AJR 2004; 183:949-958
© American Roentgen Ray Society
Diagnosis of Osteoporotic Vertebral Fractures: Importance of Recognition and Description by Radiologists
Leon Lenchik1,
Lee F. Rogers1,2,
Pierre D. Delmas3 and
Harry K. Genant4
1 Department of Radiology, Wake Forest University School of Medicine, Medical
Center Blvd., Winston-Salem, NC 27157-1088.
2 Present address: The University of Arizona Health Sciences Center, 1501 N
Campbell Ave., PO Box 245067, Tucson, AZ 85724-5067.
3 Department of Medicine, University Claude Bernard and INSERM Research Unit,
Lyon, France.
4 Department of Radiology, University of California School of Medicine, San
Francisco, CA.
Received September 9, 2003;
accepted after revision March 24, 2004.
Address correspondence to L. Lenchik
(llenchik{at}wfubmc.edu).
Introduction
Osteoporosis is a major public health concern. Recent evidence from
clinical and epidemiologic trials on osteoporosis has increased the urgency
for accurate diagnosis of vertebral fractures. Despite the fact that vertebral
fractures are very common
[18]
and are associated with decreased quality of life
[916],
they are frequently undetected by clinicians
[17,
18] and underdiagnosed by
radiologists [19,
20]. We review the clinical
consequences of vertebral fractures and explore the reasons why these
fractures often evade diagnosis. More important, we urge radiologists to play
a more active role in the diagnosis of vertebral fractures. Because many of
the clinical consequences of vertebral fractures are preventable with prompt
pharmacologic intervention, there is increasing rationale for accurate and
unambiguous diagnosis of these fractures by radiologists. With an unambiguous
approach to reporting of vertebral fractures, radiologists can make a
significant contribution to the appropriate care of patients with
osteoporosis.
Frequency of Vertebral Fractures
According to the National Osteoporosis Foundation, 30 million American
women and 14 million men are affected by osteopenia or osteoporosis
[21]. All are at an increased
risk for fracture, and some have already experienced fracture
[22,
23]. In the United Sates, the
lifetime risk of osteoporotic fracture is 40% in white women and 13% in white
men [7,
8]. Patients with osteoporosis
commonly fracture their vertebrae, proximal femur, distal radius, or proximal
humerus; the most common site is the vertebral body
[6,
8]. With approximately 700,000
cases each year in the United States, vertebral fractures account for nearly
half of all osteoporotic fractures and are at least twice as common as hip
fractures [6].
As with most other osteoporotic fractures, the incidence of vertebral
fractures increases with age. In the United States, the incidence rate for
symptomatic vertebral fractures in white women under 45 years old is 0.2 per
1,000 person-years compared with 1.2 per 1,000 person-years after 85 years old
[24]. Because many vertebral
fractures are asymptomatic, these rates grossly underestimate the scope of the
problem. More important, vertebral fractures generally occur earlier in life
than hip fractures. In a large cross-sectional study in Europe, on the basis
of standardized radiologic evaluation, the prevalence of vertebral fractures
in men and women age 50 and older varied from 10% to 24%
[1]. In both sexes, the
prevalence of vertebral fractures increases dramatically with age
[1,
2]. In one study
[2], the prevalence in women
increased from 5% to 50% between 50 and 85 years old. The epidemiology of
vertebral fracture in nonwhites has not been thoroughly studied, but it
appears that Hispanic and African American women have lower fracture rates
than whites [25,
26]. Yet, the impact of
vertebral fractures is best measured, not on the basis of their frequency, but
rather on their effect on the patient's quality of life.
Clinical Consequences of Vertebral Fractures
Increasing evidence
[916]
indicates that quality of life is diminished in patients with vertebral
fractures. Loss of physical function in patients after vertebral fracture is
substantial and comparable to that of hip fracture
[911].
Patients with vertebral fractures often have difficulty with activities of
daily living such as rising from a chair, bathing, dressing, cooking, climbing
stairs, and walking
[911].
In addition, vertebral fractures are commonly associated with chronic back
pain, limitation of spine mobility, reduction in pulmonary function, and
social isolation
[1216].
Even asymptomatic vertebral fractures have significant consequences for the
patient because of the increased risk of future fractures that may be
symptomatic. Existence of one previous vertebral fracture increases the risk
for subsequent vertebral fracture approximately fivefold and the risk of hip
fracture approximately threefold
[2729].
Furthermore, the mortality rate associated with vertebral fractures is
increased for both symptomatic (i.e., clinical) and asymptomatic (i.e.,
radiographic) fractures
[3034]
and, in some studies [30,
35], approaches that for hip
fracture.
Treatment of Patients with Vertebral Fractures
The clinical treatment of patients with vertebral fracture is largely
determined by the presence of signs and symptoms, in particular pain. The
management of pain may include physical modalities (i.e., heat, cold,
ultrasound, or electrical stimulation), physical rehabilitation and exercise
programs, pharmacologic therapy, nerve blocks, vertebroplasty and kyphoplasty,
or surgery. Pharmacologic therapy aimed at prevention of future osteoporotic
fractures is vital for patients with vertebral fractures and is applicable to
both symptomatic and asymptomatic fractures.
It is in the accurate diagnosis of asymptomatic vertebral fractures that
radiologists make perhaps the most significant contribution to patient care.
More specifically, the diagnosis of vertebral fracture by radiologists impacts
patient treatment by enabling the diagnosis of osteoporosis, helping select
patients for pharmacologic therapy, improving the ability to assess risk of
future fracture, and providing rationale for bone mineral density (BMD)
measurement.
Diagnosis of Osteoporosis
Many clinicians consider the presence of a fragility fracture as sufficient
for diagnosis of osteoporosis regardless of the patient's BMD. Although bone
densitometry is useful for assessing disease severity and monitoring therapy
in patients with fractures, densitometry is not essential for the diagnosis of
osteoporosis in this setting. Exclusion of malignancy and trauma as the cause
of fracture and biochemical evaluation of serum or urine or both to exclude
secondary causes for bone fragility are required. After the diagnosis of
osteoporosis is made, most patients are offered pharmacologic therapy aimed at
preventing future fractures. Thus, the ability to make the diagnosis of
osteoporosis on the basis of the presence of vertebral fracture is not
trivial.
Selection of Patients for Therapy
Increasing evidence
[3642]
justifies offering pharmacologic therapy for osteoporosis to patients with
vertebral fracture after nonosteoporotic causes (e.g., malignancy and trauma)
have been excluded.
The presence of vertebral fractures has been one of the most common
criteria for selecting individuals for clinical trials on osteoporosis therapy
[3642].
Individuals with existing vertebral fractures have a much higher incidence of
subsequent fractures than those without fractures and have been used in most
clinical trials on osteoporosis therapy
[3642].
Pharmacologic therapy for osteoporosis is effective in patients with vertebral
fractures: trials with alendronate, calcitonin, raloxifene, risedronate, and
teriparatide have shown 3050% reductions in fracture incidence
[3642].
Although these agents also reduce the risk of vertebral fracture in patients
with low BMD but without prevalent fractures, the absolute risk reduction is
greater in those with prevalent vertebral fractures
[3642].
Thus, the decision as to whether a patient is a candidate for therapeutic
intervention is based not only on the results of a bone densitometry
examination but also on the presence of a vertebral fracture.
Improving the Ability to Predict Fracture Risk
The presence of vertebral fracture is an important factor in predicting the
risk of future fractures. Clinical guidelines, including those from the
National Osteoporosis Foundation
[43] and the International
Osteoporosis Foundation (IOF),
[44] state that vertebral
fractures are the key risk factor, other than low BMD, in the assessment of
future fracture risk. The importance of vertebral fractures is also recognized
in the World Health Organization (WHO) classification criteria for
osteoporosis [45]. The WHO
criteria define "severe osteoporosis" as low bone mass "in
the presence of one or more fragility fractures."
Risk assessment for individual patients can be improved by combining BMD
results and vertebral fracture assessment. For example, a woman with low BMD
and one vertebral fracture has 25 times the risk of a patient with normal BMD
and no fracture [46]. Thus,
the diagnosis of vertebral fractures by radiologists helps clinicians and
their patients to be better informed about the overall fracture risk.
Indication for Bone Densitometry
Many insurance carriers (including the Centers for Medicare and Medicaid
Services) consider vertebral fractures as one of the indications for bone
densitometry. Practically, the approach of measuring BMD even in patients with
vertebral fractures has merit because patients with low bone density and
vertebral fractures are not only at the highest risk for future fractures but
are also most likely to benefit from pharmacologic therapy.
Diagnosis of Vertebral Fracture
The diagnosis of a vertebral fracture may be suspected on clinical
evaluation and confirmed with radiography. However, unlike other fractures,
vertebral fractures are commonly present on radiographs obtained for other
reasons in patients who may not show signs or symptoms suggestive of
fracture.
Clinical Diagnosis
Although vertebral fractures are common in postmenopausal women and older
men, they are often difficult to identify clinically (i.e., without
radiographs). Only about one in four vertebral fractures is clinically
recognized [47]. The lack of
recognition is due to both the absence of symptoms and the difficulty in
determining the cause of symptoms. Because most episodes of back pain are not
related to vertebral fractures, vertebral fractures are not commonly suspected
in patients reporting back pain, unless the back pain is associated with
trauma. Height loss, another indicator of vertebral fractures, is also
difficult to assess clinically
[48,
49]. Some height loss is
expected with aging, because of compression of the intervertebral disks.
Studies [48,
49] have concluded that height
loss is an unreliable indicator of fracture status until it exceeds 4 cm.
Kyphosis in the elderly is associated with vertebral fracture but is difficult
to measure in a clinical setting without the use of radiography
[50].
For these reasons, vertebral fractures are not commonly considered in the
clinical evaluation of patients. Even when patients are being evaluated for
the presence of osteoporosis, it is far less common for them to be referred
for spine radiographs than for bone densitometry.
Radiologic Diagnosis
Vertebral fractures suspected at clinical evaluation require radiologic
confirmation. Most radiologists make the diagnosis of vertebral fracture on
the basis of a qualitative impression. In contrast, those who conduct research
typically make that diagnosis on the basis of a semiquantitative assessment or
a quantitative measurement of vertebral dimensions (e.g., vertebral
morphometry).
Radiologists qualitatively analyze radiographs of the thoracolumbar spine
to identify vertebral fractures in patients whose clinical indications suggest
trauma, osteoporosis, malignancy, or acute back pain. While diagnosing the
vertebral fracture in question, the observer also considers the potential
differential diagnoses of this deformity. The radiologist's decision can be
aided by additional radiographic projections (i.e., oblique views) or by
complementary examinations (i.e., bone scintigraphy, CT, or MRI).
In a research setting, many different approaches have been used to diagnose
and characterize vertebral fractures. The most widely used have been those
initially described by Fletcher
[51], Barnett and Nordin
[52], Hurxthal
[53], Smith et al.
[54], Minne et al.
[55], Melton et al.
[56], Black et al.
[57], Eastell et al.
[58], McCloskey et al.
[59], and Genant et al.
[60]. Typically, the
approaches involve quantitative assessment of vertebral dimensions.
Unfortunately, little standardization exists in both the quantitative and
qualitative approaches to vertebral fracture diagnosis. This may, in part,
explain why a substantial proportion of vertebral fractures remains
undetected.
Underdiagnosis of Vertebral Fractures
Vertebral fractures often go undetected by clinicians and undiagnosed by
radiologists
[1720].
According to data from the National Ambulatory Medical Care Survey from 1993
to 1997, primary care physicians diagnosed vertebral fracture (or
osteoporosis) in 213% of white women age 60 years and older, whereas
the estimated prevalence in this age group was 2030%
[1718].
A recent retrospective study of 934 women 60 years old and older found
radiographic evidence for 132 moderate or severe vertebral fractures (14%) and
showed that only 50% of contemporaneous radiology reports mentioned these
fractures [19]. A
multinational study [20] of
2,000 postmenopausal women with osteoporosis was conducted, in part, to assess
the accuracy of radiographic diagnosis of vertebral fractures by comparing
results of local radiographic reports with those of subsequent central
readings. This study [20]
reported false-negative rates from 27% to 45%, despite a strict radiographic
protocol that minimized underdiagnosis due to inadequate film quality. The
investigators concluded that the failure to diagnose vertebral fracture is a
worldwide problem due in part to the lack of fracture recognition by
radiologists and the use of ambiguous terminology in radiology reports.
It would seem that the detection of vertebral fractures should pose no
great difficulty. Why then, are so many vertebral fractures being missed? One
explanation may relate to the lack of standardization in the radiologic
interpretation of vertebral fractures, especially when attention is not
focused specifically on the issue of fracture. In this setting, radiologists
often fail to recognize or mention many mild and some moderate fractures, or
they use terminology that is nonspecific and does not adequately alert the
referring clinician to the presence of a vertebral fracture. The diagnosis of
vertebral fracture is often unsuspected clinically; this oversight makes
accurate radiologic diagnosis essential for proper patient management.
Thus, we propose a call to action, in which radiologists begin to use a
simple but standardized approach to diagnosis of vertebral fracture.
Call to Action
Because of the serious clinical consequences of vertebral fractures,
radiologists must make an effort to improve the accuracy of their diagnoses.
They must also reduce the variability in terminology when describing vertebral
fractures in patients with osteoporosis. The purpose of this section is to
provide the basis for accurate radiologic interpretation and standardized
reporting.
Accurate Interpretation
When evaluating imaging studies in which the vertebrae are included (i.e.,
not just spine radiography but also lateral chest radiography), the following
questions are important.
Is there a fracture?Vertebral fracture should be diagnosed
when there is loss of height in the anterior, middle, or posterior dimension
of the vertebral body that exceeds 20%
(Fig. 1). Special effort should
be made not to hedge on the diagnosis of vertebral fractures. If the
radiologist cannot decide whether a fracture is present, additional views or
additional imaging studies should be recommended. A radiologic hedge can
adversely affect patient care by preventing a patient who would otherwise
benefit from pharmacologic therapy from receiving it.

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Fig. 1. Drawings show diagnosis and grading of vertebral fractures
using semiquantitative method
[60]. Vertebral fracture is
diagnosed when reduction of height in anterior, middle, or posterior dimension
of vertebral body exceeds 20%. Approximate degree of height reduction
determines assignment of grade to vertebra. Fractures are classified as wedge,
biconcave, or crush, depending on whether anterior, middle, or posterior
portion of vertebral body is most diminished in height.
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In addition to changes in dimension, vertebral fractures are detected on
the basis of the presence of endplate deformities, the lack of parallelism of
the endplates, and the general altered appearance compared with neighboring
vertebrae (Fig. 2A,
2B,
2C). Radiologists should become
familiar with pitfalls in the diagnosis of vertebral fractures. For example,
poor technique in which the lateral projection is really an oblique projection
may lead to the vertebrae appearing fractured (Fig.
3A,
3B). Similar pseudofractures
may be seen on lateral projections in patients with scoliosis. Other
abnormalities in vertebral shape may mimic a fracture. Examples include
cupid's bow (a developmental variant), limbus vertebra (a developmental
variant), Schmorl nodes (vertebral osteochondrosis or Scheuermann's disease),
and H-shaped vertebrae (sickle cell disease or Gaucher's disease) (Figs.
4A,
4B,
5,
6,
7,
8). Obviously not every
deformed vertebra is a vertebral fracture caused by osteoporosis.

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Fig. 2A. Pitfalls in diagnosing vertebral fractures. In all examples,
note presence of endplate deformities, lack of parallelism of endplates, or
altered appearance compared with neighboring vertebrae. Lateral radiograph of
lumbar spine shows mild wedge fracture (grade 1) of L3 vertebra.
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Fig. 2B. Pitfalls in diagnosing vertebral fractures. In all examples,
note presence of endplate deformities, lack of parallelism of endplates, or
altered appearance compared with neighboring vertebrae. Lateral radiograph of
lumbar spine shows moderate wedge fracture (grade 2) of L3 vertebra and
moderate crush fracture (grade 2) of L2 vertebra.
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Fig. 2C. Pitfalls in diagnosing vertebral fractures. In all examples,
note presence of endplate deformities, lack of parallelism of endplates, or
altered appearance compared with neighboring vertebrae. Lateral radiograph of
thoracic spine shows severe wedge fracture (grade 3) of T7 vertebra.
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What is the age of the fracture?This question is
particularly relevant in deciding whether a patient's current symptoms are due
to that fracture. Unfortunately, on conventional radiographs, it is often
difficult to determine the age of the fracture unless prior radiographs are
available. When there is cortical disruption or impaction of the trabeculae,
the diagnosis of acute fracture is obvious
(Fig. 9A). When cortical
disruption is not seen and the vertebra appears similar in density to the
adjacent vertebrae, the diagnosis of an old fracture is equally apparent
(Fig. 9B). However, in many
instances, neither criterion is met and additional imaging studies may be
useful. Lack of edema on MRI (Fig.
10A,
10B) or lack of
radiopharmaceutical uptake on a bone scan (Fig.
11A,
11B) indicates an old
fracture. However, even with advanced imaging, it may be difficult to
accurately determine the age of a vertebral fracture (Fig.
12A,
12B). Note that even old
vertebral fractures are important to mention because they increase the risk of
subsequent fractures.

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Fig. 9B. Differentiating acute and old fractures. Lateral radiograph
of lumbar spine shows old vertebral fracture. Note that fractured vertebra
appears similar in density to adjacent nonfractured vertebra.
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Fig. 10A. Lack of edema on MR images indicating old fracture. A
Sagittal T1-weighted (A) and T2-weighted fat-suppressed (B) MR
images show old L1, L2, and L3 vertebral wedge fractures. Note isointensity of
fractured vertebrae compared with nonfractured L4 vertebra.
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Fig. 10B. Lack of edema on MR images indicating old fracture. B
Sagittal T1-weighted (A) and T2-weighted fat-suppressed (B) MR
images show old L1, L2, and L3 vertebral wedge fractures. Note isointensity of
fractured vertebrae compared with nonfractured L4 vertebra.
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Can it be a pathologic fracture?Critical to the evaluation
of vertebral fractures on imaging studies is the fact that not all vertebral
fractures are due to osteoporosis. In particular, antecedent trauma,
infection, and tumor must be excluded. In many cases, MRI is useful for
differentiating osteoporotic fractures from pathologic fractures by showing
contrast enhancement of bone marrow and adjacent soft tissues in pathologic
fractures. However, early after fracture, enhancement may be seen even in the
absence of tumor (Fig. 13A,
13B).

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Fig. 13A. MRI for determining age of fracture. MR images show acute
wedge fractures of T12 and L1 and old wedge fracture of L2. T1-weighted image
shows that acutely fractured T12 and L1 vertebrae have lower signal intensity
than chronically fractured L2 vertebra.
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Fig. 13B. MRI for determining age of fracture. MR images show acute
wedge fractures of T12 and L1 and old wedge fracture of L2. T1-weighted
fat-suppressed image obtained after administration of contrast agent shows
enhancement in T12 and L1 vertebrae but no enhancement of L2 vertebra.
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Standardized Reporting
After the fracture is detected (and traumatic and pathologic fractures have
been excluded), it should be classified as wedge, biconcave, or crush (Figs.
1 and
2A,
2B,
2C). All visualized thoracic
and lumbar vertebrae that are fractured should then be graded on the basis of
the percentage of reduction in anterior height, middle height, or posterior
height (Figs. 1 and
2A,
2B,
2C). This approach to reporting
vertebral fracture assessment is based on one that has been widely used in
clinical research, the semiquantitative method of Genant et al.
[60].
Rationale for Adapting the Genant Method to Clinical Practice
In Genant's method [60],
the severity of a fracture is assessed by visual determination of the extent
of a vertebral height reduction and morphologic change, and vertebral
fractures are differentiated from other nonfracture deformities. The
approximate degree of height reduction determines the assignment of grades to
a vertebra. Unlike the other approaches, the type of the deformity (i.e.,
wedge, biconcavity, or crush) is not linked to the grading. In addition to
height reductions, careful attention is given to alterations in the shape and
configuration of the vertebra relative to adjacent vertebrae and expected
normal appearances. These features add a qualitative aspect to the
interpretation and render this method less readily definable as either
qualitative or quantitative.
The main reasons that this method is ideally suited to serve as a basis for
a standardized interpretation of vertebral fractures in clinical practice are
the following: It is less time-intensive and cumbersome than morphometric
methods (i.e., in which all vertebral dimensions are measured), it is more
accurate than nonstandardized qualitative assessment
[19], it is highly
reproducible [61,
62], and it is already well
known to most clinicians who have an interest in osteoporosis.
More Practical for Clinical Practice than Morphometry
Many standardized approaches to describing vertebral fractures have been
used in research
[5560].
Can any of these approaches be easily adapted to clinical practice? The answer
seems largely dependent on whether measurement of vertebral dimensions is
required. It is unlikely that such measurements would be practical in most
clinical settings. Ideally, the standardized assessment would assign distinct
categories (or grades) to vertebral fractures according to their severity in a
reproducible manner without making measurements of vertebral dimensions. The
Genant method [60]
accomplishes just that.
More Accurate Than Nonstandardized Qualitative Assessment
Why not use a purely qualitative approach to vertebral fracture diagnosis?
The answer is because assessment of vertebral fractures using standardized
grading schemes has been found to be more reproducible and generalizable than
the inspection of radiographs without specific criteria for fracture diagnosis
[19,
63,
64]. In the absence of
distinct characteristics of fracture, a reviewer using a solely qualitative
approach could rather arbitrarily consider a mild wedge deformity normal,
anomalous, or fractured. In such a case, well-defined quantitative criteria
may be useful. This possible arbitrary interpretation explains in part why
standardized approaches have been found to be such valid research tools
[1,
15,
5760].
High Reproducibility
The rationale for adapting this method to clinical practice is further
supported by its high reproducibility in evaluating both prevalent and
incident vertebral fractures. In the prevalent vertebral fracture study of 400
postmenopausal women with low BMD
[61], the interobserver
agreement was about 94% for the dichotomous fracturenonfracture
diagnosis and 91% using the whole-grading scale. In the study of incident
vertebral fractures in 335 women with low BMD who underwent follow-up
radiography 12 months after the initial examination
[62], the kappa scores among
the three reviewers were good, ranging from 0.80 to 0.84.
Limitations of the Genant Method
The Genant method has several limitations that may also apply to the other
standardized approaches. For example, from morphometric data on healthy
subjects, we know that vertebrae in the mid thoracic spine and in the
thoracolumbar junction are slightly more wedged than in other regions of the
spine. As a result, normal variations may be misinterpreted as mild vertebral
deformities. The same findings apply to a lesser extent to the lumbar spine,
in which some degree of biconcavity is frequently seen. Another possible
limitation is that the diagnosis of mild vertebral fractures may be quite
subjective and these fractures may be unrelated to osteoporosis
[65]. However, mild fractures
detected with the Genant method are associated with a lower BMD than normal
and predict future vertebral fractures, although to a lesser extent than
moderate or severe fractures
[66].
For these reasons and despite the stated limitations, the Genant method
should be adopted by radiologists as the standard for reporting of
osteoporotic vertebral fractures. The joint initiative of the IOF and the
European Society of Skeletal Radiology has endorsed this approach. We hope
that other professional organizations will follow their lead.
Assessment of Fractures on DXA Images
Lateral spine images obtained with fan-beam dual-energy X-ray
absorptiometry (DXA) systems (Fig.
14A,
14B) offer a potential
alternative to radiographs for vertebral fracture diagnosis because vertebral
fracture status is frequently unknown at the time of patient evaluation with
bone densitometry.
Several clinical studies have shown the feasibility of visual evaluation of
lateral DXA spine images
[6770].
A study of 161 postmenopausal women who had lateral radiographs assessed using
the Genant method reported that the DXA images permitted visual assessment of
95% of all vertebrae [70].
Among the vertebrae that could be visualized, there was 92% sensitivity and
96% specificity for detection of moderate-to-severe fractures. A strong
overall agreement was found between visual evaluation of DXA images and
radiographic results.
The same standardized approach to reporting vertebral fractures described
previously should be applied to lateral DXA images. However, some degree of
caution is warranted when using lateral DXA images for assessment of vertebral
fractures for the following reasons: Many fractures seen on DXA should be
confirmed with standard radiographs to exclude the possibility of a pathologic
fracture, and patients with indeterminate DXA images (common in the upper
thoracic spine) should be referred for radiography.
Conclusion
Despite the difficulties inherent in the assessment of vertebral fractures,
their diagnosis is essential for appropriate clinical management. Having a
vertebral fracture is a strong risk factor for subsequent fractures, both at
new vertebral sites, at the proximal femur, and at other sites susceptible to
osteoporosis. As many as two thirds of vertebral fractures do not manifest as
acute painful events; therefore, careful scrutiny of all pertinent imaging
studies (including lateral chest radiography and DXA) for the presence of
vertebral fracture should be encouraged. Using a standardized approach to
reporting of vertebral fractures should lead to better communication with
clinicians and thus improve the care of patients with osteoporosis.
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