ABSTRACT
Water, collagen and mineral are the three major components of bone. The structural organization of water and its functions within the bone were investigated using the environmental scanning electron microscope and by analyzing dimensional changes that occur when fresh equine osteonal bone is dehydrated and then rehydrated. These changes are attributed mainly to loss of bulk and weakly bound water. In longitudinal sections a contraction of 1.2% was observed perpendicular to the lamellae, whereas no contraction occurred parallel to the lamellae. In transverse sections a contraction of 1.4% was observed both parallel and perpendicular to the lamellae. SEM back scattered electron images showed that about half of an individual lamella is less mineralized, and thus has more water than the other half. We therefore propose that contractions perpendicular to lamellae are due to the presence of more water-filled rather than mineral-filled channels within the mineralized collagen fibril arrays. As these channels are also aligned with the crystal planes, the crystal arrays, oriented as depicted in the rotated plywood model for lamellar bone, facilitate or hinder contraction in different directions.
