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Flotation                                                                                        165



            a gas, ‘‘A,’’ in the aqueous phase is proportional to the partial  Given                3
            pressure of gas ‘‘A’’ at the gas–water interface, i.e.,  H(O 2 ) ¼ 0.0004383 (kg dissolved oxygen=m water=kPa
                                                                        oxygen) at 208C
                       C(gas A) ¼ H(gas A)   P(gas A)    (8:1)    X(O 2 ) ¼ 0.209 mol O 2 =mole air (Table B.7)
                                                                  P(atmosphere) ¼ 101.325 kPa (stated)
            in which                                              Required
              C(gas A) is the concentration of dissolved gas A in aque-  Calculate the concentration of dissolved oxygen at equi-
                                     3
                ous solution (kg gas A=m water)                   librium by Henry’s law.
              H(gas A) is the Henry’s constant for a given gas, e.g., ‘‘A’’
                          3                                       Solution
                (kg gas A=m water=kPa gas A)
                                                                  Substitute given data, for oxygen, in Equation 8.3,
              P(gas A) is the partial pressure of gas A above gas–water
                interface (kPa gas A)
                                                                  C(O 2 ) ¼ H(O 2 )   X(O 2 )   P(total)
              A is the designation for a particular species of a gas, e.g.,
                                                                                                 3
                                                                       ¼ 0:0004383 (kg dissolved O 2 =m water=kPa O 2 )
                O 2 or N 2
                                                                                                       (Ex8:1:1)
              Table H.5 gives Henry’s constants for different gases with
                                                                    . 0.209 mol O 2 =moles all gases in air
            temperature as a variable. In addition, coefficients, i.e., ‘‘A’’
                                                                    . 101.325 kPa total pressure
            and ‘‘B,’’ are given at the top of Table H.5 for ‘‘best-fit’’                      3
                                                                      ¼ 0:00928 kg dissolved O 2 =m water (9:3mg=L)
            empirical equations for H(gas A) vs. temperature, i.e.,
            H(gas A) ¼ A   exp(B   T8C). As a historical note, Henry’s
                                                                  Discussion
            law was mentioned by Masterson and Pratt (1958, p. 233)  As stated, the foregoing simple calculation demonstrates
            and by Eckenfelder et al. (1958, p. 251). In other words,  the application of Henry’s law. Two ideas are involved.
            application of Henry’s law to flotation has been established  First, in accordance with Henry’s law, each gas dissolves
            since the 1950s.                                      in water in proportion to its partial pressure. Second,
              The partial pressure of ‘‘gas A’’ is implied in Dalton’slaw,  Dalton’s law states that each gas in a mixture of gases exerts
            i.e., it states that the total pressure in a mixture of gases is the  a partial pressure in accordance with its respective mole
            sum of the respective partial pressures, expressed for a single  fraction, e.g., X(O 2 ). In addition, note that the units are
                                                                  delineated fully, which helps in applying Henry’s law.
            gas as
                       P(gas A) ¼ X(gas A)   P(n gases)  (8:2)
                                                                  Example 8.2 Calculation of Dissolved Nitrogen
            in which
                                                                  Concentration at Sea Level by Henry’s Law at 208C
              X(gas A) is the mole fraction of gas A in gas phase (mol
                                           3
                       3
                gas A=m =sum of mol n gases=m )
                                                                  The problem refers to water at equilibrium with air at sea
              P(n gases) is the total pressure of all gases above gas–water
                                                                  level at 208C based on 101.325 kPa total atmospheric
                interface (kPa n gases)                           pressure.
              n is the number of species of gases in a given volume
                                                                  Given
                                                                                                     3
                                                                  H(N 2 ) ¼ 0.0001875 (kg dissolved nitrogen=m water=kPa
              Then combining Equations 8.1 and 8.2,                     nitrogen) at 208C
                                                                               a
                                                                  X(N 2 ) ¼ 0.78084 moles N 2 =mole air (Table B.7)
                C(gas A) ¼ H(gas A)   X(gas A)   P(n gases)  (8:3)
                                                                  P(atmosphere) ¼ 101.325 kPa (stated)
            Equation 8.3 is the operational equation. If it happens that  Required
                                                                  Calculate the concentration of dissolved nitrogen at equi-
            P(n ¼ 1), i.e., a ‘‘pure’’ gas A is involved, then it follows
                                                                  librium by Henry’s law.
            that X(gas A) ¼ 1.0. Examples 8.1 and 8.2 illustrate the appli-
            cation of Henry’s law, which is straightforward in accordance  Solution
            with Equation 8.3. Example 8.3 shows the calculation of  Substitute given data, for nitrogen, in Equation 8.3,
            a ‘‘pseudo’’ Henry’s constant for air, H(air), which again is
            straightforward, albeit involving mole fraction weighted aver-  C(N 2 ) ¼ H(N 2 )   X(N 2 )   P(total)
            age of the respective Henry’s constant.                                                   3
                                                                            ¼ 0:0001875 (kg dissolved N 2 =m
                                                                              water=kPa air)
              Example 8.1 Calculation of Dissolved Oxygen
              Concentration at Sea Level by Henry’s Law at 208C     . 0.78084 moles N 2 =moles all gases in air
                                                                    . 101.325 kPa
                                                                                              3
              The problem refers to water at equilibrium with oxygen  ¼ 0:01483 kg dissolved N 2 =m water (14:8mg=L)
              at sea level at 208C based on 101.325 kPa total atmos-
              pheric pressure and demonstrates the application of  Discussion
              Henry’s law.                                        The relevant points are stated in Example 8.1.
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