The Journal of Kansai Medical University
Online ISSN : 2185-3851
Print ISSN : 0022-8400
ISSN-L : 0022-8400
A Case of Spontaneous Peripelvic Extravasation Associated with Ureteral Calculus
Takaya TanakaFumihiro NozuNobuaki MatsuoKenichi KatoYoshiyuki ItohNaoshi Takeyama
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JOURNAL FREE ACCESS

1988 Volume 40 Issue Supplement Pages S1-S5

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Abstract

A patient with renal extravasation due to u reteral calculus is described. A 58-year-old male visited our hospital with pain in the right lower abdomen, and showed peripelvic extravasation of the contrast medium by DIP aod CT. Extravasation was absent in DIP and the symptoms were alleviated 2 days after admission. The patient was discharged after 5days.
Peripelvic extravasation must be clearly differentiated from spontaneous rupture of the kidney. Peripelvic extravasation is a relatively uncommon condition, which is considered to be caused by renopelvic reflux due to obstruction of the urinary tract or compression of the ureter. This report describcs a patient with peripelvic urinary extravasation due to ureteral calculus.
Around noon on August 26,1987, a 58-year-old male noted pain of the right lower abdomen and right back, which disappeared spontaneously after about 2 hours. The patient presented with pollakiuria the next morning, and later developed oliguria while occasionally showing hematuria. As pain occurred at the same sites about 9 p. m. the same day and deteriorated, the patient visited our hospital.
There was no relevant clinical history. On admission, the patient had a medium body build and showed a good nutritional condition, body temperature of 36.5°C, blood pressure of 130/70 mmHg, and regular heart rate of 65/min. Slight tenderness was noted in the right lower abdomen and right back, but no external trauma was observed.
The laboratory data on admission included: RBC 489×104, WBC 9,200, Hb 14.9 g/dl, GOT 28 IU/l, GPT 16 IU/l, LDH 475 IU/l, Na 133 mEq/l, K 3.6 mEq/l, Cl 101 mEq/l, BUN 12 mg/dl, Cr 1.4 mg/dl, and blood glucose 160 mg/dl. The results of urinalysis were: protein (-), glucose (+), urobilinogen (-), and occult blood (+).
DIP was performed, suspecting ureteral calculus, and the contr a st medium was found to leak from the renal pelvis (Fig.1). Abdominal CT further suggested escape of the contrast medium into the peripelvic region (Fig.2,3). Considering the general condition and the clinical symptoms, the patient was fasted and kept at rest after securing the vein. The pain was nearly relieved and no extrarenal efflux of the contrast medium was observed by DIP after 2 days (Fig.4). The patient was discharged 5 days after the admission. Ureteral calculus was noted by DIP performed after 2 days.

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