Polycyclic Aromatic Hydrocarbons (PAHs) in the Soil of West Qurna-2 Oil Field Southern Iraq

Duha S. Karem, H. Kadhim, H. Al-Saad
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引用次数: 3

Abstract

This study focused on the determinate concentrations of polycyclic aromatic hydrocarbon by using capillary gas chromatographic for soil of ten stations in West Qurna-2 oil field. The first included light (low molecular weight) compounds with two-three fused aromatic rings which consisting of: naphthalene, acenaphthylene, acenaphthene, fluorene, phenanthrene, anthracene, and carbazole. The second included the heavy (high molecular weight) compounds with  four or more fused aromatic rings consisting of: floranthene, pyrene, benzo(a)anthracene, chrysene, benzo(b)flouranthene, benzo(k)flouranthene, benzo(a)pyrene,  indeno(1,2,3,c,d)pyrene, dibenzo(a,h)anthracene, and benzo(g,h,i)perylene. The dominant light PAHs compounds were acenaphthylene, acenaphthene, fluorene, phenanthrene, anthracene and carbazol. Whereas the dominant heavy PAHs compounds were floranthene, pyrene, benzo(a)pyrene , benzo(a)anthracene , benzo(k)flouranthene. The regional higher mean concentrations of PAHs in station 10 was (5.906 ng/g) and the lowest in station 1 (1.125 ng/g). The results of seasonal PAHs concentration in this study showed that the lowest concentrations recorded during summer (1.214 ng/g), while the highest concentrations recorded during winter (4.177ng/g). From the LMW/HMW, phenanthrene/anthracene and benzo(a)anthracene/benzo(a)anthracene+ chrysene ratios, the PAHs compound was drived from pyrogenic sources, while Flouranthene/Pyrene Ratio and InP/(InP+BghiP) Ratio was pyrogenic+ petrogenic origin and petrogenic or pyrogenic and Ant/(Ant+ Phen) Ratio was pyrolytic. Concentrations in studied stations gradually increased from station 1 to station 5, and then significantly decreased at station 6 and finally increased to station 10. The fluctuation in concentrations of compound at stations is due to distance from the flame of the flare which near to the stations 8,9,10 and far to the stations 1,2,3,4,5,6,7, while the seasonal concentration arrange as following: winter >spring >autumn>summer. There were non-significant correlation between the PAHs in soil and each of the soil texture compounds (sand, silt and clay), while there is significant correlation between the PAHs in soil and TOC%.
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伊拉克南部西古尔纳-2油田土壤中多环芳烃(PAHs
采用毛细管气相色谱法测定了西古尔纳-2油田10个测站土壤中多环芳烃的含量。第一种是轻的(低分子量的)化合物,有两三个芳香环,由萘、苊、苊、芴、菲、蒽和咔唑组成。第二种包括重(高分子量)化合物,具有四个或更多的融合芳香环,包括:芴、芘、并并(a)蒽、蒽、并并(b)芴、并并(k)芴、并并(a)芘、茚(1,2,3,c,d)芘、二苯并(a,h)蒽和并并(g,h,i)苝。轻多环芳烃化合物主要为苊、苊、芴、菲、蒽和咔唑。而多环芳烃重化合物主要为芴、芘、苯并(a)芘、苯并(a)蒽、苯并(k)芴。区域平均PAHs浓度最高的监测站10为5.906 ng/g,最低的监测站1为1.125 ng/g。各季节多环芳烃浓度变化结果显示,夏季最低(1.214 ng/g),冬季最高(4.177ng/g)。从LMW/HMW、菲/蒽和苯并(a)蒽/苯并(a)蒽+蒽比值来看,多环芳烃化合物为热生源,而氟蒽/芘比值和InP/(InP+ bghp)比值为热生+成岩源,为成岩或热生,Ant/(Ant+ Phen)比值为热解源。从1号站到5号站浓度逐渐升高,6号站浓度显著降低,最后到10号站浓度升高。站内化合物浓度的波动主要受距离耀斑火焰远近的影响,距离8、9、10站较近,距离1、2、3、4、5、6、7站较远,季节浓度的变化顺序为冬季>春季>秋季>夏季。土壤中多环芳烃含量与土壤质地化合物(砂、粉和粘土)的相关性不显著,而与TOC%的相关性显著。
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