Cooperative deformation of mineral and collagen in bone at the nanoscale

  1. Himadri S. Gupta*,,
  2. Jong Seto*,
  3. Wolfgang Wagermaier*,
  4. Paul Zaslansky*,
  5. Peter Boesecke, and
  6. Peter Fratzl*
  1. *Department of Biomaterials, Max Planck Institute of Colloids and Interfaces, D-144-24 Potsdam, Germany; and
  2. Beamline ID2, European Synchrotron Radiation Facility, F-38043 Grenoble, France
  1. Edited by William D. Nix, Stanford University, Stanford, CA, and approved October 2, 2006 (received for review May 23, 2006)

  1. Fig. 1.

    Change in tissue, fibril, and mineral particle strain in bone with applied stress. (Upper) Ratio of fibril strain to tissue strain (εFT) and mineral strain to tissue strain (εMT), averaged over n = 29 samples. Solid lines are guides to the eye, showing the expected constant strain ratio before yield. Dashed lines show how the ratio would vary if the fibril and mineral strains remain constant beyond the yield point, marked with the vertical dashed line. Error bars are standard errors of the mean. (Lower) Typical stress–strain curve of bovine fibrolamellar bone packet, showing an initial elastic increase followed by a reduced slope beyond the elastic/inelastic transition at εTY = 0.91%. The schematic on the right illustrates the different hierarchical length scales at which strain is being measured simultaneously (tissue, fibril, and mineral nanoparticle).


  2. Fig. 2.

    Correlation between mineral and fibril strain. Fibril and mineral strain are first binned in regular intervals of tissue strain, and then plotted versus each other. Open squares: wet, n = 29 samples, and filled circles: dry, n = 7 samples. Straight lines give linear regressions on the two data sets, and regression slopes give the mineral particle strain fraction in the enclosing fibril. Mineral particles take up a lower strain fraction in the fibrils when the tissue is wet. Slope for wet samples = 0.34 ± 0.15 and for dry samples = 0.53 ± 0.04. Error bars in the graph are standard errors of mean.


  3. Fig. 3.

    Mineral strain ratio as a function of sample elastic modulus. The average mineral strain ratio 〈εMT〉 is plotted, per sample, versus the elastic modulus E T. Open squares: wet, n = 29 samples and filled circles: dry, n = 7 samples. Lines show the expected nonlinear correlation between mineral strain fraction 〈εMT〉 and elastic modulus E T when stresses are transferred within and between the mineralized fibrils in a hierarchical staggered arrangement (see Fig. 4 and Eq. 1). Solid, wet collagen; dashed, dry collagen.


  4. Fig. 4.

    Schematic model for bone deformation in response to external tensile load at three levels in the structural hierarchy: at the tissue level (Left), fibril array level (Center), and mineralized collagen fibrils (Right). (Center) The stiff mineralized fibrils deform in tension and transfer the stress between adjacent fibrils by shearing in the thin layers of extrafibrillar matrix (white dotted lines show direction of shear in the extrafibrillar matrix). The fibrils are covered with extrafibrillar mineral particles, shown only over a selected part of the fibrils (red hexagons) so as not to obscure the internal structure of the mineralized fibril. (Right) Within each mineralized fibril, the stiff mineral platelets deform in tension and transfer the stress between adjacent platelets by shearing in the interparticle collagen matrix (red dashed lines indicate shearing qualitatively and do not imply homogeneous deformation).


  5. Fig. 5.

    Sample preparation setup. (a) Appearance of 50- to 100-μm-thick and ≈1-cm-wide fibrolamellar bone sheets (Left) after sectioning from pie-shaped sectors of bovine femoral bone (Right). L (longitudinal, parallel to bone long axis), R (radial, from center of bone to periosteum), and T (tangential to bone surface) denote the approximate coordinate system used. (b) A UV laser (1–2 μm diameter at focus) is rastered repeatedly (up to 10 times) over the bone sheets in the form of the elongated sample shape, until the sample is separated from the surrounding tissue, and can be removed. (c) (Left) A typical sample lying next to the source sheet from which it was taken. (Right) Schematic of sample mounted on plastic grips with cyanoacrylate glue.


  6. Fig. 6.

    In-beam microtensile schematic: Microtensile setup is inclined to the direct X-ray beam at 1/2 (2θ[0002]) ≈ 8.3° [where 2θ[0002] is the Bragg angle for (0002) hydroxyapatite c-axis reflection at λ = 0.0995 nm] to ensure that the strain from only the crystallites with c-axis along the tensile axis of the sample is measured. Sample is kept wet by enclosing within cellophane slips containing a water drop (Inset B). Tissue strain εT is determined by tracking marker lines (Inset A) in images taken by a CCD camera (not shown). SAXS and WAXD 2D images are recorded simultaneously by the FRELON 2000 CCD and Princeton Instruments CCD detectors respectively. The integrated diode on the beamstop is used for intensity normalization.


Footnotes

  • To whom correspondence should be addressed. E-mail: himadri.gupta{at}mpikg.mpg.de
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