On 20 March, 2002, a super dust storm attacked Beijing, which was stronger than any dust storm ever recorded. The con-centration of total suspended particulates (TSP) reached 10.9 mg·m-3, 54 times as high as the ...On 20 March, 2002, a super dust storm attacked Beijing, which was stronger than any dust storm ever recorded. The con-centration of total suspended particulates (TSP) reached 10.9 mg·m-3, 54 times as high as the national air quality standard. The concentrations of major crustal elements, such as Ca, AI, Fe, Na, Mg and Ti, were 30-58 times higher than those in non-dust storm days. The concentrations of pollution elements, such as Zn, Cu, Pb, As, Cd and S, were also about several or even nearly ten times higher than those in normal days. The enrichment factors of Pb, As, Cd and S in PM2.5 were as high as 12.7, 29.6, 43.5,28.4, indicating that these pollutants came from the mixing of mineral aerosol with pollution aerosol emitted by pollution sources on the way of dust storm’s long-range transport. The overlap of invaded air mass from dust with pollution air mass from Beijing local area was another reason for the enhancement of pollutants. During dust storm, fine particles (PM2.5) accounted for 30% of TSP and pollutants in PM2.5 accounted for even as high as 45%-69% of TSP. The increase of pollutants after dust storm proved further that mineral aerosol, especially the fine particles from dust storm favored the transformation and accumulation of pollutants. It must be noted that Fe (II) was detected again in this dust storm, which provided new evidence for the mechanism of coupling and feedback between iron and sulfur in the atmosphere and the ocean. The increase of both pollutants and nutrient, Fe(Ⅱ), during dust storm illuminated that dust storm is an important factor affecting the global environment change.展开更多
Methane sulphonate (MSA) and sulfate (SO4^2-),the main oxidation products of dirnethyl sulfide (DMS), arethe target of atmospheric chemistry study, as sulfate aerosolwould have important impact on the global climate c...Methane sulphonate (MSA) and sulfate (SO4^2-),the main oxidation products of dirnethyl sulfide (DMS), arethe target of atmospheric chemistry study, as sulfate aerosolwould have important impact on the global climate change. It is widely believed that DMS is rnainly emitted from phyto-plankton production in marine boundary layer (MBL), andMSA is usually used as the tracer of non-sea-salt sulfate (nss-SO4^2-) in marine and coastal areas/MSA/SO4^2- = 1/18) Manyobservations of MSA were in marine and coastal aerosols. Toour surprise, MSA was frequently (＞60%) deteeted in BeijingTSP. PM10, and PM2.5 aerosols, even in the samples collectedduring the dust storm period. The concentrations of MSAwere higher than those measured in marine aerosols. Factoranalysis, correlation analysis and meteorology analysis indi-cated that there was no obvious marine influence on Beljiagaerosols. DMS from terrestrial emissions and dimethyl sulphoxide (DMSO) from industrial wastes could be the twopossible precursors of MSA. Warm and low-pressure airmasses and long time radiation were beneficial to the forma-tion of MSA. Anthropogenlc pollution from regional andlocal sources might be the dominant contributor to MSA inBeijing aerosol. This was the first report of MSA in aerosolscollected in an inland site in China. This new finding wouldlead to the further study on the balance af sulfur in inlandcities and its global bingcoehemical cycle.展开更多
文摘On 20 March, 2002, a super dust storm attacked Beijing, which was stronger than any dust storm ever recorded. The con-centration of total suspended particulates (TSP) reached 10.9 mg·m-3, 54 times as high as the national air quality standard. The concentrations of major crustal elements, such as Ca, AI, Fe, Na, Mg and Ti, were 30-58 times higher than those in non-dust storm days. The concentrations of pollution elements, such as Zn, Cu, Pb, As, Cd and S, were also about several or even nearly ten times higher than those in normal days. The enrichment factors of Pb, As, Cd and S in PM2.5 were as high as 12.7, 29.6, 43.5,28.4, indicating that these pollutants came from the mixing of mineral aerosol with pollution aerosol emitted by pollution sources on the way of dust storm’s long-range transport. The overlap of invaded air mass from dust with pollution air mass from Beijing local area was another reason for the enhancement of pollutants. During dust storm, fine particles (PM2.5) accounted for 30% of TSP and pollutants in PM2.5 accounted for even as high as 45%-69% of TSP. The increase of pollutants after dust storm proved further that mineral aerosol, especially the fine particles from dust storm favored the transformation and accumulation of pollutants. It must be noted that Fe (II) was detected again in this dust storm, which provided new evidence for the mechanism of coupling and feedback between iron and sulfur in the atmosphere and the ocean. The increase of both pollutants and nutrient, Fe(Ⅱ), during dust storm illuminated that dust storm is an important factor affecting the global environment change.
文摘Methane sulphonate (MSA) and sulfate (SO4^2-),the main oxidation products of dirnethyl sulfide (DMS), arethe target of atmospheric chemistry study, as sulfate aerosolwould have important impact on the global climate change. It is widely believed that DMS is rnainly emitted from phyto-plankton production in marine boundary layer (MBL), andMSA is usually used as the tracer of non-sea-salt sulfate (nss-SO4^2-) in marine and coastal areas/MSA/SO4^2- = 1/18) Manyobservations of MSA were in marine and coastal aerosols. Toour surprise, MSA was frequently (＞60%) deteeted in BeijingTSP. PM10, and PM2.5 aerosols, even in the samples collectedduring the dust storm period. The concentrations of MSAwere higher than those measured in marine aerosols. Factoranalysis, correlation analysis and meteorology analysis indi-cated that there was no obvious marine influence on Beljiagaerosols. DMS from terrestrial emissions and dimethyl sulphoxide (DMSO) from industrial wastes could be the twopossible precursors of MSA. Warm and low-pressure airmasses and long time radiation were beneficial to the forma-tion of MSA. Anthropogenlc pollution from regional andlocal sources might be the dominant contributor to MSA inBeijing aerosol. This was the first report of MSA in aerosolscollected in an inland site in China. This new finding wouldlead to the further study on the balance af sulfur in inlandcities and its global bingcoehemical cycle.
