Lumbosacral Biomechanics: Difference between revisions

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'''Original Editors '''[[User:Bert Lasat|Bert Lasat]]<br>  
'''Original Editors '''[[User:Bert Lasat|Bert Lasat]]<br>Reviewed and updated by&nbsp;[http://www.physio-pedia.com/STOPS_Project Matthew Richards] 29/7/2014
</div>
 
== Search Strategy  ==
== Search Strategy  ==


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== Definition/Description  ==
== Definition/Description  ==


“Mechanics, the study of forces and their effects, when applied to humans, is called biomechanics” (Jensen 1980). Positioned below the thoracic spine, the lumbar spine normally has 5 vertebrae, while the sacrum consists of a series of usually 5 fused sacral vertebrae (Moore 1992). Together this lower portion of the vertebral column (see below) is referred to as the lumbosacral spine and is an important biomechanical region of the body. <br>  
“Mechanics, the study of forces and their effects, when applied to humans, is called biomechanics” (Jensen 1980)<ref name="Jensen">Jensen M Biomechanics of the lumbar intervertebral disk: a review. Physical Therapy. 1980; 60(6):765-773.</ref>. Positioned below the thoracic spine, the lumbar spine normally has 5 vertebrae, while the sacrum consists of a series of usually 5 fused sacral vertebrae (Moore 1992)<ref name="Moore">Moore, KL. Clinically Oriented Anatomy (3rd edition). 1992, Baltimore: Williams and Wilkins</ref>. Together this lower portion of the vertebral column (see below) is referred to as the lumbosacral spine and is an important biomechanical region of the body. <br>  


[[Image:Spine1.jpg]]  
[[Image:Spine1.jpg]]  
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== Clinically Relevant Anatomy  ==
== Clinically Relevant Anatomy  ==


As with all vertebrae in the body, the lumbar and sacral vertebrae consist of a “body” anteriorly which is larger and more cylindrical in the lumbar region and a “vertebral arch” posteriorly which encloses the vertebral foramen protecting the neural tissues (Moore 1992).  
As with all vertebrae in the body, the lumbar and sacral vertebrae consist of a “body” anteriorly which is larger and more cylindrical in the lumbar region and a “vertebral arch” posteriorly which encloses the vertebral foramen protecting the neural tissues (Moore 1992)<ref name="Moore">Moore, KL. Clinically Oriented Anatomy (3rd edition). 1992, Baltimore: Williams and Wilkins</ref>.  


<br>The vertebrae within the lumbar spine are separated by intervertebral joints which are unique articular structures, The intervertebral discs are the joint’s key component, made up of distinct features. The central paste-like nucleus pulposus consists primarily of water (70-90%) and hydrostatic proteoglycans (65% of the dry weight) loosely bound by collagen fibres (15-20% of the dry weight). The nucleus is surrounded by the strong concentric collagen layers of the annulus fibrosis consisting of water (60-70%), collagen (50-60% of the dry weight) and proteoglycans (20% of the dry weight) which are mostly aggregated. The nucleus and annulus both contain type II collagen throughout and the outer annulus contains a higher concentration of type I collagen. Elastic fibres (10%) are also found in the annulus and are arranged circularly, obliquely and vertically, with a concentration towards the attachment sites with the vertebral endplates. The vertebral endplate covers the upper and lower aspects of the disc and is strongly joined with fibrocartilage to the nuclear and annular parts of the disc. There is a greater concentration of collagen in the tissue nearer the bone (Bogduk 2012).  
<br>The vertebrae within the lumbar spine are separated by intervertebral joints which are unique articular structures, The intervertebral discs are the joint’s key component, made up of distinct features. The central paste-like nucleus pulposus consists primarily of water (70-90%) and hydrostatic proteoglycans (65% of the dry weight) loosely bound by collagen fibres (15-20% of the dry weight). The nucleus is surrounded by the strong concentric collagen layers of the annulus fibrosis consisting of water (60-70%), collagen (50-60% of the dry weight) and proteoglycans (20% of the dry weight) which are mostly aggregated. The nucleus and annulus both contain type II collagen throughout and the outer annulus contains a higher concentration of type I collagen. Elastic fibres (10%) are also found in the annulus and are arranged circularly, obliquely and vertically, with a concentration towards the attachment sites with the vertebral endplates. The vertebral endplate covers the upper and lower aspects of the disc and is strongly joined with fibrocartilage to the nuclear and annular parts of the disc. There is a greater concentration of collagen in the tissue nearer the bone (Bogduk 2012)<ref name="Bogduk">Bogduk, N. (2012). Radiological and Clinical Anatomy of the Lumbar Spine (5th ed.). China: Churchill Livingstone.</ref>.  


[[Image:Spine2.jpg]]  
[[Image:Spine2.jpg]]  


(Figure: shows the lumbar disc components (from: http://en.wikipedia.org/wiki/Annulus_fibrosus_disci_intervertebralis)<br><br>The lumbosacral transition is normally at the level of L5/S1 and the intervertebral disc at this level is wedge shaped. A “transitional vertebra” is a spinal anomaly where the lowest lumbar vertebra is to a degree fused or a failed segment of the sacrum thought to occur in 4-30% of the population (Chalian 2012, Konin 2010).  
(Figure: shows the lumbar disc components (from: http://en.wikipedia.org/wiki/Annulus_fibrosus_disci_intervertebralis)<br><br>The lumbosacral transition is normally at the level of L5/S1 and the intervertebral disc at this level is wedge shaped. A “transitional vertebra” is a spinal anomaly where the lowest lumbar vertebra is to a degree fused or a failed segment of the sacrum thought to occur in 4-30% of the population (Chalian 2012<ref name="Chalian">Chalian M, Soldatos T, Carrino JA, Belzberg AJ, Khanna J, Chhabra A. Prediction of trasitional lumbosacral anatomy on magnetic resonance imaging of the lumbar spine. World Journal of Radiology 2012; 4(3):97-101</ref>, Konin 2010<ref name="Konin">Konin GP, Walz DM. Lumbosacral transitional vertebrae: classification, imaging findings, and clinical relevance. AJNR Am J Neuroradiol 2010; 31:1778-1786</ref>).  


<br>The sacrum is a triangular wedge-shaped bone with a concave anterior aspect, a convex dorsal aspect and an apex. The sacrum is tilted forward so that the upper surface articulates with the L5 vertebra above contributing to the “lumbosacral angle”. The intervertebral disc L4/5 and L5/S1 along with the vertebral body L5 account for nearly 60% of the angular measurement of lumbosacral curvature, averaging 61 degrees (Damasceno 2006). On the anterior surface of the sacrum the superior and inferior edges of the fused vertebral bodies correspond as transverse ridges. The scarum provides strength and stability to the pelvis and transmits forces to the pelvic girdle via the sacroiliac joints (Moore 1992). The sacral vertebrae are connected to the coccyx inferiorly.<br><br>  
<br>The sacrum is a triangular wedge-shaped bone with a concave anterior aspect, a convex dorsal aspect and an apex. The sacrum is tilted forward so that the upper surface articulates with the L5 vertebra above contributing to the “lumbosacral angle”. The intervertebral disc L4/5 and L5/S1 along with the vertebral body L5 account for nearly 60% of the angular measurement of lumbosacral curvature, averaging 61 degrees (Damasceno 2006)<ref name="Damasceno">Damasceno LHF, Catarin SRG, Campos AD, Defino HLA. Lumbar lordosis: a study of angle values and of vertebral bodies and intervertebral discs role. Acta Ortop Bras 2006; 14(4):193-198</ref>. On the anterior surface of the sacrum the superior and inferior edges of the fused vertebral bodies correspond as transverse ridges. The scarum provides strength and stability to the pelvis and transmits forces to the pelvic girdle via the sacroiliac joints (Moore 1992)<ref name="Moore">Moore, KL. Clinically Oriented Anatomy (3rd edition). 1992, Baltimore: Williams and Wilkins</ref>. The sacral vertebrae are connected to the coccyx inferiorly.<br><br>  


== <br>Biomechanics of the lumbar spine and sacrum (L4-L5 L5-S1)  ==
== <br>Biomechanics of the lumbar spine and sacrum (L4-L5 L5-S1)  ==


The 3 movements in the spine are flexion, extension, rotation and lateral flexion. These movements occur as a combination of rotation and translation in the following 3 planes of motion: sagittal, coronal and horizontal (Bogduk 2012). These movements result in various forces acting on the lumbar spine and sacrum: compressive force, tensile force, shear force, bending moment and torsional moment (Adams 2002).
For example, with lumbar flexion, a compressive force is applied to the anterior aspect of the disc and a distractive force is applied to the posterior aspect of the disc. The opposite forces occur with lumbar extension (McKenzie 2003).  
The 3 movements in the spine are flexion, extension, rotation and lateral flexion. These movements occur as a combination of rotation and translation in the following 3 planes of motion: sagittal, coronal and horizontal (Bogduk 2012)<ref name="Bogduk" />. These movements result in various forces acting on the lumbar spine and sacrum: compressive force, tensile force, shear force, bending moment and torsional moment (Adams 2002).
For example, with lumbar flexion, a compressive force is applied to the anterior aspect of the disc and a distractive force is applied to the posterior aspect of the disc. The opposite forces occur with lumbar extension (McKenzie 2003)<ref name="McKenzie">McKenzie, R. (1981). The lumbar spine : mechanical diagnosis and therapy. Waikanae, New Zealand: Spinal Publications.</ref>.  


<br>The lumbar spine complex forms an effective load-bearing system. When a load is applied externally to the vertebral column, it produces stresses to the stiff vertebral body and the relatively elastic disc, causing strains to be produced more easily in the disc (White and Panjabi 1978). Pressure within the nucleus pulposus is greater than zero, even at rest, providing a “preload” mechanism allowing for greater resistance to applied forces (Hirsch 1955). Hydrostatic pressure increases within the intervertebral disc resulting in an outward pressure towards the vertebral endplates resulting in bulging of the annulus fibrosis and tensile forces within the concentric annular fibres. This transmission of forces effectively slows the application of pressure onto the adjacent vertebra, acting as a shock absorber (Bogduk 2012). The intervertebral discs are therefore an essential biomechanical feature, effectively acting as a fibrocartilage “cushion” transmitting force between adjacent vertebrae during spinal movement. The lumbar disc is more predisposed to injury compared with other spinal regions due to: the annular fibres being in a more parallel arrangement and thinner posteriorly compared with anteriorly, the nucleus being positioned more posteriorly, and the holes in the cartilaginous endplates (Jensen 1980).  
<br>The lumbar spine complex forms an effective load-bearing system. When a load is applied externally to the vertebral column, it produces stresses to the stiff vertebral body and the relatively elastic disc, causing strains to be produced more easily in the disc (White and Panjabi 1978)<ref name="White">White A, Panjabi M. Clinical Biomechanics of the Spine. 1978, Philadelphia: JB Lippincott Co.</ref>. Pressure within the nucleus pulposus is greater than zero, even at rest, providing a “preload” mechanism allowing for greater resistance to applied forces (Hirsch 1955)<ref name="Hirsch">Hirsch C. The reaction of intervertebral discs to compression forces. J Bone Joint Surg (Am) 1955; 37:1188-1191</ref>. Hydrostatic pressure increases within the intervertebral disc resulting in an outward pressure towards the vertebral endplates resulting in bulging of the annulus fibrosis and tensile forces within the concentric annular fibres. This transmission of forces effectively slows the application of pressure onto the adjacent vertebra, acting as a shock absorber (Bogduk 2012)<ref name="Bogduk" />. The intervertebral discs are therefore an essential biomechanical feature, effectively acting as a fibrocartilage “cushion” transmitting force between adjacent vertebrae during spinal movement. The lumbar disc is more predisposed to injury compared with other spinal regions due to: the annular fibres being in a more parallel arrangement and thinner posteriorly compared with anteriorly, the nucleus being positioned more posteriorly, and the holes in the cartilaginous endplates (Jensen 1980)<ref name="Jensen" />.  


<br>When a load is applied along the spine, “shear” forces occur parallel to the intervertebral disc as the compression of the nucleus results in a lateral bulging of the annulus. Shear forces also occur as one vertebra moves, for example, forwards or backwards with respect to an adjacent vertebra with flexion and extension. Torsional stresses result from the external forces about the axis of twist (Jensen 1980)
and occur in the intervertebral disc with activity such as twisting of the spine.
<br><br>The zygapophysial or “facet” joints provide stability to the intervertebral joint with respect to shear forces, whilst allowing primarily flexion and extension movement.<br>  
<br>When a load is applied along the spine, “shear” forces occur parallel to the intervertebral disc as the compression of the nucleus results in a lateral bulging of the annulus. Shear forces also occur as one vertebra moves, for example, forwards or backwards with respect to an adjacent vertebra with flexion and extension. Torsional stresses result from the external forces about the axis of twist (Jensen 1980)<ref name="Jensen" /> 
and occur in the intervertebral disc with activity such as twisting of the spine.
<br><br>The zygapophysial or “facet” joints provide stability to the intervertebral joint with respect to shear forces, whilst allowing primarily flexion and extension movement.<br>  


== <br>Mechanism of Injury / Pathological Process  ==
== <br>Mechanism of Injury / Pathological Process  ==


Experiments indicate “intervertebral disc herniation” or prolapse is likely to be as a result of a gradual or fatigue process rather than a traumatic injury (Adams 1982), however clinically there is often a report of a sudden onset of symptoms associated with an incidental high loading of the spine, often in a flexed posture. The stresses most likely to result in injury to the spine are bending and torsion, and these combined movements reflect shear, compression and tension forces (Jensen 1980). Twisting movements are more likely to injure the annulus as only half the collagen fibres are orientated to resist the movement in either direction (Bogduk 2012)  
Experiments indicate “intervertebral disc herniation” or prolapse is likely to be as a result of a gradual or fatigue process rather than a traumatic injury (Adams 1982)<ref name="Adams">Adams M., Bogduk N., Burton K. Dolan P.. The Biomechanics of Back Pain. Eds. 2002. p238</ref>, however clinically there is often a report of a sudden onset of symptoms associated with an incidental high loading of the spine, often in a flexed posture. The stresses most likely to result in injury to the spine are bending and torsion, and these combined movements reflect shear, compression and tension forces (Jensen 1980)<ref name="Jensen" />. Twisting movements are more likely to injure the annulus as only half the collagen fibres are orientated to resist the movement in either direction (Bogduk 2012)<ref name="Bogduk" />


[[Image:Spine3.jpg]]  
[[Image:Spine3.jpg]]  
Line 41: Line 41:
(Figure: posterior disc migration with flexion of the spine (from: http://en.wikipedia.org/wiki/Disc_herniation)  
(Figure: posterior disc migration with flexion of the spine (from: http://en.wikipedia.org/wiki/Disc_herniation)  


<br>The degenerative disc changes associated with aging have been considered normal. For example, the concentration levels of proteoglycans within the nucleus reduces with age, from 65% at early adulthood to 30% at the age of 60, corresponding to a reduction in nuclear hydration and concentration of elastic annular fibres over this time, resulting in a less resilient disc. Narrowing of the disc with age has long been considered, however large post-mortem studies indicate that the dimensions of the disc actually increase between the 2nd and 7th decades. Apparent disc narrowing may otherwise be considered a result of a process other than aging (Bogduk 2012).  
<br>The degenerative disc changes associated with aging have been considered normal. For example, the concentration levels of proteoglycans within the nucleus reduces with age, from 65% at early adulthood to 30% at the age of 60, corresponding to a reduction in nuclear hydration and concentration of elastic annular fibres over this time, resulting in a less resilient disc. Narrowing of the disc with age has long been considered, however large post-mortem studies indicate that the dimensions of the disc actually increase between the 2nd and 7th decades. Apparent disc narrowing may otherwise be considered a result of a process other than aging (Bogduk 2012)<ref name="Bogduk" />.  


<br>There are also reductions in vertebral endplate nutrition and vertebral body bone density levels. The reduction in support from the underlying bone results in “microfracture” and the migration of nuclear material into the vertebral body known as “Schmorl’s nodes”, usually seen in the thoracolumbar and thoracic spines and have a low incidence below the level of L2. The lumbar facet joint subchondral bone density increases until the age of 50 after which time it decreases, and the joint cartilage continues to thicken with age despite focal changes, particularly where shear forces during repeated flexion and extension are resisted. Other bony changes also occur at the facet joint including “osteophyte” and “wrap-around bumper” formation presumably due to repeated stress at the superior and inferior articular process regions respectively (Bogduk 2012).  
<br>There are also reductions in vertebral endplate nutrition and vertebral body bone density levels. The reduction in support from the underlying bone results in “microfracture” and the migration of nuclear material into the vertebral body known as “Schmorl’s nodes”, usually seen in the thoracolumbar and thoracic spines and have a low incidence below the level of L2. The lumbar facet joint subchondral bone density increases until the age of 50 after which time it decreases, and the joint cartilage continues to thicken with age despite focal changes, particularly where shear forces during repeated flexion and extension are resisted. Other bony changes also occur at the facet joint including “osteophyte” and “wrap-around bumper” formation presumably due to repeated stress at the superior and inferior articular process regions respectively (Bogduk 2012)<ref name="Bogduk" />.  


<br>The processes of degeneration have also been considered as pathological. With respect to the facet joints “osteoarthritis” and “degenerative joint disease” are common diagnoses. “Spondylosis” and “intervertebral osteochondrosis” are also terms used to describe degenerative changes at the sites of the vertebrae and neural foraminae (Fardon 2001). “Degenerative disc disease” and are also common diagnoses. <br>  
<br>The processes of degeneration have also been considered as pathological. With respect to the facet joints “osteoarthritis” and “degenerative joint disease” are common diagnoses. “Spondylosis” and “intervertebral osteochondrosis” are also terms used to describe degenerative changes at the sites of the vertebrae and neural foraminae (Fardon 2001). “Degenerative disc disease” and are also common diagnoses. <br>  
Line 51: Line 51:
Figure: Lumbar spondylosis (from: http://en.wikipedia.org/wiki/Spondylosis)  
Figure: Lumbar spondylosis (from: http://en.wikipedia.org/wiki/Spondylosis)  


<br>The process of degeneration of the lumbar spine has been described in 3 phases (Frymoyer 1985, Kirkaldy-Wallis 1978):  
<br>The process of degeneration of the lumbar spine has been described in 3 phases (Frymoyer 1985<ref name="Frymoyer">Frymoyer JW, Selby DK. Segmental instability. Spine 1985; 10:280-286</ref>, Kirkaldy-Wallis 1978)<ref name="Kirkaldy_Wallis">Kirkaldy-Wallis WH, Wedge JH, Yong-Hing K, Reilly J. Pathology and pathogenesis of lumbar spondylosis and stenosis. Spine 1978; 3(4):319-328</ref>:  


<br>• Stage 1: “Early degeneration” involves increased laxity of the facet joints, fibrillation of the articular cartilage and intervertebral discs display grade 1-2 degenerative changes. <br>• Stage 2: “Lumbar instability” at the effected level(s) develops due to laxity of the facet capsules, cartilage degeneration and grade 2-3 degenerative disc disease. Segmental Instability: may be defined as loss of motion and segmental stiffness such that force application to that motion segment will produce greater displacements than would occur in a normal structure (Frymoyer 1985). Mechanical testing suggests the intervertebral disc is most susceptible to herniation at this stage (Adams 1982). <br>• Stage 3: “Fixed deformity” results from repair processes such as facet and peridiscal osteophytes effectively stabilising the motion segment. There is advanced facet joint degeneration (or “facet joint syndrome”) and grade 3-4 disc degeneration. Of clinical importance is altered spinal canal dimensions due to fixed deformity and osteophyte formation.  
<br>• Stage 1: “Early degeneration” involves increased laxity of the facet joints, fibrillation of the articular cartilage and intervertebral discs display grade 1-2 degenerative changes. <br>• Stage 2: “Lumbar instability” at the effected level(s) develops due to laxity of the facet capsules, cartilage degeneration and grade 2-3 degenerative disc disease. Segmental Instability: may be defined as loss of motion and segmental stiffness such that force application to that motion segment will produce greater displacements than would occur in a normal structure (Frymoyer 1985)<ref name="Frymoyer" />. Mechanical testing suggests the intervertebral disc is most susceptible to herniation at this stage (Adams 1982)<ref name="Adams" />. <br>• Stage 3: “Fixed deformity” results from repair processes such as facet and peridiscal osteophytes effectively stabilising the motion segment. There is advanced facet joint degeneration (or “facet joint syndrome”) and grade 3-4 disc degeneration. Of clinical importance is altered spinal canal dimensions due to fixed deformity and osteophyte formation.  


<br>Importantly, the incidence of spondylosis and osteoarthritis are the same in patients with symptoms and without symptoms, raising the question of whether these conditions should always be viewed as pathological diagnoses (Bogduk 2012). This has clinical implications particularly with respect to interpretation of radiological investigation findings, and how results are presented to and discussed with patients. <br><br><br>  
<br>Importantly, the incidence of spondylosis and osteoarthritis are the same in patients with symptoms and without symptoms, raising the question of whether these conditions should always be viewed as pathological diagnoses (Bogduk 2012)<ref name="Bogduk" />. This has clinical implications particularly with respect to interpretation of radiological investigation findings, and how results are presented to and discussed with patients. <br><br><br>  


== Outcome Measures  ==
== Outcome Measures  ==
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== References  ==
== References  ==
see [[Adding References|adding references tutorial]].


<references />  
<references />  


[[Category:Vrije_Universiteit_Brussel_Project]]
[[Category:Vrije_Universiteit_Brussel_Project]]

Revision as of 15:12, 29 July 2014

Original Editors Bert Lasat
Reviewed and updated by Matthew Richards 29/7/2014

Search Strategy[edit | edit source]

Literature was search using digital databases including PubMed for information regarding “lumbar and lumbosacral biomechanics”. Citation searching was then performed.


Keywords: Lumbosacral biomechanics, lumbar intervertebral disc degeneration/herniation, spinal anatomy.

Definition/Description[edit | edit source]

“Mechanics, the study of forces and their effects, when applied to humans, is called biomechanics” (Jensen 1980)[1]. Positioned below the thoracic spine, the lumbar spine normally has 5 vertebrae, while the sacrum consists of a series of usually 5 fused sacral vertebrae (Moore 1992)[2]. Together this lower portion of the vertebral column (see below) is referred to as the lumbosacral spine and is an important biomechanical region of the body.

Spine1.jpg

Clinically Relevant Anatomy[edit | edit source]

As with all vertebrae in the body, the lumbar and sacral vertebrae consist of a “body” anteriorly which is larger and more cylindrical in the lumbar region and a “vertebral arch” posteriorly which encloses the vertebral foramen protecting the neural tissues (Moore 1992)[2].


The vertebrae within the lumbar spine are separated by intervertebral joints which are unique articular structures, The intervertebral discs are the joint’s key component, made up of distinct features. The central paste-like nucleus pulposus consists primarily of water (70-90%) and hydrostatic proteoglycans (65% of the dry weight) loosely bound by collagen fibres (15-20% of the dry weight). The nucleus is surrounded by the strong concentric collagen layers of the annulus fibrosis consisting of water (60-70%), collagen (50-60% of the dry weight) and proteoglycans (20% of the dry weight) which are mostly aggregated. The nucleus and annulus both contain type II collagen throughout and the outer annulus contains a higher concentration of type I collagen. Elastic fibres (10%) are also found in the annulus and are arranged circularly, obliquely and vertically, with a concentration towards the attachment sites with the vertebral endplates. The vertebral endplate covers the upper and lower aspects of the disc and is strongly joined with fibrocartilage to the nuclear and annular parts of the disc. There is a greater concentration of collagen in the tissue nearer the bone (Bogduk 2012)[3].

Spine2.jpg

(Figure: shows the lumbar disc components (from: http://en.wikipedia.org/wiki/Annulus_fibrosus_disci_intervertebralis)

The lumbosacral transition is normally at the level of L5/S1 and the intervertebral disc at this level is wedge shaped. A “transitional vertebra” is a spinal anomaly where the lowest lumbar vertebra is to a degree fused or a failed segment of the sacrum thought to occur in 4-30% of the population (Chalian 2012[4], Konin 2010[5]).


The sacrum is a triangular wedge-shaped bone with a concave anterior aspect, a convex dorsal aspect and an apex. The sacrum is tilted forward so that the upper surface articulates with the L5 vertebra above contributing to the “lumbosacral angle”. The intervertebral disc L4/5 and L5/S1 along with the vertebral body L5 account for nearly 60% of the angular measurement of lumbosacral curvature, averaging 61 degrees (Damasceno 2006)[6]. On the anterior surface of the sacrum the superior and inferior edges of the fused vertebral bodies correspond as transverse ridges. The scarum provides strength and stability to the pelvis and transmits forces to the pelvic girdle via the sacroiliac joints (Moore 1992)[2]. The sacral vertebrae are connected to the coccyx inferiorly.


Biomechanics of the lumbar spine and sacrum (L4-L5 L5-S1)
[edit | edit source]

The 3 movements in the spine are flexion, extension, rotation and lateral flexion. These movements occur as a combination of rotation and translation in the following 3 planes of motion: sagittal, coronal and horizontal (Bogduk 2012)[3]. These movements result in various forces acting on the lumbar spine and sacrum: compressive force, tensile force, shear force, bending moment and torsional moment (Adams 2002).
For example, with lumbar flexion, a compressive force is applied to the anterior aspect of the disc and a distractive force is applied to the posterior aspect of the disc. The opposite forces occur with lumbar extension (McKenzie 2003)[7].


The lumbar spine complex forms an effective load-bearing system. When a load is applied externally to the vertebral column, it produces stresses to the stiff vertebral body and the relatively elastic disc, causing strains to be produced more easily in the disc (White and Panjabi 1978)[8]. Pressure within the nucleus pulposus is greater than zero, even at rest, providing a “preload” mechanism allowing for greater resistance to applied forces (Hirsch 1955)[9]. Hydrostatic pressure increases within the intervertebral disc resulting in an outward pressure towards the vertebral endplates resulting in bulging of the annulus fibrosis and tensile forces within the concentric annular fibres. This transmission of forces effectively slows the application of pressure onto the adjacent vertebra, acting as a shock absorber (Bogduk 2012)[3]. The intervertebral discs are therefore an essential biomechanical feature, effectively acting as a fibrocartilage “cushion” transmitting force between adjacent vertebrae during spinal movement. The lumbar disc is more predisposed to injury compared with other spinal regions due to: the annular fibres being in a more parallel arrangement and thinner posteriorly compared with anteriorly, the nucleus being positioned more posteriorly, and the holes in the cartilaginous endplates (Jensen 1980)[1].


When a load is applied along the spine, “shear” forces occur parallel to the intervertebral disc as the compression of the nucleus results in a lateral bulging of the annulus. Shear forces also occur as one vertebra moves, for example, forwards or backwards with respect to an adjacent vertebra with flexion and extension. Torsional stresses result from the external forces about the axis of twist (Jensen 1980)[1] 
and occur in the intervertebral disc with activity such as twisting of the spine.


The zygapophysial or “facet” joints provide stability to the intervertebral joint with respect to shear forces, whilst allowing primarily flexion and extension movement.


Mechanism of Injury / Pathological Process
[edit | edit source]

Experiments indicate “intervertebral disc herniation” or prolapse is likely to be as a result of a gradual or fatigue process rather than a traumatic injury (Adams 1982)[10], however clinically there is often a report of a sudden onset of symptoms associated with an incidental high loading of the spine, often in a flexed posture. The stresses most likely to result in injury to the spine are bending and torsion, and these combined movements reflect shear, compression and tension forces (Jensen 1980)[1]. Twisting movements are more likely to injure the annulus as only half the collagen fibres are orientated to resist the movement in either direction (Bogduk 2012)[3]

Spine3.jpg

(Figure: posterior disc migration with flexion of the spine (from: http://en.wikipedia.org/wiki/Disc_herniation)


The degenerative disc changes associated with aging have been considered normal. For example, the concentration levels of proteoglycans within the nucleus reduces with age, from 65% at early adulthood to 30% at the age of 60, corresponding to a reduction in nuclear hydration and concentration of elastic annular fibres over this time, resulting in a less resilient disc. Narrowing of the disc with age has long been considered, however large post-mortem studies indicate that the dimensions of the disc actually increase between the 2nd and 7th decades. Apparent disc narrowing may otherwise be considered a result of a process other than aging (Bogduk 2012)[3].


There are also reductions in vertebral endplate nutrition and vertebral body bone density levels. The reduction in support from the underlying bone results in “microfracture” and the migration of nuclear material into the vertebral body known as “Schmorl’s nodes”, usually seen in the thoracolumbar and thoracic spines and have a low incidence below the level of L2. The lumbar facet joint subchondral bone density increases until the age of 50 after which time it decreases, and the joint cartilage continues to thicken with age despite focal changes, particularly where shear forces during repeated flexion and extension are resisted. Other bony changes also occur at the facet joint including “osteophyte” and “wrap-around bumper” formation presumably due to repeated stress at the superior and inferior articular process regions respectively (Bogduk 2012)[3].


The processes of degeneration have also been considered as pathological. With respect to the facet joints “osteoarthritis” and “degenerative joint disease” are common diagnoses. “Spondylosis” and “intervertebral osteochondrosis” are also terms used to describe degenerative changes at the sites of the vertebrae and neural foraminae (Fardon 2001). “Degenerative disc disease” and are also common diagnoses.

Spine4.jpg

Figure: Lumbar spondylosis (from: http://en.wikipedia.org/wiki/Spondylosis)


The process of degeneration of the lumbar spine has been described in 3 phases (Frymoyer 1985[11], Kirkaldy-Wallis 1978)[12]:


• Stage 1: “Early degeneration” involves increased laxity of the facet joints, fibrillation of the articular cartilage and intervertebral discs display grade 1-2 degenerative changes.
• Stage 2: “Lumbar instability” at the effected level(s) develops due to laxity of the facet capsules, cartilage degeneration and grade 2-3 degenerative disc disease. Segmental Instability: may be defined as loss of motion and segmental stiffness such that force application to that motion segment will produce greater displacements than would occur in a normal structure (Frymoyer 1985)[11]. Mechanical testing suggests the intervertebral disc is most susceptible to herniation at this stage (Adams 1982)[10].
• Stage 3: “Fixed deformity” results from repair processes such as facet and peridiscal osteophytes effectively stabilising the motion segment. There is advanced facet joint degeneration (or “facet joint syndrome”) and grade 3-4 disc degeneration. Of clinical importance is altered spinal canal dimensions due to fixed deformity and osteophyte formation.


Importantly, the incidence of spondylosis and osteoarthritis are the same in patients with symptoms and without symptoms, raising the question of whether these conditions should always be viewed as pathological diagnoses (Bogduk 2012)[3]. This has clinical implications particularly with respect to interpretation of radiological investigation findings, and how results are presented to and discussed with patients.


Outcome Measures[edit | edit source]

Outcome measures regarding pain and disability include:
• Oswestry Disability Index
• Roland-Morris Disability Questionnaire
• Short-form McGill Pain Questionnaire
• Spinal Cord Independence Measure
• Numeric Pain Rating Scale
• Visual Analogue Scale


For further assessment of psychosocial factors associated with lumbosacral conditions, the following outcome measures may be useful:
• Orebro Musculoskeletal Pain Screening Questionnaire
• Depression Anxiety Stress Scale
• Fear Avoidance Beliefs Questionnaire
• Tampa Scale of Kinesiophobia
• Chronic Pain Acceptance Questionnaire
• Pain Catastrophizing Scale


(also see Outcome Measures Database)

Examination[edit | edit source]

Refer to Lumbar examination.

References[edit | edit source]

  1. 1.0 1.1 1.2 1.3 Jensen M Biomechanics of the lumbar intervertebral disk: a review. Physical Therapy. 1980; 60(6):765-773.
  2. 2.0 2.1 2.2 Moore, KL. Clinically Oriented Anatomy (3rd edition). 1992, Baltimore: Williams and Wilkins
  3. 3.0 3.1 3.2 3.3 3.4 3.5 3.6 Bogduk, N. (2012). Radiological and Clinical Anatomy of the Lumbar Spine (5th ed.). China: Churchill Livingstone.
  4. Chalian M, Soldatos T, Carrino JA, Belzberg AJ, Khanna J, Chhabra A. Prediction of trasitional lumbosacral anatomy on magnetic resonance imaging of the lumbar spine. World Journal of Radiology 2012; 4(3):97-101
  5. Konin GP, Walz DM. Lumbosacral transitional vertebrae: classification, imaging findings, and clinical relevance. AJNR Am J Neuroradiol 2010; 31:1778-1786
  6. Damasceno LHF, Catarin SRG, Campos AD, Defino HLA. Lumbar lordosis: a study of angle values and of vertebral bodies and intervertebral discs role. Acta Ortop Bras 2006; 14(4):193-198
  7. McKenzie, R. (1981). The lumbar spine : mechanical diagnosis and therapy. Waikanae, New Zealand: Spinal Publications.
  8. White A, Panjabi M. Clinical Biomechanics of the Spine. 1978, Philadelphia: JB Lippincott Co.
  9. Hirsch C. The reaction of intervertebral discs to compression forces. J Bone Joint Surg (Am) 1955; 37:1188-1191
  10. 10.0 10.1 Adams M., Bogduk N., Burton K. Dolan P.. The Biomechanics of Back Pain. Eds. 2002. p238
  11. 11.0 11.1 Frymoyer JW, Selby DK. Segmental instability. Spine 1985; 10:280-286
  12. Kirkaldy-Wallis WH, Wedge JH, Yong-Hing K, Reilly J. Pathology and pathogenesis of lumbar spondylosis and stenosis. Spine 1978; 3(4):319-328