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What the Clinician Wants to Know |
1 From the Departments of Radiology and Medicine, University of British Columbia, Childrens and Womens Health Centre of BC, and Vancouver Hospital and Health Sciences Centre, Canada. Received February 12, 2002; revision requested March 2; revision received August 20; accepted August 21. Address correspondence to B.C.L., 7997 Turgoose Terr, Saanichton, British Columbia, Canada V8M 1V4 (e-mail: blentle@shaw.ca).
| ABSTRACT |
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© RSNA, 2003
Index terms: Bones, absorptiometry, 30.1299, 40.1299 Bones, diseases, 30.562, 40.562 Osteoporosis, 30.562, 40.562 Subtraction, dual-energy, 30.1299, 40.1299
| INTRODUCTION |
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The measurement of bone density does not discriminate among the causes of altered density. However, the measurement is most often undertaken in the context of hypogonadal osteoporosis (ie, that occurring as a result of amenorrhea or after menopause in women or because of inadequate serum testosterone concentration in men), and that clinical disorder is discussed in this article.
The recent past has seen a change in the perception of osteoporosis. In large degree, this is due to recently developed drugs that increase bone density and reduce fracture incidence in individuals at risk for osteoporotic fractures (3,4). Osteoporosis is thus no longer regarded as an inevitable result of aging but as a preventable and treatable disorder. At the same time, osteoporosis is no longer diagnosed only when symptomatic fractures result. Indeed, as many as 60% of vertebral fractures occur without symptoms. Unless a person has a fracture, osteoporosis usually causes no symptoms at all. So a clinically meaningful evaluation that would facilitate prevention and therapy must depend on a definition that does not require that bones fracture. It is in the context of estimation of the risk of fracture that bone densitometry serves an important clinical role. This risk is age dependent, in that a given degree of bone loss results in a different cumulative lifetime fracture risk when a person aged 40 years is compared with one aged 75, for example.
A more imaginative definition of osteoporosis has been developed that allows recognition of the disease before fractures resultnamely, "a chronic progressive disease characterized by low bone mass and microarchitectural deterioration of bone tissue, which leads to bone fragility and a consequent increase in fracture risk" (5,6).
Of the two variables identified, bone mass is the only one that can now be readily measured in life (711). That is the role of bone densitometry or other bone measurement methods. There is, however, considerable research interest in the examination of bone microarchitecture, bone fatigue damage, and cancellous bone connectivity. Potentially useful tools for application in clinical practice will likely emerge from such investigations (11).
Formerly, osteoporosis was diagnosed only when a low-trauma fracture resulted. A working group of the WHO (2) has more recently further defined osteoporosis in menopausal white women, for epidemiologic purposes, on the basis of bone mineral density (BMD) measurements, as follows: (a) normal: a value for BMD or bone mineral content (BMC) within 1 SD (score of 1T) of the young-adult reference mean; (b) low bone mass (osteopenia): a value for BMD or BMC lower than 1 SD (<1T) below the young-adult mean but not as low as 2.5 SDs (2.5T) below this value; (c) osteoporosis: a value for BMD or BMC 2.5 SDs or more (
2.5T) below the young-adult mean; (d) severe (established) osteoporosis: a value for BMD or BMC 2.5 SDs or more below the young-adult mean in the presence of one or more fragility fractures.
Notably, these definitions use bone density to categorize those at risk. While never intended as a series of intervention thresholds, they have become nearly universally used in the investigation and treatment of osteoporosis. As a result, the definitions have become the focus for communicating densitometric findings to a referring physician. However, it is important to realize that the definitions given were specifically intended to apply to menopausal white women. They do not necessarily apply to all sites measurable or all techniques that might be used (2).
The use of these definitions to reflect the risk of fracture in men or nonwhite persons or even in women before menopause, is at best an extrapolation, unsupported by firm evidence. Equally, use of the definitions is quite invalid in children or those who have not achieved or who will not, by virtue of skeletal disease (eg, types of osteogenesis imperfecta, Hadju-Cheney disease), ever achieve peak bone mass.
Bone density has a Gaussian, or normal bell-shaped, distribution in both women and men at any given age. However, the definition of osteoporosis cited earlier (5,6) makes reference to "low bone mass" while ignoring the fact that bone mass is a continuous variable. Therefore, any classification of osteoporosis based on bone density alonesuch as that described by the WHO Working Group (2)must be to some degree arbitrary. The purpose of a bone density measurement cannot be to "diagnose" osteoporosis as one might diagnose cancer by using a mammograman all-or-nothing findingrather, the purpose is to contribute to the assessment of fracture risk, which is itself a continuous variable.
Ideally, knowledge of a persons bone density should be but one part, if a very important one, of a global osteoporosis risk assessment otherwise derived from such factors as age, family history of kyphosis or low-trauma fracturing, or personal history of low-trauma fracture (considered a fragility fracture if trauma is due to a fall that is equivalent to or less than that from a standing height). A history of a late menarche or irregular menstrual cycle in women, of alcohol abuse in men, or of smoking in either sex is also part of the assessment of osteoporosis risk. It is the scale of this risk that will guide advice about fall avoidance, lifestyle modification, or treatment interventions. These risks of fracture need to be communicated, therefore, to a referring physician.
It should be noted that osteoporosis, while more common among women, is increasingly being recognized as a disease in men as well. For example, if baseline vertebral deformities, determined by using quantitative criteria, are assumed to represent osteoporotic fractures, then, in a Canadian population-based sample of persons older than 50 years (12), the prevalence in men (21.5%) is similar to that in women (23.5%).
| TOOLS FOR BONE MEASUREMENT |
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Quantitative Computed Tomography
A software package available for computed tomography (CT) devices allows the conversion of relative Hounsfield units, determined in the center of a vertebral body, to an absolute measurement of bone density of calcium in milligrams per cubic centimeter. This is usually accomplished by including standards containing known amounts of hydroxyapatite or other test material in the field of view. By using measurements of the Hounsfield units of these standards, a calibration curve is constructed and the absolute volumetric density of the vertebra being examined is calculated. A further increase in accuracy may be achieved by measuring at two x-ray energies and thus adjusting, on the basis of differential absorption, for the amount of soft tissue in the tissue volume examined (7). Care is necessary in setting the cursor to avoid partial-volume averaging artifacts if endplate or disk is included in the volume interrogated.
Because of the expense, radiation dose, and other calls on (ie, demands for other examinations with) large-aperture CT machines, very-small-aperture alternatives for peripheral quantitative CT have been built and are available commercially. These machines may be used to measure skeletal sites in the extremities (eg, distal radius, calcaneus) in the same way.
Single-Photon Absorptiometry
Although little used in North America at present, single-photon absorptiometry was used to advance bone measurement from the early days of measurement of bone size on radiographs of the hand or crude determinations of optical density from similar images. It is an effective technique for measurements of bone in the distal radius and ulna. Much of our current knowledge of osteoporosis and fracture risk was gained with this method (13). However, since the morbidity and mortality resulting from osteoporosis arise primarily from fractures of the central skeleton, the challenge of measuring bone in the proximal femur and spine prompted developments in technology.
Dual-Photon Absorptiometry and Dual X-ray Absorptiometry
Measurement of the BMC of spine and proximal femur (or any part or all of the skeleton) requires measurement of the relative attenuation of two differing photon energies to permit a correction for soft-tissue attenuation. This allows an assay of the calcium content in deeper structures, although the technique only provides an areal density of calcium (in grams per square centimeter) (7), not a true volumetric density such as may be achieved with quantitative CT (11). Standard dual x-ray absorptiometric (DXA) spinal measurements are performed in the posteroanterior projection, and both spine and proximal femur are measured most commonly (Figs 14).
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The methods used to provide the two photon energies involve either a pulsed change in peak voltage or the insertion of a cerium or samarium filter into the primary beam. Different manufacturers use one method or the other. The filter reduces "soft" radiation but also adds characteristic radiation to produce the two photon energies, the second determined by the peak voltage across the tube.
Quantitative Ultrasonography of Bone
The conceptual basis for using ultrasound transmission to interrogate bone is still poorly understood. Nevertheless, at a practical level both the speed of ultrasound through bone and the attenuation of the signal have been found to correlate well with DXA measurements of bone density (1417) and, at least in some populations, to predict fracture risk (18). However, although there has been a large increase in the use of quantitative ultrasonography (US) recently, the data produced are machine specific and subject to the use of dissimilar databases by different manufacturers. At the same time, anthropometric (19), clinical (eg, ankle edema) (20), and other variables are potential causes of error. There is also evidence that the choice of right or left heel for measurement can influence the result unduly (21).
Radiographic Absorptiometry
Radiographic absorptiometry involves digitization and computed analysis of hand radiographs acquired with inclusion of a standardized wedge used to calibrate bone density. Accuracy and precision are reported to be excellent (22), but outcome studies are lacking. More recently, a machine has been marketed that automates this analysis, eliminating the need to send images for central analysis. The advent of computed radiography may facilitate use of this method in centers without access to other technologies. However, the evidentiary basis for its adoption is modest (22,23).
Lateral Radiographs of Thoracic and Lumbar Spine
It is easy to overlook conventional radiographs in cases of osteoporosis, given the other technologies available. However, recognition of prevalent fractures implies a risk of further fracturing of the spine or hip. Fracture risk in an individual with an "asymptomatic vertebral deformity" is at least as great as that represented by 1 SD (-1T) of bone mass below peak (24). In appropriate patients, therefore, spinal radiographs may be helpful.
Surprisingly, there is still debate about what constitutes a vertebral fracture, since there are no good prospective studies of variations in vertebral morphology. Nevertheless, the identification of vertebral fractures is very important in risk estimation. As noted, the WHO Working Group defined severe osteoporosis as a bone density score of -2.5T or less and a prevalent low-trauma fracture. Indeed, the epidemiologic data suggest that one or more low-trauma fractures should be regarded as of osteoporotic provenance irrespective of bone density (25). The radiologist is thus in a strong position to guide the clinician in evaluating fracture risk.
Combined DXA and Morphometry
Some densitometers are now constructed to allow imaging of the spine in the lateral projection (26). Thus, measurements of vertebral morphometry may be made in lateral projections of the segments from T4 to L4 inclusively (26) (Fig 3). (It is usually thought that fractures above T4 are unlikely to be of osteoporotic origin, while the shape of L5 is subject to great morphologic variation and is difficult to assess quantitatively.) This may be accomplished by constructing the DXA machine as a rotating C arm or by moving the patient into a lateral decubitus position. Lateral spinal morphometry is combined with posteroanterior or lateral lumbar densitometry. Lateral densitometry may be used to assess BMC or BMD in the body of the vertebra and thus eliminate the contribution from mineral in the predominantly cortical bone in the posterior vertebral complex. This fact is offset by potential contributions from mineral in ribs or iliac crests, however. Also, there is a loss of precision due to the greater soft-tissue thickness encountered when measuring BMC or BMD in the coronal plane as compared with measurement in the sagittal plane.
The clinician needs to know the site at which bone is assayed and should be advised that any follow-up required is best performed with the same machine and in the same season. Differences exist between the measurements made with machines of different manufacturers at the same site(s), and even smaller differences exist between any two machines made by the same manufacturer. Such small differences become important when it is realized that physiologic and therapeutic changes in mineralization may amount to no more than 0.5% per year. Likewise, there are winter losses and summer gains in BMD, especially in more northerly latitudes, of about 1%.
| THE ROLE OF BONE DENSITOMETRY |
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DXA is also particularly effective in that its greater precision allows more effective use in follow-up (33) than do peripheral techniques. Thus, other applications of DXA are in the sequential examination of patients being treated for osteoporosis or of those at increased risk by virtue of factors such as medication or late perimenopause that adversely affect bone. At present, DXA is the most widely used technique for performing bone measurement in North America.
There is a trend toward increasing complexity of DXA machines. On one hand, the use of fan-beam rather than pencil-beam technology permits more rapid scanning, albeit at the cost of a small increase in radiation exposure. On the other hand, some machines now have the capacity for both lateral densitometry and morphometry, as discussed above (25).
| CONTRAINDICATIONS TO DXA |
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| SERIAL STUDIES AND PRECISION |
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It is also important to recognize that reporting of T scores in patients undergoing treatment to build bone mass is not entirely valid and may mislead about the scale of fracture risk. The data from several trials (3,4,40) indicate that drugs such as the bisphosphonates and selective estrogen receptor modulators produce a drop in fracture rates in excess of that expected on the basis of any increase in BMD that results from treatment. The slopes of the curves plotted to relate fracture incidence to BMD may, therefore, not be identical for density decreases and treatment-related increases. The relationship between serum cholesterol level and vascular disease before and after treatment with the statins is similarly complex.
Within those constraints, precision is a measure of reproducibility, and in vivo precision is determined by means of repeat examinations with repositioning of the subject between examinations. Precision is distinct from accuracy, which is a measure of how well the machine reflects realityin the case of DXA, the BMC or areal density of the bone assayed. The in vivo (short-term) precision of a DXA study of the lumbar spine has been quoted as 0.5%1.5%, but these numbers are potentially misleading. Precision expressed as a percentage varies in absolute measurements (ie, in grams per square centimeter) through the observed range of BMDs. Therefore, it is better quoted in absolute rather than relative terms. For example, authors of studies on changes in bone density commonly reported percentages. Equally, the effectiveness of medications is often compared in terms of the percentage increase in bone density. But if one study included women with osteopenia (eg, mean spinal BMD of 1.00 g · cm-2) who received medication A and another study included women with osteoporosis (eg, mean spinal BMD of 0.50 g · cm-2) who received medication B, then a 3% mean increase in both groups would represent 0.03 g · cm-2 in the first study but only 0.015 g · cm-2 in the second.
A full treatment of the statistical basis for precision measurements is beyond the scope of this article. Suffice it to say that anyone working in the field should consult the protocols for determining precision, which are readily available (41). He or she should measure precision in his or her own laboratory, with each of the technologists performing repeat DXA examinations with repositioning of the patient, then calculate either the BMC or BMD value or the percentage on a sliding scale that constitutes the least significant change at 95% (or other) confidence limits. A rigorous approach to the understanding of precision and its application to the determination of change is probably the most important contribution to be made to improving the practice of bone densitometry and providing key information to referring physicians. A report of a follow-up DXA study must provide the absolute change (in grams per square centimeter), the percentage change, and a statement as to whether this meets the criterion for real or clinically important change (exceeding the value for least significant change).
The radiologist should also be aware of the expected rates of change in age- and sex-specific populations. Thus, if bone loss is expected (eg, in a menopausal woman starting steroid treatment), stabilization of bone may reflect a treatment response as much as an increase in BMD. For an elderly person whose BMD would be expected to decrease over time, prevention of that decrease is probably important in its own right.
Short-term in vivo DXA precision errors for posteroanterior lumbar spine (L1 through L4) and total proximal femoral studies are quoted to be about 1% and 1%2% of normal densities, respectively (2), but these numbers relate to normal bone. Given the limited precision alluded to and the fact that rates of change in bone density are small (eg, 0.5% per year with aging), it is responsible at follow-up to recommend that examinations be repeated at most every 2nd year. Exceptions include cases where patients who are starting glucocorticoid (steroid) therapy, who have undergone orchidectomy, or who have undergone premenopausal ovariectomy (4244). Several investigators (45,46) have found that the most sensitive site at which to examine change in BMD is the lumbar spine (on posteroanterior images). In addition, because of small seasonal variations in BMD, successive DXA examinations should ideally be performed in the same season. Most large databases, as well as results of reported trials (eg, 3,4) of osteoporosis medications, have not systematically corrected for such artifacts.
All of these constraints may need to be alluded to in reports of bone density examinations. Referring physicians, particularly those who have a particular interest in osteoporosis, will be familiar with the rigor required in the establishment of precision and, hence, in the determination of a significant change in BMD. They may be reassured by periodic updates about the measurements from a given laboratory by means of either a brief bulletin or face-to-face meetings outside of the constraints of communicating individual patient data.
Confounding Variables
BMD may be increased artifactually in posteroanterior measurements of the lumbar spine; reasons for this include the presence of osteophytes, aortic calcifications, degenerative facet joint disease with hypertrophy and reactive bone, and degenerative disk disease (3538). These are important considerations, especially in elderly patients, since DXA measures the calcific density projected in the area of interest defined by the software (or selected by the operator). The area may thus sometimes include such "nonstructural" mineralization. Orwoll et al (35), in particular, demonstrated that in men the consequence of osteophytes can lead to misleading DXA results. Thus, radiographic correlation may be helpful in the assessment of artifact.
Similarly, since fractures reduce the projected area of a vertebra, they commonly result in an apparent increase in density, as shown by Ryan et al (38). It is helpful to examine individual segments and eliminate measurements out of step with adjacent segments. (Moving distally from L1 to L4, there is usually a small and steady increase in density from vertebra to vertebra.) However, as Ryan et al pointed out, fractures themselves cannot be reliably identified from the usual posteroanterior DXA image.
However, a major factor in the accuracy and precision of densitometers is the education and application of the technologists concerned (39) and, as noted, performance of the procedure by a few dedicated operators. Pedagogic programs such as those provided by the International Society of Clinical Densitometry are particularly relevant in this context.
The images accompanying a DXA report have a note specifically indicating that the images are not to be used for diagnostic purposes. Nevertheless, recognition of and reference to positioning errors or artifacts in the report and the choice of regions of interest (vertebrae analyzed) can help the clinician, as well as improve the quality of a DXA study. At the same time, however, it must be recognized that the fewer the vertebrae analyzed, the greater the potential for errors in accuracy and precision, such that any diagnostic inference based on one or two vertebral segments is not advised. For similar reasons, it is preferable to use segments L1 through L4 unless there is good reason to exclude L1.
Most standard DXA densitometers also allow accurate measurement of the radius or calcaneus by using regions of interest like those used in single-photon absorptiometry and single-energy absorptiometry measurements, as well as in user-defined subregions.
Referring physicians need to be made aware of the limitations of BMD measurements in the obese or if measurements are complicated by substantial weight gain or loss. BMD measured with DXA correlates positively with total body fat mass. Also, DXA measurement of the spine and BMD will be underestimated if the amount of fat overlying the spinal column is greater than that on either side of the lumbar spine (47,48). It has been reported (47) that a mean fat thickness difference of 2 cm results in a BMD error of 9%10%. For some patients, this error was as large as 16%. A change in bone marrow fat of 50% will change BMD by 5%6%. If we assume a change in yellow marrow from 40% at young-adult age to 60% at age 80 years, each year might result in a 1% error. Results of studies in cadavers (48) support these observations. Authors of more recent studies (48) of DXA measurement accuracy found similar errors for BMC, as well as for areal measurements, but smaller errors for BMD. The errors introduced by soft tissue and intramedullary fat limit the application of DXA to patients who have an abdominal anteroposterior diameter of 1530 cm (49). Weight change does, therefore, have the potential to reduce the precision of BMD measurements.
Database
BMD measurements in and of themselves would be of little intrinsic value in the estimation of osteoporosis risk (although changes in density might be informative). Their value lies in the benchmarking of measurement with a comparison population. That, after all, is the basis for T scores. At present for the total proximal femur, this is almost uniformly the measurement made as part of the third generation of the U.S. National Health and Nutrition Epidemiological Study, or NHANES III (50). Nevertheless, it has been suggested that in an ideal world the appropriate database to use should be local and certainly take into account ethnic differences. Thus, recently completed baseline measurements from the Canadian Multicentre Osteoporosis Study allow use of vertebral and femoral neck peak BMD data that are specific to urban areas of Canada (51).
Components of a Report of Bone Measurement
Lenchik et al (52) have described a model reporting format for DXA, and Stock et al (53) have noted that effective reporting of densitometric findings favorably influences physician management of osteoporosis by family doctors. However, a recent survey found that a comment about fracture risk in particular was not included by as many as 30% of the reporting centers responding (54). A description of a sample reporting format is suggested in the Appendix.
The data that each manufacturer has programmed densitometers to provide with respect to each patient probably contains more information than most consumers needknowledgeable specialists aside. However, the document will usually reflect BMD to three decimal places and, on occasion, T scores to two decimal places. This information should not to be communicated to the referring physician in the report. Such numbers far exceed the performance characteristics of the machine or (in the case of T scores) the conceptual basis of the WHO classification of the disease. Therefore, report BMD to at most two decimal places and T scores to one. To do otherwise is to misrepresent the quantitative limitations on the accuracy and precision of the technology or the arbitrariness of disease classifications in osteoporosis.
The printed output of bone densitometers includes the T score in addition to a low-resolution image. This convenience may result in the limitations of the densitometer sometimes being overlooked. The threshold T scores for diagnosis of osteopenia (-1.0T) and osteoporosis or severe osteoporosis (-2.5T) were arrived at by a WHO Working Group attempting to define osteoporosis for epidemiologic purposes in menopausal women of predominantly white extraction. As noted above, it would be inappropriate to report, without at least a caveat, T scores in persons not at an age at which peak bone mass might have been achieved or in nonwhite persons. Equally, while T scores are corrected for a database in men, it is not yet certain if the negative T scores derived have the same predictive power for fracturing as in women. For example, hip fractures are less common in women of Asian extraction than in those of white extraction, even for a given BMD value.
Purists should also note that T scores as used in osteoporosis risk assessment are slightly different from T scores as they are usually understood and applied in epidemiologic studies. The wider issue of the validity of the WHO Working Group classification (2) will be the subject of future debate.
Machine Used
Although densitometers all measure bone mass by using dual-energy x rays, which permits differential measurements of bone and soft-tissue attenuation, the machines are far from identical. The production of two energies may be achieved by rapidly alternating the voltage applied to the tube or by inserting a filter (cerium or samarium) to both reduce "soft" rays and add characteristic radiation from the filter material to the tube output. In addition, the assumptions built into the analytic software are different for each manufacturer, such that although results from a given make of densitometer are consistent, substantial systematic differences exist for measurements made between different machines fabricated by different manufacturers. Thus, as noted above, it is wise to indicate the machine used and to add a caveat to the effect that follow-up examinations are best performed with the same machine or, at the very least, one made by the same manufacturer. However, a standardized BMD has been developed in an attempt to address this issue, but it should be used only if absolutely necessary (50,55).
| DISCUSSION |
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Reports from the National Osteoporosis Foundation (31) and the Osteoporosis Society of Canada (57) point out that osteoporosis is defined in practice by an intermediate outcome (the BMD), not a health outcome (eg, fracture). The National Osteoporosis Foundation report (31) notes that "there is a strong association between BMD and the likelihood of fracture but ... other factors influence fracture risk as well. In this way, osteoporosis is similar to hypertension, diabetes mellitus, hypercholesterolemia, or atherosclerosis." Furthermore, the National Osteoporosis report (31) continues:
Because bone mass declines steadily after young adulthood, the prevalence of osteoporosis increases with age. For some women who are identified as osteoporotic, however, the risk of a fracture during their remaining lifetime is sufficiently low that treatment would not be appropriate (other than supplemental vitamin D and calcium). Conversely, many women who do not have osteoporosis might have other risk factors and circumstances that would justify treatment (such as when starting high dose prednisone therapy). Thus, although the definition of osteoporosis is based on BMD, it is not advisable to measure bone density in everyone. The decision to obtain a DXA examination should be based on each individuals risk factors ([t]able 1) and the treatment being considered. In addition, testing is not indicated unless the results might influence a treatment decision.
The risk factors mentioned in table 1 of this report (31) are summarized in the Table.
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| THE FUTURE |
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For practical purposes, in the more immediate future we believe it is desirable that fracture risk estimation based on the patients history and physical, radiologic, and biochemical examination results be synthesized into a comprehensive index of risk. The data from which to deduce the precise magnitude of that risk, in either absolute or relative terms, are or are becoming available. These data serve as a guide to advising patients about lifestyle modification, hormone use at menopause, and treatment interventions when these are appropriate (5,6,9,2931).
| CONCLUSION |
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| APPENDIX |
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| FOOTNOTES |
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| REFERENCES |
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