The flow of isotropic and liquid-crystalline hydroxypropylcellulose-wa
ter solutions is studied in a transparent slit die with several geomet
ries including divergent and convergent configurations. The flow is ob
served between crossed polars. In addition to the two different flow r
egimes that are known in shear (zones I and II), a new flow behavior i
s observed (zone III). Zone I is characterized by a large macroscopic
orientation, as seen between crossed polars. It is localized where eit
her shear rates or elongation rates are large. The extinction angle is
a function of the position in the die. It is similar to the flow-alig
ning regime observed at high shear rates. Zone II is much less oriente
d, due probably to a large density of defects. It is typical of the lo
w shear rate region observed in simple shear. Zone III exhibits a pecu
liar behavior with long-range orientation instabilities. It is always
localized after a diverging zone. Flow around obstacles and colliding
streams are also studied.