Abstract
Subchondral insufficiency fractures (SIFs) and SIFs with osteonecrosis (SIF-ONs) of the knee (previously misnamed spontaneous osteonecrosis of the knee (SONK)) are bone lesions that appear without prior traumatic, tumoral, or inflammatory event.
Both conditions are characterized in the early stages by epiphyseal bone marrow edema (BME)-like signal at MRI. However, while SIFs usually heal spontaneously, they can also evolve to osteonecrosis (i.e., SIF-ON), which may progress to an irreversible collapse of the articular surface. Careful analysis of other MRI signs may help differentiate the two conditions in the early phase. In SIFs, the BME edema-like signal extends to the area immediately adjacent to the subchondral plate, while in SIF-ONs, this subchondral area shows low signal intensity on fluid-sensitive MR images due to altered bone marrow. The thickness and length of subchondral areas with low fluid-sensitive signal intensity are important factors that determine the prognosis of SIF-ONs. If they are thicker than 4 mm or longer than 14 mm, the prognosis is poor. The differential diagnosis of SIFs and SIF-ONs include bone lesions associated with the “complex regional pain syndrome” (CRPS), epiphyseal osteonecrosis of systemic origin, and those related to cartilage pathology.
Clinical relevance statement Imaging plays an essential role in diagnosing subchondral insufficiency fractures (SIFs) from subchondral insufficiency fractures with osteonecrosis (SIF-ONs) and collapse, as well as in distinguishing them from other spontaneous knee subchondral bone lesions presenting with bone marrow edema-like signal.
Key points
• Subchondral insufficiency fractures may affect the knee, especially in older adults.
• Subchondral insufficiency fractures usually heal spontaneously.
• Sometimes, subchondral osteonecrosis and collapse may complicate subchondral insufficiency fractures.
• Bone marrow-like edema is an aspecific sign seen in all these lesions.
• Degraded marrow in osteonecrosis complicating fractures is hypointense on fluid-sensitive sequences.
Graphical Abstract
Keywords: Insufficiency fracture, Spontaneous osteonecrosis of the knee, Bone marrow edema, Knee, Subchondral bone
Background
This manuscript deals with various lesions affecting the knee epiphyses; occurring in the absence of prior trauma, tumor, inflammatory, or infectious disease; and mainly presenting as bone marrow edema (BME)-like signal at MRI, or as an epiphyseal collapse.
The lesions associated with BME-like signal changes can either heal spontaneously or progress to epiphyseal collapse associated with subchondral osteonecrosis. So, it is important to differentiate between the underlying conditions associated with BME-like signal. However, this can be a difficult task due to many sources of confusion.
The first source of difficulty is related to the fact the BME-like signal is an aspecific MRI sign which may be associated with very different pathophysiological processes. For example, BME-like signal can be the consequence of insufficiency fractures or associated with a clinical entity that is not fully understood, called “complex regional pain syndrome” (CRPS) (previously referred to as “reflex sympathetic dystrophy syndrome, algodystrophy, or transient osteoporosis”). In addition, similar lesions can be observed in osteoarthritis, which may be associated with a variable amount of subchondral BME-like signal and osteonecrosis.
Second, some of the conditions associated with BME-like signal may themselves have very different origins. Epiphyseal osteonecrosis may for example complicate insufficiency fractures, but it can also be of ischemic origin, due to various systemic hemodynamic or metabolic disorders.
Third, there is great confusion around the terminology used in the literature. For example, some authors use the term “secondary osteonecrosis” in reference to osteonecrosis complicating insufficiency fractures [1], while others use it to designate osteonecrosis of systemic origin [2, 3]. Another source of confusion is the use of the term “Spontaneous osteonecrosis of the knee” (SONK) to either refer to spontaneous lesions that can heal or to those that are complicated by collapse [4, 5]. Others have used using the term “Subchondral insufficiency fracture” (SIF) to refer to both types of lesions: those which heal spontaneously and those that progress to collapse [6–8]. This is reflected in a recent opinion paper where the experts of the “International Skeletal Society” have proposed to completely abandon the term “SONK” in favor of “SIF” [1, 9].
In this review, we discuss the pathological conditions associated with BME-like signal in the knee epiphysis, presenting key imaging features allowing the differential diagnosis between lesions that may have a very different prognosis.
To avoid confusion between entities that have a different clinical significance, in the rest of the manuscript, we will distinguish between “simple insufficiency fractures” (SIFs) and fractures complicated by irreversible collapse, referred to as “osteonecrosis after insufficiency fractures” (SIF-ONs) (Fig. 1). We will also use the term “Osteonecrosis of systemic origin” to designate epiphyseal osteonecrosis complicating ischemic lesions.
Subchondral insufficiency fractures, without (SIF) or with osteonecrosis (SIF-ON)
The subchondral area of the epiphyses of the knees can be the site of SIFs, which are potentially transient, but can also become irreversible if evolving to osteonecrosis (i.e., SIF-ON) and collapse.
Historical background
Spontaneous epiphyseal collapses (referred to as “idiopathic osteonecrosis of the knee”) have been described as a distinct entity by Ahlbäck et al. in 1968, with very precise descriptions of the clinical context [10]. With the advent of magnetic resonance imaging (MRI), it became evident that these collapses were preceded by areas of bone marrow edema (BME)-like signal changes, which were visible on MRI before radiographic collapse. Consequently, the term “spontaneous osteonecrosis of the knee (SONK)” has been extensively used to describe any spontaneous onset of pain that is associated with subchondral BME-like signal at MRI, or epiphyseal uptake on bone scans [11–13].
Other authors have noted similarities between spontaneous BME-like signal changes that are transient and those followed by focal subchondral osteonecrosis. These observations have led these authors to consider a common etiology and the hypothesis that an insufficiency fracture could represent the triggering event in both cases [14–22].
A histological study by Yamamoto and Bullough in 2000 has largely contributed to advancing the debate. These authors retrospectively reviewed the histological material of surgically treated lesions that had been previously diagnosed as “SONK” based on the clinical presentation, imaging studies (including MRI), and pathologic findings. They found two types of lesions in histology: first, lesions that have a subchondral fracture line with no evidence of associated osteonecrosis, and second, lesions that have a subchondral fracture line associated with focal osteonecrosis (Fig. 2). Since the osteonecrotic area was strictly confined to the area between the fracture line and the articular surface, the authors concluded that the fracture is probably the primary event [23].
A few years later in 2008, another histological study of lesions diagnosed as “SONK” by Takeda et al. found that while in the early stages without collapse no osteonecrosis was seen, such features were visible in more advanced stages and confined to the area distal to the site of the fracture, which showed impaired healing [24] (Fig. 3).
Clinical context
The clinical context of SIFs is the same as that of the so-called SONKs [25]. Both types of lesions occur mainly in patients above 60 years of age, mainly females, without any specific history of metabolic disorder or therapeutic intervention [6, 10, 25–28]. A potential link with underlying osteopenia is suggested by some studies, but not all [28–30]. However, it should be noted that insufficiency fractures may be particularly large or numerous in patients with conditions leading to bone fragility such as in renal transplant recipients or in cases of osteomalacia [18, 31] (Fig. 4).
The onset of symptoms is sudden in almost three-quarters of cases and occurs after a minor trauma or even after a wrong move. The onset is so sudden that patients commonly remember the exact moment it occurred [14, 26].
The lesions are predominantly located in the medial femoral condyle (in about 65% of cases), in the weight-bearing area [14, 26, 30]. The lateral condyle is much more rarely affected (in about 15% of cases), just as the medial tibial plateau. Involvement of the lateral plateau is very rare [28].
The association with chondrosis varies greatly depending on the series, from intact cartilage to severe chondrosis in cases with advanced collapse [7, 9, 30]. The association with a meniscal tear, on the other hand, has been consistently reported (in up to 76–94% of cases) [25]. In particular, the association with radial tears of the posterior horn of the medial meniscus or its attachment is found in more than 50% of cases [25, 27]. These meniscal tears are almost always associated with meniscal extrusions of 3 mm or more beyond the joint space margin [28] (Fig. 1d). They destabilize the meniscus and increase the mechanical strain on the articular surfaces by more than 25%, to the same extent as large meniscectomies [32] (Fig. 5). Similarly, subchondral fractures or osteonecrosis may also occur following meniscectomy [17, 25, 33–35] (Fig. 6).
Radiographic appearance
For non-complicated insufficiency fractures (i.e., SIFs), radiographs are normal or show subtle abnormalities with subchondral radiolucencies and/or slight flattening of the convexity of the condyle (Fig. 7a) [23]. In the event of an insufficiency fracture associated with osteonecrosis (i.e., SIF-ON), the area of subchondral collapse becomes markedly heterogeneous and is surrounded by a sclerotic halo (Fig. 1b). At this stage, the articular surface may present signs of “macroscopic” fracture, with focal depression or disruption of the subchondral bone plate, or with separation of the subchondral bone plate adherent to the cartilage from the rest of the bone (showing as a subchondral radiolucent line—the crescent sign—or “eggshell” subchondral dissection) (Fig. 8). These signs are pathognomonic of osteonecrosis, whether related to an insufficiency fracture or systemic in origin. These abnormalities can be seen on radiographic views tangent to the area of interest, possibly performed in traction to open the subchondral separation (Fig. 9a and b). Later, secondary osteoarthritic changes become apparent (Fig. 9c) [23].
MRI appearance
Classic appearance of BME-like signal
The key finding of SIFs is BME-like signal. However, this MRI sign is far from specific. At histology, actual BME (extracellular fluid) is rarely seen, and the MRI signal alterations originally described as edema are due to a variable amount of vascular dilatation, interstitial hemorrhage, cellular infiltration, granulation tissue, microfracture and callus formation, necrosis, and fibrosis, depending on the etiology [29, 36]. At imaging, it is therefore recommended to avoid the terms “edema” or “edematous signal” in favor of “edema-like signal.” In the rest of this article, we will refer to these MRI signal alterations of the bone marrow as “BME-like signal” or “BME-like pattern” [1, 9].
BME-like signal refers to an ill-defined area of bone marrow with moderately decreased signal intensity on T1-weighted images and with increased signal intensity on T2-weighted images, more evident on fat-suppressed fluid sensitive images (Fig. 7b, c) (i.e., fat-suppressed T2 (T2FS), short-tau inversion recovery (STIR), fat-suppressed proton density (DPFS), Dixon T2 “Water” images). For the sake of simplicity, we will refer to all types of fat-suppressed fluid-sensitive sequences as “T2FS.” After intravenous injection of contrast media, the signal on T1-weighted sequences enhances and becomes practically similar to that of normal bone marrow (Fig. 10) [8, 22, 37].
The location and extension of BME-like signal changes vary depending on their origin. In SIFs, the signal abnormality predominates near the articular surface and extends in a gradient over a variable portion of the epiphysis. On the other hand, BME-like changes in osteoarthritis are generally more confined [25]. The extension of the BME-like signal has no prognostic value [25].
BME-like pattern may be accompanied by a thin high signal intensity line on T2FS images, immediately adjacent to the subchondral bone plate, which could be related to hyperemia in this richly vascularized area [38]. In cases of SIF, this aspect is present in more than half of cases, especially in the acute (< 3 months) or subacute (3–6 months) phase [39]. In addition to the intraosseous BME-like signal, adjacent soft tissue edema signal may also be seen and has been reported in the vast majority of SIFs involving a femoral condyle (Fig. 11) [28].
Importantly, the BME-like signal in SIF has poorly defined borders, opposite to osteonecrosis of systemic origin where the lesion is surrounded by a distinct, geographic rim of sclerosis/low signal intensity line [20, 21, 27, 40].
Visibility of the fracture line and its hypothetical pathogenic implication
When visible, the fracture has the appearance of a thin, somehow curvilinear line located at a short distance from the articular surface. This line shows low signal intensity on all sequences and is best visible in T2FS images because on T1-weighted images, it can be masked by the adjacent low-intensity BME-like signal changes. Importantly, in SIFs, the BME-like pattern is present on both sides of the fracture line (Figs. 7c and 12).
One possible pathogenic hypothesis explaining the difference between a SIF that evolves towards a SIF-ON and a SIF that heals may be related to how the fracture line isolates completely or not the adjacent subchondral area (Fig. 13). The presence of a complete fracture line isolating entirely the subchondral bone between the fracture and the articular surface may compromise the vascularization of the isolated subchondral area, possibly leading to necrosis. On the other hand, if the fracture line does not isolate completely an area of subchondral bone, a continuity persists with the rest of the epiphysis, and the vascularization may be preserved in this area, preventing osteonecrosis (Fig. 12c and d).
This pathogenic hypothesis is based on the assumption that the normal vascular supply of the epiphyseal subchondral bone results from a network of anastomotic terminal arterioles. This seems to be well-illustrated in an anatomical study by Reddy and Frederick (Fig. 14) [41]. But, even in case of persistent communication between the remaining epiphysis and the subchondral bone adjacent to the fracture, there may still be inadequate blood flow in certain cases, especially if the area is too large to be fully supported by the remaining micro-arterial network.
Another hypothesis could be that necrosis occurs following pseudarthrosis of the insufficiency fracture, resulting in the separation of a distal bone fragment that has become unstable, with the loss of its blood supply ultimately leading to osteonecrosis [24]. But this hypothesis does not account for the subchondral bone signal alterations (low signal on T2-weighted and post-contrast T1-weighted images) which can be observed in some early lesions without collapse or subchondral separation (see below).
Evolution of SIFs
In SIFs, conservative treatment with protected weight-bearing generally allows a reduction in pain and healing without sequelae [3, 4, 26, 42]. The treatment generally consists of protected weight-bearing for a period of 6 weeks using crutches, followed by gradual weight-bearing using walking sticks. Physiotherapy can help prevent muscle atrophy. Adjuvant treatment with bisphosphonates is suggested by some [43, 44]. In uncomplicated SIFs, the BME-like signal normalizes within a few months (Fig. 12).
Evolution of SIF-ONs
A marked collapse of the articular surface indicates decompensation of the lesion. The subchondral bone under the collapsed articular surface may become disorganized and present various aspects (Fig. 15). Later in the disease, subchondral fractures can turn into transchondral fractures releasing fragments from the articular surface.
Even before the macroscopic fracture stage, the bone marrow immediately adjacent to the subchondral bone may show decreased signal on T2w images [13, 20, 21, 40, 45–48]. This low signal intensity bone marrow may correspond histologically to degraded, “saponified,” solidified marrow fat [49]. This area shows no enhancement on post-contrast T1-weighted images (Fig. 16) [20, 40, 47]. When it is thin, this area of low intensity on T2-weighted images can be difficult to distinguish from a thickened subchondral bone plate [48].
Prognostic value of bone marrow low signal intensity on T2-weighted or post-contrast T1-weighted images
The pejorative prognostic value of bone marrow low signal on T2-weighted images was described as early as in 1990 [13]. Subchondral areas of low T2 signal intensity thicker than 4 mm or longer than 14 mm were shown to be predictive of irreversible lesions, with sensitivities/specificities of about 100%/80% for the thickness and nearly 90%/90%, for the length, respectively (Fig. 17) [20, 21]. Subchondral bone marrow areas of more than 3 cm2 not enhancing on post-contrast T1-weighted images were also shown to be a factor of poor prognosis [40]. Other poor prognostic factors include a clear deformation of the articular surface and the location of fracture lines far from the articular surface (Fig. 18) [21].
On the other hand, a subchondral low T2 signal intensity area thinner than 2 mm is usually indicative of a reversible lesion [20, 21]. In this case, this low signal intensity area most likely corresponds to a very limited area of superficial osteonecrosis, or to granulation and fracture repair tissue.
Lesions with subchondral low T2 signal intensity areas between 2 and 4 mm should be considered of uncertain prognosis and be followed up (Fig. 19).
However, these prognostic factors are merely indicative, and an initially uncomplicated SIF may still decompensate at a later stage (Fig. 20), either spontaneously or following a destabilizing meniscectomy.
The prognostic value of T2-weighted MR images is summarized in Fig. 21.
Late evolution of lesions
The occurrence of complications depends on multiple factors, including the patient’s weight, degree of osteopenia, treatment delay, the extent of chondrosis, and degree of meniscal extrusion associated with a radial tear or root tear of the posterior horn of the medial meniscus [4, 7, 28].
The evolution towards a progression of the articular surface collapse is obviously related to the size of the necrotic area. For example, the prognosis is unfavorable when the width of the area of necrosis is greater than 40–50% of the width of the condyle (Fig. 22) or when its area is greater than 5 cm2, while smaller collapses may stabilize spontaneously [16, 26, 30] (Fig. 23). The prognostic value of the dimensions of the lesion is also important for the tibial plateaus [50].
Other causes of bone marrow edema-like signal intensity
Many other conditions can cause a BME-like signal in a knee, for example in reaction to inflammatory disorders (osteitis, arthritis), inflammatory benign tumors (e.g., osteoid osteoma, chondroblastoma, etc.), or malignant tumors, with clinically distinct presentations. Sometimes the cause is obvious, such as post-traumatic bone contusions, which disappear after a few weeks or months [51]. In other cases, the cause is a transient or non-transient reaction to a chronic condition (osteoarthritis for example) or part of a condition of unknown origin referred to as the complex regional pain syndrome type 1.
Complex regional pain syndrome type 1 (CRPS 1)
Formerly called algodystrophy or reflex sympathetic dystrophy, CRPS 1 is a polymorphic disorder, without a specific biological, bacteriological, or anatomical substrate, of which the presumptive diagnosis is based on a combination of clinical and imaging criteria including local or loco-regional pain, cutaneous hyperesthesia, vascular disturbances, local or loco-regional edema, radiological bone rarefaction, and increased or decreased bone activity at bone scan [52].
The condition can be triggered by anything (including trauma, surgery, insect bites…), or it can occur without any identifiable trigger at all [52]. Its etiology remains unknown. It has been suggested that a local ischemic episode may initiate a chain of events resulting in BME, but this hypothesis lacks convincing arguments [53]. The pathogenesis of pain is poorly understood and probably multifactorial: neurovegetative dysregulation, increased intraosseous pressure with irritation of sensory nerves within the bone, and increased bone turnover with or without microfractures [53].
The clinical criteria have poor specificity and there is no “reference standard” to formally establish the diagnosis. Pain is usually out of proportion at physical examination. But pain and edema are not sufficient for the diagnosis, and the presence of other sensory, vasomotor, sudomotor, trophic, and motor criteria is required to improve specificity (“Budapest criteria”) [54]. Ultimately, this remains a diagnosis of exclusion, which is why imaging can be a valuable tool in confirming or ruling out other potential causes [53].
In the radiological literature, this entity is also referred to as “transient osteoporosis,” because osteopenia is usually seen on radiographs, or “migratory osteoporosis” when the condition moves between joints. At MRI, BME-like signal changes are seen, preceding the radiographic changes; therefore, the term “transient bone marrow edema syndrome” has been used [1, 9].
The typical radiographic appearance is increased bone transparency, sometimes heterogeneous (“speckled” or “dappled”), visible from 1 to 3 months after the onset of symptoms and which can, in the knee, persist for months. This increased bone transparency may only affect a portion of the anatomical area, particularly in early lesions (Fig. 24a) [55].
On MRI, the alterations are similar to those seen in most transient epiphyseal lesions: BME-like signal changes which are more or less extensive, predominate near the articular surfaces, and are associated with edema-like signal in the adjacent soft tissues (Fig. 24c-e) [56]. A fine high-intensity line is also frequently present immediately adjacent to the subchondral bone lamina on T2FS images (Fig. 24c) [39].
MRI changes in the bone marrow precede the radiographic bone rarefaction by several weeks and may regress before it. Therefore, in the case of chronic CRPS 1, the MRI may be normal, contrasting with radiological and clinical alterations [53, 57].
In practice, there is no notable difference between the MRI appearance of CRPS 1 and that of other transient epiphyseal lesions, except that in CRPS 1 edema-like alterations in the bone and soft tissues are often more intense and last longer than in SIF. To add to the confusion, subtle deformations of the subchondral surface and thin subchondral fracture lines may also be seen in CRPS 1 (Fig. 25) [58, 59].
The migration of the BME-like pattern from one portion of the epiphysis to another or from one epiphysis to another can be observed at follow-up imaging. This migration of the BME-like pattern is the only definitive characteristic at MRI that distinguishes CRPS 1 from SIF (Fig. 26) [56, 60, 61].
In summary, the MRI appearance of CRPS 1 lesions is almost similar to that of SIF, apart from the usually greater intensity of BME-like signal changes and the frequent migration of lesions at follow-up.
BME-like signal associated with chondral lesions
The so-called BME-like lesions are frequently seen in osteoarthritis and are typically associated with pain [62]. At histology, these lesions correspond to a number of abnormalities, including bone marrow necrosis, bone marrow fibrosis, and necrotic or remodeled trabeculae, but edema is not a major constituent [63]).
BME-like signal changes are generally less intense and less extensive in osteoarthritis than in SIF and their location is more variable [64]. BME-like signal can either be homogeneous (Fig. 27) or heterogeneous, especially in cases of advanced osteoarthritis, due to associated structural bone changes (hyperostosis, necrosis, geodes, etc.) (Fig. 28) [8].
It is therefore possible to confuse BME-like lesions associated with osteoarthritis, with that associated with SIF or SIF-ON, particularly since the latter is also found in the elderly population, who often present with a certain degree of chondrosis. This confusion is evident in some studies on lesions described as SIFs, where knees with complete cartilage destruction and those with intact cartilage are included in the same series [7].
It is important clinically to distinguish BME-signal changes related to osteoarthritis, from those related to SIF, because the latter may be reversible, whereas in progressive osteoarthritis, the prognosis depends on the cartilage disease rather than the BME-like signal intensity (Fig. 29). When facing a BME-like signal, the radiologist should diligently look for cartilage abnormalities. Indeed, the presence of a cartilage lesion may not always be immediately apparent and may require a thorough and detailed examination.
In brief, in the event of a BME-like pattern secondary to a cartilage lesion, the prognosis does not depend on the BME but on the evolution of the cartilage disease itself.
Osteonecrosis of systemic origin
Nosological context
Ischemic or avascular osteonecrosis results from impaired blood supply to the bone, causing irreversible death of bone cells (osteoblasts, osteoclasts, osteocytes) and bone marrow cells (mainly adipocytes in the knee epiphysis) [9].
Apart from traumatic causes, osteonecrosis can occur by systemic mechanisms that are not always well understood, in subjects with various risk factors (including hypercorticism, alcoholism, hyperuricemia, lupus erythematosus, sickle cell disease, and HIV) [3, 47, 65]).
Systemic osteonecrosis occurs in the epiphyses and in the diaphyseal and metaphyseal regions, particularly in or near the hips and knees. Lesions are bilateral in more than 80% of cases (Fig. 30) [2].
Depending on the location, osteonecrosis was previously termed “avascular necrosis,” “aseptic necrosis,” or “ischemic necrosis” (if located in the epiphysis), or “bone infarction” (if located in the metaphysis or diaphysis) [9]. However, the term osteonecrosis is appropriate for all locations of devitalized bone [65].
In the absence of mechanical collapse, these lesions are generally asymptomatic (so-called silent osteonecrosis). It is when a collapse occurs that the lesion becomes symptomatic [2, 25].
Radiographic appearance
Radiography is normal for early lesions. In more advanced stages, osteonecrosis appears as irregular densification with a serpentine sclerotic border, better depicted on CT (Fig. 31).
The collapse of an epiphyseal lesion is associated with deformation or disruption of the subchondral bone plate, sometimes with separation of the subchondral bone plate from the rest of the lesion (i.e., subchondral dissection). Epiphyseal deformity may evolve towards osteoarthritis [65].
MRI appearance
On MRI, osteonecrosis of systemic origin appears as an area of yellow marrow surrounded by a serpentine or curvilinear low signal intensity rim on all sequences [65]. The rim corresponds to the reactive tissue around the area of osteonecrosis. When the necrotic area extends to the bone surface, the edge of the peripheral rim presents a roughly hemispherical or conical appearance occupying part of the epiphysis [65].
In non-collapsed lesions, the content of the necrotic area has a normal fatty appearance, hyperintense on T1-weighted images. It corresponds to “mummified” fatty marrow [59, 66]. In collapsed lesions, areas of modified necrotic marrow show low signal intensity on T2-weighted images, due to progressive physicochemical degradation, or saponification of the medullary fat (Fig. 32) [59]. In the acute phase of collapse, the bone marrow around areas of osteonecrosis may show BME-like signal [8, 67].
The peripheral rim may show a double-line pattern on T2-weighted images. The outer, low signal intensity line is generally considered to correspond to a layer of sclerosis, and the inner, high signal intensity line to a layer of granulation tissue [65, 68]. This sign is considered pathognomonic for osteonecrosis [1, 65, 66]. However, this double line could also correspond to “chemical-shift artifact” [59, 69] (Fig. 33a). With fat suppression, the outer low-intensity line may be completely invisible, as it can be obscured by the surrounding low-intensity fat (Fig. 33b).
Evolution and prognosis
Osteonecrosis located in the diaphyses or metaphyses has a good prognosis, just as epiphyseal lesions that do not contact the articular surface [2].
For the epiphyseal lesions contacting the articular surface, the prognosis is influenced by the dimensions of the articular surfaces concerned, as for SIF-ONs. One method of evaluation consists in measuring the angles covering the necrotic surfaces from the center of the condyles, on frontal and profile radiographs. When the combined necrotic angle is greater than 250°, the prognosis is significantly worse [2].
Conclusions
Spontaneous epiphyseal lesions include simple insufficiency fractures (SIFs) and osteonecrosis complicating insufficiency fractures (SIF-ONs), which constitute a common nosological entity, with different prognoses. Indeed, there are two types of subchondral insufficiency fractures: those that heal (i.e., SIFs) and those that evolve poorly towards osteonecrosis (i.e., SIF-ONs) and collapse. In the early stages, analysis of the subchondral area can help recognize the risk of progression from a SIF to a SIF-ON. A collapsed articular surface evolves towards osteoarthritis, especially when large. When the collapse is very limited, it may remain stable over time.
BME-like signal may also be related to cartilage lesions and be mistaken for a sign of SIF. However, BME-like signal secondary to cartilage lesions should be recognized as such, as their prognosis does not depend on the BME-like changes but on the evolution of the cartilage disease itself.
Osteonecrosis of systemic origin results from ischemia, is delimited by a characteristic serpentine peripheral rim, and is sometimes complicated by epiphyseal collapse.
Finally, while CRPS 1 may share some similarities with SIF, it is generally characterized by a more intense BME-like signal, longer-lasting symptoms, and a tendency to migrate to different locations. Furthermore, in the vast majority of cases, CRPS 1 is still reversible.
Abbreviations
- BME
Bone marrow edema
- CRPS
Complex regional pain syndrome
- MRI
Magnetic resonance imaging
- SIF-ON
Subchondral insufficiency fracture with osteonecrosis
- SIF
Subchondral insufficiency fracture
- SONK
Spontaneous osteonecrosis of the knee
- STIR
Short-tau inversion recovery
- T2FS
Fat-suppressed T2-weighted MR image (and all types of fat-suppressed fluid-sensitive images)
Authors’ contributions
All authors participated in substantially revising the manuscript, approved the submitted version, and agreed both to be personally accountable for the author’s own contributions and to ensure that questions related to the accuracy or integrity of any part of the work, even ones in which the author was not personally involved, are appropriately investigated and resolved and the resolution documented in the literature. JM contributed to the conception and design of the work and drafted the manuscript.
Funding
No funding was received.
Availability of data and materials
Not applicable.
Declarations
Ethics approval and consent to participate
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Consent for publication
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Competing interests
No conflict of interest to declare for any of the authors.
Footnotes
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