ed~tedby MARY VIRGINIAORNA, 0.S U College of New Rochelle thumbnail hetchw New Rochelle NY 10801
The Third Law of Thermodynamics and the that of the carp, and therefore, the feed he gave the cows in- Residual Entropy of Ice: creased their entropy rather than increasing his farm profits (fi).,-, "Stillwater" or AS''~''~,T=~= 0 Forty years after Nernst's paper, Max Planck gave a Maureen M. Julian stronger statement of the Third Law (7) As the temperature diminishes indefinitely, the entropy of a ehem~eallyhomogeneous body of finite density approaches indef- initely near to the value of zero. Frank H. Stillinger Bell Laboratories A modern definition of entropy derived from statistical Murray Hill, NJ 07974 mechanics would have to contain safeguards against meta- stable states such as supercooled liquids and gases. Little is Roger R. Festa known about the entropy of the nucleus which ultimately must School of Education U-33 he considered. Since absolute zero is unattainable, the prop- University of Connecticut Storrs. CT 06268 erties must be smoothly extrapolated to zero degrees from the lowest attainable temperature. Sometimes the entropy does :Is lne lctnper>iturt.dw11er ;VT> ,.lo,er arid cI,,scr I(,:iL,- not go to zero, as for example, in the case of configurational IIIW wro, i1,c iltternal tnoliw~I,, a
Volume GO Number 1 January 1983 65 The authors have taken a liherty in the title of this article. In 1936, the year following Pauling's calculations, W. F. Indeed, the residual entropy of water, although small, is not Giauaue and J. W. Stout (17) im~rovedtheir calorimetric zero (8). In 1933, W. F. Giauque and M. F. Ashley at Berkeley, measurement and experimentally found So = 0.82 i 0.15 eu California, (9) measured the residual entropy of ice. Their data (3.4 f 0.6 J K-'1. Thus. the measured and theoretical values comhinedwith that of A. R. Gordon (10) gave an experimental value of 0.87 entropy units (eu) which is 3.6 J K-'. The first estimate& incredibly accurate due to the fact that a-large number of closely lying quantum states are nearly equally populated. In 1964, E. A. DiMarzio and F. H. Stillinger (18) Reactants AST 1- pq calculated that the Pauling estimate was 1%too low. Then in 1966, J. F. Nagle (19) calculated SO= R In 1.5069 = 0.8151 eu (3.410 J K-I). Both Pauling's and Nagle's values lie well within the 1936 exnerimental limits. Paulinz's calculations are based on the assumption that all ~ernal-~iwlerice structures have the same enerev.." and therefore have eaual a orcon nrobahili- Reactants % ties. However, these structures are not precisely equal in en- 1 OK 1 erev, hut suread out over a band of states. Conseauentlv the major theoretical interpretation is due to Linus Pauling (11) in 1935. His calculations were based on the interpretation of the'energy dispersion. the randomness of the hydrogen bonds in water. Indeed, many A complicating experimental feature is that crystal im- of the unusual properties of water (12,131 are due to hydrogen perfections such as vacancies, dislocations, grain houndaries, bonding: (1) the negative volume of melting; (2) density and impurities would tend to increase So. Their influence maximum in the normal liauid ranee-. (at 4°C):., 131. . isothermal~ ~ would have to he very carefully assessed. Perhaps this suggests compressibility minimum in the normal liquid range (at a series of So determinations on ice samples with different 46'C):.. (41. . at least nine crvstalline oolvmornhs:. . . ,.. (51 hieh " di- formation conditions, such as freezing rate, impurity doping, electric constant; (6) anomalously high melting, boiling, and and annealing. critical temueratures for a low-molecular-weight substance The last calorimetric measurements of the entropy of ice were made in 1936. With new theoretical results the issue is far from closed. The time is now ripe for a modern experi- H+ and OH- ions. mental redetermination of the residual entropy of ice. If Pauling's argument on residual entropy is to he under- stood, the structure of ice must also he considered. The ar- Acknowledgment rangement of the oxygen atoms is known from X-ray dif- The authors would like to thank Professor Beniamin fraction (14,15). Each oxygen is tetrahedrally surrounded by Widom of Cornell.University for helpful conversatio& and for his suapestion.- to MMJ and RRF of collaboration with FHS. in ice: (2) the hvdroeen atoms are directed more closelv to two Literature Cited of the four neaily teiradedrally surrounded oxygen atoms; (3) (1) Tiernan,N.F., J. CrnM. EDUC., in press. the orientations of adjacent water molecules are such that 12) Lewis, G. N., and Randall, M. "Thermodynamics and the Free Energy af Chemical exactly one hydrogen atom lies 6n each oxygen-oxygen axis; Substances? McGraw~Hill.New York. 1923. (3) Nernst. W., Nachr. COP Wim Coettingen. Klanno Math. Phys., p. i 11906). (4) interactions hevond nearest neighbor interactions mav be (4) Rickford, F. R., J. CHEM. EOUC., 59,817 (1982). neglected. (5) James. R. W., andFirth,E..Pmc.Roy. Soc London.Al17.62-87 (19271. (6) Mendeissohn, K.,'The Queat for Absolute Zero,)( McGiaw~Hill,New Vork, 1966. From assumption 2, there are six possible tetrahedral (7) Planck, M.,'Treatise on Thermodynamics," 3rd ed., trans. Ogg, Longmans, London, configurations of HOH. Now consider the adjacent water 1948, p. 270. Eisenberg, D., and Ksurmann. W., "The s,ructure and Properties orwater.' molecule. The probability that one of the two more closely University Press, New York. 1969, p. 102. honded sites is occupied is '12, Since each oxygen in water has Giauque, W. F.. and Ash1ey.M. F.,Phys. Rro.,B,81 (1933). two associated hydrogens, the probability that both of the two Cnrdnn,A.R., J. Chem. Phys., 2.65 (19%). Pnuling. L., J, Amen Chem Soc, 57, 26r0 (19361. more closely bonded sites are occupied is Thus the total Stillinger. F. H., Science, 209,451 (1980). number of configurations, W, for Avogadro's numher of Oma, M. V., J. CHEMEDUC.57.PISl llX3O). Rragg, W. H.. Pror Roy. Soc.,34,98 (19221. molecules, N, is W = (6 X %)N= (3/2)N.Substituting in S = Lonsdale, K.,Pmc. Roy. Soc London, A247,424 11958). RIN In W for one mole, S = (RIN) = R l11(~/2),which Bernal, J. D., andFow1er.R. H.J. Chem Phys.. 1, hi5 (19:131. = ~iauque,W. F.. and st our,^. W.J. ~rnwthem soc .&a,1144 (19361. yields SO 0.805 eu (3.37 J K-I) where So is the entropy at DiManio,E.A., mdStil1inger.F. H., J. Chrm Phys,40,1577 11964). absolute zero. Nagle. J.F., J Math. Phys.,?, 1484-91 (1966).
Misconceptions What misconceptions about science and chemistry do your students have? We all have some that plague us in our teaching. From the field of physics, for example, it is commonly believed hy beginning students that rockets need something to "push" against, that satellites stay aloft because gravity is weak high above the earth, and that a dam's strength must he in proportion to the size of the lake formed. Biology students believe that Balsa is a softwood. A post-doctoral researcher was recently heard to say that asolution whose pH = 2 is twice as acidic as one whose pH = 4! Equilibrium is oftenused when "steadv-state" is meant. or vice-versa.
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66 Journal of Chemical Education