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Basic environmental chemistry                                          21

                      Calculate the free energy  change for the formation of one mole of calcium  carbonate  at
                      25 °C according to this reaction, given ΔH = -178.2 kJ per mole and ΔS = -160.6 J per
                      mole. Is this reaction spontaneous?

                      Solution
                      This is a straightforward application of Equation (2.7):
                       G       H   T  S     178  2 .  298 . 15  . 0  1606    130  kJ mol -1

                      Note that the J–kJ conversion must be accounted for in the calculation.
                         The value of  ΔG is negative, indicating that the reaction proceeds spontaneously.
                      From Equation (2.7) it can also be seen that ΔG becomes zero at a temperature above
                      25 °C. Thus, if the temperature is sufficiently high, the above reaction will proceed in the
                      reverse direction, i.e. calcium  carbonate  will decompose into calcium oxide and carbon
                      dioxide  gas.



                   2.5  PHASES AND PHASE TRANSITIONS
                   2.5.1  Phases

                   Substances can occur in three states: solid, liquid, and gas. A  phase  is a distinct and
                   homogeneous state of a material with no visible boundary separating it into parts. As a
                   rule, there is always only one gas phase , as gaseous substances mix fully. There may be more

                   than one liquid phase  (e.g. oil and water). Liquids of one particular substance always mix
                   fully, except for liquid helium that may occur in two phases. Many substances may occur

                   in different solid phases ; for example, carbon may occur in both the diamond and graphite
                   phase, and silicon dioxide may occur in a crystalline (quartz ) or amorphous , glassy phase.

                   Chemicals that are dissolved in water occur in the so-called dissolved phase , which is also
                   called the soluble phase or aqueous phase. Sometimes the term liquid phase is used to refer


                   to the dissolved phase , but it should be noted that this term ignores the difference between
                   pure liquids and aqueous solutions. The solid phase  is a generic but ill-defined term for all
                   chemicals that are in soil and sediment solids, or in suspended solids  in water. There are also
                   various other terms specifying particular components of the solid phase. The term adsorbed
                   phase    refers to chemicals adsorbed to solid surfaces or suspended matter. Substances
                   associated with suspended solids in water, i.e. adsorbed onto or incorporated in suspended
                   particles, are also referred to as the particulate phase  or suspended phase.

                   2.5.2  Thermodynamic considerations on phase  transitions

                   Chemicals may occur in multiple phases at the same time. The conversion between phases is
                   called a phase transition. Table 2.4 shows the most important phase transitions of chemicals
                   in soil, water, and air. Chemicals tend to establish equilibrium  among the different phases,
                   which ultimately results in an equilibrium distribution. As seen in the previous section, this
                   equilibrium state is characterised by a zero change in free energy  (ΔG = 0). From Equation
                   (2.7) it follows that:
                    H      T  S                                                         (2.8)

                   The enthalpy  changes primarily due to a change in volume (see Equation 2.5). Because
                   gases have more entropy  than liquids, which, in turn, have more entropy than solids, it takes










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