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M. Iannone M.U. 6/20/2012 Determination of the Distribution Coefficient of I 2 between Water and an Organic Solvent Iodine is somewhat soluble in both water and organic solvents. In water it associates strongly with I - to form I 3 - ion. In this experiment, you will extract aqueous iodine/iodide solutions with dichloromethane or another solvent to determine how I 2 distributes itself between the two phases. Two equilibria are involved: (1) I 3 - (aq) F I - (aq) + I 2 (aq) K = (1.38 ± 0.03)×10 -3 at 25 0 C [1] (2) I 2 (aq) F I 2 (CH 2 Cl 2 ). K D The distribution coefficient is the equilibrium constant of equation 2: (3) K I I D CH Cl HO = [ ] [ ] 2 2 2 2 2 . Procedure: [2] 1. Solutions: Prepare 0.200M I - solution (A). Prepare 100 mL of solution B by adding 2.0×10 -4 mol of solid I 2 to 100 mL of solution A. (I 2 dissolves very slowly—stir or sonicate.) Because of reaction 1, solution B will have [I - ] 0.198M and [I 3 - ] 0.002M. 2. Dilute aliquots of solution B with solution A to form 4 solutions with known [I 3 - ] ranging from 0.001M to 0.0002M.[3] Also, prepare “solution X” in which solution B is diluted 1:1 with water—to test if K D depends on [I - ]. Measure absorbance of each in a spectrometer or colorimeter at 475 nm. Use solution A as the blank. 3. Extract an aliquot of each solution with an equal volume of dichloromethane (or cyclohexane, toluene, hexane etc.). Important: allow enough time and mixing to reach equilibrium. Measure absorbance of the aqueous layer in the colorimeter, using solution A as the blank. The liquid must have a depth of at least 1” in the cuvette. Calculations and error analysis: Find slope of calibration data by linear regression. Report it with the standard error. Include graph in report. Note: force zero intercept by entering zero in the “Const” box of the Linest function dialog box. Use spectrophotometric measurement and calibration data to determine [I 3 - ] in the aqueous layer after extraction for each solution. Propagate error of slope. Determine K D for each trial. Use the equilibrium constant for reaction (1) to find [I 2 (aq)]. Find the weighted average value for K D with uncertainty. Discussion: Your discussion should relate the nature of the I 2 molecule and the two solvents to the value obtained for the distribution coefficient. Discuss the role of the I 2 - I 3 - equilibrium in the aqueous phase. Does K D depend upon [I - ], (1) in theory and (2) according to the results from solution X? Can you think of a better way to measure K D ? 1 Average of 16 values given in J. Sol. Chem., 13, 9 (1984) 2 G. Weiss, T. Greco and L. Rickard, Experiments in General Chemistry, Prentice Hall, New York (1997), pages 155-159 3 Under the conditions of this experiment (0.2M I - ), over 99% of the aqueous I 2 is converted: I 2 + I - I 3 - .

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  • M. Iannone M.U. 6/20/2012

    Determination of the Distribution Coefficient of I2 between Water and an Organic Solvent

    Iodine is somewhat soluble in both water and organic solvents. In water it associatesstrongly with I- to form I3- ion. In this experiment, you will extract aqueous iodine/iodidesolutions with dichloromethane or another solvent to determine how I2 distributes itself betweenthe two phases. Two equilibria are involved:(1) I3(aq) F I(aq) + I2(aq) K = (1.38 0.03)103 at 250C [1](2) I2(aq) F I2(CH2Cl2). KDThe distribution coefficient is the equilibrium constant of equation 2:

    (3) K IID

    CH Cl

    H O

    =[ ][ ]

    2

    2

    2 2

    2

    .

    Procedure: [2]1. Solutions:Prepare 0.200M I solution (A).Prepare 100 mL of solution B by adding 2.010-4 mol of solid I2 to 100 mL of solution A. (I2dissolves very slowlystir or sonicate.) Because of reaction 1, solution B will have [I] 0.198M and [I3] 0.002M.2. Dilute aliquots of solution B with solution A to form 4 solutions with known [I3] rangingfrom 0.001M to 0.0002M.[3] Also, prepare solution X in which solution B is diluted 1:1 withwaterto test if KD depends on [I-]. Measure absorbance of each in a spectrometer orcolorimeter at 475 nm. Use solution A as the blank.3. Extract an aliquot of each solution with an equal volume of dichloromethane (or cyclohexane,toluene, hexane etc.). Important: allow enough time and mixing to reach equilibrium. Measureabsorbance of the aqueous layer in the colorimeter, using solution A as the blank. The liquidmust have a depth of at least 1 in the cuvette.

    Calculations and error analysis: Find slope of calibration data by linear regression. Report it with the standard error. Include

    graph in report. Note: force zero intercept by entering zero in the Const box of the Linestfunction dialog box.

    Use spectrophotometric measurement and calibration data to determine [I3] in the aqueouslayer after extraction for each solution. Propagate error of slope.

    Determine KD for each trial. Use the equilibrium constant for reaction (1) to find [I2(aq)]. Findthe weighted average value for KD with uncertainty.

    Discussion:Your discussion should relate the nature of the I2 molecule and the two solvents to the valueobtained for the distribution coefficient. Discuss the role of the I2 I3 equilibrium in theaqueous phase. Does KD depend upon [I], (1) in theory and (2) according to the results fromsolution X? Can you think of a better way to measure KD?

    1 Average of 16 values given in J. Sol. Chem., 13, 9 (1984)

    2 G. Weiss, T. Greco and L. Rickard, Experiments in General Chemistry, Prentice Hall, New York (1997), pages

    155-1593 Under the conditions of this experiment (0.2M I), over 99% of the aqueous I2 is converted: I2 + I I3.

  • M. Iannone M.U. 6/20/2012

    Sample calculations of distribution coefficient: forced intercept

    Absorbance of I3- solutions at 475 nm before andafter extraction with CH2Cl2

    [I3-]/Mbefore extraction

    Absorbancebefore extraction

    Absorbanceafter extraction

    C 1.0010-3 0.653 0.360D 6.0010-4 0.410 0.215

    E 4.0010-4 0.280 0.152 F 2.0010-4 0.145 0.080X 1.0010-3 0.645 0.260

    Abs = [I3- ] (67019)M1

    [I3-] for solution F after extraction

    13 M)19670(080.0]I[

    =

    = (1.19 0.03) 10-4 M (propagation of error formula used)[I2] in organic layer = [I3-]before [I3-]after (if equal volumes solution & CH2Cl2 used)

    = (2.0010-4 M) - (1.19 0.03) 10-4 M=(8.10.3)10-5 M

    [I2] in aqueous layer after extraction, from equilibrium expression:( )M10)3.02.8(]I[

    X] sol.for 0.100 [* ]I[

    ]I[ ]I[*200.0]I[

    ]I][I[10)02.038.1(K7

    2

    3

    23

    3

    23

    =

    ===

    399][][

    2

    2

    =

    =aqueous

    organicD I

    IK

    Values for KD from all solutions:C 1256 weight = 1/42 = 0.06D 1266 0.06E 1116 0.07F 995 0.08X 1145 0.09

    The Beers law plot is not the primary source of imprecision in the data. The 95% confidencelimits reflect the overall reliability of the result for KD, which should be reported as:

    KD = 114 16.

    Linest results: (do notinclude in body of report)

    670.3125 018.738929 #N/A0.9968837 0.02998231279.5731 41.1502563 0.0035957

    Weighted average = (data wt)/wts= 114

    Uncertainty = 2wts/1 =

    Standard deviation of KD values = 1295% conf. limit = 16