A threefold helical crystal structure of Bombyx mori silk fibroin has been
observed in films prepared from aqueous silk fibroin solutions using the La
ngmuir-Blodgett (LB) technique. The films were studied using a combination
of transmission electron microscopy and electron diffraction techniques. Fi
lms prepared at a surface pressure of 16.7 mN/m have a uniaxially oriented
crystalline texture, with the helical axis oriented perpendicular to the pl
ane of the LB him. Films obtained from the air-water interface without comp
ression have a different orientation, with the helical axes lying roughly i
n the plane of the film. In both cases the d-spacings observed in electron
diffraction are the same and match a threefold helical model crystal struct
ure, silk III, described in previous publications. Differences in the relat
ive intensities of the observed reflections in both types of oriented sampl
es, as compared to unoriented samples, allows estimations of orientation di
stributions and the calculations of orientation parameters. The orientation
of the fibroin chain axis in the plane of the interfacial film for uncompr
essed samples is consistent with the amphiphilic behavior previously postul
ated to drive the formation of the threefold helical silk III conformation.
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