Three approaches are currently used in kinetic models (UKMs) to account for
the postdialysis rebound in urea concentration, and thereby accurately mea
sure the hemodialysis dose, KT/V (where K,T,V denote dialyzer clearance, di
alysis duration, and urea distribution volume, respectively). The approach
developed by Smye uses an intradialytic sample to predict the postdialysis
equilibrium concentration, C-e, which is then used in a single pool UKM to
give KT/V. A second approach developed by Tattersall introduces a patient c
learance time, t(p). The true dialysis dose is then given by T/(T + t(p)) x
apparent dose, and t(p) is estimated to be 36 minutes. The Daugirdas analy
sis uses an empiric regression equation to give the true dose; KT/V)(true)
from the single pool value, KT/V)(sp); KT/V)(true) = KT/V)(sp) - (36/T)(KT/
V)(sp) + 0.03. The analysis confirms the equivalence of all three formulas,
which arises from the observation that during the later stages of dialysis
, the urea concentration decreases as a single exponential. The formulas ar
e independent of whether a flow or diffusion model is used to describe the
kinetics of urea removal. The original analysis assumed constant volumes, b
ut he effect of ultrafiltration volume u on C-e may be accounted for by mul
tiplying by (1 + u/V). The Smye equation is more vulnerable to error in pra
ctice, because small errors in the intradialytic sample give larger errors
in the equilibrium concentration estimate, whereas dose estimates based on
the Tattersall and Daugirdas equations are less affected by sampling errors
. However, unlike the Smye approach, these two formulas would need adaptati
on for use with other solutes. The advent of continuous urea monitoring sho
uld permit more accurate, prospective estimates of equilibrium concentratio
ns and dialysis dose.