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Автор Murtuza Lokhandwalla
Автор Bradford Sturtevant
Дата выпуска 2000-07-01
dc.description Focused shock waves administered during extracorporeal shock-wave lithotripsy (ESWL) cause stone fragmentation. The process of stone fragmentation is described in terms of a dynamic fracture process. As is characteristic of all brittle materials, fragmentation requires nucleation, growth and coalescence of flaws, caused by a tensile or shear stress. The mechanisms, operative in the stone, inducing these stresses have been identified as spall and compression-induced tensile microcracks, nucleating at pre-existing flaws. These mechanisms are driven by the lithotripter-generated shock wave and possibly also by cavitation effects in the surrounding fluid. In this paper, the spall mechanism has been analysed, using a cohesive-zone model for the material. The influence of shock wave parameters, and physical properties of stone, on stone comminution is described. The analysis suggests a potential means to exploit the difference between the stone and tissue physical properties, so as to make stone comminution more effective, without increasing tissue damage.
Формат application.pdf
Издатель Institute of Physics Publishing
Название Fracture mechanics model of stone comminution in ESWL and implications for tissue damage
Тип paper
DOI 10.1088/0031-9155/45/7/316
Electronic ISSN 1361-6560
Print ISSN 0031-9155
Журнал Physics in Medicine and Biology
Том 45
Первая страница 1923
Последняя страница 1940
Аффилиация Murtuza Lokhandwalla; Graduate Aeronautical Laboratories, California Institute of Technology, Pasadena, California, USA
Аффилиация Bradford Sturtevant; Graduate Aeronautical Laboratories, California Institute of Technology, Pasadena, California, USA
Выпуск 7

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