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土耳其一工业用地中影响有机氯农药(OCPs)在土壤和空气中迁移的过程。

Processes affecting the movement of organochlorine pesticides (OCPs) between soil and air in an industrial site in Turkey.

机构信息

Department of Environmental Engineering, Faculty of Engineering, Dokuz Eylul University, Kaynaklar Campus, Buca 35160, Izmir, Turkey.

出版信息

Chemosphere. 2009 Nov;77(9):1168-76. doi: 10.1016/j.chemosphere.2009.09.032. Epub 2009 Oct 15.

Abstract

Soil and atmospheric concentrations, dry deposition and soil-air gas exchange of organochlorine pesticides (OCPs) were investigated at an industrial site in Aliaga, Izmir, Turkey. Current-use pesticides, endosulfan and chlorpyrifos, had the highest atmospheric levels in summer and winter. Summertime total (gas+particle) OCP concentrations in air were higher, probably due to increased volatilization at higher temperatures and seasonal local/regional applications of current-use pesticides. Particle deposition fluxes were generally higher in summer than in winter. Overall average dry particle deposition velocity for all the OCPs was 4.9+/-4.1 cm s(-1) (average+/-SD). SigmaDDXs (sum of p,p'-DDT, p,p'-DDD, and p,p'-DDE) were the most abundant OCPs in Aliaga soils (n=48), probably due to their heavy historical use and persistence. Calculated fugacity ratios and average net gas fluxes across the soil-air interface indicated volatilization for alpha-CHL, gamma-CHL, heptachlorepoxide, cis-nonachlor, trans-nonachlor, and p,p'-DDT in summer, and for alpha-CHL, gamma-CHL, trans-nonachlor, endosulfan sulfate, and p,p'-DDT in winter. For the remaining OCPs, soil acted as a sink during both seasons. Comparison of the determined fluxes showed that dry particle, gas-phase, and wet deposition are significant OCP input mechanisms to the soil in the study area.

摘要

在土耳其伊兹密尔的阿里阿加(Aliaga)工业场地,研究了有机氯农药(OCPs)在土壤和大气中的浓度、干沉降以及土壤-空气气体交换。当前使用的农药硫丹和毒死蜱在夏季和冬季的大气中浓度最高。夏季空气中总(气+粒)OCP 浓度较高,可能是由于温度升高导致挥发增加,以及当前使用的农药季节性的局部/区域施用。夏季的颗粒沉降通量通常高于冬季。所有 OCP 的总平均干颗粒沉降速度为 4.9+/-4.1 cm s(-1)(平均值+/-标准差)。ΣDDXS(p,p'-DDT、p,p'-DDD 和 p,p'-DDE 的总和)是阿里阿加土壤中最丰富的 OCP(n=48),可能是由于它们的大量历史使用和持久性。通过计算逸度比和土壤-空气界面的平均净气体通量,表明在夏季 α-CHL、γ-CHL、七氯环氧、顺式-十氯、反式-十氯和 p,p'-DDT 挥发,冬季 α-CHL、γ-CHL、反式-十氯、硫丹硫酸盐和 p,p'-DDT 挥发。对于其余的 OCPs,土壤在两个季节都充当汇。通过比较确定的通量,表明干颗粒、气相和湿沉降是研究区域中 OCP 向土壤输入的重要机制。

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