megn 536 – computational biomechanics prof. anthony j. petrella bone material properties
TRANSCRIPT
Bone Macrostructure
Long bone Epiphysis Diaphysis Compact bone (cortical) Spongy bone (cancellous)
1www.agen.ufl.edu/~chyn/age2062/lect/lect_19/lect_19.htm2webschoolsolutions.com/patts/systems/skeleton.htm
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Bone Microstructure
Cortical bone Note circumferential layers Structure influences the material properties
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Bone Microstructure
Cancellous Bone Trabeculae – struts Notice axial alignment Some plate-like structures
40x1academic.wsc.edu/faculty/jatodd1/351/ch4outline.html2www.gla.ac.uk/ibls/fab/public/docs/xbone1x.html
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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 inhomogeneousand anisotropic Inhomogeneous – properties vary with location Anisotropic – properties vary with direction of loading
Modulus for cortical bone usually in the 15-20 GPa range, cancellous bone in the 100-500 MPa range
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: s = E e
We also need to know Poisson’s ratio: n Isotropic elastic requires only two constants: E, n
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 ofbone structure…
Constitutive Models for Bone
A transverse isotropic model requiresfive elastic constants:
Ez, Exy, nxz = nyz, nxy, Gxz = Gyz
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
zxy
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/cm3) Your usual density measure Mass of sample divided by total volume of sample
Ash density (range: 0.03 – 1.2 g/cm3) 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
r = a + b * HU (g/cm3)
Modulus and strength have been shown to obey a power-law relationship to density
E = c + d * re (GPa)S = f + g * rh (MPa)
Coefficients vary among different studies, but exponents are usually in the 1-3 range
-- Keller, J.Biomech, 1994
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 100-500 range --Taddei, J.Biomech, 2006
We will use 10 materials