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Persistent organic pollutants in rain at Niigata, Japan

机译:日本新泻雨中的持久性有机污染物

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Atmospheric monitoring of POPs (α-HCH, HCB and p,p'-DDT) was conducted at three different sites in Niigata area, Japan, the first characterized as remote (top of a mountain, 634m height), the second suburb and third urban. Concurrent and continuous samplings through seven days of environmental air and rain were carried out in the term from May to November 2001. Weighted average concentrations in rain are 585-710pg l~(-1) for α-HCH, 67-80 pg l~(-1) for HCB and 30-52 pg l~(-1) for p,p'-DDT. No significant difference was observed in weight average concentrations of POPs in rain among the three sites, while the average atmospheric concentration of POPs at the remote site was lower than those at other sites. The concentrations of HCB and DDT in rain varied depending on the rainfall: the concentrations of DDT and HCB showed higher values in the less rainfall weeks. On the other hand, the concentration of α-HCH hardly depended on the rainfall. The H' value defined as the ratios of POPs concentrations in air to those in rain were calculated and compared to the Henry's law constant, H. The H' value of α-HCH at high temperature is compatible with H value, which indicates that equilibrium is established between a-HCH in rain and that in ambient gaseous phase. However, the H' values were lower than the H values at lower temperature, and larger difference between H' and H was observed at the lower temperature. This could be interpreted by an increase of particulate α-HCH existing in solid phases such as suspended particles or dry depositions. For HCB and DDT, the H' values were smaller than the H values in all the temperature ranges, indicating that these substances tend to be adsorbed on particulate matter in ambient air, and tend to be deposited on the ground directly and/or by rain.
机译:在日本新泻地区的三个不同地点进行了对持久性有机污染物(α-六氯环己烷,六氯苯和p,p'-DDT)的大气监测,第一个监测点是偏远地区(山顶,海拔634m),第二个监测点是郊区城市。在2001年5月至11月期间,对7天的环境空气和雨水进行了连续不断的采样。α-六氯环己烷的雨水加权平均浓度为585-710pg l〜(-1),67-80 pg l〜。对于HCB为(-1),对于p,p'-DDT为30-52 pg l〜(-1)。在这三个地点之间,雨中持久性有机污染物的重量平均浓度没有观察到显着差异,而偏远地点的持久性有机污染物的平均大气浓度低于其他地点。雨中六氯苯和六氯苯的浓度因降雨而异:在较少的降雨周中,六氯苯和六氯苯的浓度显示较高的值。另一方面,α-六氯环己烷的浓度几乎不取决于降雨。计算出H'值,定义为空气中POPs浓度与雨中POPs的比率,并将其与亨利定律常数H进行比较。高温下α-HCH的H'值与H值兼容,这表明平衡在雨中的六氯环己烷和周围的气相中建立了六氯环己烷。然而,H'值低于在较低温度下的H值,并且在较低温度下观察到H'和H之间的较大差异。这可以用固相(例如悬浮颗粒或干沉积)中存在的颗粒状六氯环己烷增加来解释。对于六氯代苯和滴滴涕,在所有温度范围内,H'值均小于H值,表明这些物质倾向于吸附在周围空气中的颗粒物上,并倾向于直接和/或通过雨水沉积在地面上。

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