Carbonyl sulfide （COS） and dimethyl sulfide （DMS） fluxes from as urban Cynodon dactylon lawn and adjacent bare soil were measured during April-July 2005 in Guangzhou, China. Both the lawn and bare soil acted as si...Carbonyl sulfide （COS） and dimethyl sulfide （DMS） fluxes from as urban Cynodon dactylon lawn and adjacent bare soil were measured during April-July 2005 in Guangzhou, China. Both the lawn and bare soil acted as sinks for COS and sources for DMS. The mean fluxes of COS and DMS in the lawn （-19.27 and 18.16 pmol/（m^2.sec）, respectively） were significantly higher than those in the bare soil （-9.89 and 9.35 pmol/（m^A2.sec）, respectively）. Fluxes of COS and DMS in mowed lawn were also higher than those in bare soils. Both COS and DMS fluxes showed diurnal variation with detectable but much lower values in the nighttime than in the daytime. COS fluxes were related significantly to temperature and the optimal temperature for COS uptake was 29℃. While positive linear correlations were found between DMS fluxes and temperature. COS fluxes increased linearly with ambient COS mixing ratios, and had a compensation point of 336 ppt.展开更多
基金supported by the National Natural Science Foundation of China (No. 40821003, 40971260)the Foundation for University by the Fujian Provincial Department of Science and Technology (No. 2008F5013)
文摘Carbonyl sulfide （COS） and dimethyl sulfide （DMS） fluxes from as urban Cynodon dactylon lawn and adjacent bare soil were measured during April-July 2005 in Guangzhou, China. Both the lawn and bare soil acted as sinks for COS and sources for DMS. The mean fluxes of COS and DMS in the lawn （-19.27 and 18.16 pmol/（m^2.sec）, respectively） were significantly higher than those in the bare soil （-9.89 and 9.35 pmol/（m^A2.sec）, respectively）. Fluxes of COS and DMS in mowed lawn were also higher than those in bare soils. Both COS and DMS fluxes showed diurnal variation with detectable but much lower values in the nighttime than in the daytime. COS fluxes were related significantly to temperature and the optimal temperature for COS uptake was 29℃. While positive linear correlations were found between DMS fluxes and temperature. COS fluxes increased linearly with ambient COS mixing ratios, and had a compensation point of 336 ppt.
