Isotope analysis based source identification for atmospheric CH sub(4) and CO sampled across Russia using the Trans-Siberian railroad

The isotopic composition of carbon monoxide ( super(13)C, super(14)C, super(18)O) and methane ( super(13)C, D) was measured on air samples collected between Vladivostok and Moscow using the Trans-Siberian railroad during August 1996. Apart from short term fluctuations in the direct vicinity of sources, continuous measurements of CO and CH sub(4) showed sustained, elevated mixing ratios over several hundreds of kilometers indicating the large scale influencing of traversed air masses by significant sources. Persistent, enhanced CH sub(4) levels were found over the west Siberian lowlands concurrent with significantly depleted delta super(13)C and delta D values. The derived isotopic signature of the CH sub(4) source ( delta super(13)C = -62.5 plus or minus 4.7ppt V-PDB; delta D = -311 plus or minus 14ppt V-SMOW) clearly indicates the dominance of biogenic CH sub(4), with the west Siberian wetlands being the most likely candidate. A second major feature in the data set is the enormous enhancement of CO (up to 1500 nmol/mol) east of Chita, extending over a 2000 km section along the river Amur. The super(14)CO measurements and back trajectory analyses identify biomass burning as the origin of the highly elevated CO. This is further supported by the delta super(18)O(CO) and the delta super(13)C/ delta D signature of the accompanying moderate CH sub(4) enhancement.