We compared different methods of bone densitometry in women with spinal osteoporosis and normal subjects to assess their discriminatory capability. The methods used included: quantitative computed tomography of the spine (QCT) specified as to trabecular (QCTtrab) and cortical bone (QCTcort), dual-photon absorptiometry of the spine (DPAspine), single-photon absorptiometry of the distal and proximal forearm (SPAdist and SPAprox), and quantitative roentgen microdensitometry of the phalanx (QMD). A total of 25 postmenopausal osteoporotic women and 24 healthy comparison subjects matched for age and years since menopause were studied. In the osteoporotic group an average decrement of the axial bone mineral density of -50% (p less than 0.001) and -20% (p less than 0.001) were observed for QCTtrab and QCTcort, respectively. For DPAspine, SPAdist, SPAprox, and QMD the difference between normal and osteoporotic subjects was -20% (p less than 0.001), -12% (p less than 0.05), -7% (NS), and -6% (NS), respectively. With the peripheral measurements (SPA and QMD), alone or in combination, no adequate discrimination between women with or without vertebral compression fractures could be obtained. Although QCTtrab showed the highest diagnostic sensitivity (81%), it appears not to be superior to DPAspine. Combinations of the various axial and peripheral measurements did not result in an essentially better sensitivity. In normal women as well as in osteoporotic individuals the trabecular and cortical QCT measurements showed two opposite trends, suggesting an increase in cortical and a decrease in trabecular density from L1 to L3.
Thin‐slice contiguous computed tomographic scanning was performed in four postmortem hearts with calcific aortic valve stenosis (mean weight: 583 ± 78 g; mean age: 65 ± 10 years) before, during, and after balloon valvuloplasty. Balloons of increasing diameter (15–19 mm single balloons, and 3 × 12‐mm trefoil‐shaped balloon) were positioned across the aortic valve and manually inflated to pressures of 3 to 4 atmospheres. During inflation of the 3 × 12‐mm balloon a larger residual orifice, potentially free for blood passage, was observed in the two cases with bicuspid valves and in one case with a fused tricuspid valve, while the reverse was noted in one case with a tricuspid valve without fusion. In most cases valvular orifice enlargement only occurred with larger diameter balloons. After valvuloplasty aortic valve area increased from 0.72 (range 0.20–0.95) cm2 to 2.36 (range 0.95–3.14) cm2. The smallest orifice enlargement after dilatation occurred in case 1, where valvular calcified deposits had the largest volume and the highest computed tomographic attenuation value. In each patient macroscopic changes (fracture of nodular calcifications, commissural splitting, tearing of the central raphe) were noted. No calcium dislodgement or aortic ring damage was observed. In autopsy specimens computed tomography provided accurate evaluation of aortic valve morphology, extent of valve calcification, balloon‐leaflet relationship during inflation, and effects of the dilatation on valve leaflets and commissures. Advances in computed tomographic cardiovascular imaging may achieve similar results in the clinical setting, and allow a more rational, individualized approach to the valvuloplasty procedure. (J Interven Cardiol 1988:1:2)
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