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 |