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外源含硫化合物对土壤挥发性有机硫化合物交换通量的影响
引用本文:易志刚,王新明.外源含硫化合物对土壤挥发性有机硫化合物交换通量的影响[J].环境科学,2011,32(8):2236-2239.
作者姓名:易志刚  王新明
作者单位:1. 中国科学院广州地球化学研究所有机地球化学国家重点实验室,广州510640 福建农林大学资源与环境学院,福州350002
2. 中国科学院广州地球化学研究所有机地球化学国家重点实验室,广州,510640
基金项目:有机地球化学国家重点实验室开放基金项目(OGL-200708);福建省科技计划资助省属高校项目(2008F5013)
摘    要:通过静态箱采样和Entech7100预浓缩仪-GC-MS分析了半胱氨酸、硫化钠和硫酸钠对土壤吸收或释放羰基硫(COS)、二甲基硫醚(DMS)、二硫化碳(CS2)和二甲二硫醚(DMDS)等4种挥发性有机硫化合物(VOSCs)的影响.结果表明,添加半胱氨酸后,土壤由COS和CS2汇转变为源,DMS和DMDS通量显著增加,且...

关 键 词:半胱氨酸  硫化钠  硫酸钠  羰基硫  二甲基硫醚  二硫化碳  二甲二硫醚  交换通量
收稿时间:2010/9/26 0:00:00
修稿时间:2010/12/23 0:00:00

Influence of Exogenous Sulfur-containing Compounds on the Exchange Fluxes of Volatile Organic Sulfur Compounds
YI Zhi-gang and WANG Xin-ming.Influence of Exogenous Sulfur-containing Compounds on the Exchange Fluxes of Volatile Organic Sulfur Compounds[J].Chinese Journal of Environmental Science,2011,32(8):2236-2239.
Authors:YI Zhi-gang and WANG Xin-ming
Affiliation:State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China. zgyi@fjau.edu.cn
Abstract:The influences of cysteine, sodium sulfide (Na2S) and sodium sulfate (Na2SO4) on the soil-air exchange fluxes of volatile organic sulfur compounds (VOSCs), including carbonyl sulfide (COS), dimethyl sulfide (DMS), carbon disulfide (CS2) and dimethyl disulfide (DMDS), were studied employing static chamber enclosure followed by laboratory determination using an Entech 7100 preconcentrator coupled with an Agilent 5973 GC-MSD. The results showed that after the addition of cysteine, the soil for the exchange fluxes of COS and CS2 shifted to be the source from sink and the emissions of DMS and DMDS increased significant. The emission amount of DMS and CS2 accounted for 89.2% to the total VOSCs after the addition of cysteine, implying that cysteine is an important precursor for DMS and CS2 in the soil. The amount of DMDS accounted for 93.2% to the total sulfur from the soil after addition of Na2S, indicating that Na2S is a key precursor for DMDS. No significant difference of VOSCs fluxes was found between the controlled soil and the soil with addition of Na2SO4, suggesting Na2SO4 was not the direct precursor for VOSCs in soil. VOSCs exchange rates reached the maximum at 6 to 8 days after addition of cysteine. As for addition of Na2S, the maximal emission rates of different VOSCs appeared at different dates, and the dates differed significantly from those after addition of cysteine, implying that the formation process of VOSCs from the soil with addition of Na2S was more complex and different from the soil with addition of cysteine.
Keywords:cysteine  sodium sulfide  sodium sulfate  carbonyl sulfide (COS)  dimethyl sulfide (DMS)  carbon disulfide (CS2)  dimethyl disulfide (DMDS)  exchange flux
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