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العنوان
Prognostic factors for extracorporeal shock-wave lithotripsy of renal stones /
المؤلف
Seida, Mohamed Attia Atwa.
هيئة الاعداد
باحث / محمد عطيه عطوه سعده
مشرف / محمود ربيع القناوى
مشرف / أحمد ممدوح شومه
مشرف / خالد زكى شعير
مناقش / عبدالرحيم حجازى
الموضوع
Kidneys-- Calculi-- Treatment.
تاريخ النشر
2008.
عدد الصفحات
105 p. :
اللغة
الإنجليزية
الدرجة
الدكتوراه
التخصص
جراحة المسالك البولية
تاريخ الإجازة
1/1/2008
مكان الإجازة
جامعة المنصورة - كلية الطب - المسالك
الفهرس
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Abstract

Between November 2004 and February 2007, 100 patients with single renal stone were ‎treated by ESWL in Urology and Nephrology Centre. Sixty two males and 38 females were included in ‎this study with mean patient age 41.36±11.18 years and mean BMI 28.68±5.27. Those patients have ‎single renal stone. All patients underwent full medical evaluation. Computed tomography was used to ‎evaluate stone volume, volume of the containing stone site, and the ratio between them. Stone density ‎was evaluated by estimation of hounsfield units of the stone. For lower pole stones, lower pole ‎anatomical features of the treated kidney were measured and analyzed. These features were ‎infundibular width, length and surface area, pelvicalyceal height and infundibulopelvic angle. ‎ The stones were located in 47 right and 53 left renal units. Sixty percent of the treated stones ‎were found in renal pelvis while 7%, 8% and 25% of the treated stones were found in the upper calyx, ‎middle calyx and lower calyx respectively. Mean volume of the stone was 1207±884.54mm3 while ‎mean volume of the containing renal site was 3509.28±2400mm3 and the mean ratio in-between was ‎‎0.42±0.25. Mean housenfield unit through bone window was 745.1±208.5 and through tissue window ‎was 660.15±192.89. Anatomical features of the lower pole anatomy showed that mean infundibular ‎length was 19.72±6.44mm, mean infundibular width was 5.19±2.35mm, mean infundibular surface ‎area was 69.54±57.9mm2 and mean infundibulopelvic angle was 51±20.55º.‎ ESWL was performed as an out-patient procedure under sedation using the electromagnetic ‎lithotripter (DoLi S, Dornier med Tech). A total of 3000 shock waves delivered for each session. After ‎the session, patients were evaluated using X-ray and ultrasound to evaluate the results of the treatment ‎and to identify the need for retreatment. The interval between sessions was not less than one week. All ‎patients were followed up 4 weeks after the last session by computed tomography.‎ Success rate of ESWL was 83% while free rate was 72%. Univariate analysis of the results ‎showed that none of the studied factors showed significant impact on the results of ESWL. However, ‎success rate was higher with some numerical factors like: smaller body mass index, smaller stone ‎volume, shorter infundibular length, wider infundibular width, larger infundibular surface area and ‎wider infundibulopelvic angle. Univariate analysis of categorical factors showed that none of these ‎factors has a significant effect on the results of ESWL. In spite of this result, success rate and free rate ‎were affected more with some factors. Success rate for renal pelvic stones was 86.7% while it was ‎‎85.7%, 62.5% and 80% for stone in upper calyx, middle calyx and lower calyx respectively. Radio ‎opaque stone has success rate 84.3% while faint or radiolucent stone has success rate 72.7%. Normal ‎morphological kidney showed success rate 83.9% while it was 71.4% for hydronephrotic kidneys. ‎ We concluded that ESWL is one of the successful methods of treatment of renal stones. ‎There were no identifiable factors which affect results of ESWL significantly, but we identified some ‎numerical and categorical factors which give better success and free rates with ESWL. To evaluate ‎which of these factors has more significance, a new study was required with larger number of patients. ‎