Predicting Factors for Spontaneous Passage of Ureteral Calculi Based on Unenhanced Helical CT Findings.
10.4111/kju.2008.49.12.1094
- Author:
Dong Woo SONG
1
;
Tae Yung JEONG
;
Sang Ik LEE
;
Dong Jun KIM
Author Information
1. Department of Urology, Myongji Hospital, College of Medicine, Kwandong University, Goyang, Korea. urokdj@hotmail.com
- Publication Type:Original Article
- Keywords:
Ureteral calculi;
Helical computed tomography
- MeSH:
Edema;
Humans;
Hydronephrosis;
Incidence;
Prospective Studies;
Shock;
Tomography, Spiral Computed;
Ureter;
Ureteral Calculi;
Ureteroscopy
- From:Korean Journal of Urology
2008;49(12):1094-1099
- CountryRepublic of Korea
- Language:Korean
-
Abstract:
PURPOSE: We performed a prospective study to determine whether unenhanced helical computed tomography(UHCT) findings predict the spontaneous passage of ureteral calculi. MATERIALS AND METHODS: Between April 2006 and June 2007, 175 patients with a single ureteral calculus <1cm in diameter were enrolled in this study, and a UHCT was performed. All of the patients were managed conservatively for 2 weeks. Patients without spontaneous passage of ureteral calculi within 2 weeks were treated by ureteroscopy or extracorporeal shock wave lithotripsy(ESWL). The secondary signs (hydronephrosis, perinephric edema, and the tissue rim sign) were graded on a scale of 0-3. We evaluated whether spontaneous passage of ureteral calculi was associated with stone diameter, location, Hounsfield units(HU), and the degree of secondary signs. RESULTS: Ninety-two patients(52.6%) had spontaneous passage of ureteral calculi. The mean stone diameter was significantly smaller in the passage group than the non-passage group(4.28mm vs. 6.73mm, p=0.002). The rate of spontaneous passage was significantly higher involving distal ureteral calculi(66.1%) than proximal ureteral calculi(30.3%, p<0.001). The incidences of hydronephrosis and perinephric edema were significantly lower in the spontaneous passage group than the non-passage group(8.7% vs. 73.5% and 5.4% vs. 69.9%, respectively). The grades of hydronephrosis and perinephric edema were significantly lower in the spontaneous passage group than the non-passage group(p=0.001). Although there was a tendency toward increasing grades of hydronephrosis and perinephric edema with increasing stone size, the grades were more frequent and severe in the non-passage group in patients with similarly sized stones. CONCLUSIONS: The degree of hydronephrosis and perinephric edema are useful ancillary signs in predicting the likelihood of spontaneous passage of ureteral calculi.
