Table 3.8.
Source or sink | COS (1012 g S /yr) | References |
---|---|---|
Sources | ||
Oceans | 0.04a | Kettle et al., 2002 |
Anoxic soils | 0.03 | Kettle et al., 2002 |
Biomass burning | 0.31–0.60 | Andreae, 2019 |
Stinecipher et al., 2019 | ||
Industrial | 0.26 | Campbell et al., 2015 |
Volcanoes | 0.02 | Chin and Davis, 1993 |
Oxidation of natural CS2 | 0.14b | Kettle et al., 2002 |
Campbell et al., 2015 | ||
Oxidation of DMS | 0.15 | Kettle et al., 2002 |
Total sources | 0.95–1.25 | |
Sinks | ||
Vegetation uptake | 0.24–0.74 | Kettle et al., 2002 |
Berry et al., 2013 | ||
Soil uptake (oxic) | 0.13 | Kettle et al., 2002 |
Oxidation by OH | 0.09 | Kettle et al., 2002 |
Stratospheric photolysis | 0.02 | Kettle et al., 2002 |
Total sinks | 0.48–0.98 |
net.
assumes that 44% of the global annual CS2 source is industrial.