OSTEOPOROSIS is as universal an alteration of aging bone as is osteoarthritis of aging joints. Together these comprise the main symptom-producing manifestations of skeletal senility. Although osteoporosis appears to be physiological in aging bone, its degree is very variable from person to person.
PATHOLOGICAL PHYSIOLOGYPathologically, osteoporotic bone is characterized by fewer and less thick trabeculae. Functionally such bone is more susceptible to compression and fracture, but until fracture occurs there is preservation of bone contour. So far as is now known, there is no biochemical difference between the thin trabeculae and those of normal presenile bone ; the protein matrix is the same, as is the bone salt, which is deposited in the matrix in an apatite crystal lattice. The ratio of minerals to matrix is probably the same in osteoporotic as in normal bone.The skeleton is normally in a state of dynamic equilibrium, with bone resorption and bone production occurring constantly at dif¬ ferent trabecular surfaces (Fig., left). Re¬ sorption of bone salt is a passive process, which occurs because the body fluids are undersaturated with respect to calcium and phosphorus, the main components of the bone salt. Concomitant with résorption of the bone salt the matrix in which it had been deposited disappears. Osteoclasts are an index of this process and are engaged in the removal of the matrix. Bone production is an active process : Osteoblasts manufacture ma¬ trix and the enzyme alkaline phosphatase, which increases the local concentration of phosphorus by its action on organic phos¬ phates. The increased phosphorus concen¬ tration permits immediate precipitation of bone salt into the newly formed bone matrix.The number of osteoblasts is an index of the activity of bone production. The level of the serum alkaline phosphatase is a rough index of osteoblastic activity.In osteoporosis (Fig., right) the serum levels of calcium and phosphorus are normal, and the rate of bone résorption is therefore assumed to be normal. The thin trabeculae, then, must be due to an underproduction of sufficient new bone to maintain normal bal¬ ance.Histologically, the osteoblasts and osteoclasts appear qualitatively and quantita¬ tively normal. The level of the serum alka¬ line phosphatase also tends to be normal in osteoporosis. Thus, proof that osteoporosis is due to decreased bone production rather than to increased bone résorption is not avail¬ able histologically or chemically. It none¬ theless appears to be the more logical cause of osteoporosis if it is agreed that résorption is a passive process, while production of bone is a more complicated active process.The slowness with which senile osteo¬ porosis develops suggests that the decrease in osteoblastic activity is exceedingly small relative to continuing bone production, and a decrease in osteoblasts would not be ex¬ pected to be observable by routine histological study. Similarly, a decrease in alkaline phosphatase would not be anticipated.With equilibrium of bone résorption and ...