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Oxygenated polycyclic aromatic hydrocarbons and azaarenes in urban soils: A comparison of a tropical city (Bangkok) with two temperate cities (Bratislava and Gothenburg)

机译:城市土壤中的氧化多环芳烃和氮杂芳烃:热带城市(曼谷)与两个温带城市(布拉迪斯拉发和哥德堡)的比较

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摘要

Environmental conditions in the tropics favor the formation of polar polycyclic aromatic compound (polar PACs, such as oxygenated PAHs [OPAHs] and azaarenes [AZAs]), but little is known about these hazardous compounds in tropical soils. The objectives of this work were to determine (ⅰ) the level of contamination of soils (0-5 and 5-10 cm layers) from the tropical metropolis of Bangkok (Thailand) with OPAHs and AZAs and (ⅱ) the influence of urban emission sources and soil properties on the distribution of PACs. We hypothesized that the higher solar insolation and microbial activity in the tropics than in the temperate zone will lead to enhanced secondary formation of OPAHs. Hence, OPAH to related parent-PAH ratios will be higher in the tropical soils of Bangkok than in temperate soils of Bratislava and Gothenburg. The concentrations of ∑15OPAHs (range: 12-269 ng g~(-1)) and ∑4AZAs (0.1-31 ng g~(-1)) measured in soils of Bangkok were lower than those in several cities of the industrialized temperate zone. The ∑15OPAHs (r = 0.86, p < 0.01) and ∑4AZAs (r = 0.67, p < 0.01) correlated significantly with those of ∑20PAHs highlighting similar sources and related fate. The octanol-water partition coefficient did not explain the transport to the subsoil, indicating soil mixing as the reason for the polar PAC load of the lower soil layer. Data on PAC concentrations in soils of Bratislava and Gothenburg were taken from published literature. The individual OPAH to parent-PAH ratios in soils of Bangkok were mostly higher than those of Bratislava and Gothenburg (e.g. 9-fluorenone/fluorene concentration ratio was 12.2 ± 6.7, 5.6 ± 2.4, and 0.7 ± 02 in Bangkok, Bratislava and Gothenburg soils, respectively) supporting the view that tropical environmental conditions and higher microbial activity likely lead to higher OPAH to parent-PAH ratios in tropical than in temperate soils.
机译:热带地区的环境条件有利于形成极性多环芳族化合物(极性PAC,例如氧化的PAH [OPAH]和氮杂[AZA]),但对于热带土壤中的这些有害化合物知之甚少。这项工作的目的是确定(ⅰ)OPAH和AZAs对来自热带都市曼谷(泰国)的土壤(0-5和5-10 cm层)的污染程度,以及(ⅱ)城市排放的影响来源和土壤特性对PACs的分布。我们假设热带地区的日照和微生物活性高于温带地区,将导致OPAH的次级形成增加。因此,在曼谷的热带土壤中,OPAH与相关母体PAH的比率要比在布拉迪斯拉发和哥德堡的温带土壤中的高。在曼谷的土壤中测得的∑15OPAHs(范围:12-269 ng g〜(-1))和∑4AZA(0.1-31 ng g〜(-1))的浓度低于工业化温带几个城市的浓度区。 ∑15OPAHs(r = 0.86,p <0.01)和∑4AZAs(r = 0.67,p <0.01)与∑20PAHs显着相关,强调了相似的来源和相关的命运。辛醇-水分配系数不能解释向地下土壤的运移,表明土壤混合是下部土壤层极性PAC负荷的原因。布拉迪斯拉发和哥德堡土壤中PAC浓度的数据取自已发表的文献。曼谷土壤中单个OPAH与母体PAH的比率大多高于布拉迪斯拉发和哥德堡(例如,曼谷,布拉迪斯拉发和哥德堡的土壤中9-芴酮/芴的浓度比为12.2±6.7、5.6±2.4和0.7±02分别支持以下观点:热带环境条件和较高的微生物活性可能导致热带地区的OPAH与母体PAH的比例高于温带土壤。

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