TY - JOUR
T1 - A multi-phase SPH method for macroscopic and mesoscopic flows
AU - Hu, Xiang Yu
AU - Adams, N. A.
PY - 2006/4/10
Y1 - 2006/4/10
N2 - A multi-phase smoothed particle hydrodynamics (SPH) method for both macroscopic and mesoscopic flows is proposed. Since the particle-averaged spatial derivative approximations are derived from a particle smoothing function in which the neighboring particles only contribute to the specific volume, while maintaining mass conservation, the new method handles density discontinuities across phase interfaces naturally. Accordingly, several aspects of multi-phase interactions are addressed. First, the newly formulated viscous terms allow for a discontinuous viscosity and ensure continuity of velocity and shear stress across the phase interface. Based on this formulation thermal fluctuations are introduced in a straightforward way. Second, a new simple algorithm capable for three or more immiscible phases is developed. Mesocopic interface slippage is included based on the apparent slip assumption which ensures continuity at the phase interface. To show the validity of the present method numerical examples on capillary waves, three-phase interactions, drop deformation in a shear flow, and mesoscopic channel flows are considered.
AB - A multi-phase smoothed particle hydrodynamics (SPH) method for both macroscopic and mesoscopic flows is proposed. Since the particle-averaged spatial derivative approximations are derived from a particle smoothing function in which the neighboring particles only contribute to the specific volume, while maintaining mass conservation, the new method handles density discontinuities across phase interfaces naturally. Accordingly, several aspects of multi-phase interactions are addressed. First, the newly formulated viscous terms allow for a discontinuous viscosity and ensure continuity of velocity and shear stress across the phase interface. Based on this formulation thermal fluctuations are introduced in a straightforward way. Second, a new simple algorithm capable for three or more immiscible phases is developed. Mesocopic interface slippage is included based on the apparent slip assumption which ensures continuity at the phase interface. To show the validity of the present method numerical examples on capillary waves, three-phase interactions, drop deformation in a shear flow, and mesoscopic channel flows are considered.
KW - Macroscopic and mesoscopic flows
KW - Multi-phase flows
KW - Particle method
UR - http://www.scopus.com/inward/record.url?scp=32644451844&partnerID=8YFLogxK
U2 - 10.1016/j.jcp.2005.09.001
DO - 10.1016/j.jcp.2005.09.001
M3 - Article
AN - SCOPUS:32644451844
SN - 0021-9991
VL - 213
SP - 844
EP - 861
JO - Journal of Computational Physics
JF - Journal of Computational Physics
IS - 2
ER -