Back-leak of pelvic urine to the bloodstream.

The aim of the present investigation was to measure the back-leak of pelvic urine to the blood circulation. In normopenic hydronephrotic, dehydrated hydronephrotic and dehydrated control kidneys the back-leak was estimated from a servocontrolled machine which regulated infused saline to keep a present pelvic pressure constant. The disappearance of fluid from the renal pelvis could be measured at different pressure levels, and a pressure-dependent outflow of fluid was found. From these measurements a back-leak conductance could be calculated which proved to be independent of pressure. In the lower pressure range (15-20 mmHg) there was a significantly lower conductance in the dehydrated controls compared with the dyhydrated hydronephrotic kidneys, while in the higher pressure range (25-30 mmHg) no difference was found. From electron microscopical studies the pyelorenal back-leak of fluid in both hydronephrotic and control animals seemed to be most pronounced in the fornix region, as documented by a heavy presence of horseradish peroxidase in the intracellular spaces there. Other experiments with radioactively labelled inulin, which was injected into the pelvic cavity, indicated that most of the back-leak occurred via the renal blood vessels and not through the lymphatic system. The importance of this back-leak was evident from the measurements of the total kidney glomerular filtration rate (GFR) at a slightly increased pelvic pressure, where some of the urine with radioactive tracer flows back to circulation. The back-leak of pelvic urine could also affect the concentration mechanism by removing diluted urine which had flowed over the renal papilla, and through water and urea diffusion increased papillary interstitial osmolarity.