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Congress: ECR25
Poster Number: C-22298
Type: Poster: EPOS Radiologist (educational)
Authorblock: C. C. F. C. Ferreira, E. F. M. P. Negrao, G. Afonso, A. X. Francisco Mesquita, A. C. Afonso Silva; Porto/PT
Disclosures:
Catarina Costa Filipa Costa Ferreira: Nothing to disclose
Eduardo Francisco Miranda Peres Negrao: Nothing to disclose
Guilherme Afonso: Nothing to disclose
António Xavier Francisco Mesquita: Nothing to disclose
Ana Catarina Afonso Silva: Nothing to disclose
Keywords: Anatomy, Management, Musculoskeletal bone, Conventional radiography, Education, Education and training, Image verification
Findings and procedure details

Wrist and hand x-ray projections

The standard wrist and hand radiographs projections includes posteroanterior, oblique, and lateral views [3,4].

  • Posteroanterior (PA) projection: The best for visualizing and inspecting bone alignment, the joint spaces of the carpal bones and the distal radioulnar joint. This projection is obtained with the shoulder abducted 90°, the elbow flexed at 90°, and the forearm in a pronated position, with the palm facing down [5].
  • Lateral projection: The essential view to assess the alignment of the radius, lunate, and capitate. This projection is obtained with the elbow flexed at 90° and adducted against the trunk. The forearm should be in a mid-prone position, with the fingers and metacarpals superimposed [5,6].
  • Oblique projection: It is an important view to evaluate the scaphoid tuberosity, scaphotrapeziotrapezoidal joint and trapeziometacarpal articulation. This projection is obtained like the PA view, but with the wrist and hand rotated laterally 45° from the pronated position [5,6].

Additional projections may be necessary when initial radiographs are normal but a fracture is still suspected. For instance, a PA view with ulnar deviation is useful for detecting potentially hidden scaphoid fractures [5].

Fig 1: A) PA projection of the hand and anatomy. The X-ray central beam should be aligned with third metacarpophalangeal joint. B) PA projection of the wrist and anatomy. The X-ray central beam should be directed to midcarpal area. MCPJ: metacarpophalangeal joint; PIPJ: proximal interphalangeal joint; DIPJ: distal interphalangeal joint. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Fig 2: Lateral projection of the wrist. For the lateral projection of the wrist, the X-ray central beam should be directed to the midcarpal area. In contrast, for the lateral view of the hand, the X-ray central beam should be aligned with the second to fifth metacarpophalangeal joints. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Fig 3: A) Oblique projection of the hand. The X-ray central beam should be aligned with the third metacarpophalangeal joint. B) Oblique projection of the wrist. The X-ray central beam should be directed to the midcarpal area. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Systematic wrist and hand radiographs approach

  • Bone alignment

Evaluating the alignment of the carpal bones, metacarpals, and phalanges is crucial [7]. The carpal alignment is guided by four key principles:

- Gilula three carpal arcs: Gilula’s arcs are evaluated in wrist PA radiographs. Any disruption suggests a ligamentous injury or fracture [8].

- Rule of the spaces: the joint space between the carpal bones carpal bones should be consistent (1-2 mm) [9].

- Rule of the parallelism: the articular surfaces of the adjacent carpal bones should be parallel to each other [9].

- Lateral carpal alignment: In the lateral wrist projection, the longitudinal axes of the third metacarpal, lunate, capitate and radius should be aligned. Any deviation indicates carpal instability [8].

Fig 4: PA radiograph of the wrist illustrating the Gilula’s arcs. The proximal (red) arc outlines the proximal surfaces of the scaphoid, lunate, and triquetrum. The middle (blue) arc outlines the distal surface of the scaphoid, lunate, and triquetrum. The distal (yellow) arc outlines the proximal surface of the capitate and hamate. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Fig 5: A) PA radiograph of the hand illustrating the rule of the spaces. B) Wrist PA radiograph illustrating an abnormal widening of the scapholunate joint associated with a scaphoid non-union fracture. The scapholunate interval (interval >3 mm) is the gap between the scaphoid and lunate bones, which can indicate a scapholunate dissociation. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Fig 6: Neutral lateral wrist radiograph showing normal alignment and a radius fracture (red arrow). Colour delimitations highlight key structures: blue (radius), yellow (lunate), orange (capitate), and green (third metacarpal). © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

The rules of spaces and parallelism apply not only to carpal alignment but also to the metacarpophalangeal and interphalangeal joints.

- Subluxation: refers to an insufficient joint surface contact in these joints and is commonly seen in conditions such as rheumatoid arthritis, psoriatic arthritis, and osteoarthritis [10]. 

Fig 7: PA radiograph of the right-hand showing subluxation of the proximal phalanges in an ulnar and palmar direction in relationship to the adjacent metacarpals, a characteristic feature commonly associated with a history of rheumatoid arthritis. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

  • Cortical integrity

The cortex should appear continuous. Any interruption or disruption of the cortical outline may indicate a fracture. Fractures of the scaphoid and triquetrum are the most common fractures of the carpal bones [11,12].

When a fracture is identified, it is crucial to assess various factors, including the fracture morphology (e.g., transverse, oblique, or spiral), location, intra-articular extension, impaction, displacement, angulation, and any associated fractures or soft tissue injuries [13].

A potential differential diagnosis for a fracture includes vascular lines, which may mimic cortical irregularities but are, in fact, a normal anatomical feature [11,12].

Fig 8: PA hand radiograph showing transverse lucent line through of the mid pole of the scaphoid indicating fracture (red arrow), with sclerosis and hypertrophic changes of the fracture margins indicating non-union with pseudoarthrosis. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Fig 9: A and B) PA wrist projection showing an oblique, well-defined lucent line passing through the shaft of the fifth metacarpal, characteristic of a vascular line. Vascular lines represent vascular structures passing obliquely through the cortex and may exhibit a corticated edge. Unlike fractures, they do not disrupt bone alignment. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

  • Trabecular patterns

Alterations on trabecular patterns could indicate a bone lesion. Besides, subtle increase in density could suggest a minor fracture [14]. 

Fig 10: PA wrist projection showing a lytic lesion with well-defined edges in the capitate, without radiographic signs of aggressiveness, such as periosteal reaction or endosteal scalloping. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

  • Joint abnormalities

Cartilage is radiolucent; however, the cartilage can be assessed by evaluating the preservation of joint space width. Potential joint pathological findings include joint space narrowing and the presence of erosions [10].

- Loss of joint space: Asymmetric joint loss is commonly associated with osteoarthritis, whereas symmetrical joint loss is typically linked to inflammatory arthropathies, such as rheumatoid and psoriatic arthritis [10].

- Erosions: Marginal erosions are characteristic of rheumatoid and psoriatic arthritis; central erosions are typical of erosive osteoarthritis; and periarticular erosions are commonly observed in gout [10].

Fig 11: PA hand projection demonstrating degenerative changes of the hand, including asymmetric joint space narrowing, subchondral sclerosis, and marginal osteophytosis. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Fig 12: PA hand radiographs showing: A) Marginal erosion (orange arrow) in a patient with rheumatoid arthritis; B) Central erosion (green arrow) creating a "seagull" configuration, typical of erosive osteoarthritis; C) Periarticular erosion (yellow arrow) associated with a lumpy-bumpy soft tissue swelling, typically seen in gout. Small elevated ridges of bone at the margins of the erosion are consistent with an "overhanging edge". © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

  • Abnormalities in the surrounding soft tissues

Soft tissue abnormalities in the hand and wrist include a wide range of conditions, from normal variants to cystic lesions, post-traumatic changes, inflammatory and infectious disorders, vascular anomalies, metabolic issues, and other miscellaneous conditions [15].

Soft tissue abnormalities are often key in assessing arthropathies, especially inflammatory or depositional arthritis. Symmetrical soft tissue swelling around a joint suggests synovitis, and swelling may appear focal, diffuse, symmetric, asymmetric, or lumpy-bumpy [10]. 

Fig 13: A) PA hand projection. B) Oblique hand projection. These radiographs reveal soft tissue swelling on the ulnar aspect of the wrist (red arrow). (C) Transverse ultrasound image demonstrating a well-defined anechoic structure on the ulnar aspect of the wrist, consistent with a ganglion cyst. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Fig 14: Radiographs showing calcinosis cutis circumscripta. Calcinosis may be caused by various etiologies, such as systemic sclerosis. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Critical standard diagnostic measurements

  • Bone mineralization

Osteoporosis is a systemic metabolic disorder characterized by a decline in bone quality and mass, leading to increased bone fragility and an increased risk of fracture [16].

The main radiographic finding in osteoporosis is thinning of the cortex. Bone mineralization can be assessed through a measurement on hand and wrist radiographs by calculating a ratio. This ratio is derived from the transverse diameter of the trabecular bone of the second or third metacarpal shaft, divided by the maximum diameter of the respective metacarpal shaft. A ratio less than 0.5 is considered normal, while a ratio greater than 0.5 indicates a subjective reduction in bone mineral density [17]. 

Fig 15: PA radiographs demonstrating how bone mineralization should be assessed. A) Normal bone mineral density, where the ratio is less than 0.5. B) Subjective decrease in bone mineral density, where the ratio is greater than 0.5. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

  • Radial inclination and height

Radial inclination and radial height are key measurements in the evaluation and treatment of distal radius fractures. A decrease in either the radial inclination angle or radial height may indicate a radial fracture. [18].

- Radial inclination: Angle between the articular surface of the radius and a line perpendicular to the diaphysis. Normal: 21º-25º [18].

- Radial height: Distance between two lines perpendicular to the radial shaft: a line passing through the styloid process of the radius and a line parallel and adjacent to the distal articular surface of the ulna. Normal: 8 to 14 mm [18].

Fig 16: PA hand radiographs showing how to access to radial inclination (A) and radial height (B). © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

  • Ulnar variance

Ulnar variance is measured by drawing a line along the distal articular surface of the radius and determining the distance to the distal surface of the ulna [19]:

- Neutral: The radial and ulnar surfaces are at the same level.

- Negative: The ulna is more than 2.5 mm proximal to the radius articular surface.

- Positive: The ulna is more than 2.5 mm distal to the radius articular surface.

Ulnar variance is unaffected by the length of the ulnar styloid process. Accurate measurement requires a true PA view, as supination or pronation alters the apparent lengths of the radius and ulna. If the ulnar styloid process overlaps the head, ulnar variance cannot be measured reliably [19].

Fig 17: PA wrist radiographs showing the different types of ulnar variance. Neutral ulnar variance (A) occurs when both ulnar and radial articular surfaces are at the same level. Negative ulnar variance (B) is when the ulnar articular surface is ≤2.5 mm than the radial articular surface. Positive ulnar variance (C) occurs when the ulnar articular surface is >2.5 mm beyond the radial articular surface. A well-defined lytic lesion is present on the distal articular surface of the radius (C), consistent with a subchondral cyst. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

  • Scapholunate and capitolunate angles

When carpal instability is suspected, the scapholunate and capitolunate angles should be measured. These angles can only be assessed on a neutral lateral wrist radiograph [8]:

- Scapholunate angle: Determined by a line drawn along the long axis of the scaphoid and another along the mechanical axis of the lunate. The normal range is 30° to 60°;

- Capitolunate angle: Determined by the same lunate axis line compared to the long axis of the capitate. The normal range is 0° to 30°.

Any deviation from the normal ranges for these angles suggests carpal instability [8].

Fig 18: Radiographs demonstrating how to approach the standard lateral view of the wrist. It is essential to evaluate the alignment along the longitudinal axes of the radius, lunate, capitate, and third metacarpal (A). The scapholunate angle (B) is the angle between the long axis of the scaphoid and the mid-axis of the lunate, and it should be between 30° and 60°. The capitolunate angle (C) is the angle between the long axis of the capitate and the mid-axis of the lunate, and it should be less than 30°. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Normal anatomical variants

Recognizing normal anatomic variations, such as accessory ossicles, epiphyseal spurs, and persistent ulnar styloid ossicles, is crucial to prevent misdiagnosing these structures as fractures or degenerative changes, thereby avoiding unnecessary investigations and treatments that may harm the patient [20].

Fig 19: PA hand radiographs showing persistent ulnar styloid ossicle (A) and Os triangulare (B). They are usually identified as bony structures with smooth, well-corticated margins, without associated surrounding soft tissue swelling. These two anatomical variants should not be misdiagnosed as ununited ulnar styloid fractures. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

Fig 20: PA hand radiograph showing an accessory bone (Os radiale externum), located laterally to the scaphoid and trapezium bones. © Department of Radiology, Unidade Local de Saúde São João, Porto/Portugal.

GALLERY