Aliphatic ethers of cellulose are found to form stable monolayers
when spread from dilute chloroform
solution at the air−water interface. Monolayer pressure−area
isotherms exhibit a liquid analogous phase
followed by a transition region of relatively high compression at
constant pressure. Limiting molecular
areas are found to depend on side-chain length, indicating that the
hydrocarbon substituents do not adopt
an orientation strictly perpendicular to the water surface.
Monolayers of mixed ethers containing, on
average, a single long chain substituent per repeat unit, form liquid
analogous phases at molecular areas
equivalent to the area of the anhydroglucose ring. It is thus
concluded that the cellulose backbone lies
flat on the water surface. The transition region observed upon
compression beyond the liquid analogous
phase is attributed to the formation of bi- or multilayers, with
molecules leaving the water surface. This
interpretation is consistent with the observed decrease in plateau
pressure with increasing temperature.