Abstract
The study of viscosity of blood at high heamatocrits and of packed cell systems leads to a conclusion that the interior of the red cell is fluid. The internal viscosity is suggested to be in the range from 2 to 20 centipoises. If the red cell is to exhibit fluidity, transfer of the tangential stresses (in flow) from the exterior to the interior of the red cell must not be inhibited by a rigid membrane. Consequently, the red cell membrane should be characterized by extremely low surface (interfacial) viscosity. It is suggested that a feasible model of the red cell membrane could be formed by a liquid-crystalline or micellar lattice arrangement of lipids and proteins. Such model would account naturally for the surface heterogeneity of the red cell and would supply a basis for the catalytic chemical reactions and the active transport considered to exist in the membrane.