Macroscopic longitudinal shrinkage of beech and poplar tension wood is high
er than in normal wood. This shrinkage is the result of mechanical interact
ions of cell wall layers. SEM observation of cut, dried surfaces showed tha
t longitudinal. shrinkage is much greater in the gelatinous layer than in o
ther layers. AFM topographic images of the same cells, both in water and in
air-dry conditions, confirm this result. Measurements on sections indicate
around 4.7% longitudinal shrinkage for the G layer.