Page 328 - Academic Press Encyclopedia of Physical Science and Technology 3rd Chemical Engineering
P. 328

P1: GSY/GSR/GLT  P2: GLM Final Pages
 Encyclopedia of Physical Science and Technology  EN007E-968  June 30, 2001  17:35






               374                                                                         High-Pressure Synthesis (Chemistry)


               mercury, and tantalum, generally show a fall in their super-
               conducting critical temperatures as pressure increases. In-
               teresting exceptions are lanthanum, silver, Mo 6 Se 8 , and a
               few other ternary compounds. However, some substances
               require pressure for superconductivity—for example, an-
               timony, arsenic, barium, yttrium, germanium, or cesium
               in their high-pressure forms. The critical temperatures of
               the latter at first rise with increasing pressure but then
               usually fall at still higher pressures. Phase changes may
               complicate this simple picture. So far it appears that
               the superconductivity in nearly all materials can be ex-
               plained by the BCS type of electron pairing. Increased
               understanding will follow as X-ray diffraction studies re-
               veal the crystal structures of the various superconducting
               substances.



               V. PRACTICAL USES OF VERY
                  HIGH PRESSURES                                 FIGURE 8 Carbon phase diagram showing diamond synthesis
                                                                 regions.
               Some modern metalworking processes use very high pres-
               sures in extrusion or cold-forming operations simply be-  sures of this level are easily reached and tiny diamonds
               cause the metals being worked are relatively strong and  can be made for lapping and polishing, as mentioned
               the tools are made of even stronger cemented tungsten  earlier.
               carbides. High hydrostatic pressures, 1–2 MPa, have been  The bulk of industrial diamond production is done at
               used to form special pieces that could otherwise be formed  pressures and temperatures in the range 4.5–6.0 GPa and
               only by more expensive methods. Usually the high ini-  1400–1800  K,  a  range  indicated  in  Fig.  8  by  a  cross-
               tial and continuing costs of very high pressure equipment  hatched area. The transformation of graphite to diamond is
               make it a last resort.                            madepossiblebyusingcatalystsolvents,whicharemolten
                                                                 (carbon-saturated) metals such as alloys picked from man-
                                                                 ganese, iron, cobalt, and nickel. Platinum and palladium
               A. Diamond Synthesis
                                                                 are also effective but cost more and require higher tem-
               Very high pressures probably find their widest use in the  peratures and pressures. (Some carbon solvents, such as
               commercial synthesis of diamond from graphite. The high  AgCl or CdO, do not form diamond from graphite at
               valueoftheproductsmakestheefforteconomicallyviable,  5.5 GPa. Diamond-forming catalysts usually carry pos-
               and several tons of industrial diamonds are synthesized  itively charged carbon in solution.)
               each year in dozens of plants throughout the world.  Apparatus of the “belt” type is often used. Pieces
                 Figure 8, the carbon phase diagram, forms a basis for  of graphite and metal occupy the heated zone of the
               discussing the processes involved. Ideal graphite has a  high-pressure chamber. When the chamber pressure has
               density of 2.2 and diamond, 3.52, so 1 ml of graphite  become suitably high, the hot zone temperature is in-
               becomes 0.63 ml of diamond, a relatively large change.  creased until the metal melts and becomes saturated with
               Diamond is favored to form at pressures and temper-  carbon. At this point, diamond begins to deposit from the
               atures where it is stable, but the carbon atoms must  molten metal and graphite dissolves. Only a thin layer of
               be in the proper environment, particularly at the milder  metal is involved, and the diamond replaces the graphite.
               conditions.                                       Figure 9 is a photograph of a thin layer of nickel catalyst
                 At temperatures above about 2500 K, thermal agitation  on the surface of a mass of freshly grown diamonds. The
               alone is usually sufficient to make the stable phase form  diamonds are recovered after acid treatment.
               in a few seconds or less. Diamond can form from molten  The higher the pressure over equilibrium, the higher
               carbon (4000 K) in a few milliseconds. The pressures re-  the diamond nucleation and growth rate and the smaller
               quired for diamond stability are then upwards of 10 GPa,  and less perfect the crystal. Lower synthesis temperatures
               which are not economic for static apparatus, and the di-  favor cubes and higher ones, octahedra. Suitable control
               amond crystals are very small. However, dynamic pres-  of these variables permits the growth of selected types of
   323   324   325   326   327   328   329   330   331   332   333