The oxygen mass transfer coefficient often serves compare the efficiency of
bioreactors and their mixing devices as well as being an important scale-u
p factor. In submerged fermentation, four methods are available to estimate
the overall oxygen mass transfer coefficient (K(L)a): the dynamic method,
the stationary method based on a previous determination of the oxygen uptak
e rate (Q(O2)X), the gaseous oxygen balance and the carbon dioxide balance.
Each method provides a distinct estimation of the value of K(L)a. Data rec
onciliation was used to obtain a more probable value of K(L)a during the pr
oduction of Saccharomyces cerevisiae, performed in 22.5-l fed-batch bioreac
tor. The estimate of K(L)a is obtained by minimising an objective function
that includes measurement terms and oxygen conservation models, each being
weighted according to their level of confidence. Weighting factors of measu
rement terms were taken as their respective inverse variance whereas weight
ing factors of oxygen conservation models were obtained using Monte Carlo s
imulations. Results show that more coherent and precise estimations of K(L)
a are obtained.