J. Waniewski et al., SIMPLE-MODELS FOR FLUID TRANSPORT DURING PERITONEAL-DIALYSIS, International journal of artificial organs, 19(8), 1996, pp. 455-466
Peritoneal fluid transport can be predicted using different simplified
formulas. To evaluate three such models, fluid transport was studied
in 38 single six hour dwell studies using standard glucose 1.36% (n=9)
, 2.27% (n=9) and 3.86% (n=20) dialysis fluids as well as amino acid 2
.70% fluid (n=8) in 33 patients on continuous ambulatory peritoneal di
alysis (GAPD). Dialysate volume and the peritoneal absorption rate wer
e measured using radioiodinated serum albumin (RISA) as a marker. The
dialysate volume over dwell time curves were examined using three math
ematical models of fluid transport for solutions with a crystalloid os
motic agent: Model P based on phenomenologically derived exponential f
unction of time (Pyle, 1981), Model OS based on linear relationship be
tween the rate of net volume change, Qv, to the difference of osmolali
ty in dialysate and blood, and Model G based on linear relationship be
tween Qv and the difference of glucose concentration in dialysate and
blood. All these models provided a good description of the measured di
alysate volume over time curves, however the descriptions with Models
OS and G for glucose 3.86% fluid were slightly but significantly less
precise. The coefficients of Model:OS were stable in time, but the coe
fficients of Model G and P dependend in general on the time period use
d for their estimation, especially for glucose 3.86% dialysis fluid. T
he evaluation of dwell studies with solutions containing amino acid 2.
70% (instead of glucose) as osmotic agent, using Model OS and P showed
that the transport coefficients were stable in time and both models p
rovided equally precise descriptions. These results suggested that all
three models can be used but models P and OS can be preferred for pra
ctical applications such as predictions of fluid transport with altern
ative cristalloid osmotic agents. Furthermore, we found that the perit
oneal barrier for fluid transport may change transiently during exchan
ges with the standard glucose - based dialysis fluid, whereas such cha
nges were not observed with the amino acid-based fluid. This discrepan
cy may be due to a different composition of the dialysis fluids, inclu
ding osmotic agent, buffer and pH.