Fj. Vanhellemondt et al., STRESS RADIOGRAPHY AND STRESS EXAMINATION OF THE TALOCRURAL AND SUBTALAR JOINT ON HELICAL COMPUTED-TOMOGRAPHY, Foot & ankle international, 18(8), 1997, pp. 482-488
The main objective of this study was to compare subtalar inversion str
ess views using the Broden view with inversion stress views on helical
computed tomography (CT). One of the drawbacks of routine radiography
is the imaging of three-dimensional structures In a two-dimensional p
lane. We investigated whether the use of helical CT would lead to a mo
re objective and clearer measurable method to determine the amount of
tilt in the subtalar joint. A group of 15 patients with unilateral chr
onic instability complaints and clinically suspected subtalar instabil
ity was examined. The contralateral asymptomatic foot was used as cont
rol. A variable amount of subtalar tilt (range, 4 degrees to 18 degree
s) was demonstrated in all cases on stress radiographs, without findin
g significant difference between the symptomatic and asymptomatic feet
, However, contrary to the findings at the talocrural level, subtalar
tilt was found in none of the patients using helical CT. Thus, we now
doubt that the tilt seen during stress examination using the Broden vi
ew is the true amount of tilt, It may be that the lateral opening, see
n on these radiographs, largely results from imaging two planes that h
ave made a translatory and rotatory movement relative to each other in
an oblique direction. It is concluded that the Broden stress examinat
ion might not be useful for screening patients with subtalar instabili
ty. Associated anomalies not visible on the radiographs were detected
by helical CT. In four cases, narrowing of the articular cartilage and
irregular and hypertrophic bone formation at the middle facet joint o
f the subtalar joints were found. It. is likely that these changes cau
se disturbance of function of this joint and it is suggested that the
subjective complaint of instability with ''giving way'' is not only ca
used by hypermobility, but can be caused by other disturbances of norm
al motion.