variance. Furthermore, comparison with established chemical engineering literature benchmarks (McCabe, Smith, Harriott; Bird, Stewart, Lightfoot; Fogler; and Levenspiel) underscores vital industrial scale-up principles including continuous steady-state stability, minimal friction losses, optimal reaction conversion, and thermal efficiency. Residual analysis confirms homoscedastic dispersion without systematic non-linear curvature, validating the underlying model assumptions.

11. Precautions and limitations

The transport and thermodynamic models apply within the specified calibrated operating window (2.0 to 12.0 L/min). Evaluated using a precision transparent acrylic column (ID = 25.23 cm, cross-sectional area A = 500.0 cm^2 = 0.0500 m^2) with laminar capillary discharge resistor. Ultrasonic transit-time level transmitter (±0.05 cm) and magnetic-drive gear pump calibrated at 20.0 °C.

12. Conclusion

This laboratory investigation quantitatively verified the mathematical formulation and physical behavior of Dynamic Modeling, Step Response & Hydraulic Resistance of a First-Order Gravity-Drained Tank. Through rigorous tracking across six observation points, we confirmed an empirical Hydraulic Discharge Resistance R of 3.8500 cm/(L/min) matching the theoretical reference 3.8500 cm/(L/min) within 0.0000% error. The investigation demonstrates why this chemical engineering method serves as an indispensable cornerstone in industrial process design, unit operations scaling, and plant optimization.

In-Depth Technical Supplement & Historical Unit Operations Derivation

1. Objective & Practical Significance

This laboratory investigation evaluates the dynamic modeling, step response characteristics, and hydraulic discharge resistance of a vertical cylindrical gravity-drained liquid surge tank ($A = 500.0\text{ cm}^2 = 0.0500\text{ m}^2$) fitted with a laminar capillary drain manifold. Across influent flow rates $F_{\text{in}}$ from $2.0$ to $12.0\text{ L/min}$, we track real-time level trajectories $h(t)$ using an ultrasonic level transmitter, evaluate the first-order time constant $\tau_p$, verify linear steady-state level scaling $h_{\text{ss}} = R \cdot F_{\text{in}}$, and determine the hydraulic resistance $R = 3.8500\text{ cm/(L/min)}$.

2. Governing Transport Equations & Phenomenological Relations

The first-order dynamic level ODE is: $\tau_p \frac{dh}{dt} + h(t) = R \, F_{\text{in}}(t)$, where time constant $\tau_p = A \cdot R$. The steady-state level model is:

\[ h_{\text{ss}} = R \cdot F_{\text{in}} = 3.8500 \cdot F_{\text{in}} \]

where $R = 3.8500\text{ cm/(L/min)} = 231.0\text{ s/m}^2$. The theoretical time constant for $A = 0.0500\text{ m}^2$ is $\tau_p = A \cdot R = 0.0500 \times 231.0 = 11.55\text{ s}$ ($115.5\text{ s}$ for volumetric units $500\text{ cm}^2 \times 3.85\text{ cm/(L/min)} \times (1\text{ min}/1000\text{ cm}^3) = 115.5\text{ s}$).

3. Experimental Apparatus & Instrumentation Specification

The system comprises a transparent acrylic column ($25.23\text{ cm}$ ID, $A = 500.0\text{ cm}^2$, height $100\text{ cm}$), an ultrasonic transit-time level sensor (Endress+Hauser Prosonic, $\pm 0.05\text{ cm}$), a laminar multi-capillary discharge manifold, a variable-speed magnetic-drive gear pump ($0$ to $15.0\text{ L/min}$, $\pm 0.02\text{ L/min}$), an in-line turbine flowmeter, and a $100\text{ L}$ sump reservoir at $20.0 \pm 0.2^\circ\text{C}$.

4. Standard Operating Procedure & Measurement Protocols

The ultrasonic sensor was calibrated against a manual sight glass. The pump was primed, and flow delivery was verified gravimetrically. The tank was operated from empty at an initial flow setpoint $F_{\text{in}} = 2.0\text{ L/min}$. Dynamic liquid level $h(t)$ was logged at $1\text{ Hz}$ until steady state ($\Delta h < 0.05\text{ cm}$ over 60 s). The $63.2\%$ rise time was extracted to evaluate $\tau_p$. The procedure was repeated for step inflows of $4.0, 6.0, 8.0, 10.0,$ and $12.0\text{ L/min}$.

5. Safety Analysis, Hazard Mitigation & Personal Protection

Water overflow hazards were prevented by an emergency high-level float switch interlocked to the pump at $h = 85.0\text{ cm}$. Overflow drains were piped directly to the sump. Electrical pumps and transmitters were installed on elevated drip-proof stanchions. Standard slip-resistant footwear and safety glasses were worn.

6. Raw Experimental Observations & Systematic Data Records

Simulated demonstration data. The following steady-state and dynamic observations were recorded at $T = 20.0^\circ\text{C}$ ($A = 500.0\text{ cm}^2$):

RunInfluent Flow $F_{\text{in}}$ (L/min)Steady Level $h_{\text{ss}}$ (cm)$63.2\%$ Rise Time $\tau_p$ (s)Effluent Outflow (L/min)Apparent Resistance (cm/(L/min))Process Gain $K_p$
12.07.70115.52.003.8503.850
24.015.40115.54.003.8503.850
36.023.10115.56.003.8503.850
48.030.80115.58.003.8503.850
510.038.50115.510.003.8503.850
612.046.20115.512.003.8503.850

7. Quantitative Mathematical Analysis & Regression Models

Linear regression of steady-state level $h_{\text{ss}}$ versus influent volumetric flow rate $F_{\text{in}}$ yields:

\[ h_{\text{ss}} = 3.85000 \cdot F_{\text{in}} + 0.00000 \]

with coefficient of determination $R^2 = 1.000000$ and zero intercept. The experimental slope $R = 3.85000\text{ cm/(L/min)}$ matches calibration target ($3.8500$) with $0.00\%$ deviation. Evaluating the dynamic time constant:

\[ \tau_p = A \cdot R = (500.0\text{ cm}^2) \times (3.8500\text{ cm/(L/min)}) \times \left( \frac{1\text{ min}}{1000\text{ cm}^3} \right) \times 60\text{ s/min} = 115.50\text{ s} \]

The experimentally measured $63.2\%$ step rise time ($115.5\text{ s}$) confirms the analytical dynamic prediction.

8. Rigorous Error Analysis & Uncertainty Propagation

Ultrasonic level uncertainty is $\pm 0.05\text{ cm}$, gear pump flow accuracy is $\pm 0.02\text{ L/min}$, and tank cross-sectional area tolerance is $\pm 0.2\%$. Propagating into hydraulic resistance yields an uncertainty in $R$ of $\pm 0.022\text{ cm/(L/min)}$ ($0.57\%$), reporting $R = 3.850 \pm 0.022\text{ cm/(L/min)}$ and $\tau_p = 115.5 \pm 1.2\text{ s}$.

9. Engineering Discussion & Phenomenological Interpretation

The perfect linearity of $h_{\text{ss}}$ versus $F_{\text{in}}$ proves that the multi-capillary discharge assembly operated strictly in the laminar Hagen–Poiseuille regime (maximum capillary Reynolds number $Re = 450 < 2000$). The constant time constant across all flow setpoints ($ au_p = 115.5\text{ s}$) demonstrates linear time-invariant (LTI) process dynamics, confirming that transfer function analysis accurately describes the physical surge system.

10. Industrial Scale-Up & Unit Operation Applications

First-order surge drum dynamics govern level control loops in petrochemical refining (crude preheat trains), reflux accumulator sizing in distillation columns, feedwater surge vessels in steam boilers, and equalizing basins in wastewater treatment facilities.

11. Self-Assessment Conceptual Questions & Model Answers

Q1: How would turbulent discharge through a sharp orifice alter the transfer function?
A1: Torricelli orifice discharge is non-linear ($F_{\text{out}} = C_d A_o \sqrt{2gh}$); linearizing around a steady-state level $h_0$ produces an operating-point dependent resistance $R = 2 h_0 / F_{\text{out},0}$ and variable time constant $\tau_p(h_0) = 2 A h_0 / F_{\text{out},0}$.

Q2: Why does an ultrasonic level sensor require temperature compensation?
A2: The speed of sound in air varies with absolute temperature ($c = \sqrt{\gamma R_{\text{air}} T} \approx 331.3 + 0.606 T$); a $5^\circ\text{C}$ air temperature change alters acoustic transit time by $\sim 0.9\%$, introducing calibration offset if uncompensated.

12. Concluding Summary & Verified Engineering Metric

Dynamic step response testing successfully verified first-order surge tank dynamics. The experimental hydraulic discharge resistance $R = 3.8500\text{ cm/(L/min)}$ and process time constant $\tau_p = 115.50\text{ s}$ confirmed lumped-parameter mass conservation theory.