Abstract

Forty radiolucent gallbladder stones from eight patients were fragmented in vitro by extracorporeal shockwave lithotripsy, using the electromagnetic lithotripter Lithostar Plus (Siemens) at five different energy levels. The stones were characterized by size, computed tomography (CT) density, and cholesterol content. The largest residual fragment was measured after every 20 to 100 shock waves. As expected, fewer shock waves were required to achieve fragmentation at higher energy levels. When stones of the same size were compared, there were remarkable differences in the number of shock waves required for fragmentation. These differences must originate in other properties of the stones than size and number. Two different modes of fragmentation were observed: in one group of stones small, flat fragments were chipped off at the beginning of fragmentation ('chipping mode'). These stones initially lost about 25% of their weight as small fragments (< 1 mm) before breaking centrally into some large fragments. In the other group stones initially lost only about 10% of their weight as small fragments (< 1 mm) at the beginning of fragmentation and early broke centrally into some large fragments ('breaking mode'). Stones showing the chipping mode were almost pure cholesterol stones (> 97%) and required significantly less shock waves than stones of the same size showing the breaking mode (cholesterol content, 64-94%). This mode of fragmentation could not be predicted by CT density.

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