Abstract
Bone is unique among structural materials in that it is self-repairing and can alter its properties and configuration in response to changes in mechanical demand (Hayes, 1979; Hayes and Snyder, 1981; Jowsey, 1977; Lane and Vigorita, 1983; Woo et al, 1981). Certain skeletal conditions such as osteoporosis can seriously compromise the structural integrity of the skeleton (Avioli, 1983; Jowsey, 1977). The associated reduction in bone mass gradually increases vulnerability to fracture, particularly of the femoral neck and vertebrae (Jowsey, 1977; Kelsey et al, 1978; Lane and Vigorita, 1983). The frequency of osteoporosis in the United States is well recognized, with 50% of women 45 years of age or older exhibiting radiographic evidence of osteoporosis of the lumbar spine (Kelsey et al, 1978). From 16–18 million women in the United States have a significant degree of vertebral atrophy and over 4 million women aged 50 years or older have osteoporosis severe enough to cause vertebral fractures. Epidemiologic studies suggest that from 15-30% of all white women in the United States develop symptomatic osteoporosis (Kelsey et al, 1978; Lane and Vigorita, 1983). Of approximately one million fractures experienced each year by women 45 years or older in the United States, about 700,000 are incurred by women with osteoporosis.
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Hayes, W.C. (1986). Basic Biomechanics of the Skeleton. In: Uhthoff, H.K. (eds) Current Concepts of Bone Fragility. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-70709-4_1
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DOI: https://doi.org/10.1007/978-3-642-70709-4_1
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