Hostname: page-component-78c5997874-s2hrs Total loading time: 0 Render date: 2024-11-09T16:02:32.218Z Has data issue: false hasContentIssue false
  • English
  • Français

The Effect of Impurities on the Surface Structure of Evaporating Ice

Published online by Cambridge University Press:  30 January 2017

J.D. Cross
J.D. Cross*
Affiliation:
Inland Waters Branch, Department of Energy, Mines and Resources, Ottawa, Ontario, Canada
Rights & Permissions [Opens in a new window]

Abstract

Micrographs of the surface of evaporating polycrystalline ice containing impurities are presented. The micrographs show that impurities that enter the ice lattice substitutionally enhance the fine structure on the surface, but impurities rejected by the lattice suppress the fine structure. It is concluded that the observed fine structure is not an artifact of the machine but a real property of evaporating ice dependent upon the defects at the surface.

Résumé

Résumé

Des micrographies de la surface d'une glace polycristalline contenant des impuretés sont présentées. Les micrographies montrent que les impuretés qui pénètrent dans le réseau cristallin de la glace favorise par compensation une structure déliée en surface, mais que le rejet des impuretés par le réseau cristallin supprime cette structure fine. On conclut que la structure déiée observée n'est pas un artefact de l'appareillage; il s'agit d'une véritable propriété de la surface en cours d'évaporation sous la dépendance des défauts existants en surface.

Zusammenfassung

Zusammenfassung

Es werden Mikroaufnahmen der Oberfläche von verdunstendem polykristallinem Eis mit Verschmutzungen vorgelegt. Die Mikroaufnahmen zeigen, dass Verschmutzungen, die in das Eisgef¨ge eindringen, die Feinstruktur auf der Oberfläche wesentlich verstärken, dass dagegen Verschmutzungen, die vom Gefüge abgewiesen werden, die Feinstruktur unterdrücken. Es wird geschlossen, dass die beobachtete Feinstruktur nicht ein künstliches Ergebnis der Apparatur ist; sie ist vielmehr eine spezifische Eigenschaft verdunstenden Eises, die von den Defekten an der Oberfläche abhängt.

Type
Research Article
Information
Journal of Glaciology , Volume 10 , Issue 59 , 1971 , pp. 287 - 292
Copyright
Copyright © International Glaciological Society 1971

Introduction

Recent studies of polycrystalline ice surfaces with a scanning electron microscope (Reference Odencrantz, Odencrantz, McEwan, Amand and FinneganOdencrantz and others, 1968; Reference CrossCross, 1969[a],[b]) have revealed a complex surface structure containing fine filaments less than one micrometre thick. Such surface structure could contribute to the electrificaiion and nucleation processes in clouds (Reference Cross and SpeareCross and Speare, 1969; Reference RuskinRuskin, 1969). The existence of a highly disordered surface layer with a large concentration of defects has been indicated by deformation studies (Reference Muguruma, Riehl, Riehl, Bullemer and EngelhardtMuguruma, 1969), andReference JaccardJaccard (1967) has reported that evaporation changes the electrical conductivity of ice, probably by producing defects at the surface. Theoretical and experimental studies of ice evaporating in a controlled environment have been carried out byReference Gukbman and VolynetsGukhman and Volynets (1968) and Reference Novikov and VagnereNovikov and Vagner (1968). These studies deal with the heat and mass transfer conditions for subliming polycrystalline ice in the pressure range 1 0-5 to 105 N m -2. The mass loss was found to be mainly controlled by the radiant heat flux to the specimen rather than by conduction and convection. The evaporation was not confined to the geometric surface of the ice but occurred over an extended region, producing a rough surface. These reports support the supposition that the observed structure is a natural structure for pure polycrystalline ice related to the disordered conditions at the surface, and is not an artifact of the microscope, If water containing ionic impurities is frozen, the impurity ions are not generally incorporated into the ice lattice but accumulate at grain boundaries. Ammonium and fluoride ions are an exception. In small concentrations these ions are incorporated substitutionally into the ice lattice and create respectively D and L Bjerrum defects. If the surface structure of evaporating polycrystalline ice is not an artifact of the microscope it should be sensitive to the addition of impurities to the water forming the ice and a different behaviour is to be expected in the influence of impurities rejected by the ice and those incorporated in the lattice. This investigation was carried out in order to check the effect of impurities on the surface structure.

Experimental Procédure

AU water used in this work was obtained from a commercial still producing water with a resistivity of 6 MΩ cm. This distilled water will be referred to as pure water. Dilute solutions of the following compounds were made with the pure water: NH4OH, HF, NH4C1, NaCl, and HCl. Polycrystalline ice samples were prepared from the solutions by attaching a droplet (approximately 2 mm in diameter) to a fine glass fibre mounted on the standard scanning electron microscope specimen stub (Reference Cross and CrossCross and Cross, 1968) and then freezing the droplet at — 50°C. The ice samples were then examined directly in the microscope without the use of replicas. A frozen droplet in the microscope takes roughly thirty minutes to evaporate to the point at which it falls from the fibre and is lost. Several samples of each type of ice were studied and the micrographs presented here were chosen as being representative of the appearance of each type of ice.

Fig. 1. Fig. 1 (top left). The surface of pure polycrrstalline ice, after 10 min evaporation. Instrument magnification× 2200.

Fig. 2a (top right). NH4OH doped ice, immediately after insertion in the microscope. Instrument magnification ×.2700.

Fig. 2b (bottom left). NH4OH doped ice, after 10 min evaporation. Instrument magnification × 2 600.

Fig. 2c (bottom right). NH4OH doped ice, after 15 min evaporation. Instrument magnification × 2 600.

Results

A typical micrograph of pure ice after ten minutes in the microscope is shown in Figure 1). The surface has the fine structure reported previously. Figure 2 shows three micrographs typical of dilute solutions of NH4OH. Concentrations of 10 parts per million and 100 parts per million were studied and no significant difference was seen between them. Soon after insertion in the microscope the surface had crystalline features as shown in Figure 2a. As evaporation proceeded the complex structures shown inFigure 2b and c developed.

Dilute solutions of HF behaved somewhat similarly, to the. NH4OH solutions. Initially the surface had a marked crystalline appearance as inFigure 3a and as the evaporation proceeded a complex surface structure developed but the structure varied with the concentration of HF. With a concentration of 10 parts per million the appearance was almost indistinguishable from the NH4OH solutions, as shown in Figure 3b. With 100 parts per million of HF the surface structure was lower and less delicate as shown in Figure 3c.

Fig.3. Fig·3a (top left) HF doped ice, immediately after insertion in the microscope. Instrument magnification × 700.

Fig.3b (top right). HF doped ice, 10p.p.m. after 10 min evaporation. Instrument magnification × 2300.

Fig.3c (bottom left). HF doped ice, 100 p.p.m. after 10 min evaporation. Instrument magnification × 2 300.

Fig.4a (bottom right). NH4Cl doped ice, immediately after insertion in the microscope. Instrument magnification × 250.

Ice made from dilute solutions of NH4C1 is initially crystalline in appearance as inFigure 4a and evaporation reveals an extremely complex surface structure as inFigure 4b and c. Increasing the concentration of NH4C1 from 10 parts per million to 100 parts per million produced a slightly more compact surface structure as in Figure 4c.

Fig. 4. Fig. 4b (top left). NH4C1 doped ice, 10 p.p.m. after 15 min evaporation. Instrument magnification × 1 200.

Fig. 4c (top right). NH4C1 doped ice, 100 p.p.m. after 15 min evaporation. Instrument magnification × 2500

Fig 5a (bottom left). HCl doped ice 4 p.p.m. after 15 min evaporation. Instrument magnification × 1 300.

Fig 5b (bottom right). HCl doped ice 40 p.p.m. after 10 min evaporation. Instrument magnification × 880

Ice doped with 4 parts per million and 40 parts per million of HC1 was examined and all specimens had a crystalline appearance as shown inFigure 5a and b. No fibrous surface structures were seen on any of the HC1 doped samples. A similar result was obtained with ice containing 10 parts per million of NaCl. A crystalline appearance as shown inFigure 6a was typical of this ice and in some cases at grain boundaries small spheroids of what appeared to be rejected impurities could be seen as inFigure 6b.

Fig.6. Fig. 6a (left). NaCl doped ice 10 p.p.m. after 10 min evaporation. Instrument magnification × 1300. Fig. 6b (right).NaCl doped ice 10 p.p.m after 10 min evaporation. Instrument magnification × 880.

Discussion

The micrographs show clearly that the presence of small quantities of impurities modifies the surface structure. Impurities that can be incorporated into the lattice enhance the surface structure as shown in Figures 2, 3 and 4. Impurities that are rejected by the ice suppress the fibrous surface completely structure. Ammonium tons and fluoride ions are only incorporated in the lattice in small quantities, therefore when water containing 100 parts per million of NH4OH, HF or. NH4C1 is frozen some of these impurities are rejected and accumulate at the grain boundaries. In the case of NH4OH the impurity is more volatile than the ice, and during evaporation the concentration of impurity at grain boundaries will remain small. In the case of HF and NH4C1 evaporation will result in an accumulation of impurities and the surface structure in these cases is less prominent. In the case of NaCl and HCl doping, the impurities are rejected and no surface structure develops. The conclusion to be drawn from these results is that the fibrous surface structure observed on evaporating polycrystalline ice is in some way a result of the large number of defects present and it is through the extra defects introduced by the ions that enter the lattice substitutionally that these ions enhance the complex surface structure. The fine structure cannot be attributed to an artifact of the microscope and it is possible (hat such a structure may exist in ice evaporating naturally.

Acknowledgements

The author wishes to thank Dr T. Nakaruma of the Department of Energy, Mines and Resources for providing the solutions used in this work and the Department of Agriculture for use of the scanning electron microscope.

Footnotes

page note *

Present address; Department of Electrical Engineering, University of Walerloo, Waterloo, Ontario, Canada.

References

Cross, J.D. 1969[a] Stunning electron microscopy of evaporating ice. Science, Vol. 164, No. 3876 p. 174–75. CrossRefGoogle Scholar
Cross, J.D. 1969[b] Study of the surface of ice with a scanning electron microscope, (In Riehl, N.,others, ed Physics of ice: proceedings of the international symposium on physics of ice, Munich, Germany, September 9–14, 1968 Edited by Riehl, N.,Bullemer, B.,Engelhardt, H.. New York, Plenum Press p. 81–94.) CrossRefGoogle Scholar
Cross, J.D. Cross, P.M. 1968 Scanning electron microscopy of materials containing water. Journal of Scientific Instruments (Journal of Physics, E) , Ser. 2, Vol. 1, No. 10, p. 1123–24. CrossRefGoogle ScholarPubMed
Cross, J.D. Speare, P.A. 1969 Electrical aspects of the evaporation of ice. British Journal of Applied Physics (Journal of Physics, D), Ser. 2, Vol. 2, No. 7, p. 1021–25. Google Scholar
Gukbman, A.A. Volynets, A.Z. 1968 O kharaktere sublimatsii l'da v vakuume [Nature of ice sublimation in vacuo]. Inzhenemo–Fizicheskiy Zhurnal, Tom 15, No. 5, p. 777–81. Google Scholar
Jaccard, C. 1967 Electrical conductivity of the surface layer of ice. (In Ōura H.,ed. Physics of snow and ice: international conference on low temperature science.… 1966… Proceedings, Vol. 1, Pt. 1. [Sapporo]. Institute of Low Temperature Science, Hokkaido University p. 173–79.) Google Scholar
Muguruma, J. 1969 Influence of the surface layer on the plastic deformation of ice single crystals. (In Riehl, N., ed. Physics of ice: proceedings of the international symposium on physics of ice, Munich, Germany, September 9–14, 1968 Edited by Riehl, N.,Bullemer, B.,Engelhardt, H..New York, Plenum Press p. 213–16.) CrossRefGoogle Scholar
Novikov, P.A. Vagnere, Y.A. 1968 Issledovaniye mekhanizma teplo– i massoobmena pri sublimatsii l'da y vakuume [Heat and mass transfer mechanism during ice sublimation in vacuo], Inzhenerno–Fizicheskiy Zhurnal, Tom 15, No. 5, p. 788–93. Google Scholar
Odencrantz, F.K. 1968 Mechanism for multiplication of atmospheric ice crystals: apparent charge distribution on laboratory crystals, by Odencrantz, F.K.,McEwan, W.S.,Amand, P. st,Finnegan, W.G.. Science, Vol. 160, No. 3834 p. 1345–46. CrossRefGoogle ScholarPubMed
Ruskin, R.E. 1969 Multiplication of ice embryos by ice–whisker sheddings. Science, Vol. 166, No. 3907 p. 906. CrossRefGoogle Scholar
Figure 0

Fig. 1. Fig. 1 (top left). The surface of pure polycrrstalline ice, after 10 min evaporation. Instrument magnification× 2200.Fig. 2a (top right). NH4OH doped ice, immediately after insertion in the microscope. Instrument magnification ×.2700.Fig. 2b (bottom left). NH4OH doped ice, after 10 min evaporation. Instrument magnification × 2 600.Fig. 2c (bottom right). NH4OH doped ice, after 15 min evaporation. Instrument magnification × 2 600.

Figure 1

Fig.3. Fig·3a (top left) HF doped ice, immediately after insertion in the microscope. Instrument magnification × 700.Fig.3b (top right). HF doped ice, 10p.p.m. after 10 min evaporation. Instrument magnification × 2300.Fig.3c (bottom left). HF doped ice, 100 p.p.m. after 10 min evaporation. Instrument magnification × 2 300.Fig.4a (bottom right). NH4Cl doped ice, immediately after insertion in the microscope. Instrument magnification × 250.

Figure 2

Fig. 4. Fig. 4b (top left). NH4C1 doped ice, 10 p.p.m. after 15 min evaporation. Instrument magnification × 1 200.Fig. 4c (top right). NH4C1 doped ice, 100 p.p.m. after 15 min evaporation. Instrument magnification × 2500Fig 5a (bottom left). HCl doped ice 4 p.p.m. after 15 min evaporation. Instrument magnification × 1 300.Fig 5b (bottom right). HCl doped ice 40 p.p.m. after 10 min evaporation. Instrument magnification × 880

Figure 3

Fig.6. Fig. 6a (left). NaCl doped ice 10 p.p.m. after 10 min evaporation. Instrument magnification × 1300. Fig. 6b (right).NaCl doped ice 10 p.p.m after 10 min evaporation. Instrument magnification × 880.