The traditional classification is based on the type of injurious force, such as flexion type, extension type, rotational type, and longitudinal pressure injury, etc. This traditional classification method is not ideal because one force can cause more than one type of spinal injury, and the old classification method does not help in the selection of treatment methods. Canadian Armstrong, integrating his own experience and the classifications of some Western authors, proposed a classification based on the morphological damage, dividing spinal fractures into seven types. Each type has its unique characteristics and is associated with specific treatment methods. The new classification method makes the treatment of spinal fractures more scientific. The characteristics of each type are described as follows:
7. Compression fractures
Compression fractures are caused by anterior or lateral bending forces, the most common being anterior wedge fractures with reduced anterior vertebral body height. In addition, there are lateral compression fractures, where the heights on both sides of the vertebral body are different. These wedge changes often accompany injuries to the vertebral endplates and intervertebral discs, and the intervertebral disc can be compressed into the vertebral body. However, the height of the posterior edge of the vertebral body in compression fractures remains unchanged, which is different from rupture fractures.
5. X-ray examination of rotational injuries
The X-ray examination of rotational injuries shows one vertebral body rotating on another. Sometimes, it can be seen that the intervertebral space narrows, mainly due to injuries to the annulus fibrosus and nucleus pulposus. The upper angle of the anterior edge of the next vertebral body can be torn off a small piece by the annulus fibrosus, but the vertebral height remains unchanged. A few cases only have narrowing of the intervertebral space without annular fibrosis tear.
3. Rupture fractures
Rupture fractures are caused by violent forces acting along the longitudinal axis of the body. The intervertebral disc is compressed into the vertebral endplate, entering the cancellous bone and causing injury. The vertebral body cracks like an 'explosion' from the center, pushing the fragments in all directions, with posterior vertebral body edge fractures and fragments piercing into the spinal canal. The distance between the pedicles is cracked and widened. It often accompanies longitudinal fractures of the posterior vertebral plates, and the larger the anterior vertebral body crack, the more obvious the vertebral plate fracture. Sometimes, there is only an endplate fracture within the vertebral plate, which can only be detected by CT scan. Rupture fractures can also be divided into five types:
1. There are both upper and lower endplate injuries, accompanied by posterior vertebral body fragments piercing into the spinal canal, compressing the spinal cord, and causing neurological symptoms.
2. Fracture of the upper half of the vertebral body, with compression of the posterior part of the vertebral body, a fracture fragment rotates into the spinal canal, this type is the most common.
3. Injury to the inferior vertebral endplate.
4. Explosive fractures combined with rotational fractures, in addition to the characteristics of explosive fractures, there are also rotational spinous process deviations to one side;
5. Explosive fractures combined with lateral compression fractures, the fracture line obliquely crosses the vertebral body, the distance between the vertebral pedicles is widened, the heights on both sides of the vertebral body are different, and it often accompanies multiple transverse process fractures. This type is the most unstable. The main characteristics of explosive fractures are: widened interpedicular distances, posterior vertebral body compression, reduced height, and widened vertebral transverse diameter. Almost all explosive fractures have neurological symptoms.
IV. Shear fractures
Shear fractures, also known as slice-like fractures (slicefracture). They are often caused by flexion and rotation forces. All ligaments in the anterior and posterior parts of the spine are torn, and there may be fractures of one or both sides of the small joints, transverse processes, and pedicles, but the vertebral bone destruction is not obvious, and the vertebral height remains unchanged. However, the rotational shear force can tear off a small piece of bone from the superior margin of the next vertebral body, just like cutting off a thin slice. Since all structures are almost completely transversely cut, the fracture height is highly unstable, and patients often suffer from complete paraplegia. X-ray films show the characteristics of 'sliced' fracture fragments and widened vertebral spaces.
V. Posterior vertebral body fractures
Posterior vertebral body fractures, also known as seatbelt fractures (seatbelt fracture). This fracture was first described by Chance in 1948, hence the literature often refers to it as the Chance fracture, which is a type of flexion extension fracture. The typical injury mechanism is that the seat belt of a car is fastened around the patient's waist and abdomen. When a car traveling at high speed suddenly decelerates or collides, the trunk above the seat belt pivot point bends forward, and the forward thrust also produces a force that pushes a forward transverse process, then it pierces a threaded rod and tightens the nut to apply pressure and fix it. It should be pointed out that for those with widened posterior vertebral disc spaces and avulsion fractures, it indicates disc injury. Sometimes, after using the Harrington compression technique to reduce the fracture, neurological symptoms may appear. This is due to the herniation of the damaged intervertebral disc into the spinal canal and compressing the spinal cord. For such fractures, the injured intervertebral disc should be removed first before compression reduction.