We aim to demonstrate the key features to recognise VFFs. They should not be confused with expected age-related degenerative remodelling, features including sclerotic endplates with the cortices intact and normal bone density.
Vertebral fragility fractures can be characterised by morphometric or morphologic evaluation. This presentation aims to demonstrate morphometric evaluation of VFF on radiographs, CT and MRI, and associated pitfalls.
How to recognise VFFs:
- Disruption of the cortices of the endplates and anterior border.
- Loss of vertebral body height compared to adjacent vertebrae.
- Overall reduction in bone mineral density.
- Compare with previous imaging – is there a new vertebral deformity?
Studies have demonstrated the use of average Hounsfield units (HU) on computer tomography (CT) to predict osteoporosis. The suggested threshold for diagnosing osteoporosis is 87-111 HU, with the threshold for ruling out osteoporosis/osteopenia being 99-125 HU3. This method has the potential to do quick opportunistic bone density assessments on readily available imaging thus eliminating the need for extra tests such as dual-energy X-ray Absorptiometry (DEXA) to diagnose osteoporosis.
Manifestations and evaluation of VFF on different imaging modalities utilising:
Different classification systems for assessment of vertebral fragility fractures:
A recent National UK audit with the Royal College of Radiologists used the Genant’s semi-quantitive method to assess for Grade 1, 2 and 3 vertebral fractures. We therefore aim to describe vertebral fractures using X-ray, CT and MRI using the Genant Semi-quantitative method. Using this method, the shape of the fracture has been described as wedge, biconcave and crush fractures (fig.2). The shape has not been shown to have bearing on clinical symptoms or presentation and most fractures demonstrate a combination of deformity shapes5.
According to the Genant’s semi-quantitive method, a wedge fracture is defined as a difference in height between the anterior and posterior vertebral borders of >20%. When using this technique, it is important to take into consideration the appearance of adjacent vertebral bodies5. Age-related remodelling can also demonstrate a loss of >20% vertebral height without endplate disruption and should not be interpreted as fractures.
Grade 1 20-25% vertebral body height loss with structural evidence of fracture:
Grade 2: 26-40% vertebral body height loss with structural evidence of fracture.
Grade 3: >40% vertebral body height loss with structural evidence of fracture.
When assessing for vertebral fragility fractures it is important to consider fracture mimics. For which we will address below:
Mimics: Schmorl’s nodes and Sheuermann’s disease
Figures 10 and 11 demonstrate typical appearances of Schmorl’s nodes (arrow head). Schmorl’s nodes are caused by invagination or herniation of intervertebral disc material into the vertebral body endplate. Adjacent to the Schmorl’s nodes you often see marginal sclerosis of the bone adjacent to the node due to bone remodelling.
Scheuermann disease is defined as multiple schmorl’s nodes causing wedging and kyphosis:
- Schmorl’s nodes in ≥ 3 contiguous vertebrae
- usually in the thoracic spine
- at least 5o of wedging at each level
Mimics: Malignant fractures
There are features that can help distinguish between a benign vs. malignant fracture:
Mimics: Multiple Myeloma