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Soft Tissue Research Clinical Investigations of Gravity Inversion Traction and Spondylolytic Anterolisthesis by Daniel J. Murphy, DC, FACO
Hypotheses as to cause of spondylolytic anterolisthesis are
many. A leading hypothesis indicates that the separation of the pars
interarticularis is a stress fracture, meaning it is caused from a
series of stresses in the region rather than by a single traumatic
event (Cox, Yochim). Between 5% to 7% of the adult white population
will have an anterolithesis. Approximately 90% of anterlisthesis are
found at L5 (Yochum). Therefore, this study primarily evaluates the
L5-sacrum articulation.
Gravity inversion traction has been around for several decades.
Its formal usage can be traced back to Dr. Robert M. Martin (1975 and
1982) who has claimed to have multiple degrees, including that of
medical physician, osteopath, and chiropractor. Dr. Martin spearheaded
the current trend in gravity inversion traction devices within
chiropractic through his Gravity GuiderTM system. This is the
traditional ankle gravity boot inversion system that has been used
both with, and without, a swinging bed. In the past decade, numerous
other gravity inversion traction devices have surfaced. These other gravity inversion traction
devices are marketed directly to the health care provider for
in-office use, as well as being marketed directly to the consumer.
Each unit is different in design in terms of ease of use and patient
comfort. Also, there are mechanical differences to the clinician,
using different varieties of gravity inversion traction units.
The most significant mechanical differences are those
attributed to the inversion traction devices in which one hangs
primarily from the thighs. My intention for this article is to discuss
the mechanical differences between the two basic, different varieties
of gravity inversion traction units as well as discussing indications
and contradictions for their usage. I will also describe a clinical
protocol for the safe introduction of inversion gravity traction for
patient care.
I have a particular interest in the usage of gravity inversion
traction devices, as I have used them extensively in my private
practice for the last ten years, and personally over the past twelve
years. The following information is based upon my own clinical
experiences and personal clinical research, performed in my office
over the past ten years. My clinic has used inversion traction on
approximately one thousand different patients in the past decade.
Approximately 10% of these, or one hundred patients, eventually
purchased a home gravity inversion device for home use. This study
specifically relates to gravity inversion traction and spondylolytic
anterolisthesis.
When one views a lateral lumbar radiograph, there is a lumbar
lordosis and an angulation to the sacral base. This
sacral base angle is approximately 40 degrees in normal standing
averages (Janik, 1998). When viewing the lumbosacral spine in the
lateral dimension, if we were to eliminate the forces in this region
created by the ligaments, muscles, discs, and pars interarticularis,
etc., we would have, in simple terms, a block on an inclined plane
(Fig. 1). This is not to say that the forces produced by these other
tissues are negligible in comparison to the force of gravity. The
force of gravity will now affect the lumbosacral spine as a block on
an inclined plane. With this analysis, we will have two forces that
affect the articulation (Fig. 1). These forces are:
1) Those that are parallel to the joint surface.
2) Those that are perpendicular to the joint surface.
By doing a simple force vector addition, we would have the
straight vertical force of gravity. In dealing with the topic of
anterolisthesis (Fig. 2), it is noted that when there is an
interruption of the pars interarticularis, it is the force component
that is parallel to the joint surface that will pull the L5 vertebra
forward on the sacral base. The average appearance of our patient with
an anterior spondylolisthesis is that there is also a narrowing of the
disc spacing between L5 and S1. This narrowing is attributed to the
perpendicular component of the forces that are acting over the L5-S1
interbody articulation.
When one is hanging in an inverted position, the vectors are
reversed (Fig 3). The component vector, that is parallel to the joint
surface, will pull the vertebrae toward posterior, or toward
correction, while the component that is perpendicular to the surface,
will enlarge the disc space. This simple vector analysis for the
temporary reduction of spondylolytic anterolisthesis is verified with
radiographic studies mentioned below. Before proceeding, however, an
understanding of the principles of viscoelastic creep is necessary.
Viscoelastic creep is a characteristic of biological tissue.
Discussions regarding viscoelastic creep can be found in tests by White and Panjabi, 1990, and
Bogduk, 1987. An example of a typical creep curve from White and
Panjabi is noted in Fig. 4. In a creep curve, deformation of the
tissue is plotted as a function of time. The principle of creep is
that the tissues will continue to deform over time, even though the
load on the tissues will take place, creating a lasting alteration in
the tissue mechanics, giving a lasting benefit to the forces that were
applied to the tissues.
Over the past ten years, we have done a radiological study of
30 patients with spondylolytic anterolisthesis. Our study consisted of
exposing radiographs in the upright and inverted, gravity traction
positions. We carefully analyzed these radiographs for millimeters of
anterior slippage, and also measured the height of the intervertebral
disc. The subjects used in this study were all patients seen in the
general practice of a chiropractor. Their ages ranged between 11-70
years of age. Twenty of the patients were male, ten were female. No
patient had an anteriolisthesis greater than Grade II. All of these
patients were suspended straight, vertically using Gravity GuiderTM
boots when the inverted gravity traction radiographs were exposed. A
few of these patients also were radiographed using thigh-gravity (OrthopodTM)
inversion traction as well. All patients were radiographed in a least
the lateral dimension. Some were also radiographed in the AP
dimension. In all patients, gravity inversion radiographs were exposed
at intervals of one minute. A second radiograph was exposed either at
an interval of five minutes, or ten minutes of traction, depending on
the tolerance of the patient. This was done in an effort to observe
the phenomenon of visoelastic creep.
The average amount of reduction in anterior millimeters of
displacement throughout this entire series was seven millimeters in
patients with spondylolytic anterolisthesis. The additional reduction
of forward slippage, caused by creep, averaged two additional
millimeters per patient, within the five to ten minute time frame
used. The spacing of the intervertebral disc, on average,
approximately doubled in size between L5 and S1. The smallest
millimetric reduction, while under gravity inversion traction, was
4mm. The largest millimetric reduction was 12mm.
Cases I (26 year old male) and Case II (18 year old male),
discussed below are representative of the study. These drawings Figs.
5, 6, 7, 8, 9, and 10 for Case I, and 11, and 12 for Case II are
proportional reduction of actual tracings of the radiographs. Figure 5
is an upright, neutral lateral, lumbar radiography. Figure 6 was
exposed after 60 seconds of inversion gravity traction. Figure 7 was
exposed after 10 minutes of inversion gravity traction. Note the
additional creep between the 60 second and 10 minute radiographs. Note
that the size of the intervertebral disc has more than doubled. Note,
that within 10 minutes, the anterolisthesis has completely reduced.
Figure 11 is an upright, neutral of a different patient, (Case
II). Note that the 60 second vertical inversion traction radiograph is
the same patient in Figure 12.
We have done one long-term follow-up study on one of the
subjects involved in this study. The long-term study is the same
patient as in Case I, above. The long-term benefits of inversion,
noted in this single study, reveal a progressive reduction in the
millimetric magnitude of the anterior displacement of L5 on the
sacrum, and a gradual increase in the height of the intervertebral
disc. Figure 8 and 9 are tracings of upright radiographs, exposed on
the same patient as in Figures 5, 6, and 7. Figure 8 was exposed in
1983, and Figure 9 was exposed in 1991. The original radiographs
(Figs. 5, 6, and 7) were exposed in 1981.
An interesting comparison is made in Case I by overlapping the
original upright radiograph (Fig. 5) with the ten minute inversion
radiograph (Fig. 7). This is done in Figure 10. Note the complete
reduction of the anterolisthesis, and that the intervertebral disc has
more than doubled in size.
Our study showed that, when doing straight vertical ankle
inversion, the lumbar lordosis is increased in size. This is
apparently because the sacroiliac articulation rocks forward, when one
is inverted to align with the acetabulum. This forward-rocking
projects as a greater curve in the lumbar lordosis. As a result, this
will increase the magnitude of the vector, that is parallel with the
joint surface, making it more advantageous for the reduction of the
anterior slippage (Fig. 13).
The major difference between ankle inversion and thigh (OrthopodTM)
inversion is that, for the most part, in the latter, there is an
elimination of the component of force, that is parallel to the joint
surface. Therefore, the major and, in some cases, the only vector
remaining is that which is perpendicular to the joint surface (Fig.
14).
Anterolisthesis is, however, still reduced through thigh
gravity inversion traction because of the crisscross micro-mechanics
of the annular disc fibers. This was clearly shown on the additional
radiographs of two of the thirty people involved in this study. A
comparison of the differences between OrthopodTM (thigh inversion) and
ankle vertical gravity inversion follows:
Straight, vertical ankle inversion has the largest
(parallel-to-joint surface) component of force for the reduction of
the anterior slippage in a spondylolisthesis. This component is
minimized in thigh inversion, yet there is still a positive benefit on
reduction of anterolisthesis with thigh inversion because of the
crisscross alignment of the annular disc fibers. However, individuals
with a retrolisthesis at L5 or L4 should use vertical ankle gravity
inversion with caution, as the retrolisthesis tend to be displaced
more toward the posterior. This principle is clearly seen at the L-4
level on Case I, when inverted. This adverse vector component is
minimized during thigh (OrthopodTM) inversion and, therefore, it is
the inversion traction of choice for those with retrolisthesis.
With thigh (OrthopodTM) inversion, one is either inverted all
the way or not inverted at all. An additional advantage to the ankle
inversion, particularly with the addition of the swing or bed
apparatus, is that the degrees of angulation can be controlled. None
of us would invert an eight-month pregnant woman on a thigh (OrthopodTM)
inversion unit. However, we can easily put this same woman in an ankle
inversion apparatus, with the swing or bed, at approximately ten
degrees of angulation, with the head being slightly lower than the
feet, and achieve a traction benefit.
The protocols for inversion therapy that we have developed in
our office follow:
1. Be aware of the medical contradictions to gravity-inversion
therapy. These include: high blood pressure, retinopathy, diabetes,
obesity, age or cardiovascular disease, etc. (This list is not
all-inclusive and common sense should be used.)
2. Be aware of the mechanical contradictions to gravity
inversion therapy. The most noted mechanical contradiction for ankle
inversion, in the authorŐs opinion and experience, is the presence of
a retrolisthesis of the lumbar or lumbossacral spine. Again, there are
other mechanical contradictions, and the provider should use common
sense.
A second mechanical consideration for inversion traction is the
presence of lumbar spine central canal spinal stenosis. During thigh
inversion (Fig. 14), the lumbar spine is flexed, enlarging the central
canal sagittal dimension by two to three millimeters (Cox). This does
not adversely affect those with lumbar spine central canal spinal
stenosis, and our clinical studies suggest a benefit to the patient.
However, as noted above, ankle inversion increases the lumbar lordosis,
thereby narrowing the sagittal dimension of the central canal. This
mechanical change could potentially adversely affect those with
pre-existing absolute or relative lumbar spine central canal spinal
stenosis. Therefore, we discourage the use of straight vertical ankle
gravity inversion traction for those with lumbar spine central canal
spinal stenosis.
If no obvious medical or mechanical contradictions to inversion
traction are noted, one can proceed. The following protocols were
developed by the author over the past ten years, using both ankle and
thigh gravity inversion in clinical practice. It is recommended that
the first time inverting, the patient be inverted for a maximum of 60
seconds. The doctor should remain with the patient the entire 60
seconds to make sure there are not problems. Questioning the patient
throughout the procedure assures that he/she is getting along
adequately. If, during this 60 second initial trial period of
inversion, the patient complains of dizziness, nausea, headache, or
significant increase in back pain, inversion should be discontinued,
and possibly attempted once again on another day. The patient should
arise promptly at the end of 60 seconds and, if this rising causes no
immediate or subsequent increase in symptomatology, the second session
of inversion therapy can be increased to two minutes, and third visit
to three minutes, the fourth visit to four minutes. The ultimate goal
would be achieved on the fifth visit Ń and that would be five
minutes. We do not recommend that anyone use gravity inversion
traction in excess of five minutes at any given time. It is duly
noted, that inversion therapy increases blood pressure, as do most
forms of exercise. We discourage the use of inversion for those with
systolic pressure greater than 150 mm of mercury.
It is noted in GuytonŐs physiology, that when one exercises,
blood pressure increases. Part of the reason is caused by a
vasodilation of the muscles that are being exercised, with a
vasoconstriction in other regions of the body. Therefore, the common
practice of having a patient do exercises, while inverted, does not
make rational sense and in fact, could be dangerous. Recalling that
blood pressure increases while inverted, if one then exercises,
causing a reflex vasoconstriction in regions that are not be
exercised, there could be a dramatic increase in overall systolic
blood pressure, potentially dangerous consequences. Therefore, our
recommendation is that inversion should be done with the greatest
degree of relaxation, and no exercise should be performed during
inversion. This is also how one takes best advantage of the
visoelastic creep forces which are necessary when attempting to reduce
spondylolytic anterolisthesis. It is this authorŐs opinion and
experience that the use of gravity inversion traction is a useful and
beneficial mechanical adjunct to chiropractic health care in the
management of spondylolytic anterolisthesis.
It is not the intent of this paper to promote specific brands
of gravity inversion devices, or to discourage the use of others not
mentioned. Rather, the purpose is to share clinical investigations
using inversion gravity devices. References
Bogduk, Nikolai and Twomey, Lance T, Clinical Anatomy of the
Lumbar Spine, Churchill Livingstone, (1987).
Cox James M., D.C., Low Back Pain, Williams and Wilkins,
(1990).
Jayson, Malcom, I.V., M.D., The Lumbar Spine and Back Pain,
Churchill Livingstone, (1987).
Janik TJ, Harrison DD, Cailliet R, Troyanovich SJ, Harrison DE.
Can the Sagittal Lumbar Curvature be Closely Approximated by an
Ellipse? J. Orthop Res. 1998; 16(6):766-770
Martin Robert M., M.D., The Gravity Guiding System, Gravity
Guidance Inc., (1982).
White A.A., M.D., and Panjabi M.M., PhD., Clinical Biomechanics
of the Spine, Lippincott, (1990).
Yochum Terry, and Rowe Lindsay, Essentials of Skeletal
Radiology, Williams and Wilkins, (1987).
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