A. Bergstra et al., ASSUMED OXYGEN-CONSUMPTION BASED ON CALCULATION FROM DYE DILUTION CARDIAC-OUTPUT - AN IMPROVED FORMULA, European heart journal, 16(5), 1995, pp. 698-703
This study was performed because of observed differences between dye d
ilution cardiac output and the Fick cardiac output, calculated from es
timated oxygen consumption according to LaFarge and Miettinen, and to
find a better formula for assumed oxygen consumption. In 250 patients
who underwent left and right heart catheterization, the oxygen consump
tion VO2 (ml.min(-1)) was calculated using Ficks principle. Either pul
monary or systemic flow, as measured by dye dilution, was used in comb
ination with the concordant arteriovenous oxygen concentration differe
nce. In 130 patients, who matched the age of the LaFarge and miettinen
population, the obtained values of oxygen consumption VO2(dd) were co
mpared with the estimated oxygen consumption values VO2(lfm), found us
ing the LaFarge and Miettinen formulae. The VO2(lfm) was significantly
lower than VO2(dd); -21.8 +/- 29.3 ml.min(-1) (mean +/- SD), P<0.001,
95% confidence interval (95% CI) -26.9 to -16.7, limits of agreement
(LA) -8-.4 to 36.9. A new regression formula for the assumed oxygen co
nsumption VO2 (ass) was derived in 250 patients by stepwise multiple r
egression analysis. The VO2(dd) was used as a dependent variable, and
body surface area BSA (m(2)), Sex (0 fro female, 1 for male), Age (yea
rs), Heart rate (min(-1)) and the presence of a left to right shunt as
independent variables. The best fitting formula is expressed as: VO2(
ass)=(157.3 x BSA + 10.0 x Sex-10.5 x ln Age + $.) ml.min(-1), where
ln Age=the natural logarithm of the age. This formula was validated pr
ospectively in 60 patients. A non-significant difference between VO2(a
ss) and VO2(dd) was found; mean 2.0 +/- 23.4 ml.min(-1). P=0.771, 95%
Cl=-4.0 to +8.0, LA -44.7 to +48.7. In conclusion, assumed oxygen cons
umption values, using our new formula, are in better agreement with th
e actual values than those found according to LaFarge and Miettien's f
ormulae.