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PRESSURE AND TEMPERATURE CHANGES WITH A SINGLE-COMPONENT SYSTEM        185


                              73
                             Applied pressure p/p O  5.1  Solid  Liquid







                               1                     Gas

                                      −78.2  56.6            31
                                               Temperature T/°C
             Figure 5.5 Phase diagram of a system that sublimes at room temperature: phase diagram of carbon
             dioxide. (Note that the y-axis here is logarithmic)

               Incidentally, the water in the bucket is essential for generating the effect of theatrical
             ‘smoke’ because the large volumes of CO 2(g) entrap minute particles of water (which
             forms a colloid; see Chapter 10.2). This colloidal water is visible because it creates
             the same atmospheric condition known as fog, which is opaque.
               Look at the phase diagram of CO 2 in Figure 5.5, which is clearly similar in general
             form to the schematic phase diagram in Figure 5.1. A closer inspection shows that
             some features are different. Firstly, notice that the phase boundary between solid and
             liquid now has a positive gradient; in fact, water is almost unique in having a negative
             gradient for this line (see Section 5.1). Secondly, the conditions of room temperature
                                  O
             (T = 298 K and p = p ) relate to conditions of the solid–gas phase boundary rather
             than the liquid–gas phase boundary.
               By drawing a horizontal line across the figure at p = p , we see how the line cuts
                                                               O
                                                ◦
             the solid–gas phase boundary at −78.2 C. Below this temperature, the stable form
             of CO 2 is solid dry ice, and CO 2(g) is the stable form above it. Liquid CO 2 is never
                              O
             the stable form at p ; in fact, Figure 5.5 shows that CO 2(l) will not form at pressures
                          O
             below 5.1 × p . In other words, liquid CO 2 is never seen naturally on Earth; which
             explains why dry ice sublimes rather than melts under s.t.p. conditions.


              How does freeze-drying work?
             Effect of pressure change on a phase change


             Packets of instant coffee proudly proclaim that the product has been ‘freeze-dried’.
             In practice, beans of coffee are ground, boiled in water and filtered to remove the
             depleted grounds. This process yields conventional ‘fresh’ coffee, as characterized
             by its usual colour and attractive smell. Finally, water is removed from the coffee
             solution to prepare granules of ‘instant’ coffee.
               In principle, we could remove the water from the coffee by just boiling it off, to
             leave a solid residue as a form of ‘instant coffee’. In fact, some early varieties of
             instant coffee were made in just this way, but the flavour was generally unpleasant as
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