We have developed a rapid and simple measurementsystem for both content and stable isotopic compositions(
13C and
18O) of atmospheric CO, using continuous-flowisotope ratio mass spectrometry by simultaneously monitoring the CO
+ ion currents at masses 28, 29, and 30.The analytical system consisted sequentially of a sampletrapping port (liquid nitrogen temperature silica gel andmolecular sieve 5A), a gas dryer, a CO purification column(molecular sieve 5A), a cryofocusing unit, and a finalpurification column using a GC capillary. Analytical precision of 0.2 for
13C and 0.4 for
18O can be realizedfor samples that contain as little as 300 pmol of CO within40 min for one sample analysis. Analytical blanks associated with the method are less than 1 pmol. The extent ofanalytical error in
13C due to mass-independent fractionation of oxygen in natural CO is estimated to be lessthan 0.3. Based on this system, we report herein akinetic isotopic effect during CO consumption in soil.