Is tomography of intervertebral disc calcification useful in children?

In the past ten years, we have found cervical intervertebral disc calcifications in three children on plain films of the cervical spine made because of cervical pain. In each case, we required further radiological investigations, antero-posterior and lateral linear tomography for two children and an axial computed tomography for one child. In each case, tomography revealed no supplementary useful information. On retrospect, we think that these examinations caused unnecessary irradiation and that they should only be carried out in the rare circumstances when disc calcification is associated with neurological symptoms

Magnetic resonance imaging of nontraumatic shoulder instability in children.

Nontraumatic shoulder instability is infrequent in children. We examined prospectively with high-field magnetic resonance imaging (MRI) 11 patients with this disorder, including 2 with Holt-Oram syndrome and 11 healthy control subjects. The MR findings in the glenohumeral joint in normally growing children are presented. Two patients with shoulder instability were considered as normal, one presented with type 2 (Zlatkin) labral lesions, three, type 3 and one, type 4 lesions. Close attention to the normal imaging patterns of the maturing glenohumeral joint is required to avoid pitfalls in the interpretation of the images

Rôle respectif de la taille, de la localisation et de la composition du calcul en tant que déterminant du succès thérapeutique après lithotritie par ondes de choc extracorporelles dans la lithiase rénale [Respective role of the size, location and composition of the calculus as determinants of therapeutic success after extracorporeal shock wave lithotripsy in renal lithiasis].

We evaluated the respective role of size, location and composition of renal stones as determinants of the outcome of extracorporeal shock wave lithotripsy (ESWL). The analysis of the chemical composition and of the morphology of the fragments eliminated by hundred patients who underwent ESWL has been made by X-rays diffraction. Results showed that the larger the stone, the higher the risk of having to perform an extra intervention (additional sessions of ESWL, percutaneous nephrostolithotomy, nephrolitholapaxy) or of finding residual fragments at the three month check-point. In addition, the location of the stone in a calice, especially a lower calice, strongly predisposes to incomplete elimination of the fragments. Finally, two types of stones appear to lessen the probability of success of ESWL: those of struvite and those of cystine. Indeed, out of eleven ESWL performed on struvite stones (pure or mixed), two had to be completed by percutaneous nephrolitholapaxy and even one by a nephrectomy because of superinfection. Out of the four patients with cystine stones, two had to be treated by additional percutaneous nephrolitholapaxy because of inadequate fragmentation after ESWL. However, for the remaining types of stones (pure or mixed) chemical composition seems to be less important than size or location