MEGN 536 – Computational Biomechanics Prof. Anthony J. Petrella Bone Material Properties
Bone Macrostructure Long bone Epiphysis Diaphysis Compact bone (cortical) Spongy bone (cancellous) webschoolsolutions.com/patts/systems/skeleton.htm 12
1 academic.wsc.edu/faculty/jatodd1/351/ch4outline.html 2 castlefordschools.com/Kent/Lessons/Advanced%20Biology%20Lessons/chapter%2037/… Advanced%20Biology%20Chapter%2037%20Introduction%20to%20Body%20Structure_files/image026.jpg 2 Bone Microstructure Cortical bone Note circumferential layers Structure influences the material properties 1
Bone Microstructure Cancellous Bone Trabeculae – struts Notice axial alignment Some plate-like structures 40x 1 academic.wsc.edu/faculty/jatodd1/351/ch4outline.html
Bone Constituents Red marrow Red blood cells, platelets, most white blood cells arise in red marrow Found in flat bones (sternum, pelvis) and epiphyses Yellow marrow Some white blood cells arise here Color comes from much higher fat content Found in medullary canals of diaphyses in long bones Both types of marrow contain numerous vessels Lots of “squishy” stuff here
Bone Properties Like many biological tissues with “squishy” stuff, bone can behave viscoelastically -- Guedes et al., J.Biomech, 2006 Some studies have shown tensile and compressive behavior similar and linear elastic -- Keaveny et al., J.Biomech, 1994 Many studies have shown that bone is inhomogeneous and anisotropic Inhomogeneous – properties vary with location Anisotropic – properties vary with direction of loading Modulus for cortical bone usually in the GPa range, cancellous bone in the MPa range
Example: Inhomogeneous Strength
Inhomogeneity The inhomogenous nature of bone suggests that it’s important to model the material properties with correct spatial variation A recent study shows that patient-specific models are inaccurate without a correct inhomogeneous mapping of material properties -- Taddei et al., J.Biomech, 2006 One of the advantages of Mimics… the software can automate this inhomogeneous mapping
Hooke’s Law Recall Hooke’s law for a linear elastic, isotropic material: = E We also need to know Poisson’s ratio: Isotropic elastic requires only two constants: E, Many studies have shown that bone is transversely isotropic, which means the axial direction behaves differently than the radial direction Transverse isotropic materials exhibit properties that are invariant under axial rotation Recall axial alignment of bone structure…
Constitutive Models for Bone A transverse isotropic model requires five elastic constants: E z, E xy, xz = yz, xy, G xz = G yz These constants can be found experimentally, but most basic bone models in the literature still use an isotropic model for simplicity A transverse isotropic model also cannot be easily parameterized using CT data z x y
Bone Density Bone contains many internal structures/spaces and constituents besides calcified tissue Some density metrics try to account for this Apparent density (range: 0.05 – 2.0 g/cm 3 ) Your usual density measure Mass of sample divided by total volume of sample Ash density (range: 0.03 – 1.2 g/cm 3 ) Seeks to eliminate non-calcified tissue Mass of bone ash divided by volume of bone only Bone ash created by drying out bone and incinerating
Modulus Relationship to Density Density can be expressed as linear function of Hounsfield units = a + b * HU (g/cm 3 ) Modulus and strength have been shown to obey a power-law relationship to density E = c + d * e (GPa) S = f + g * h (MPa) Coefficients vary among different studies, but exponents are usually in the 1-3 range -- Keller, J.Biomech, 1994
Modulus-Density Relation also Inhomogeneous
Mapping Properties with Mimics For simplicity, we stay with a linear elastic, isotropic constitutive model Use Mimics automatic mapping to account for inhomogeneity Necessary number of materials depends on the specific model How much density variation is there? How large is the domain? Typical numbers of distinct materials in validation studies are in the range --Taddei, J.Biomech, 2006 We will use 10 materials