|  | List of Accepted Contributions - NP6.07 Turbulence and dispersion in particle-laden geophysical flows: theory and models (co-listed in HS & SSP) 
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  |  | EGU2007-A-00736 Horvai, P; Nazarenko, S; Stein, T
 Coalescence of gravitationally settling particles
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  |  | EGU2007-A-01645 Wilkinson, M. ; Mehlig, B.; Ostlund, S. ; Duncan, K.
 Unmixing in random flows
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  |  | EGU2007-A-01897 Calzavarini, E.; Biferale, L.; Cencini, M.; Lohse, D.; Toschi, F.
 Preferential concentrations of finite-size massive particles by turbulence
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  |  | EGU2007-A-02381 Wilkinson, M; Mehlig, B; Uski, V; Bezuglyy, V
 Caustics, Collisions and the Stokes Trap
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  |  | EGU2007-A-02457 Grabowski, W. W.; Wang, L.-P.; Vaillancourt, P.
 Impact of cloud turbulence on growth of cloud droplets
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  |  | EGU2007-A-02749 Chauchat, J.; Guillou, S.; Nguyen, K.D.
 A 2D vertical two-phase flow model for sediment laden flows
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  |  | EGU2007-A-07184 Bourgoin, M.; Qureshi, N.; Cartellier, A.; Gagne, Y. ; Baudet, C.
 Turbulent transport of material particles
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  |  | EGU2007-A-10345 Hill, K; DellAngelo, L; Shaffer, G
 Model studies of different sized tracer particles in bedload transport
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  |  | EGU2007-A-10565 Leung, V.; Mohrig, D.
 Establishing an Unambiguous Connection between Grain Size, Basal Shear Stress and Style of Sediment Transport in the Lower Niobrara River, Nebraska, USA
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  |  | EGU2007-A-10785 Xu, H.; Bodenschatz, E.
 Experimental study of inertial particles in fully developed turbulence
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  |  | EGU2007-A-10965 Bazarov, Y.B.; Levushov, A.E.; Meshkov, E.E.; Polovnikov, A.A:
 Self-organizing of Fibre-like Structures in Turbulent Gas and Dust Clouds (withdrawn)
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  |  | EGU2007-A-11075 Le Louvetel-Poilly, J; Bigillon, F; Champagne, JY
 Experimental investigation on the turbulent structures involved in particle motion (withdrawn)
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  |  | EGU2007-A-11452 Bec, J.; Cencini, M.; Hillerbrand, R.
 Very heavy particles in incompressible flows: the large Stokes number asymptotics
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  |  | EGU2007-A-11468 Seminara, A.; Celani, A. ; Lanotte, A. ; Toschi, F.
 Microdroplets growth by condensation in warm clouds
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