阿拉伯湾东北部伊拉克南部沙特阿拉伯河沉积物中脂肪烃的评价

W. A. Farid
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引用次数: 4

摘要

阿拉伯河是伊拉克南部巴士拉市重要的供水、工业和灌溉河流之一。它还为该地区的用户提供饮用水。尽管这条河具有重要的意义,但对石油污染的研究,特别是对河流沉积物中有机质的分子示踪法的地球化学研究还很缺乏。因此,在元素和分子水平上对这条河中石油碳氢化合物的鉴定和定量将是最大的兴趣。对阿拉伯河9个站点的沉积物进行了分析。质地为粉质粘土或粉质砂。TOC和TN分别为0.39 ~ 0.90和0.02 ~ 0.16%。OM变化范围为17.43 ~ 34.36µg g-1 dw,占总TOC的0.27 ~ 0.87%。AHs范围为3.19 ~ 10.27µg g-1 dw,占OM的16.07 ~ 29.88%。总正构烷烃浓度范围为0.08 ~ 42.58µg g-1 dw,碳数为c11 ~ c34。与世界范围内受石油污染的地点相比,正构烷烃含量相对较低。偶碳数正构烷烃(C11-C20)以CPI和LMW/HMW值接近1的正构烷烃为主。U/R(1.27 ~ 2.45)、pri/phy(0.82 ~ 1.00)、C17/pri(0.70 ~ 1.94)和C18/phy(0.95 ~ 1.56)比值和UCM的存在证实了这一点。C17-C31的正构烷烃分布中存在生物成因贡献,CPI和LMW/HMW值均<1,主要与陆生植物、浮游植物、藻类和细菌来源有关,TAR(0.79-2.15)和C31/C19比值(0.28-1.62)值证实了这一点。然而,生物烃的贡献被石油来源的正构烷烃所掩盖。UCM的存在很明显地说明了这一点。主成分分析结果与正构烷烃比值一致,表明沉积物中正构烷烃来源混合。沉积物中的藿烷和甾烷具有相似的特征,是原油污染对成熟有机质贡献的特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of Aliphatic Hydrocarbons in Sediments of Shatt Al-Arab River, Southern Iraq, North East Arabian Gulf
Shatt Al-Arab River is one of the important rivers for water supply, industry and irrigation in Basrah City, south of Iraq. It's also supply drinking water to users in the region. Despite the significance of this river, there is a lack of previous studies dealing with petroleum pollution especially for geochemical studies of organic matter in the river sediments using molecular tracer methods. Therefore, the identification and quantification of petroleum hydrocarbons in this river at the elemental and molecular levels will be of the utmost interest. Sediments were analyzed in nine Shatt Al-Arab River stations. Texture was silty clay or silty sand. TOC and TN ranged from 0.39-0.90 and 0.02-0.16%. OM varied from 17.43-34.36 µg g-1 dw, representing 0.27-0.87% of TOC. AHs ranged from 3.19-10.27 µg g-1 dw and constituted 16.07-29.88% of OM. Total n-alkanes concentrations ranged from 0.08-42.58 µg g-1 dw with carbon numbers from C11-C34 were identified. N-alkanes content was relatively moderate compared to sites contaminated with oil worldwide. Dominance of even carbon number n-alkanes (C11-C20) with CPI and LMW/HMW values close to unity, indicated to oil-related n-alkanes. This was verified by the values of U/R (1.27-2.45), pri/phy (0.82-1.00), C17/pri (0.70-1.94) and C18/phy (0.95-1.56) ratios and the presence of UCM. Biogenic contributions were detected within the n-alkanes distribution of C17-C31 and CPI and LMW/HMW values of <1 that mainly related to terrestrial plants, phytoplankton, algae and bacteria sources, confirmed by TAR (0.79-2.15) and C31/C19 ratio (0.28-1.62) values. However, the contribution from biogenic hydrocarbons is overshadowed by petroleum origin n-alkanes. This was obvious by the presence of UCM. PCA showed concordant results with n-alkanes ratios indicating mixed n-alkanes sources in sediments. Hopanes and steranes in sediments displayed similar signatures that were characteristic of mature organic matter contribution from oil contaminations.
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