Je. Steele et al., GRAVIMETRIC METHOD FOR THE DYNAMIC MEASUREMENT OF URINE FLOW, Proceedings of the Society for Experimental Biology and Medicine, 204(1), 1993, pp. 70-74
The rate of urine formation is a primary index of renal function, but
no techniques are currently available to accurately measure low rates
of urine flow on a continuous basis, such as are normally found in rat
s. We developed a gravimetric method for the dynamic measurement of ur
ine flow in anesthetized rats. Catheters were inserted directly into t
he ureters close to the renal pelves, and a siphon was created to coll
ect all of the urine formed as rapidly as it was produced. Urine flow
was determined by measuring the weight of the urine using a direct-rea
ding analytical balance interfaced to a computer. Basal urine flow was
measured at 2-sec intervals for 30 to 60 min. The dynamic response of
urine flow to a rapid decrease in arterial pressure produced by a bol
us intravenous injection of acetylcholine (0.5 mu g) was also measured
. Intrinsic drift, evaporative losses, and the responsiveness of the s
ystem to several fixed pump-flows in the low physiologic range were ev
aluated in vitro. The gravimetric method described was able to continu
ously measure basal urine flows that averaged 37.3 +/- 12.4 mu l/min.
Error due to drift and evaporation was negligible, totaling less than
1% of the measured urine flow. Acetylcholine-induced declines in arter
ial pressure were followed within 8 sec by a decline in urine flow. Th
ese data demonstrate that this new gravimetric method provides a simpl
e, inexpensive, dynamic measurement of urine flow in the mu l/min rang
e.