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45. Sampaio, F. J. and Aragao, A. H. M.: Limitations of extracorpo- real shock wave lithotripsy for lower calyceal stones: anatomic insight. J Endourol, 8: 241, 1994 46. Sampaio, F. J., D’Anunciacao, A. L. and Silva, E. C.: Compara- tive follow-up of patients with acute and obtuse infundibulum- pelvic angle submitted to extracorporeal shock wave litho- tripsy for lower calyceal stones: preliminary report and proposed study design. J Endourol, 11: 157, 1997 47. Elbahnasy, A. M., Clayman, R. V., Shalhav, A. L. et al: Lower pole calyceal stone clearance after shock wave lithotripsy, percutaneous nephrolithotomy, and flexible ureteroscopy: im- pact of radiographic spatial anatomy. J Endourol, 12: 113, 1998 48. Gupta, N. P., Singh, D. V., Hemal, A. K. et al: Infundibulopelvic anatomy and clearance of inferior caliceal calculi with shock wave lithotripsy. J Urol, 163: 24, 2000 49. Pace, K. T., Weir, M. J., Tariq, N. et al: Individual patient variation and inter-rater reliability of lower calyceal infundib- ular width on routine intravenous pyelography. J Urol, suppl., 163: 341, abstract 1511, 2000 50. Madbouly, K., Sheir, K. Z. and Elsobky, E.: Impact of lower pole renal anatomy on stone clearance after shock wave lithotripsy: fact or fiction? J Urol, 165: 1415, 2001 51. Streem, S. B., Yost, A. and Mascha, E.: Clinical implications of clinically insignificant stone fragments after extracorporeal shock wave lithotripsy. J Urol, 155: 1186, 1996 52. Grasso, M., Loisides, P., Beaghler, M. et al: The case for primary endoscopic management of upper urinary tract calculi: a crit- ical review of 121 extracorporeal shock wave lithotripsy fail- ures. Urology, 45: 363, 1995 53. Fabrizio, M. D., Behari, A. and Bagley, D. H.: Ureteroscopic management of intrarenal calculi. J Urol, 159: 1139, 1998 54. Yowell, C. W., Delvechio, F. C., Preminger, G. M. et al: Ureteroscopic management of lower pole renal calculi. J Urol, 161: 370, 1999 55. Grasso, M., Conlin, M. and Bagley, D.: Retrograde ureteropyelo- scopic treatment of 2 cm. or greater upper urinary tract and minor Staghorn calculi. J Urol, 160: 346, 1998 56. Grasso, M. and Ficazzola, M.: Retrograde ureteropyeloscopy for lower pole caliceal calculi. J Urol, 162: 1904, 1999 57. Kumar, P. V. S., Joshi, H. B., Keeley, F. X. et al: An acute infundibulopelvic angle predicts failure of flexible uretero- renoscopy for lower calyceal stones. J Urol, suppl., 163: 339, abstract 1505, 2000 58. Mobley, T. B., Myers, D. A., Grine, W. B. et al: Low energy lithotripsy with the Lithostar: treatment results with 19,962 renal and ureteral calculi. J Urol, 147: 1419, 1992 59. El-Damanhourry, Y., Scarfe, T., Rith, I. et al: Extracorporeal shock wave lithotripsy of urinary calculi: experience in treatment of 3,278 patients using the Siemens Lithostar. J Urol, 149: 1419, 1993 60. Netto, N. R., Jr., Claro, J. F., Lemos, G. C. et al: Renal calculi in lower pole calices: what is the best method of treatment? J Urol, 146: 721, 1991 61. Elashry, O. M., DiMeglio, R. B., Nakada, S. Y. et al: Intracorpo- real electrohydraulic lithotripsy of ureteral and renal calculi using small caliber (1.9Fr) electrohydraulic lithotripsy probes. J Urol, 156: 1581, 1996 62. Gould, D. L.: Holmium:YAG laser and its use in the treatment of urolithiasis: our first 160 cases. J Endourol, 12: 23, 1998 63. Grasso, M. and Chalik, Y.: Principles and applications of laser lithotripsy: experience with the holmium laser lithotrite. J Clin Laser Med Surg, 16: 3, 1998 64. Menezes, P., Dickinson, A. and Timoney, A. G.: Flexible uretero- renoscopy for the treatment of refractory upper urinary tract stones. BJU Int, 84: 257, 1999 65. Tawfiek, E. R. and Bagley, D. H.: Management of upper urinary tract calculi with ureteroscopic techniques. Urology, 53: 25, 1999 66. Sofer, M., Wollin, T. A., Nott, L. et al: Endoscopic holmium laser lithotripsy for upper urinary tract calculi. J Urol, submitted for publication EDITORIAL COMMENT Albala et al present a prospective randomized multicenter trial com- paring shock wave lithotripsy to percutaneous nephrolithotomy for management of stones up to 3 cm. in length isolated to the lower pole collecting system. The authors conclude that shock wave lithotripsy is a reasonable first line therapy only for stones less than 1 cm. in length but for those larger than that percutaneous nephrolithotomy is preferable due to the “high degree of efficacy and acceptably low morbidity.” As this study is prospective and randomized, the objective results can be accepted as presented. However, the Conclusions and recommendations can and should be open to one’s own interpretation. It is surprising that these authors would use only a single dimension to measure and categorize stone size, especially as the corresponding author was among the first investigators to suggest and support the use of stone surface area for all such research, presentations and publica- tions (J Urol, 148: 1026, 1992; J Urol, 147: 1219, 1992). As a result, from this study the authors would recommend treatment of a 0.9 0.9 cm. (0.81 cm. 2 ) calculus with shock wave lithotripsy but in contrast, recom- mend that a 1.2 0.5 cm. (0.6 cm. 2 ) calculus be treated primarily with percutaneous nephrolithotomy. The reader may have difficulty recon- ciling this recommendation. The definition of “success” of treatment in this study is still unclear. Obviously, if only stone-free rates are used, percutaneous nephrolitho- tomy will ultimately prove superior. However, there are many patients with symptomatic calculi at the outset who become asymptomatic after shock wave lithotripsy and in fact have minimal residual “dust” that may be seen on nephrotomography. Surely, most such patients as well as the treating urologists consider the treatment successful and in fact, the quality of life data reported here clearly confirm that. Moreover, it would be interesting to see the quality of life data stratified by stone size, especially for the controversial 1 to 2 cm. group. The reader may also harbor concern regarding the frequency and severity of complications in those patients treated with shock wave lithotripsy versus percutaneous nephrolithotomy. Although the au- thors found no statistically significant difference in the frequency of complications, which in fact occurred twice as often in the percuta- neous nephrolithotomy group, the lists hardly appear comparable. I suspect most urologists would opt for the shock wave lithotripsy group, from which one may fail to discern a single significant com- plication compared to the percutaneous nephrolithotomy group with the sepsis, perforations, transfusions and anteriovenous fistulas. We are grateful to have this published data from a prospective randomized trial performed by highly regarded investigators and clinicians. However, we should all retain the right to interpret the data ourselves and form our own conclusions. Personally, I agree that with few exceptions, stones in the lower pole or anywhere else in the pyelocaliceal system less than 1 cm. can and should be treated primarily with shock wave lithotripsy, while those greater than 2 cm. should generally be treated with percutaneous nephrolithotomy. However, it has been our practice that for patients with stones between those parameters shock wave lithotripsy can generally be performed successfully, although many factors must be considered to recommend the most appropriate management. These factors in- clude but are not limited to presumed stone composition and fragil- ity, concomitant medical problems, body habitus, pyelocaliceal anat- omy, and overall and ipsilateral renal function. Our interpretation of the data presented here has served only to reinforce that protocol. Stevan B. Streem Department of Urology Cleveland Clinic Cleveland, Ohio REPLY BY AUTHORS The Lower Pole Study Group chose to focus on maximal stone diameter as this is the standard that has been used worldwide for classifying nonstaghorn stones. The references cited by Streem re- garding the use of stone surface area refer to staghorn calculi and were never intended nor suggested to be used for “all research, presentations and publications.” The Lower Pole Study Group used the same criterion in categorizing stones, namely that of maximal stone diameter, as this is the standard universally used by urologists and is pervasive in the literature relating to outcomes for nonstag- horn stone disease (JAMA, 260: 978, 1988; J Urol, 158: 1915, 1997). Moreover, few (if any) urologists currently use or have access to stone surface area methodology. The only universally agreed upon definition of successful stone treatment is stone-free. Much has been written over the years re- garding residual stone fragments or “dust” and their significance. Streem has condemned use of the term “clinically insignificant re- sidual fragments” in a recent article (J Urol, 155: 1186, 1996). Ultimately, clinical decision making is no better than the informa- tion used in the decision making process. This study provides the most objective data to date for urologists to use in counseling pa- tients regarding the outcomes of various treatment choices for the treatment of lower pole calculi. LOWER POLE NEPHROLITHIASIS 2080

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45. Sampaio, F. J. and Aragao, A. H. M.: Limitations of extracorpo-real shock wave lithotripsy for lower calyceal stones: anatomicinsight. J Endourol, 8: 241, 1994

46. Sampaio, F. J., D’Anunciacao, A. L. and Silva, E. C.: Compara-tive follow-up of patients with acute and obtuse infundibulum-pelvic angle submitted to extracorporeal shock wave litho-tripsy for lower calyceal stones: preliminary report andproposed study design. J Endourol, 11: 157, 1997

47. Elbahnasy, A. M., Clayman, R. V., Shalhav, A. L. et al: Lowerpole calyceal stone clearance after shock wave lithotripsy,percutaneous nephrolithotomy, and flexible ureteroscopy: im-pact of radiographic spatial anatomy. J Endourol, 12: 113, 1998

48. Gupta, N. P., Singh, D. V., Hemal, A. K. et al: Infundibulopelvicanatomy and clearance of inferior caliceal calculi with shockwave lithotripsy. J Urol, 163: 24, 2000

49. Pace, K. T., Weir, M. J., Tariq, N. et al: Individual patientvariation and inter-rater reliability of lower calyceal infundib-ular width on routine intravenous pyelography. J Urol, suppl.,163: 341, abstract 1511, 2000

50. Madbouly, K., Sheir, K. Z. and Elsobky, E.: Impact of lower polerenal anatomy on stone clearance after shock wave lithotripsy:fact or fiction? J Urol, 165: 1415, 2001

51. Streem, S. B., Yost, A. and Mascha, E.: Clinical implications ofclinically insignificant stone fragments after extracorporealshock wave lithotripsy. J Urol, 155: 1186, 1996

52. Grasso, M., Loisides, P., Beaghler, M. et al: The case for primaryendoscopic management of upper urinary tract calculi: a crit-ical review of 121 extracorporeal shock wave lithotripsy fail-ures. Urology, 45: 363, 1995

53. Fabrizio, M. D., Behari, A. and Bagley, D. H.: Ureteroscopicmanagement of intrarenal calculi. J Urol, 159: 1139, 1998

54. Yowell, C. W., Delvechio, F. C., Preminger, G. M. et al: Ureteroscopicmanagement of lower pole renal calculi. J Urol, 161: 370, 1999

55. Grasso, M., Conlin, M. and Bagley, D.: Retrograde ureteropyelo-scopic treatment of 2 cm. or greater upper urinary tract andminor Staghorn calculi. J Urol, 160: 346, 1998

56. Grasso, M. and Ficazzola, M.: Retrograde ureteropyeloscopy forlower pole caliceal calculi. J Urol, 162: 1904, 1999

57. Kumar, P. V. S., Joshi, H. B., Keeley, F. X. et al: An acuteinfundibulopelvic angle predicts failure of flexible uretero-renoscopy for lower calyceal stones. J Urol, suppl., 163: 339,abstract 1505, 2000

58. Mobley, T. B., Myers, D. A., Grine, W. B. et al: Low energylithotripsy with the Lithostar: treatment results with 19,962renal and ureteral calculi. J Urol, 147: 1419, 1992

59. El-Damanhourry, Y., Scarfe, T., Rith, I. et al: Extracorporeal shockwave lithotripsy of urinary calculi: experience in treatment of 3,278patients using the Siemens Lithostar. J Urol, 149: 1419, 1993

60. Netto, N. R., Jr., Claro, J. F., Lemos, G. C. et al: Renal calculi inlower pole calices: what is the best method of treatment?J Urol, 146: 721, 1991

61. Elashry, O. M., DiMeglio, R. B., Nakada, S. Y. et al: Intracorpo-real electrohydraulic lithotripsy of ureteral and renal calculiusing small caliber (1.9Fr) electrohydraulic lithotripsy probes.J Urol, 156: 1581, 1996

62. Gould, D. L.: Holmium:YAG laser and its use in the treatment ofurolithiasis: our first 160 cases. J Endourol, 12: 23, 1998

63. Grasso, M. and Chalik, Y.: Principles and applications of laserlithotripsy: experience with the holmium laser lithotrite.J Clin Laser Med Surg, 16: 3, 1998

64. Menezes, P., Dickinson, A. and Timoney, A. G.: Flexible uretero-renoscopy for the treatment of refractory upper urinary tractstones. BJU Int, 84: 257, 1999

65. Tawfiek, E. R. and Bagley, D. H.: Management of upper urinarytract calculi with ureteroscopic techniques. Urology, 53: 25, 1999

66. Sofer, M., Wollin, T. A., Nott, L. et al: Endoscopic holmium laserlithotripsy for upper urinary tract calculi. J Urol, submittedfor publication

EDITORIAL COMMENT

Albala et al present a prospective randomized multicenter trial com-paring shock wave lithotripsy to percutaneous nephrolithotomy formanagement of stones up to 3 cm. in length isolated to the lower polecollecting system. The authors conclude that shock wave lithotripsy is areasonable first line therapy only for stones less than 1 cm. in length butfor those larger than that percutaneous nephrolithotomy is preferabledue to the “high degree of efficacy and acceptably low morbidity.” As

this study is prospective and randomized, the objective results can beaccepted as presented. However, the Conclusions and recommendationscan and should be open to one’s own interpretation.

It is surprising that these authors would use only a single dimensionto measure and categorize stone size, especially as the correspondingauthor was among the first investigators to suggest and support the useof stone surface area for all such research, presentations and publica-tions (J Urol, 148: 1026, 1992; J Urol, 147: 1219, 1992). As a result, fromthis study the authors would recommend treatment of a 0.9 � 0.9 cm.(0.81 cm.2) calculus with shock wave lithotripsy but in contrast, recom-mend that a 1.2 � 0.5 cm. (0.6 cm.2) calculus be treated primarily withpercutaneous nephrolithotomy. The reader may have difficulty recon-ciling this recommendation.

The definition of “success” of treatment in this study is still unclear.Obviously, if only stone-free rates are used, percutaneous nephrolitho-tomy will ultimately prove superior. However, there are many patientswith symptomatic calculi at the outset who become asymptomatic aftershock wave lithotripsy and in fact have minimal residual “dust” thatmay be seen on nephrotomography. Surely, most such patients as wellas the treating urologists consider the treatment successful and in fact,the quality of life data reported here clearly confirm that. Moreover, itwould be interesting to see the quality of life data stratified by stonesize, especially for the controversial 1 to 2 cm. group.

The reader may also harbor concern regarding the frequency andseverity of complications in those patients treated with shock wavelithotripsy versus percutaneous nephrolithotomy. Although the au-thors found no statistically significant difference in the frequency ofcomplications, which in fact occurred twice as often in the percuta-neous nephrolithotomy group, the lists hardly appear comparable. Isuspect most urologists would opt for the shock wave lithotripsygroup, from which one may fail to discern a single significant com-plication compared to the percutaneous nephrolithotomy group withthe sepsis, perforations, transfusions and anteriovenous fistulas.

We are grateful to have this published data from a prospectiverandomized trial performed by highly regarded investigators andclinicians. However, we should all retain the right to interpret thedata ourselves and form our own conclusions. Personally, I agreethat with few exceptions, stones in the lower pole or anywhere else inthe pyelocaliceal system less than 1 cm. can and should be treatedprimarily with shock wave lithotripsy, while those greater than 2 cm.should generally be treated with percutaneous nephrolithotomy.However, it has been our practice that for patients with stonesbetween those parameters shock wave lithotripsy can generally beperformed successfully, although many factors must be considered torecommend the most appropriate management. These factors in-clude but are not limited to presumed stone composition and fragil-ity, concomitant medical problems, body habitus, pyelocaliceal anat-omy, and overall and ipsilateral renal function. Our interpretation ofthe data presented here has served only to reinforce that protocol.

Stevan B. StreemDepartment of UrologyCleveland ClinicCleveland, Ohio

REPLY BY AUTHORS

The Lower Pole Study Group chose to focus on maximal stonediameter as this is the standard that has been used worldwide forclassifying nonstaghorn stones. The references cited by Streem re-garding the use of stone surface area refer to staghorn calculi andwere never intended nor suggested to be used for “all research,presentations and publications.” The Lower Pole Study Group usedthe same criterion in categorizing stones, namely that of maximalstone diameter, as this is the standard universally used by urologistsand is pervasive in the literature relating to outcomes for nonstag-horn stone disease (JAMA, 260: 978, 1988; J Urol, 158: 1915, 1997).Moreover, few (if any) urologists currently use or have access to stonesurface area methodology.

The only universally agreed upon definition of successful stonetreatment is stone-free. Much has been written over the years re-garding residual stone fragments or “dust” and their significance.Streem has condemned use of the term “clinically insignificant re-sidual fragments” in a recent article (J Urol, 155: 1186, 1996).

Ultimately, clinical decision making is no better than the informa-tion used in the decision making process. This study provides themost objective data to date for urologists to use in counseling pa-tients regarding the outcomes of various treatment choices for thetreatment of lower pole calculi.

LOWER POLE NEPHROLITHIASIS2080