A melt of linear diblock copolymers (A(n)B(m)) can form a diverse range of
microphase separated structures. The detailed morphology of the microstruct
ure depends on the length of the polymer blocks A(n) and B-m and their mutu
al solubility. In this paper, the role of hydrodynamic forces in microphase
formation is studied. The microphase separation of block copolymer melts i
s simulated using two continuum methods: dissipative particle dynamics (DPD
) and Brownian dynamics (BD). Although both methods produce the correct equ
ilibrium distribution of polymer chains, the BD simulation does not include
hydrodynamic interactions, whereas the DPD method correctly simulates the
(compressible) Navier Stokes behavior of the melt. To quantify the mesophas
e structure, we introduce a new order parameter that goes beyond the usual
local segregation parameter and is sensitive to the morphology of the syste
m. In the DPD simulation, a melt of asymmetric block copolymers rapidly evo
lves towards the hexagonal structure that is predicted by mean-field theory
, and that is observed in experiments. In contrast, the BD simulation remai
ns in a metastable state consisting of interconnected tubes, and fails to r
each equilibrium on a reasonable time scale. This demonstrates that the hyd
rodynamic forces play a critical part in the kinetics of microphase separat
ion into the hexagonal phase. For symmetric block copolymers, hydrodynamics
appears not to be crucial for the evolution. Consequently, the lamellar ph
ase forms an order of magnitude faster than the hexagonal phase does, and t
hus it would be reasonable to infer a higher viscosity for the hexagonal ph
ase than for the lamellar phase. The simulations suggest that the underlyin
g cause of this difference is that the hexagonal phase forms via a metastab
le gyroid-like structure, and therefore forms via a nucleation-and-growth m
echanism, whereas the lamellar phase is formed via spinodal decomposition.
(C) 1999 American Institute of Physics. [S0021-9606(99)51819-9].