The role of stress waves and cavitation in stone comminution in shock wave lithotripsy.

Using an experimental system that mimics stone fragmentation in the renal pelvis, we have investigated the role of stress waves and cavitation in stone comminution in shock-wave lithotripsy (SWL). Spherical plaster-of-Paris stone phantoms (D = 10 mm) were exposed to 25, 50, 100, 200, 300 and 500 shocks at the beam focus of a Dornier HM-3 lithotripter operated at 20 kV and a pulse repetition rate of 1 Hz. The stone phantoms were immersed either in degassed water or in castor oil to delineate the contribution of stress waves and cavitation to stone comminution. It was found that, while in degassed water there is a progressive disintegration of the stone phantoms into small pieces, the fragments produced in castor oil are fairly sizable. From 25 to 500 shocks, clinically passable fragments (< 2 mm) produced in degassed water increases from 3% to 66%, whereas, in castor oil, the corresponding values are from 2% to 11%. Similar observations were confirmed using kidney stones with a primary composition of calcium oxalate monohydrate. After 200 shocks, 89% of the fragments of the kidney stones treated in degassed water became passable, but only 22% of the fragments of the kidney stones treated in castor oil were less than 2 mm in size. This apparent size limitation of the stone fragments produced primarily by stress waves (in castor oil) is likely caused by the destructive superposition of the stress waves reverberating inside the fragments, when their sizes are less than half of the compressive wavelength in the stone material. On the other hand, if a stone is only exposed to cavitation bubbles induced in SWL, the resultant fragmentation is much less effective than that produced by the combination of stress waves and cavitation. It is concluded that, although stress wave-induced fracture is important for the initial disintegration of kidney stones, cavitation is necessary to produce fine passable fragments, which are most critical for the success of clinical SWL. Stress waves and cavitation work synergistically, rather than independently, to produce effective and successful disintegration of renal calculi in SWL

[1]  G. Preminger,et al.  A comparison of stone damage caused by different modes of shock wave generation. , 1992, The Journal of urology.

[2]  P. Zhong,et al.  Dynamic photoelastic study of the transient stress field in solids during shock wave lithotripsy. , 2000, The Journal of the Acoustical Society of America.

[3]  F. Cocks,et al.  Extracorporeal shock wave lithotripsy: the use of chemical treatments for improved stone comminution. , 1987, The Journal of urology.

[4]  P. Zhong,et al.  Improvement of stone fragmentation during shock-wave lithotripsy using a combined EH/PEAA shock-wave generator-in vitro experiments. , 2000, Ultrasound in medicine & biology.

[5]  F. Hauser,et al.  Deformation and Fracture Mechanics of Engineering Materials , 1976 .

[6]  C J Chuong,et al.  Propagation of shock waves in elastic solids caused by cavitation microjet impact. I: Theoretical formulation. , 1993, The Journal of the Acoustical Society of America.

[7]  G. Preminger,et al.  Characterization of fracture toughness of renal calculi using a microindentation technique , 1993 .

[8]  B. Sturtevant,et al.  Fracture mechanics model of stone comminution in ESWL and implications for tissue damage. , 2000, Physics in medicine and biology.

[9]  R. Boving,et al.  Incidence of cavitation in the fragmentation process of extracorporeal shock wave lithotriptors , 1994 .

[10]  J. Seifert,et al.  The mechanisms of stone disintegration by shock waves. , 1991, Ultrasound in medicine & biology.

[11]  G M Preminger,et al.  Propagation of shock waves in elastic solids caused by cavitation microjet impact. II: Application in extracorporeal shock wave lithotripsy. , 1993, The Journal of the Acoustical Society of America.

[12]  L A Crum,et al.  Cavitation microjets as a contributory mechanism for renal calculi disintegration in ESWL. , 1988, The Journal of urology.

[13]  B. Sturtevant,et al.  In vitro study of the mechanical effects of shock-wave lithotripsy. , 1997, Ultrasound in medicine & biology.

[14]  D Jocham,et al.  Extracorporeal shock wave lithotripsy. , 1986, Urologia internationalis.

[15]  W. Brendel,et al.  A mechanism of gallstone destruction by extracorporeal shock waves , 1988, Naturwissenschaften.

[16]  G. Preminger,et al.  Quantification of the tip movement of lithotripsy flexible pneumatic probes. , 2000, The Journal of urology.

[17]  A. Hendrikx,et al.  Efficacy of second generation lithotriptors: a multicenter comparative study of 2,206 extracorporeal shock wave lithotripsy treatments with the Siemens Lithostar, Dornier HM4, Wolf Piezolith 2300, Direx Tripter X-1 and Breakstone lithotriptors. , 1992, The Journal of urology.

[18]  P. Zhong,et al.  Suppression of large intraluminal bubble expansion in shock wave lithotripsy without compromising stone comminution: methodology and in vitro experiments. , 2001, The Journal of the Acoustical Society of America.

[19]  C. Church,et al.  A theoretical study of cavitation generated by an extracorporeal shock wave lithotripter. , 1988, The Journal of the Acoustical Society of America.

[20]  P. Alken,et al.  Extracorporeal shock wave lithotripsy of ureteral stones: clinical experience and experimental findings. , 1986, The Journal of urology.

[21]  S. Gracewski,et al.  Internal stress wave measurements in solids subjected to lithotripter pulses. , 1993, The Journal of the Acoustical Society of America.

[22]  B. Finlayson,et al.  Morphology of urinary stone particles resulting from ESWL treatment. , 1986, The Journal of urology.

[23]  W. F. Brace,et al.  A note on brittle crack growth in compression , 1963 .

[24]  E. G. Bombolakis Photoelastic study of initial stages of brittle fracture in compression , 1968 .

[25]  W Eisenmenger,et al.  The mechanisms of stone fragmentation in ESWL. , 2001, Ultrasound in medicine & biology.

[26]  B. Finlayson,et al.  An experimental model for the systematic investigation of stone fracture by extracorporeal shock wave lithotripsy. , 1988, The Journal of urology.

[27]  F. Cocks,et al.  Fracture strength studies of renal calculi , 1985 .

[28]  P. Zhong,et al.  Dynamics of bubble oscillation in constrained media and mechanisms of vessel rupture in SWL. , 2001, Ultrasound in medicine & biology.

[29]  Michael Ortiz,et al.  Microcrack coalescence and macroscopic crack growth initiation in brittle solids , 1988 .

[30]  J. Field,et al.  The physics of liquid impact, shock wave interactions with cavities, and the implications to shock wave lithotripsy. , 1991, Physics in medicine and biology.

[31]  W. Lauterborn,et al.  Cavitation erosion by single laser-produced bubbles , 1998, Journal of Fluid Mechanics.

[32]  C. Chaussy Extracorporeal Shock Wave Lithotripsy: New Aspects in the Treatment of Kidney Stone Disease , 1982 .

[33]  S. Gracewski,et al.  Finite difference predictions of P-SV wave propagation inside submerged solids. II. Effect of geometry. , 1997, The Journal of the Acoustical Society of America.

[34]  M. Delius Minimal static excess pressure minimises the effect of extracorporeal shock waves on cells and reduces it on gallstones. , 1997, Ultrasound in medicine & biology.

[35]  L A Crum,et al.  Acoustic cavitation generated by an extracorporeal shockwave lithotripter. , 1987, Ultrasound in medicine & biology.