Stable carbon and oxygen isotopic analysis of atmospheric carbon monoxide using continuous-flow isotope ratio MS by isotope ratio monitoring of CO.
We have developed a rapid and simple measurement system for both content and stable isotopic compositions (13C and 18O) of atmospheric CO, using continuous-flow isotope ratio mass spectrometry by simultaneously monitoring the CO+ ion currents at masses 28, 29, and 30. The analytical system consisted sequentially of a sample trapping port (liquid nitrogen temperature silica gel and molecular sieve 5A), a gas dryer, a CO purification column (molecular sieve 5A), a cryofocusing unit, and a final purification column using a GC capillary. Analytical precision of 0.2 per thousand for 13C and 0.4 per thousand for 18O can be realized for samples that contain as little as 300 pmol of CO within 40 min for one sample analysis. Analytical blanks associated with the method are less than 1 pmol. The extent of analytical error in delta13C due to mass-independent fractionation of oxygen in natural CO is estimated to be less than 0.3 per thousand. Based on this system, we report herein a kinetic isotopic effect during CO consumption in soil.
Tsunogai
Urumu
U
Division of Earth & Planetary Sciences, Graduate School of Science, Hokkaido University, Kita-10 Nishi-8, Kita-ku, Sapporo, 060-0810 Japan. urumu@ep.sci.hokudai.ac.jp
Nakagawa
Fumiko
F
Komatsu
Daisuke D
DD
Gamo
Toshitaka
T
D000395:Air Pollutants, Occupational / Q000032:analysis*; D000465:Algorithms; D002247:Carbon Isotopes; D002248:Carbon Monoxide / Q000032:analysis*; D013058:Mass Spectrometry; D010103:Oxygen Isotopes; D012987:Soil / Q000032:analysis
D000395:Air Pollutants, Occupational; D002247:Carbon Isotopes; D010103:Oxygen Isotopes; D012987:Soil; D002248:Carbon Monoxide