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Department of Chemistry, North Carolina State University, Dabney Hall, Campus Box 8204, Raleigh, North Carolina, 27695-8204, U.S.A., e-mail: marta.cerruti@gmail.com
Department of Geology and Geophysics, Department of Chemistry, Environmental Chemistry and Technology Program, University of Wisconsin, Madison, Wisconsin, 53706, U.S.A., e-mail: sahai@geology.wisc.edu
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| INTRODUCTION |
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In this chapter, we will provide a brief history of the use of implants, and review the requirements that a biomaterial must fulfill to be used effectively as an orthopaedic or dental implant, the chemical composition-structure-activity of different types of silicate biomaterials including glasses and ceramics, the chemical reactions that occur at the silicate implant/solution interface involving inorganic ions and organic biomolecules (mainly proteins). We will also review studies that show the effects of different synthetic solutions, used experimentally to mimic human blood plasma, on in vitro tests of bioactivity. Our focus will be on dense silicate biomaterials that have up to ~20% porosity and high mechanical strength, in contrast to porous biomaterials with ~4060% porosity and scaffold materials that have ~80% porosity and almost no mechanical
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N. Sahai, M. A. A. Schoonen, and H. C. W. Skinner The Emergent Field of Medical Mineralogy and Geochemistry Reviews in Mineralogy and Geochemistry, January 1, 2006; 64(1): 1 - 4. [Full Text] [PDF] |
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