How can bone turnover modify bone strength independent of bone mass.pdf

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doi:10.1016/j.bone.2008.02.001
Bone 42 (2008) 1014
1020
www.elsevier.com/locate/bone
Review
How can bone turnover modify bone strength independent of bone mass?
C.J. Hernandez
Musculoskeletal Mechanics and Materials Laboratory, Case Western Reserve University, Cleveland, OH, USA
Department of Mechanical and Aerospace Engineering, Case Western Reserve University, Cleveland, OH, USA
Department of Orthopaedics, Case Western Reserve University, Cleveland, OH, USA
Received 2 January 2008; revised 22 January 2008; accepted 2 February 2008
Available online 20 February 2008
Abstract
The amount of bone turnover in the skeleton has been identified as a predictor of fracture risk independent of areal bone mineral density (aBMD)
and is increasingly cited as an explanation for discrepancies between areal bone mineral density and fracture risk. A number of mechanisms have been
proposed to explain how bone turnover influences bone biomechanics, including regulation of tissue degree of mineralization, the disconnection or
fenestration of individual trabeculae by remodeling cavities, and the ability of cavities formed during the remodeling process to act as stress risers.
While these mechanisms can influence bone biomechanics, they also modify bone mass. If bone turnover is to explain any of the observed
discrepancies between fracture risk and areal bone mineral density, however, it must not only modify bone strength, but must also modify bone
strength in excess of what would be expected from the associated change in bone mass. This article summarizes biomechanical studies of how tissue
mineralization, trabecular disconnection, and the presence of remodeling cavities might have an effect on cancellous bone strength independent of
bone mass. Existing data support the idea that all of these factors may have a disproportionate effect on bone stiffness and/or strength, with the
exception of average tissue degree of mineralization, which may not affect bone strength independent of aBMD. Disproportionate effects of mineral
content on bone biomechanics may instead come from variation in tissue degree of mineralization at the micro-structural level. The biomechanical
explanation for the relationship between bone turnover and fracture incidence remains to be determined, but must be examined not in terms of bone
biomechanics, but in terms of bone biomechanics relative to bone mass.
© 2008 Elsevier Inc. All rights reserved.
Keywords: Bone turnover; Bone remodeling; Bone quality; Bone biomechanics
Contents
Introduction ............................................................... 1014
Bone volume ............................................................ 1015
Tissue degree of mineralization ................................................... 1016
Disconnection of trabeculae ..................................................... 1017
Remodeling cavities ......................................................... 1017
Conclusions ............................................................... 1018
Acknowledgments ............................................................ 1019
References ................................................................ 1019
Introduction
Glennan 615A, 10900 Euclid Avenue, Cleveland, OH 44106-7222, USA.
Bone turnover represents the total volume of bone that is
both resorbed and formed over a period of time [1] . In adults,
bone turnover occurs primarily through bone remodeling, a
focal process that involves the coupled activity of osteoclasts
8756-3282/$ - see front matter © 2008 Elsevier Inc. All rights reserved.
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C.J. Hernandez / Bone 42 (2008) 1014 1020
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Table 1
The reduction in human cancellous bone stiffness and strength associated with a 6% difference in bone volume or mass is shown
Process through which bone
remodeling modifies bone mass
Difference in
bone mass
Expected reduction
in stiffness
Expected reduction
in strength
Source
Reduction in bone volume
6% (volume)
12 16%
9 14%
Empirical power law models
[14,17 21]
Reduction in average tissue degree of
mineralization from 65% to 62%
ash by weight
6% (bone mineral content)
11 13%
11 13%
95% confidence interval from
empirical power law models
[41]
Intraspecimen variation in tissue
degree of mineralization
0% reduction in bone mass;
increase in COV of tissue
mineralization from 20% to 50%
14 24%
Not yet evaluated Micro-computed tomography
based finite element models
[45,46]
6% (volume) 3 39% 18 35% 3D cellular solid finite element
models [50,51]
Addition of remodeling cavities 6% (volume) 12 47% 13 61% Micro-computed tomography
based finite element models
[53,55]
The 95%confidence interval is reported if available, otherwise the range across all cited studies is shown. A factor that causes a greater change in bone stiffness or strength
than that caused by a 6% reduction in bone volume (the first row) has the potential to explain how bone turnover can influence fracture risk independent of bone quantity.
and osteoblasts [2] . Changes in the amount of bone turnover
cause local changes in bone volume and affect the average age of
tissue in a bone, resulting in alterations in tissue degree of
mineralization and trabecular microarchitecture. Clinical find-
ings that biochemical markers of bone turnover can predict
fracture risk independent of areal bone mineral density (aBMD)
have led to the suggestion that the amount of bone turnover in
the skeleton can have a biomechanical effect independent of
bone mass 1
summarized in Table 1 a 6% decline in bone mass was
selected as it is the estimated size of the remodeling space in
the spine [11] .
Bone volume
8] , and that bone turnover may help to explain
discrepancies between aBMD and fracture risk [5,6] . The
biomechanical effects of alterations in bone turnover are
commonly attributed to modifications in tissue degree of
mineralization, the fenestration or disconnection of individual
trabeculae, and/or remodeling cavities acting as stress risers
[4,6
[3
Because the first step in the remodeling process is bone
resorption, each remodeling event is associated with the for-
mation of a temporary cavity. The total volume of bone oc-
cupied by all remodeling cavities and unmineralized bone tissue
(osteoid) is known collectively as the remodeling space [12] .
Increases in bone turnover result in an increase in the volume
occupied by the remodeling space and cause a corresponding
reduction in mineralized bone volume.
Biomechanical testing of cancellous bone specimens has
shown that bone stiffness and strength are related to apparent
density (
9] . While these mechanisms can influence bone strength,
they also modify bone mass. If one of these mechanisms is to
explain any of the discrepancies between aBMD and fracture
risk, however, it must have an effect on bone strength that is
much larger than would be expected from the change in bone
mass alone. The purpose of this article is to review the
biomechanical effects of changes in bone that can be caused
by bone turnover. The current article concentrates on the
biomechanics of human cancellous bone specimens 3
, g/cm 3 ) through power law relationships. Because
apparent density is directly related to bone volume fraction (BV/
TV) [13] , the same power law relationships are valid for bone
volume fraction as well. These power law relationships can be
expressed as follows:
ρ
5mmin
smallest dimension, as that is the scale at which the mecha-
nisms mentioned above all have biomechanical significance.
Biomechanics of bone at this size scale is also important
because a factor that does not have a disproportionate bio-
mechanical effect at this scale could not have a dispropor-
tionate biomechanical effect at the scale of the whole bone
[10] . The biomechanical effects of a 6% difference in bone
mass caused by different aspects of bone turnover are
E
~ q
A
~
BV
=
TV
Þ
A
;
ð
1
Þ
r Ult ~ q
B
~
ð
BV
=
TV
Þ
B
;
ð
2
Þ
σ Ult is
the strength (ultimate stress) in compression, and A and B are
constants [14] (for a comprehensive review please see [15,16] ).
Studies of human cancellous bone [ 14,17
21 ] have reported the
exponent A to be as small as 1.2 [20] or as large as 3.0 [14] ,
suggesting that a bone specimen with 6% less bone mass due to
less bone volume is expected to be 7
17% less stiff. The
exponent B used to predict bone strength has been reported to be
as small as 1.48 [22] or as large as 2.47 [19] , suggesting that a
specimen with 6% less bone mass is expected to be 9
1 The term bone mass will be used here to describe the total mass of
mineralized tissue in a bone specimen (g) and should not be confused with
aBMD, a measure of bone density performed using dual-energy X-ray
absorptiometry that is expressed in the unit g/cm 2 .
14% less
strong ( Table 1 ).
Removal of trabeculae
ð
where E is the stiffness of the specimen (elastic modulus),
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1016
C.J. Hernandez / Bone 42 (2008) 1014 1020
Tissue degree of mineralization
applied this statistical approach to human bone and found the
following relationships [41] :
After a new volume of bone is formed, it begins to accu-
mulate mineral in a process that can continue for years after-
wards [23,24] . As a result, the degree of mineralization of older
bone tissue is greater than that of newly formed tissue, so that
the amount of bone turnover can influence the average tissue
degree of mineralization [25,26] .
Examination of mineralized tissues across a wide range of
species (including deer and whales) has associated increased
tissue degree of mineralization with increased bone stiffness
and strength and, in some cases, increased brittleness (the term
ð Þ~
ð
BV
=
TV
Þ
2 : 58 F 0 : 02
a
2
74
F
0
13
;
ð
3
Þ
r Ult MPa
Þ~
ð
BV
=
TV
Þ
1
92
F
:
02
a
2 : 79 F 0 : 09
;
ð
4
Þ
is the degree
of mineralization (measured as ash mass / dry bone mass), and
the exponents are expressed as mean± standard error. This
analysis is the only study of cancellous bone to detect and
quantify the independent effects of bone volume and average
tissue degree of mineralization on bone biomechanics. With
regard to bone strength (Eq. (4)), the exponent applied to tis-
sue degree of mineralization (2.79) is much greater than the
exponent applied to bone volume fraction (1.92), suggesting
that cancellous bone strength is much more sensitive to
differences in tissue degree of mineralization. It is possible,
however, that clinical measures of bone mass might capture
some of this effect. Clinical measures of bone mass evaluate the
total amount of mineral present (both mineralized volume and
degree of mineralization). Assuming clinical evaluation of bone
mineral content (BMC) is directly related to the inorganic
content in bone (the ash content), BMC can be expressed as:
σ Ult and BV/TV are defined as above,
α
is used here in an engineering sense expressing a
material property) [27,28] . While these studies demonstrate
that tissue degree of mineralization can be biomechanically
important, most do not include analyses of bone porosity and
therefore cannot be used to examine the biomechanical effects
of tissue degree of mineralization independent of bone volume.
In addition, it is important to keep in mind that trends observed
among species do not necessarily apply within a species. For
example, consider the commonly held idea that
hyperminer-
bone tissue is more brittle, a concept frequently noted
when discussing possible adverse effects of long-term inhibi-
tion of bone turnover. Although comparisons among animals
suggest that more highly mineralized tissue is more brittle,
only two studies of human bone specimens have shown in-
creased tissue degree of mineralization to be associated with
increased brittleness (evaluated as impact energy in cortical
bone specimens) [29,30] . Indeed, other studies of human bone
specimens have found increased tissue degree of mineralization
to be associated with reduced brittleness (measured as com-
pressive toughness in cancellous bone [31] , or fracture
toughness evaluated in cortical bone [32] ). Additionally, a
number of studies of human bone specimens did not observe a
relationship between tissue degree of mineralization and
brittleness (measured as toughness or energy to failure in
cortical or cancellous bone [33
BMC
~
ð
BV
=
TV
Þ q t a;
ð
5
Þ
ρ t is the density of the mineralized bone tissue (in grams),
a parameter that is linearly related to tissue degree of mine-
ralization [13,41] . By combining Eqs. (3), (4) and (5) we can
estimate the differences in bone biomechanics associated with a
6% difference in BMC caused entirely by reductions in average
tissue degree of mineralization (this change in BMC corre-
sponds to a reduction in tissue degree of mineralization from
65% to 62% ash by weight). This difference in BMC is
associated with a difference in specimen stiffness of 11
13%
36] ). While comparisons among
species suggest that highly mineralized bone specimens are
more brittle, it is not yet clear that human bone can become
brittle through an increase in average tissue degree of mineral-
ization alone.
With regard to bone stiffness and strength, few studies have
been designed to separate the biomechanical effects of tissue
degree of mineralization from those of bone volume. Follet et al.
found that average tissue degree of mineralization (measured
through quantitative contact radiography) was positively cor-
related with cancellous bone stiffness, strength and brittleness
(brittleness evaluated as toughness) [31] , and that tissue degree
of mineralization had a biomechanical effect independent of
bone volume. Others have used power law models to predict
the biomechanical effects of tissue degree of mineralization in
cortical bone [18,37
13% (both of these
ranges are expressed using the 95% confidence interval of the
regression coefficients above).
Another way of comparing the biomechanical effects of bone
volume and tissue degree of mineralization is to examine the
relationship between bone mineral content and bone strength
[10] . Fig. 1 shows the percent change in bone strength expected
from a hypothetical reduction in bone mineral content under two
different conditions: 1) when changes in bone mineral content
are caused entirely by bone volume (lower region with dark blue
shading); and 2) when changes in bone mineral content are
caused entirely by tissue degree of mineralization (upper region
with lighter orange shading). That these two confidence intervals
overlap suggests that alterations in tissue degree of mineraliza-
tion may not modify the relationship between bone strength and
clinical measures of BMC. Hence, alterations in average tissue
degree of mineralization may have little effect on the ability of
BMC to predict bone strength and are therefore not expected to
be responsible for discrepancies between fracture incidence and
aBMD. Additional studies are needed to confirm this analysis
(Eqs. (3) and (4)) and to determine if the average degree of
40] , but only two of these studies
accounted for variation in bone volume fraction (both using
non-human tissue [38,40] ). Currey suggested that the separate
effects of bone volume and tissue degree of mineralization
could be expressed with a two-parameter power law model and
applied the approach to non-human tissue [38] . Hernandez et al.
:
:
E GPa
:
0
ð
where E,
brittle
alized
where
and a difference in bone strength of 11
C.J. Hernandez / Bone 42 (2008) 1014 1020
1017
coefficient of variation of tissue stiffness from 20% to 50% is
expected to cause a 14% reduction in cancellous bone elastic
modulus.
Disconnection of trabeculae
9] . Quantifying the
effect of trabecular disconnection experimentally is challenging
because of technical difficulties in identifying and counting
individual trabeculae (only recently have techniques for directly
counting individual trabeculae in micro-CT images of cancel-
lous bone been presented [47,48] ). Existing biomechanical
analyses have therefore used cellular solid models with tra-
becular-like microarchitectures to mimic cancellous bone struc-
ture. Two- and three-dimensional cellular solid models indicate
that removal of individual trabeculae can result in reductions
in cancellous bone stiffness and strength that are greater than
would be expected from the associated change in bone volume
[49
Fig. 1. The predicted reduction in strength caused by a reduction in bone mineral
content or bone mineral density (as would be measured by dual-energy X-ray
absorptiometry) is shown. 1) a hypothetical case where changes in bone mineral
content are caused entirely by changes in volume fraction (dark blue region) and
2) a hypothetical case where changes in bone mineral content are caused entirely
by reductions in tissue degree of mineralization (light orange region). The
overlapping regions are based on the 95% confidence interval of the regression
model reported by Hernandez et al. [41] .
51] . Three-dimensional models suggest that a 6% differ-
ence in bone volume caused by removal of trabeculae can
reduce cancellous bone stiffness by 3% (only horizontal trabe-
culae removed) to 39% (only vertical/oblique trabeculae re-
moved) and compressive strength by 18% (only horizontal
trabeculae) to 35% (only vertical/oblique trabeculae) [51] .As
these simulations represent extreme cases where only horizontal
or only vertical/oblique trabeculae are removed, the actual
changes in bone biomechanics resulting from trabecular dis-
connection are expected to be somewhere in between these
values.
mineralization can have disproportionate effects on other me-
chanical properties (brittleness for example) or under different
loading conditions (impact, shear, etc.).
While most studies have concentrated on the biomechanical
effects of average tissue degree of mineralization, variation of
tissue degree of mineralization at the micro-scale has also been
implicated as a factor that can influence bone biomechanics.
Byaltering the number and/or size of new remodeling events,
bone turnover will not only modify the average tissue degree
of mineralization, but also the variability of tissue degree of
mineralization. Changes in variation of tissue degree of
mineralization have been associated with alterations in bone
turnover during bisphosphonate therapy and in metabolic bone
disease [42,43] . Variability of tissue degree of mineralization
can also differ among regions of the skeleton (iliac crest v.
calcaneous) [31] .
Micro-computed tomography based finite element models
have been useful for studying the biomechanical consequences
of variation in tissue degree of mineralization because they
make it possible to consider the biomechanical effects of tissue
degree of mineralization independent of bone volume or micro-
architecture. Finite element studies suggest that an increase
in intraspecimen variation in tissue degree of mineralization
(modeled as local variation in tissue stiffness) can cause a
reduction in cancellous bone stiffness, even when trabecular
microarchitecture and average tissue degree of mineralization
are maintained constant [44
Remodeling cavities
It has been proposed that cavities formed during bone remo-
deling (Howship's lacunae) can act as stress risers, causing
disproportionate reductions in the biomechanical performance
of cancellous bone. Experimental evaluation of the effects of
remodeling cavities on cancellous bone has been limited be-
cause a repeatable technique for making three-dimensional
measures of remodeling cavities in cancellous bone has not
yet been demonstrated. Existing data is therefore limited to
predictions made from finite element models. A number of
biomechanical analyses have illustrated how the presence of
a cavity on the surface of a single trabecula may increase the
stresses and strains in surrounding tissue [52
46] . Jaasma et al. determined that
an increase in the coefficient of variation (standard deviation/
mean) of the tissue stiffness from 20% to 50% would result in a
reduction in elastic modulus of cancellous bone by 19
5 mm in smallest
dimension [53,55] . A reduction in bone volume of 6% caused
by the addition of remodeling cavities was predicted to reduce
the elastic modulus by 12
24%,
even when average tissue degree of mineralization was main-
tained constant. More recently, Bourne and van der Meulen
measured variation in mineral content directly using calibrated
micro-computed tomography and found that an increase in the
47% and the compressive strength
61%. The ranges for these predictions are large because
the biomechanical effects of remodeling cavities can be
influenced by a number of factors including the initial bone
volume fraction (more porous bone can be more sensitive to
It is commonly stated that cavities formed during remodeling
can disconnect or fenestrate trabeculae, modifying trabecular
microarchitecture and potentially cause a disproportionate
change in cancellous bone strength [7
54] . Additionally,
two finite element analyses have suggested that remodeling
cavities can have a disproportionate effect on cancellous bone
stiffness and strength in specimens 3
by 13
721192101.003.png
1018
C.J. Hernandez / Bone 42 (2008) 1014 1020
remodeling cavities) and the placement of remodeling cavities
in the cancellous bone structure. When placed in regions of
high strain within the cancellous bone structure (where tissue
microdamage and mechanical stresses are expected to be
greatest) remodeling cavities can have a large, dispropor-
tionate effect on cancellous bone biomechanics [55] .Asa
result, the degree to which remodeling cavities are targeted to
tissue damage or tissue strain (two factors believed to stimulate
bone remodeling) will modulate the effect of bone remodeling
on bone biomechanics.
Additionally, the number and size (length, width, depth) of
remodeling cavities may have biomechanical significance.
Although an increase in bone turnover is commonly interpreted
as an increase in the number of remodeling events, two-dimen-
sional histomorphometry measurements cannot differentiate
an increase in the number of remodeling events from an increase
in the size of each individual event (width, length and depth)
[56] , a distinction that can result in very different stress dis-
tributions within cancellous bone. Simple mechanical analyses
suggest that the number and size of remodeling cavities may
influence the mechanical performance of a trabecula indepen-
dent of bone volume or total amount of bone turnover ( Fig. 2 ).
The number and size of remodeling cavities may also influence
intraspecimen variation in tissue degree of mineralization by
determining the size of each osteon or hemi-osteon and may
also influence the rate at which trabeculae are disconnected by
remodeling events (deeper cavities are more likely to disconnect
trabeculae [57] ). Unfortunately, little is known about the com-
plete size and shape (length, width and depth) of remodeling
cavities in human cancellous bone because two-dimensional
techniques cannot obtain measures of all three of these size
dimensions at once [58,59] . Micro-computed tomography is not
as helpful as one would expect because few imaging systems
can obtain the resolution needed to detect the scalloped surface
of a remodeling cavity. Those imaging systems with such high
resolution have a very limited field of view such that only one or
two cavities can be viewed per specimen, far too few to
characterize the population of remodeling events in cancellous
bone. Recently, serial block-face imaging using an automated
microtome or milling machine has been used to image
remodeling cavities in three dimensions, and may prove useful
in determining the placement and size of remodeling cavities in
human bone biopsies or cadaver tissue [54,60] .
Conclusions
Table 1 provides a unique way of comparing the biomecha-
nical effects of bone remodeling for a given difference in bone
mass (in this case a 6% difference in bone mass). An aspect of
bone that has the potential to explain discrepancies between
aBMD and fracture incidence will have a biomechanical effect
that is greater than would be expected from that caused by bone
volume alone. For example, a 6% difference in bone mass
caused by the average tissue degree of mineralization (second
row in Table 1 ) is associated with an 11
14%,
first row of Table 1 ). As a result, this analysis suggests that it is
unlikely that differences in average tissue degree of mineraliza-
tion can have a disproportionate effect on cancellous bone
compressive strength, and that average tissue degree of
mineralization would be unlikely to contribute to a biomecha-
nical explanation for discrepancies between aBMD and fracture
incidence.
Two conclusions can be made from comparing the remaining
factors in Table 1 to the effect of bone volume. First, existing
experimental and computational data suggest that, while aver-
age tissue degree of mineralization can influence bone strength,
it may not be able to explain discrepancies between bone
biomechanics and clinical measures of bone mass. Local vari-
ability of tissue degree of mineralization is a more likely
explanation. Secondly, while existing biomechanical analyses
support the idea that trabecular disconnection and remodeling
cavities may have a disproportionate effect on bone biomecha-
nics (i.e. the biomechanical effects can exceed those expected
from difference in bone volume), there is a considerable overlap
between the biomechanical effects of these factors and the
biomechanical effects of differences in bone volume alone. As a
result, further work is needed to determine if bone remodeling
may have a disproportionate effect on bone biomechanics.
Whether or not these aspects of bone remodeling have a
biomechanically relevant effect independent of bone mass will
depend on characteristics that we currently know little about,
such as the number and size of remodeling events and how well
remodeling cavities are targeted to mechanical stress/strain and
microscopic tissue damage. Additionally there is growing evi-
dence that the concentration of naturally occurring non-
Fig. 2. Three cylindrical trabeculae (150 μ m in diameter) are shown with remodeling cavities wrapped around them circumferentially. The remodeling cavities in each
image occupy the same volume (i.e. the same amount of bone turnover is depicted) but the number, surface size and depth of the cavities differs within the range
observed histologically. The bending moment and critical load for Euler buckling (calculated within the tapered region only) is presented relative to that in the first
image and is shown to vary by as much as an order of magnitude among the three possibilities.
13% difference in bone
strength, a range that is well within what is expected for the
same reduction in bone mass caused by bone volume (9
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