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MECHANOBIOLOGY OF FRACTURE HEALING

Fracture healing is one of the most frequently employed scenarios for studies of the effects the local mechanical environment on skeletal tissue differentiation. Mechanical

loading of a fracture callus occurs most commonly as a consequence of weight bearing; however, dynamization, or applied micromotion, of the fracture gap has also been investigated. Results of these studies have shown that the effects of loading depend heavily on the mode [35], rate [36], and magnitude of loading [37], as well as gap size [37]

and the time during healing at which the dynamization is enacted (eg, [38]). Application of cyclic compressive dis- placements can enhance healing through increased callus formation and more rapid ossification and bridging [39].

However, the benefits of applied cyclic compressive dis- placements appear to be limited to displacements that induce an interfragmentary strain (defined as the ratio of applied displacement to the gap size) of 7% or less [35,37].

Moreover, dynamization of the fracture gap appears to be detrimental in the very  early stage of healing [38], yet beneficial during later stages [40,41].

As evidenced by the success of distraction osteogenesis in both experimental and clinical settings, application of successive tensile displacements across an osteotomy gap can also promote bone formation. In contrast to the effects of cyclic compressive loading, however, bone formation in distraction osteogenesis occurs primarily via intramem- branous ossification. These characteristics of distraction also appear to hold when the tensile displacements are applied for only 2 days at a time, followed by shortening of the osteotomy gap to its original length [42], but not when the tensile displacements are applied in a true oscillatory manner (eg, 1 to 10 Hz frequency) [35]. The effects of shear or transverse movement at the fracture site are controver- sial [43]. Studies investigating the use of a bending motion to an osteotomy gap reported formation of cartilage rather than bone within the gap [44].

In parallel with some of the earlier experimental inves- tigations summarized earlier, and Perren and Cordey [45]

proposed the interfragmentary strain theory, which states that only tissue that is capable of withstanding the pre- sent value of interfragmentary strain can form in the fracture gap. This theory is consistent with observations that granulation tissue forms initially in the gap, followed by cartilage and then bone. The successive formation of each type of tissue further reduces the interfragmentary strain that occurs as a result of the applied load and allows a stiffer tissue to form next.

The interfragmentary strain theory presents an over- simplified description of the mechanical environment within the fracture gap in that it uses one scalar (inter- fragmentary strain) to describe a multiaxial strain field that varies as a function of position within the gap.

More recent models of the mechanobiology of skeletal tissue differentiation have sought to account for this complexity by considering the distributions of local mechanical stimuli present throughout the fracture gap (Fig.  14.5A–C) [46–48] and the interplay between osteogenesis and angiogenesis (Fig. 14.5D) [49]. Carter and colleagues have proposed that different combina- tions of hydrostatic pressure and tensile strain promote the formation of different skeletal tissues [46], while Claes and Heigle have postulated that these two Fig.  14.4. An application of RUST scores to each of the four

cortices visible on the anterior–posterior and lateral radiographs of a tibial shaft fracture. The RUST score for this callus was 8 out of a maximum of 12. The score for each cortex was: medial cortex (RUST = 2), lateral cortex (RUST = 3), anterior cortex (RUST = 2), and posterior cortex (RUST = 1). Source: [33] (images not to scale).

Reproduced with permission of Lippincott Williams & Wilkins.

stimuli regulate intramembranous versus endochon- dral ossification [47]. Shefelbine and colleagues adapted this model to also include bone resorption and tissue failure [30]. Lacroix and Prendergast have instead proposed that the two key stimuli are shear strain and fluid flow [48]. Direct comparison of these models’ pre- dictions to histological analyses of bone healing, and also experimental measurement of local mechanical

stimuli such as shear strain within a bone defect, sug- gests that the most accurate predictions are those based on shear strain and fluid flow [44,50]. However, each of these theories is unable to predict certain histologi- cal features of the fracture healing process [48,50]

indicating that the definitive role of the local mechani- cal environment in modulating healing has yet to be elucidated fully.

Principal tensile strain history

Fibro-

cartilage Fibrous tissue Tension line

Cartilage

Pressure line

(–) Compression Tension (+)

Hydrostatic stress history 0

Bone (A)

Strain [%]

15

–0.15 5

–5 –15

Connective tissue or fibrocartilage Intramembranous ossification Endochondral ossification

Hydrostatic pressure [MPa]

0.15 (B)

Fluid flow

Fluid flow

Tissue shear strain

Resorption Granulation tissue

(mesenchymal cells)

Time = 0

Time

Bone Cartilage

Fibrous connective

tissue (C)

Tissue shear strain

Resorption Granulation tissue

(mesenchymal cells)

Time = 0

Time

Bone Cartilage

Fibrous connective

tissue

Rules:

IF (S = ‘bone’ AND O

2

low) THEN CARTILAGE

IF (S = ‘bone’ AND O

2

high) THEN BONE

(D)

Fig. 14.5. Models of the mechanobiology of skeletal tissue differentiation by: (A) Carter and colleagues; (B) Claes and Heigle; (C) Lacroix and Prendergast; and (D) Checa and Prendegast. (A) Source: [46]. Reproduced with permission of Wolter Kluwer. (B) Source:  [47]. Reproduced with permission of Elsevier. (C) Source: [48]. Reproduced with permission of Elsevier. (D) Source: [49].

Reproduced with permission of Springer.

­eferences 113

SUMMARY

An essential outcome in fracture healing is restoration of sufficient mechanical integrity to allow weight bearing and activities of daily living. Thus, biomechanical analyses of fracture healing are critical for thorough assessment of the repair process. At present, the biomechanical progression of secondary fracture healing is well characterized, and standardized in vitro methods of quantifying the extent of healing have been established. Noninvasive methods of measuring the regain of bone stiffness have also been reported; however, development of noninvasive methods of measuring the regain of strength has lagged behind.

Studies to date on the effects of mechanical factors indicate that it is possible to augment healing via mechanical load- ing, and the growing body of literature in this area suggests that further enhancements in healing may be possible.

Thus, an understanding of the biomechanics of fracture healing can be applied not only to the assessment of heal- ing but also to development of new repair strategies.

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Primer on the Metabolic Bone Diseases and Disorders of Mineral Metabolism, Ninth Edition. Edited by John P. Bilezikian.

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