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Volumn 126, Issue 11, 2007, Pages

Crystalline ice growth on Pt(111) and Pd(111): Nonwetting growth on a hydrophobic water monolayer

Author keywords

[No Author keywords available]

Indexed keywords

CRYSTALLINE ICE GROWTH; HYDROPHOBIC WATER MONOLAYER; LONE PAIR ELECTRONS;

EID: 34047176048     PISSN: 00219606     EISSN: None     Source Type: Journal    
DOI: 10.1063/1.2672869     Document Type: Article
Times cited : (68)

References (51)
  • 26
    • 0030284533 scopus 로고    scopus 로고
    • 26P. Löfgren, P. Ahlström, D. V. Chakarov, J. Lausmaa, and B. Kasemo, Surf. Sci. Lett. 367, L19 (1996).
    • 26P. Löfgren, P. Ahlström, D. V. Chakarov, J. Lausmaa, and B. Kasemo, Surf. Sci. Lett. 367, L19 (1996).
  • 30
    • 34047100632 scopus 로고    scopus 로고
    • For the results presented here, the important point is that the ASW films cover the water monolayer. As discussed in Ref. 16, the underlying reasons for this behavior, while not fully understood, may have both kinetic and energetic origins.
    • For the results presented here, the important point is that the ASW films cover the water monolayer. As discussed in Ref. 16, the underlying reasons for this behavior, while not fully understood, may have both kinetic and energetic origins.
  • 38
    • 34047096143 scopus 로고    scopus 로고
    • Since the second layer of Kr on Pt(111) is more stable than the first layer of Kr on the ice crystallites, the nominal ∼1.2 ML Kr adsorbs in two layers on the bare Pt(111) regions of the sample with the remainder adsorbing on the ice crystallites and producing the small peak at ∼ 38 K in the Kr TPD.
    • Since the second layer of Kr on Pt(111) is more stable than the first layer of Kr on the ice crystallites, the nominal ∼1.2 ML Kr adsorbs in two layers on the bare Pt(111) regions of the sample with the remainder adsorbing on the ice crystallites and producing the small peak at ∼ 38 K in the Kr TPD.
  • 39
    • 34047131482 scopus 로고    scopus 로고
    • Note that the shape assumed for the ice crystallites does not qualitatively change the model, while it does influence the specific numbers extracted from the model for the average spacing of ice crystallites
    • Note that the shape assumed for the ice crystallites does not qualitatively change the model, while it does influence the specific numbers extracted from the model for the average spacing of ice crystallites.
  • 44
    • 0003752338 scopus 로고
    • Cambridge University Press, Cambridge
    • A. Zangwill, Physics At Surfaces (Cambridge University Press, Cambridge, 1988).
    • (1988) Physics At Surfaces
    • Zangwill, A.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.