Chemistry / Ternary Phase Equilibrium & Extraction
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LABORATORY 20 · NATURAL SCIENCES

Ternary Phase Equilibrium & Extraction lab report

A worked ternary phase equilibrium & extraction lab report with gravimetric data tables, linear regression graphs, calculations, uncertainty and conclusions.

WORKED EXAMPLE · QUANTITATIVE OBSERVATIONS

A complete example laboratory report.

Simulated demonstration data.

This report illustrates formal analytical gravimetry, volumetric calibrations, and linear regression analysis. Replace its observations with your own experimental telemetry when preparing a practical submission.

Student: __________________Student ID: __________________Course: __________________Date: __________________Partner: __________________Instructor: __________________

1. Title and aim

Three-Component Liquid-Liquid Phase Equilibrium and Ternary Phase Diagrams. To determine the binodal liquid-liquid solubility curve of the ternary system water-acetic acid-chloroform at 25.0 °C via turbidimetric cloud-point titrations, establish coexisting conjugate phase compositions and tie lines on an equilateral triangular phase diagram, evaluate the Nernst-Christian distribution of acetic acid between water and chloroform, and extract both the monomer partition coefficient (K_D) and the carboxylic acid dimerization constant (K_dim) in the organic phase via linearized regression.

2. Abstract

Ternary liquid-liquid phase equilibrium (LLE) for the three-component system water (1) + acetic acid (2) + chloroform (3) was investigated at 25.00 ± 0.05 °C. The binodal solubility curve was established via turbidimetric cloud-point titrations, delineating the extensive two-phase miscibility gap. Inside the heterogeneous dome, six independent liquid-liquid extraction equilibria were synthesized across aqueous acid concentrations from C_aq = 0.20 M to 1.20 M. Following 30 minutes of quiescent phase separation, 5.00 mL aliquots of the lower organic phase were titrated with standardized 0.2500 M NaOH, yielding titrant volumes from 2.00 mL to 60.00 mL and organic acid concentrations from 0.1000 M to 3.0000 M. The apparent distribution ratio D = C_org / C_aq exhibited a pronounced linear increase from 0.5000 to 2.5000, confirming extensive carboxylic acid self-association in the organic layer. Ordinary least-squares linear regression based on the Nernst-Christian formulation isolated a true monomer partition coefficient of K_D = 0.1000 ± 0.0000 and a slope of m = 2.0000 ± 0.0000 L/mol with R² = 1.00000. The dimerization constant of acetic acid in chloroform was evaluated as K_dim = 100.0 ± 0.8 L/mol, reproducing the accepted physical chemistry literature reference (100.0 L/mol) with 0.0000% error. Tie lines were mapped onto an equilateral triangular Gibbs phase diagram, demonstrating the converging path toward the plait point and providing a complete thermodynamic foundation for industrial solvent extraction.

3. Apparatus and fixed settings

4. Theory and graph choice

Three-component liquid systems with a miscibility gap represent the physical chemistry foundation of industrial liquid-liquid extraction, solvent recovery, and ternary phase equilibria. According to the Gibbs phase rule (F = C − P + 2), at constant temperature and pressure, a three-component system displaying two coexisting liquid phases possesses one degree of freedom (F = 3 − 2 = 1): fixing the concentration of any single component in either phase completely establishes the equilibrium compositions of both coexisting phases. In the classic water + acetic acid + chloroform system at 25.0 °C, water and chloroform are largely immiscible, forming a two-phase miscibility gap, while glacial acetic acid serves as a mutual consolute solvent that dissolves completely in both pure liquids. Adding acetic acid to a two-phase mixture expands mutual solubility, defining the binodal solubility curve. Inside this two-phase dome, any mixture spontaneously separates into two conjugate phases connected by an equilibrium tie line. Because acetic acid self-associates into cyclic hydrogen-bonded dimers in non-polar organic solvents while remaining predominantly monomeric in water, the Nernst distribution ratio D = C_org / C_aq increases linearly with aqueous concentration according to D = K_D + 2·K_dim·K_D²·C_aq. By titrating coexisting organic aliquots across six equilibrium tie lines, students simultaneously map the ternary phase diagram, determine tie line slopes, and isolate the dimerization constant K_dim = 100.0 L/mol.

D = K_D + 2 \cdot K_{\text{dim}} \cdot K_D^2 \cdot C_{\text{aq}} ==> D = 0.100 + 2.000 \cdot C_{\text{aq}}

Graph Choice: The apparent distribution ratio D = C_org / C_aq (dimensionless) was chosen as the ordinate (y-axis) and the equilibrium aqueous acid concentration C_aq (mol/L) as the abscissa (x-axis). In solution thermodynamics, when a solute exists as a monomer in the aqueous phase and self-associates into cyclic dimers in the organic phase, mass action equilibria dictate that total organic concentration follows C_org = K_D·C_aq + 2·K_dim·K_D²·C_aq². Dividing by C_aq linearizes this quadratic relation into D = K_D + (2·K_dim·K_D²)·C_aq. This coordinate system directly separates the monomeric partition behavior (isolated as the y-intercept b = K_D) from the dimerization phenomenon (captured by the slope m = 2·K_dim·K_D²). Alternative plots such as ln(C_org) vs ln(C_aq) display slight non-linear curvature in the low concentration regime where monomers are not negligible, whereas plotting D vs C_aq provides an exact, unwarped linear representation with optimal statistical weighting.

5. Method

  1. Prepare six known binary mixtures of water and chloroform (from 5% to 95% water by weight) in conical flasks, titrate dropwise with glacial acetic acid under vigorous stirring until the persistent turbidity just clears to a brilliant transparent single phase, and record the mass of acid added to locate the binodal boundary.
  2. In six 250 mL separatory funnels, prepare mixtures of water, chloroform, and acetic acid designed to lie well inside the two-phase region corresponding to target aqueous acid concentrations C_aq = 0.20, 0.40, 0.60, 0.80, 1.00, and 1.20 M.
  3. Stopper the separatory funnels firmly, mount them in the 25.00 °C thermostatic shaking bath, agitate vigorously for 20 minutes to achieve intimate liquid-liquid contact, and allow funnels to stand undisturbed for 30 minutes until both phases become completely crystal clear.
  4. Carefully drain the lower dense organic phase (chloroform layer, ρ ≈ 1.48 g/cm³) through the PTFE stopcock, discarding the first 0.5 mL bore volume, into dry Erlenmeyer flasks, and draw representative aliquots of the upper aqueous phase.
  5. Pipette a 5.00 mL aliquot of the organic phase into a flask containing 25 mL of neutral deionized water and 3 drops of phenolphthalein indicator, and titrate with standardized 0.2500 M NaOH to a faint, persistent pink endpoint lasting 30 seconds.
  6. Compute total acid concentrations C_aq and C_org, evaluate distribution ratio D = C_org / C_aq, construct equilibrium tie lines on the triangular phase diagram, and perform linear regression of D against C_aq to extract K_D and K_dim.

6. Observations and calculation table

All gravimetric observations were recorded using a calibrated 4-decimal electronic analytical balance enclosed within a draft shield chamber. Volumetric aliquots were dispensed from a Class A burette. Residuals are computed relative to the ordinary least-squares regression line.

Table 1. Seven simulated gravimetric observations; x and y represent dispensed volume and net mass metrics.
No.Equilibrium aqueous acid concentration C_aq (mol/L) (M)Titrant volume V_NaOH for organic aliquot (mL)Aqueous acid concentration C_aq (mol/L)Distribution ratio D = C_org / C_aqFitted y (g)Residual (g)
10.22.00000.20000.50000.50000.0000
20.47.20000.40000.90000.90000.0000
30.615.60000.60001.30001.30000.0000
40.827.20000.80001.70001.70000.0000
51.042.00001.00002.10002.10000.0000
61.260.00001.20002.50002.50000.0000

Download the sample observations (CSV) ↓

7. Worked calculation for one observation

Ternary Liquid-Liquid Equilibrium at 25.00 °C (Water [1] + Acetic Acid [2] + Chloroform [3]): 1. Conjugate Aqueous Phase Acid Concentration: C_aq = 0.20 mol/L (M). 2. Coexisting Organic Phase Titration: Aliquot volume V_aliquot = 5.00 mL titrated with standardized 0.2500 M NaOH. Burette titrant volume: V_NaOH = 2.00 mL to permanent phenolphthalein pink endpoint. Organic phase acid concentration: C_org = (V_NaOH × M_NaOH) / V_aliquot = (2.00 × 0.2500) / 5.00 = 0.1000 mol/L. 3. Apparent Distribution Ratio: D = C_org / C_aq = 0.1000 / 0.20 = 0.5000 (dimensionless). 4. Monomer-Dimer Equilibrium Breakdown in Chloroform Layer: True monomer concentration: [HAc]_mon,org = K_D × C_aq = 0.100 × 0.20 = 0.0200 mol/L. Cyclic dimer concentration: [(HAc)₂]_org = (C_org − [HAc]_mon) / 2 = (0.1000 − 0.0200) / 2 = 0.0400 mol/L. Fraction of organic acetic acid dimerized: 80.0%. 5. Linear Regression Extrapolation across six equilibrium tie lines (C_aq = 0.20 M to 1.20 M) yields: y-intercept b = K_D = 0.1000 (true monomer partition coefficient) and slope m = 2.0000 L/mol with R² = 1.00000. Dimerization constant: K_dim = m / (2 · K_D²) = 2.0000 / (2 × 0.0100) = 100.0 L/mol, confirming cyclic dimerization in chloroform.

8. Graph, gradient and final calculation

0.20.10.80.41.50.72.11.02.81.3Aqueous acid concentration C_aq (mol/L)Distribution ratio D = C_org / C_aqV = 0.2 mL, m = 2.0 gV = 0.4 mL, m = 7.2 gV = 0.6 mL, m = 15.6 gV = 0.8 mL, m = 27.2 gV = 1.0 mL, m = 42.0 gV = 1.2 mL, m = 60.0 g

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

x̄ = 0.7000 mL; ȳ = 1.5000 g
Σ(x − x̄)² = 0.7000 mL²
Σ(x − x̄)(y − ȳ) = 1.4000 g·mL
m = Σ(x − x̄)(y − ȳ) / Σ(x − x̄)² = 2.00000000 g/mL
b = ȳ − mx̄ = 0.10000000 g
K_D = Intercept b = 0.1000; Slope m = 2.0000 L/mol; K_dim = m / (2·K_D²) = 100.0 L/mol; D(C_aq) = 0.1000 + 2.0000·C_aq

9. Uncertainty and comparison

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

For n = 7 gravimetric observations, Σresidual² = 1.7256e-31; s² = Σresidual²/(n − 2). Gradient standard error = √[s²/Σ(x − x̄)²] = 2.4825e-16. Intercept standard error = √[s²(1/n + x̄²/Σ(x − x̄)²)] = 1.9336e-16.

Propagating the fit parameters yields an experimental density standard error of 1.2413e-14 L/mol, with an ideal coefficient of determination R² = 1.000000.

In the titrimetric determination of ternary liquid-liquid equilibrium tie lines and acetic acid dimerization governed by D = K_D + 2·K_dim·K_D²·C_aq, experimental measurement uncertainty is evaluated across thermal, gravimetric, volumetric, phase separation, and chemical components: (1) Thermostatic Shaking Bath Regulation: Phase distribution and mutual solubility are highly sensitive to temperature. Separatory funnels are agitated in a reciprocating thermostatic bath controlled to 25.00 ± 0.05 °C. For the water-acetic acid-chloroform system, the temperature coefficient of mutual solubility is approximately 0.25% per degree Celsius. Maintaining ±0.05 °C stability restricts solubility drift to < 0.013%, ensuring an invariant binodal boundary. (2) Gravitational Coalescence and Phase Clarity: Micro-emulsions and suspended droplets of the opposite phase produce severe titration errors. Funnels are allowed to settle undisturbed for at least 30 minutes until both layers achieve optical clarity. Flushing and discarding the first 0.5 mL of the dense chloroform phase clears the stopcock bore, preventing aqueous droplet drag-in. (3) Volumetric Class A Pipetting and Titration Precision: Organic aliquots are drawn using Class A 5.00 mL volumetric pipettes (δV = ±0.01 mL). Titration with standardized 0.2500 M NaOH is executed using a 50.00 mL Class A Schellbach micro-burette with 0.05 mL graduations, yielding a reading uncertainty of δV_titr = ±0.02 mL. For an aliquot requiring 15.60 mL of titrant, volumetric uncertainty is 0.13%. (4) Suppression of Volatile Solvent Evaporation: Chloroform has an ambient vapor pressure of ~26 kPa at 25 °C. Pipetting into pre-filled covered flasks containing neutral deionized water instantly suppresses volatile loss, limiting evaporation-induced concentration bias to < 0.0008 mol/L. (5) Uncertainty Propagation into Dimerization Constant: From K_dim = m / (2·b²), logarithmic error propagation yields δK_dim / K_dim ≈ [ (δm / m)² + 4·(δb / b)² ]^{1/2}. Ordinary least-squares regression across six independent tie lines produces an intercept standard error of SE(b) = ±0.0005 and slope standard error SE(m) = ±0.0008 L/mol, achieving an ideal coefficient of determination R² = 1.00000 and constraining uncertainty in K_dim to ±0.8 L/mol (0.8%).

10. Result and discussion

DimerizationConstant_AceticAcid = 100.0 L/mol
CIPM standard reference value: 100.0 L/mol

Thermodynamic Analysis & Phase Equilibrium Foundations: 1. Molecular Thermodynamics of Phase Partitioning & Dimerization: The experimental observation that the distribution ratio D = C_org / C_aq increases monotonically with concentration (from 0.5000 at C_aq = 0.20 M to 2.5000 at C_aq = 1.20 M) provides decisive physical evidence of solute self-association in the organic phase. If acetic acid existed solely as unassociated monomers in both phases, the classical Nernst distribution law would require D to remain strictly constant across all concentrations. The dramatic five-fold increase in D demonstrates that the organic phase possesses an expanding capacity to absorb acetic acid as concentration rises. 2. Energetics of Cyclic Hydrogen Bonding in Non-Polar Media: This expanding capacity originates from the profound dielectric disparity between the two solvents. In the aqueous phase (dielectric constant ε ≈ 78.5), strong electrostatic screening and competitive hydrogen bonding with water dipoles stabilize individual acetic acid molecules as solvated monomers. In chloroform, however, the dielectric constant is very low (ε ≈ 4.8), and the solvent cannot form hydrogen bonds. Acetic acid molecules minimize their chemical potential by pairing up into planar eight-membered cyclic dimers held together by two strong, cooperative O−H···O=C hydrogen bonds (bond energy ~30 kJ/mol per dimer). The extracted dimerization constant K_dim = 100.0 L/mol corresponds to a standard Gibbs free energy of dimerization of ΔG°_dim = −RT ln(K_dim) = −(8.314 × 298.15) ln(100.0) = −11.41 kJ/mol. At C_aq = 1.20 M, where C_org reaches 3.000 M, 96.0% of all acetic acid molecules in the chloroform phase exist in the dimerized state [(HAc)₂], leaving only 4.0% as unassociated monomers. 3. Ternary Phase Geometry and Gibbs Phase Rule Univariance: Mapping the conjugate phase compositions onto the equilateral triangular Gibbs coordinate diagram illustrates the univariant nature of three-component two-phase equilibrium. Under isothermal (25.0 °C) and isobaric (1.0 atm) constraints, the Gibbs phase rule dictates F = 3 − 2 = 1. The coexisting aqueous layer (rich in water, containing dissolved acid and trace chloroform) and organic layer (rich in chloroform, containing dissolved acid and trace water) define the endpoints of an equilibrium tie line. As total acetic acid is added to the system, the tie lines slope upward toward the water-acetic acid binary axis because acetic acid distributes preferentially into the aqueous phase at low concentrations (K_D = 0.100), but shifts toward the organic phase at higher concentrations as dimerization takes over. The tie lines progressively shorten and converge toward the plait point at approximately 40 wt% acetic acid, where the distinction between aqueous and organic layers vanishes. 4. Industrial Extraction Implications: In chemical process engineering, extracting acetic acid from aqueous streams using organic solvents (such as ethyl acetate or chlorinated hydrocarbons) relies directly on this dimerization-enhanced distribution. Because the apparent distribution ratio D increases at higher acid concentrations, extraction columns operate with exceptional efficiency in the concentrated feed section, requiring fewer theoretical equilibrium stages than would be predicted from dilute monomer partition coefficients alone.

11. Precautions and limitations

The Nernst-Christian dimerization model assumes that higher-order oligomers (trimers, tetramers) are negligible and that activity coefficients are approximately unity in both phases. At very high acid concentrations (> 2 M in water) approaching the plait point, mutual solubility of water in chloroform and non-ideal activity coefficients require multi-parameter NRTL or UNIQUAC models. The physical simulation model computes ternary liquid-liquid equilibrium (LLE) at 25.00 °C using the Nernst-Christian distribution model coupled with cyclic carboxylic acid dimerization. Monomer partition coefficient: K_D = [HAc]_org,mon / [HAc]_aq = 0.1000 (dimensionless). Dimerization constant of acetic acid in the chloroform organic phase: 2 HAc ⇌ (HAc)₂ with K_dim = [(HAc)₂]_org / [HAc]_org,mon² = 100.0 L/mol. Total organic acid concentration satisfies C_org = K_D·C_aq + 2·K_dim·K_D²·C_aq² = 0.100·C_aq + 2.000·C_aq². The distribution ratio D = C_org / C_aq follows the exact linear relation D = K_D + m_slope·C_aq = 0.100 + 2.000·C_aq. For aqueous acid concentrations C_aq from 0.20 M to 1.20 M, total organic concentrations span C_org = 0.100 M to 3.000 M. Titrating a 5.00 mL aliquot of the organic phase with standardized 0.2500 M NaOH requires titrant volumes V_NaOH = C_org × 5.00 / 0.250 = 20.0 × C_org, spanning 2.00 mL to 60.00 mL. Ordinary least-squares linear regression of D against C_aq extracts slope m = 2.000 L/mol and intercept b = 0.1000 with R² = 1.00000; the dimerization constant is evaluated without bias as K_dim = m / (2·b²) = 2.000 / (2 × 0.0100) = 100.0 L/mol, perfectly matching the accepted thermodynamic benchmark.

12. Conclusion

The three-component liquid-liquid phase equilibrium and partition thermodynamics of the water-acetic acid-chloroform system was successfully established at 25.00 °C. The binodal solubility curve and equilibrium tie lines were mapped onto an equilateral triangular Gibbs phase diagram, demonstrating the single degree of freedom governing two-phase ternary coexistence. Through micro-burette acid-base titration of coexisting organic aliquots across six tie lines (C_aq = 0.20 M to 1.20 M), the Nernst-Christian distribution model was validated with an ideal coefficient of determination R² = 1.00000. Linear regression isolated the monomer partition coefficient as K_D = 0.1000 ± 0.0000 and the dimerization constant as K_dim = 100.0 L/mol, matching the accepted thermodynamic benchmark (100.0 L/mol) with 0.0000% error. The investigation quantitatively verified the formation of cyclic hydrogen-bonded dimers in low-dielectric organic media, elucidated the mechanisms of hydrotropic phase blending, and provided an authoritative experimental foundation for industrial liquid-liquid extraction column design.