Chemical & Process Engineering / Gas Absorption in Packed Column
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LABORATORY 18 · CHEMICAL & PROCESS ENGINEERING

Gas Absorption in Packed Column lab report

A worked gas absorption in packed column 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

Packed Column Gas Absorption & Volumetric Mass Transfer Coefficient K_G a. Operate a continuous counter-current packed absorption column absorbing carbon dioxide from air into water, measure inlet and outlet gas concentrations, and evaluate the volumetric overall mass transfer coefficient K_G a and Height of a Transfer Unit (HTU).

2. Abstract

Six controlled chemical process engineering observations were systematically evaluated across operational settings Liquid Rate L = 10.0 L/(min·m^2) to Liquid Rate L = 60.0 L/(min·m^2) for Packed Column Gas Absorption & Volumetric Mass Transfer Coefficient K_G a. Ordinary least-squares regression yielded an empirical Absorption Mass Transfer Slope S of 0.0820 kmol/(m^3·h·bar)/(L/(min·m^2))^0.7 (difference from theoretical reference = 0.0019%). 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

Gas absorption (scrubbing) is a fundamental mass transfer separation operation in chemical plants, environmental emissions control, and synthesis gas purification, responsible for removing acid gases (CO_2, H_2S, SO_2) from gas streams by dissolving them into a liquid solvent. In a counter-current packed tower, gas enters at the bottom and ascends through packing, while liquid solvent is distributed over the top and trickles downward over packing elements (such as Raschig rings or structured gauze). Interfacial mass transfer is described by the two-film theory of Whitman (1923), which posits stagnant gas and liquid films on either side of the phase interface. The volumetric mass transfer rate is N_A · a = K_G a · (P_A - P_A*), where K_G a is the overall volumetric gas-phase mass transfer coefficient, 'a' is the effective gas-liquid interfacial area per unit packed volume, P_A is solute partial pressure in the bulk gas, and P_A* is equilibrium partial pressure over the liquid. For physical absorption of sparingly soluble gases like carbon dioxide in water, liquid film resistance dominates overall transport: 1 / K_G a = 1 / (k_G a) + H / (k_L a), where H is Henry's law constant. According to Onda's classic packed bed mass transfer correlations, liquid-side mass transfer coefficient k_L and wetted specific area 'a' scale with liquid mass velocity as L^0.7. In this laboratory investigation, an instrumented 1.5-meter packed tower absorbing CO_2 into water is operated across liquid irrigation rates from 10.0 to 60.0 L/(min·m^2) to measure K_G a, verify L^0.7 scaling, and determine the Height of a Transfer Unit (HTU).

K_G a = S · L^0.7 = 0.0820 · L^0.7

The governing phenomenological transport or equilibrium relationship was linearized into the coordinate form y = mx + b. Here, the independent coordinate x represents Liquid irrigation factor L^0.7 ((L/(min·m^2))^0.7), and the dependent coordinate y represents Volumetric mass transfer coefficient K_G a (kmol/(m^3·h·bar)). The gradient m directly determines Absorption Mass Transfer Slope S, 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. Start air blower and open CO_2 cylinder; adjust rotameters to establish 5.00 mol% CO_2 in air at total gas flux G = 25.0 kg/(h·m^2); calibrate NDIR analyzer zero and span.
  2. Start water pump at moderate flow to pre-wet the Raschig ring packing completely for 10 minutes to eliminate dry spots.
  3. Adjust water flow to establish liquid irrigation rate L = 10.0 L/(min·m^2); verify gas pressure drop across bed is stable.
  4. Allow 15 minutes to establish mass transfer steady state; sample column inlet gas y_in and top exit gas y_out via NDIR analyzer.
  5. Step liquid irrigation rate through 20.0, 30.0, 40.0, 50.0, and 60.0 L/(min·m^2), logging inlet and exit CO_2 concentrations at each plateau.
  6. Compute log mean concentration driving force, calculate K_G a for each run, plot K_G a versus L^0.7, and evaluate the scaling slope S.

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.Liquid Solvent Irrigation Rate L (L/(min·m^2))Mass Transfer Factor (K_G a) (kmol/(m^3·h·bar))Liquid irrigation factor L^0.7 ((L/(min·m^2))^0.7)Volumetric mass transfer coefficient K_G a (kmol/(m^3·h·bar))Fitted yResidual
110.00.4115.01190.41100.41100.0000
220.00.66768.14180.66760.6676-0.0000
330.00.886710.81400.88670.8867-0.0000
440.01.084613.22641.08461.08460.0000
550.01.267915.46251.26791.2679-0.0000
660.01.440517.56731.44051.44050.0000

Download the sample observations (CSV) ↓

7. Worked calculation for one observation

For input Liquid Rate L = 10.0 L/(min·m^2): Measured Mass Transfer Factor (K_G a) = 0.4110 kmol/(m^3·h·bar). Transformed process coordinates: independent x = 5.0119, dependent y = 0.4110.

8. Graph, gradient and final calculation

0.263.510.597.400.9311.291.2615.181.5919.07Liquid irrigation factor L^0.7 ((L/(min·m^2))^0.7)Volumetric mass transfer coefficient K_G a (kmol/(m^3·h·bar))

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

x̄ = 11.7040; ȳ = 0.9597
Σ(x − x̄)² = 109.0879
Σ(x − x̄)(y − ȳ) = 8.9450
m = Σ(x − x̄)(y − ȳ) / Σ(x − x̄)² = 0.08199844
b = ȳ − mx̄ = 8.310e-06
y = 0.0820 · x + 8.310e-06 ⟹ Target Absorption Mass Transfer Slope S = 0.0820 kmol/(m^3·h·bar)/(L/(min·m^2))^0.7 (theoretical = 0.0820)

9. Uncertainty and comparison

Percentage difference = |estimate − theoretical value| / |theoretical value| × 100 = 0.0019%.

For n = 6 observations, Σresidual² = 4.999e-09; s² = Σresidual²/(n − 2). Gradient standard error = √[s²/Σ(x − x̄)²] = 3.385e-06. Intercept standard error = √[s²(1/n + x̄²/Σ(x − x̄)²)] = 4.216e-05.

Propagating the fit parameters yields a fit standard error of 3.385e-06 kmol/(m^3·h·bar)/(L/(min·m^2))^0.7, 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

Absorption Mass Transfer Slope S = 0.0820 kmol/(m^3·h·bar)/(L/(min·m^2))^0.7
Theoretical reference value: 0.0820 kmol/(m^3·h·bar)/(L/(min·m^2))^0.7

The empirical laboratory observations provide rigorous quantitative verification of Packed Column Gas Absorption & Volumetric Mass Transfer Coefficient K_G a. 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 = 0.0820 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 (10.0 to 60.0 L/(min·m^2)). Evaluated using a 100 mm ID acrylic column packed to 1.50 m with 10 mm ceramic Raschig rings (specific area a_p = 440 m^2/m^3). Gas feed contains 5.0 mol% CO_2 in air at constant flow G = 25.0 kg/(h·m^2). Linear regression models K_G a versus L^0.7.

12. Conclusion

This laboratory investigation quantitatively verified the mathematical formulation and physical behavior of Packed Column Gas Absorption & Volumetric Mass Transfer Coefficient K_G a. Through rigorous tracking across six observation points, we confirmed an empirical Absorption Mass Transfer Slope S of 0.0820 kmol/(m^3·h·bar)/(L/(min·m^2))^0.7 matching the theoretical reference 0.0820 kmol/(m^3·h·bar)/(L/(min·m^2))^0.7 within 0.0019% 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 determines the volumetric overall mass transfer coefficient $K_G a$ and Height of an Overall Transfer Unit ($HOG$) for the absorption of carbon dioxide into water in a counter-current packed column ($D = 100\text{ mm}$, packed height $Z = 1.50\text{ m}$, $10\text{ mm}$ ceramic Raschig rings). Across liquid irrigation rates $L$ from $10.0$ to $60.0\text{ L/(min}\cdot\text{m}^2)$ at constant gas flux ($G = 25.0\text{ kg/(h}\cdot\text{m}^2)$, $5.0\text{ mol}\%$ inlet $\text{CO}_2$), we evaluate $K_G a$, verify the $L^{0.7}$ Onda scaling model, and determine the absorption slope $S = 0.0820\text{ kmol/(m}^3\cdot\text{h}\cdot\text{bar)/(L/(min}\cdot\text{m}^2))^{0.7}$.

2. Governing Transport Equations & Phenomenological Relations

Total $\text{CO}_2$ absorbed is $\dot{n}_A = \frac{G A_{col}}{M_{air}} (y_{in} - y_{out}) = K_G a V_{bed} \Delta P_{lm}$. The volumetric mass transfer coefficient follows the Onda power-law model:

\[ K_G a = S \cdot L^{0.7} \]

where $S = 0.0820$ represents the experimental mass transfer coefficient slope. The height of a transfer unit is computed via $HOG = \frac{G}{K_G a P_{atm}}$.

3. Experimental Apparatus & Instrumentation Specification

The column consists of a transparent acrylic tube ($D = 100.0\text{ mm}$, cross-sectional area $A_{col} = 7.854 \times 10^{-3}\text{ m}^2$) packed to $Z = 1.50\text{ m}$ with $10\text{ mm}$ ceramic Raschig rings (specific area $a_p = 440\text{ m}^2/\text{m}^3$, voidage $\varepsilon = 0.72$, packed volume $V_{bed} = 0.01178\text{ m}^3$). An NDIR optical sensor logs inlet and outlet gas $\text{CO}_2$ concentrations ($0\text{--}10.0\%$, accuracy $\pm 0.01\%$). Liquid flow is metered by a calibrated variable-area rotameter.

4. Standard Operating Procedure & Measurement Protocols

Air and $\text{CO}_2$ flows were blended to establish $y_{in} = 5.00\text{ mol}\%$ at total gas rate $G = 25.0\text{ kg/(h}\cdot\text{m}^2)$. Water was turned on at $L = 10.0\text{ L/(min}\cdot\text{m}^2)$ ($T = 20.0^\circ\text{C}$). The system was operated for 15 minutes to reach steady mass transfer equilibrium. Inlet and exit gas concentrations ($y_{in}, y_{out}$) and bed pressure drop were recorded. Liquid flow was incremented through $20.0, 30.0, 40.0, 50.0,$ and $60.0\text{ L/(min}\cdot\text{m}^2)$.

5. Safety Analysis, Hazard Mitigation & Personal Protection

Carbon dioxide is a colorless, odorless asphyxiant gas. The absorption column exhaust was vented directly into the laboratory exhaust system. Ambient $\text{CO}_2$ room monitors were active with audible alarms set at $5,000\text{ ppm}$. Safety glasses and lab coats were worn.

6. Raw Experimental Observations & Systematic Data Records

Simulated demonstration data. The following measurements were recorded at constant gas feed $G = 25.0\text{ kg/(h}\cdot\text{m}^2)$, $y_{in} = 5.00\text{ mol}\%$, and water temperature $T = 20.0^\circ\text{C}$:

RunLiquid Rate $L$ (L/(min·m$^2$))$L^{0.7}$Exit Gas $y_{out}$ (mol%)$\text{CO}_2$ Removed (%)$K_G a$ (kmol/(m$^3$·h·bar))$HOG$ (m)
110.05.0124.3213.60.4112.08
220.08.1403.9521.00.6671.28
330.010.8253.6826.40.8880.96
440.013.2383.4630.81.0860.79
550.015.4603.2834.41.2680.67
660.017.5343.1237.61.4380.59

7. Quantitative Mathematical Analysis & Regression Models

Linear regression of volumetric mass transfer coefficient $K_G a$ versus $L^{0.7}$ yields:

\[ K_G a = 0.08200 \cdot L^{0.7} + 0.00000 \]

with coefficient of determination $R^2 = 0.999999$. The experimental slope $S = 0.08200\text{ kmol/(m}^3\cdot\text{h}\cdot\text{bar)/(L/(min}\cdot\text{m}^2))^{0.7}$ matches the design target ($0.0820$) with $0.00\%$ deviation. As liquid irrigation rate expanded from $10$ to $60\text{ L/(min}\cdot\text{m}^2)$, $K_G a$ grew from $0.411$ to $1.438\text{ kmol/(m}^3\cdot\text{h}\cdot\text{bar)}$, while transfer unit height $HOG$ contracted from $2.08\text{ m}$ to $0.59\text{ m}$.

8. Rigorous Error Analysis & Uncertainty Propagation

Uncertainty in NDIR gas analysis is $\pm 0.01\text{ mol}\%$, rotameter liquid flow error is $\pm 1.0\%$, and packed volume uncertainty is $\pm 0.5\%$. Propagating errors into $K_G a$ yields an experimental uncertainty of $\pm 1.4\%$, reporting $S = 0.0820 \pm 0.0011$.

9. Engineering Discussion & Phenomenological Interpretation

The $L^{0.7}$ dependence confirms Onda's wetted area formulation. At low irrigation rates, substantial portions of the ceramic Raschig rings remain un-wetted. Increasing liquid flow spreads liquid into continuous thin films over packing surfaces, multiplying interfacial contact area $a$ and thinning the liquid diffusion sublayer.

10. Industrial Scale-Up & Unit Operation Applications

Packed absorption columns are central to natural gas sweetening (acid gas scrubbing) and post-combustion carbon capture. In commercial amine scrubbers, structured packings (Mellapak) are chosen over random rings to provide higher specific surface area ($> 250\text{ m}^2/\text{m}^3$) and lower pressure drop.

11. Self-Assessment Conceptual Questions & Model Answers

Q1: Why is water a poor solvent for industrial $\text{CO}_2$ capture from flue gas?
A1: Water relies purely on physical solubility, which is low at atmospheric pressure and flue gas temperatures ($40\text{--}50^\circ\text{C}$); huge liquid circulation rates would be required, whereas chemical solvents like $30\text{ wt}\%$ MEA react chemically with $\text{CO}_2$, providing orders of magnitude higher capacity.

Q2: What is the effect of gas maldistribution on absorption column efficiency?
A2: Maldistribution causes gas and liquid to flow through separate cross-sectional channels (bypassing), reducing local contact area and causing the apparent HTU to increase dramatically.

12. Concluding Summary & Verified Engineering Metric

The packed column absorption experiment confirmed two-film mass transfer and Onda liquid-film scaling. The measured coefficient slope $S = 0.0820\text{ kmol/(m}^3\cdot\text{h}\cdot\text{bar)/(L/(min}\cdot\text{m}^2))^{0.7}$ ($K_G a = 0.0820 \cdot L^{0.7}$) validated liquid irrigation rate enhancement for chemical absorption processes.