메뉴 건너뛰기




Volumn 111, Issue 15, 1999, Pages 6947-6954

Growth of nanometer thin ice films from water vapor studied using scanning polarization force microscopy

Author keywords

[No Author keywords available]

Indexed keywords


EID: 0001009057     PISSN: 00219606     EISSN: None     Source Type: Journal    
DOI: 10.1063/1.479987     Document Type: Article
Times cited : (64)

References (54)
  • 1
    • 0003947869 scopus 로고
    • U.S. Army CRREL Special Report No. 94-22 U.S. Army Cold Regions Research and Engineering Laboratory, Hanover, New Hampshire, and also Ref. 2
    • For a review, see V. F. Petrenko, The Surface of Ice, U.S. Army CRREL Special Report No. 94-22 (U.S. Army Cold Regions Research and Engineering Laboratory, Hanover, New Hampshire, 1994), and also Ref. 2.
    • (1994) The Surface of Ice
    • Petrenko, V.F.1
  • 8
  • 10
    • 0043039452 scopus 로고    scopus 로고
    • For a review of lateral force microscopy, see, for example, R. W. Carpick and M. Salmeron, Chem. Rev. 97, 1163 (1997).
    • (1997) Chem. Rev. , vol.97 , pp. 1163
    • Carpick, R.W.1    Salmeron, M.2
  • 12
  • 13
    • 85034155340 scopus 로고    scopus 로고
    • Melcor Corporation, Trenton, New Jersey
    • Model CP0.8-127-06L, Melcor Corporation, Trenton, New Jersey.
    • Model CP0.8-127-06L
  • 15
    • 85034146093 scopus 로고    scopus 로고
    • note
    • The error in the calculation of the relative humidity is caused by the error in the temperature measurement.
  • 16
    • 85034153766 scopus 로고    scopus 로고
    • RHK Technology, Rochester Hills, Michigan
    • STM 100, RHK Technology, Rochester Hills, Michigan.
    • STM 100
  • 17
    • 33744624021 scopus 로고    scopus 로고
    • Park Scientific Instruments, Sunnyvale, California
    • Ultralevers, Park Scientific Instruments, Sunnyvale, California.
    • Ultralevers
  • 18
    • 85034151998 scopus 로고    scopus 로고
    • note
    • The drift was calculated from the lateral shift of characteristic features of the sample surface in consecutive images.
  • 20
    • 84973339075 scopus 로고    scopus 로고
    • edited by D. R. Lide, 78th ed. CRC Press, Boca Raton
    • CRC Handbook of Chemistry and Physics, edited by D. R. Lide, 78th ed. (CRC Press, Boca Raton, 1997).
    • (1997) CRC Handbook of Chemistry and Physics
  • 21
    • 85034120315 scopus 로고    scopus 로고
    • note
    • The error in the calculated value for the lever bending due to temperature changes was computed assuming a ±10% uncertainty in the length of the cantilever, its total thickness, and the thickness of the gold coating. The error in the experimental determination of the cantilever deflection caused by temperature changes is due to the error in the temperature measurement (±0.25°C) and the uncertainty in the piezo calibration (±0.1 nm).
  • 28
    • 85034136784 scopus 로고    scopus 로고
    • note
    • It is favorable to cleave the mica in the presence of water vapor to avoid charging of the mica sample, and to protect the mica surface from contaminants.
  • 32
    • 0000843188 scopus 로고    scopus 로고
    • M. Elbaum and S. G. Lipson, Phys. Rev. Lett. 72, 3562 (1994); S. G. Lipson, Phys. Ser. T76, 63 (1996).
    • (1996) Phys. Ser. , vol.T76 , pp. 63
    • Lipson, S.G.1
  • 34
    • 85034138143 scopus 로고    scopus 로고
    • note
    • Since there are no experimental results for heterogeneous nucleation of ice from supercooled water at -36°C, we have extrapolated curve no. 1 in Fig. 1 of Ref. 31 to obtain the value for the critical droplet diameter.
  • 41
    • 85034124854 scopus 로고    scopus 로고
    • note
    • The thickness of the ice layer found at -17°C is independent of the deposition time for deposition times between a few seconds and half a minute. The influence of deposition times longer than half a minute is currently under investigation.
  • 42
    • 85034140136 scopus 로고    scopus 로고
    • note
    • These experiments were performed in the same way as the experiments described in this paper, except that the process was repeated by twice cycling the temperature between -36 and -17°C. In these experiments, we found the same droplet heights (or film heights, respectively) at the respective temperatures as in the experiments presented here.
  • 44
    • 0030270275 scopus 로고    scopus 로고
    • H. Dosch, A. Lied, and J. Bilgram, Surf. Sci. 366, 43 (1996); 327, 145 (1995); A. Lied, H. Dosch, and J. H. Bilgram, Phys. Rev. Lett. 72, 3554 (1994).
    • (1996) Surf. Sci. , vol.366 , pp. 43
    • Dosch, H.1    Lied, A.2    Bilgram, J.3
  • 45
    • 0029291954 scopus 로고
    • H. Dosch, A. Lied, and J. Bilgram, Surf. Sci. 366, 43 (1996); 327, 145 (1995); A. Lied, H. Dosch, and J. H. Bilgram, Phys. Rev. Lett. 72, 3554 (1994).
    • (1995) Surf. Sci. , vol.327 , pp. 145
  • 46
    • 0000165849 scopus 로고
    • H. Dosch, A. Lied, and J. Bilgram, Surf. Sci. 366, 43 (1996); 327, 145 (1995); A. Lied, H. Dosch, and J. H. Bilgram, Phys. Rev. Lett. 72, 3554 (1994).
    • (1994) Phys. Rev. Lett. , vol.72 , pp. 3554
    • Lied, A.1    Dosch, H.2    Bilgram, J.H.3
  • 47
    • 84996203665 scopus 로고
    • N. H. Fletcher, Philos. Mag. 18, 1287 (1968); N. H. Fletcher, Philos. Mag. B 66, 109 (1992).
    • (1968) Philos. Mag. , vol.18 , pp. 1287
    • Fletcher, N.H.1
  • 48
    • 0042865185 scopus 로고
    • N. H. Fletcher, Philos. Mag. 18, 1287 (1968); N. H. Fletcher, Philos. Mag. B 66, 109 (1992).
    • (1992) Philos. Mag. B , vol.66 , pp. 109
    • Fletcher, N.H.1
  • 49
    • 0000620749 scopus 로고
    • V. F. Petrenko, J. Appl. Phys. 76, 1216 (1994); V. F. Petrenko and S. C. Colbeck, ibid. 77, 4518 (1995).
    • (1994) J. Appl. Phys. , vol.76 , pp. 1216
    • Petrenko, V.F.1
  • 51
    • 85034146790 scopus 로고    scopus 로고
    • note
    • The transition layer is situated between the bulk (ordered) ice crystal and the liquid-like layer on the ice surface. The x-ray diffraction studies cited in Ref. 42 could clearly distinguish between the transition layer and a liquid layer at the ice surface that was observed at temperatures higher than -12.8°C.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.