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K. Morgenstern, G. Rosenfeld, B. Poelsema, G. Comsa, Phys. Rev. Lett. 74, 2058 (1995); J.M. Wen, J.W. Evans, M.C. Bartelt, J.W. Burnett, P.A. Thiel, Phys. Rev. Lett. 76, 652 (1996); W.W. Pai, A.K. Swan, Z. Zhang, J.F. Wendelken, Phys. Rev. Lett. 79, 3210 (1997).
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K. Morgenstern, G. Rosenfeld, B. Poelsema, G. Comsa, Phys. Rev. Lett. 74, 2058 (1995); J.M. Wen, J.W. Evans, M.C. Bartelt, J.W. Burnett, P.A. Thiel, Phys. Rev. Lett. 76, 652 (1996); W.W. Pai, A.K. Swan, Z. Zhang, J.F. Wendelken, Phys. Rev. Lett. 79, 3210 (1997).
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edited by L. Pietronero, E. Tosatti Elsevier, Amsterdam
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M.H. Ernst, in Fractals in Physics, edited by L. Pietronero, E. Tosatti (Elsevier, Amsterdam, 1986) p. 289.
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The inclusion of this logarithmic factor ultimately leads to the flux rescaling F → F ln(1/F) in our primary results given in equations (8) (P.L. Krapivsky, J.F.F. Mendes, S. Redner, in preparation)
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The inclusion of this logarithmic factor ultimately leads to the flux rescaling F → F ln(1/F) in our primary results given in equations (8) (P.L. Krapivsky, J.F.F. Mendes, S. Redner, in preparation).
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14
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0009413920
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Similar rate equations describe the model of mobile adatoms and immobile islands, leading to somewhat similar island mass distribution. See e.g., N.V. Brilliantov, P.L. Krapivsky, J. Phys. A 24, 4787 (1991); J.A. Blackman, A. Wielding, Europhys. Lett. 16, 115 (1991); M.C. Bartelt, J.W. Evans, Phys. Rev. B 46, 12675 (1992).
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84956259961
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Similar rate equations describe the model of mobile adatoms and immobile islands, leading to somewhat similar island mass distribution. See e.g., N.V. Brilliantov, P.L. Krapivsky, J. Phys. A 24, 4787 (1991); J.A. Blackman, A. Wielding, Europhys. Lett. 16, 115 (1991); M.C. Bartelt, J.W. Evans, Phys. Rev. B 46, 12675 (1992).
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Wielding, A.2
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35949005765
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Similar rate equations describe the model of mobile adatoms and immobile islands, leading to somewhat similar island mass distribution. See e.g., N.V. Brilliantov, P.L. Krapivsky, J. Phys. A 24, 4787 (1991); J.A. Blackman, A. Wielding, Europhys. Lett. 16, 115 (1991); M.C. Bartelt, J.W. Evans, Phys. Rev. B 46, 12675 (1992).
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Note, however, that within the point-island description, the submonolayer regime is defined by the less stringent criterion N ≪ 1. This means that relatively long simulations are still within the submonolayer regime (Fig. 1)
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Note, however, that within the point-island description, the submonolayer regime is defined by the less stringent criterion N ≪ 1. This means that relatively long simulations are still within the submonolayer regime (Fig. 1).
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20
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0002986609
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J. Villain, A. Pimpinelli, D.E. Wolf, Comments Cond. Mat. Phys. 16, 1 (1992); I. Furman, O. Biham, Phys. Rev. B 55, 7917 (1997).
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Comments Cond. Mat. Phys.
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Villain, J.1
Pimpinelli, A.2
Wolf, D.E.3
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J. Villain, A. Pimpinelli, D.E. Wolf, Comments Cond. Mat. Phys. 16, 1 (1992); I. Furman, O. Biham, Phys. Rev. B 55, 7917 (1997).
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