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11.
Fangdon Yin Daniel Grosjean Richard C. Flagan John H. Seinfeld 《Journal of Atmospheric Chemistry》1990,11(4):365-399
The mechanisms for atmospheric photooxidation of CH3SCH3 and CH3SSCH3 developed in Part I are evaluated by a series of outdoor smog chamber experiments. Measured product yields, including SO2, H2SO4, CH3SO3H and HCHO, are reported. The predictions of the mechanisms developed in Part I are found to be in substantial agreement with the measured concentrations from the smog chamber. By comparison of mechanism predictions and observations, critical uncertainties in the mechanism are identified. 相似文献
12.
Detailed theoretical (Part I, this article) and experimental (Part II) investigations are presented for the mechanism of the atmospheric photooxidation of dimethyl sulfide (CH3SCH3) and dimethyl disulfide (CH3SSCH3). In this paper, comprehensive mechanisms for the atmospheric chemistry of CH3SCH3 and CH3SSCH3 are developed based on fundamental considerations of all available kinetic and mechanistic information. 相似文献
13.
The full spectrum of volatile sulfur compounds was detected in the water column of the permanently stratified meromictic Lake Cadagno. Besides hydrogen sulfide it included methanethiol, carbonyl sulfide, dimethyl sulfide, carbon disulfide, and dimethyl disulfide. Their distribution in the water column suggests that these compounds are of biogenic origin. Except for carbon disulfide which is present in all layers of Lake Cadagno, these volatile organic sulfur compounds are restricted to the anoxic part of the lake. For methanethiol, dimethyl sulfide, and carbon disulfide maximum concentrations were observed in the redox transition zone and in the sediment porewater. Carbon disulfide is the most abundant volatile organic sulfur compound with concentrations of up to 60 μmol L–1. The concentrations of the methylated sulfides are in the nmolar range. Although their concentrations varied during the summer months, seasonal trends of the concentrations of volatile organic sulfur compounds did not follow a consistent pattern. The restriction of most sulfur species to the anoxic layers of the lake indicates that their production originates from anaerobic microbial degradation of biomass and not from its release from a specific precursor like dimethylsulfoniumpropionate as in marine environments. 相似文献
14.
Measurements of DMS and other reduced sulfur compounds in surface waters have been carried out from a helicopter in the seas surrounding Scandinavia. Average summer time concentrations of DMS ranged from 70 to 150 ngS L-1. Simultaneous measurements of biological and physical parameters revealed no correlation between DMS and phytoplankton species, species assemblages, total phytoplankton biomass, chlorophyll a, temperature, and salinity. The only exception was a correlation between DMS concentration, Chrysochromulina spp. belonging to the Prymnesiophyceae, and salinity over a narrow range of salinity in the Baltic Sea.The flux of reduced sulfur to the atmosphere in July in this region is estimated to be 120–170 gS m-2 d-1 from the Baltic, 240–810 in the Kattegat/Skagerrak, and 120–690 in the North Sea. Annual fluxes are roughly 100 times higher than these daily fluxes. On an annual basis, biogenic sulfur emissions from the coastal seas are negligible (<1%) compared to the anthropogenic emissions in northern Europe. However, during the summer months, the biogenic sulfur emissions from the seas surrounding the Scandinavian peninsula are estimated to be as high as 20–70% of the anthropogenic emissions in Scandinavia. This makes it of interest to incorporate the biogenic emissions in calculations of long-range transport and deposition of sulfur within the region.Other volatile sulfur species, mainly methyl mercaptan, contribute about 10% of the total flux of reduced sulfur. Estimated fluxes of CS2 to the atmosphere ranged from 1 gS m-2 d-1 in the Baltic Sea to 6 gS m-2 d-1 in the North Sea. No emissions for H2S or COS were detected. 相似文献
15.
Byron W. Blomquist Alan R. Bandy Donald C. Thornton Shaoming Chen 《Journal of Atmospheric Chemistry》1993,16(1):23-30
Developments allowing the direct determination of sulfur dioxide and dimethyl sulfide in grab samples by gas chromatography/mass spectrometry with isotopically labeled standards (GC/MS/ILS) are reported. Isotopomers of DMS and SO2 are used as internal standards. Spiked air samples are dried to a dew point of <–60 °C and trapped cryogenically in loops of Teflon tubing. Sealed samples are transported to the laboratory under liquid nitrogen and later subjected to GC/MS analysis. Holding times of up to one month do not result in significant sample loss. For samples collected in a clean marine environment, concentrations of SO2 and DMS greater than 5 and 8 pptv, respectively, are significantly different from blanks at the 95% confidence level. Average measurement precision derived from a propagation of errors are 9% for SO2 and 42% for DMS at concentrations from 5–15 pptv.Improvements are outlined which should provide sensitivity and precision comparable to that of on-site GC/MS. The technique will allow increased flexibility for the determination of trace sulfur species in the field under conditions where deployment of a mass spectrometer is not possible. 相似文献
16.
研究硫化物暴露后单环刺组织细胞色素氧化酶(CCO)、琥珀酸脱氢酶(SDH)、延胡索酸还原酶(FRD)等呼吸代谢酶活性的变化,初步探讨了单环刺对硫化物的呼吸代谢适应。将虫体暴露于50,150μmol/L 2个硫化物组和不含硫化物的对照组水体中,分别于暴露后0,2,12,24,48 h和解除暴露后48 h取体壁、呼吸肠等组织进行酶活性分析。结果显示:暴露2 h时,硫化物组CCO活性上升。24 h时,150μmol/L组CCO活性显著低于对照组,到48 h时接近于0,而SDH活性显著低于对照组,FRD活性极显著高于对照组。解除暴露后48 h,虫体的呼吸代谢酶活性与对照组无显著差异。可见,硫化物暴露后,短期内虫体呼吸代谢提高,可能进行硫化物氧化解毒。而随着暴露时间的延长,虫体的呼吸代谢减弱,FRD活性极显著增高,推测体内可能存在将延胡索酸还原成琥珀酸的无氧代谢方式。解除硫化物暴露后,虫体具有较强的自我恢复能力。 相似文献
17.
Gordon V. Wolfe Maurice Levasseur Guy Cantin Sonia Michaud 《Deep Sea Research Part I: Oceanographic Research Papers》2000,47(12):687
We adapted the dilution technique to study microzooplankton grazing of algal dimethylsulfoniopropionate (DMSP) vs. Chl a, and to estimate the impact of microzooplankton grazing on dimethyl sulfide (DMS) production in the Labrador Sea. Phytoplankton numbers were dominated by autotrophic nanoflagellates in the Labrador basin, but diatoms and colonial Phaeocystis pouchetii contributed significantly to phytomass at several high chlorophyll stations and on the Newfoundland and Greenland shelfs. Throughout the region, growth of algal Chl a and DMSP was generally high (0.2–1 d−1), but grazing rates were lower and more variable, characteristic of the early spring bloom period. Production and consumption of Chl a vs. DMSP followed no clear pattern, and sometimes diverged greatly, likely because of their differing distributions among algal prey taxa and size class. In several experiments where Phaeocystis was abundant, we observed DMS production proportional to grazing rate, and we found clear evidence of DMS production by this haptophyte following physical stress such as sparging or filtration. It is possible that grazing-activated DMSP cleavage by Phaeocystis contributes to grazer deterrence: protozoa and copepods apparently avoided healthy colonies (as judged by relative growth and grazing rates of Chl a and DMSP), and grazing of Phaeocystis was significant only at one station where cells were in poor condition. Although we hoped to examine selective grazing on or against DMSP-containing algal prey, the dilution technique cannot differentiate selective ingestion and varying digestion rates of Chl a and DMSP. We also found that the dilution method alone was poorly suited for assessing the impact of grazing on dissolved sulfur pools, because of rapid microbial consumption and the artifactual release of DMSP and DMS during filtration. Measuring and understanding the many processes affecting organosulfur cycling by the microbial food web in natural populations remain a technical challenge that will likely require a combination of techniques to address. 相似文献