Component characteristics of polycyclic aromatic compounds in sediments of the South Mid-Atlantic Ridge
-
摘要: 我们测试了南大西洋洋中脊附近10个海底沉积物中芳香化合物的组成和丰度。样品中总芳香化合物含量在2.768-9.826μg/g沉积物干重之间, 22V-TVG10和26V-TVG05站位样品中含量较高, 最低值出现在22V-TVG14站位, 表明样品中芳香化合物含量与热液活动密切相关, 暗示出样品中芳香化合物具有热液起源。其中主要有9种芳香化合物及其同系物被检测出来。被检测到的芳香化合物以三环和四环等低分子质量芳香化合物为主, 其中含量最高的为荧蒽, 含量在0.913-3.157μg/g沉积物干重之间。样品中检测到的芳香化合物种类最丰富的为菲同系物。菲与甲基菲的比值范围在0.097-1.602之间, 最大值出现在22V-TVG10站位, 其次为26V-TVG05和22V-TVG11站位, 表明这些站位样品受热液蚀变影响程度较大, 也进一步暗示出样品中多环芳香化合物可能主要来源于海底热液蚀变。Abstract: 10 samples of sediments obtained from the South Mid-Atlantic Ridge were measured for the abundances and distributions of polycyclic aromatic compounds (PAHs). The total concentrations of PAHs (∑PAHs) ranged from 2.768 to 9.826 μg/g dry sediment. The ∑PAHs was higher in sample 22V-TVG10 and sample 26V-TVG05 which were close to hydrothermal fields, with the lowest value in sample 22V-TVG14 which was farthest from hydrothermal fields, suggesting a probable hydrothermal origin of ∑PAHs of samples. Approximately nine kinds of PAHs were identified, and low molecular mass tricyclic and tetracyclic aromatic compounds were predominant in the samples. The concentrations of fluoranthene which were typical as hydrothermal alteration compounds were the highest among PAHs with dry weight between 0.913-3.157 μg/g. The phenanthrene homologue was most abundant in the samples, and the ratios between parent phenanthrene and methylphenanthrene which probably reflected the degree of hydrothermal alteration ranged from 0.097 to 1.602. The sample 22V-TVG10 possessing a maximum ratio value showed the intense influence of the hydrothermal alteration on this sample, which might further imply that PAHs in sediments were mainly derived from the hydrothermal alteration.
-
Belt J Q, Rice G K. 1996. Offshore 3D seismic, geochemical data integration, Main Pass project, Gulf of Mexico. Oil Gas J, 94(14): 76-81 Boleneus D. 1994. Guidelines for surface geochemical surveying. Oil Gas J, 92(23): 59-63 Brault M, Marty J C, Saliot A. 1984. Fatty acids from particulate matter and sediment in hydrothermal environments from the east Pacific rise, near 13°N. Organic Geochemistry, 6: 217-222 Chernova T G, Paropkari A L, Pikovskii Y I, et al. 1999. Hydrocarbons in the Bay of Bengal and Central Indian Basin bottom sediments: indicators of geochemical processes in the lithosphere. Mar Chem, 66(3-4): 231-243 Chernova T G, Rao P S, Pikovskii Y I, et al. 2001. The composition and the source of hydrocarbons in sediments taken from the tectonically active Andaman Backarc Basin, Indian Ocean. Mar Chem, 75(1-2): 1-15 Cui Zhisong, Lai Qiliang, Dong Chunming, et al. 2008. Biodiversity of polycyclic aromatic hydrocarbon-degrading bacteria from deep sea sediments of the Middle Atlantic Ridge. Environmental Microbiology, 10(8): 2138-2149 Delacour A, Früh-Green G L, Bernasconi S M, et al. 2008. Carbon geochemistry of serpentinites in the Lost City Hydrothermal System (30°N, MAR). Geochim Cosmochim Acta, 72(15): 3681-3702 DeMets C, Gordon R G, Argus D F, et al. 1994. Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions. Geophys Res Lett, 21(20): 2191-2194 Geptner A R, Ricter B, Pikovskii Y I, et al. 2006a. Polycyclic aromatic hydrocarbons as evidence of hydrocarbon migration in marine and lagoon sediments of a recent rift zone (Skjálfandi and Öxarfjörður), Iceland. Chemie der Erde, 66(3): 213-225 Geptner A R, Ricter B, Pikovskii Y I, et al. 2006b. Hydrothermal polycyclic aromatic hydrocarbons in marine and lagoon sediments at the intersection between Tjörnes Fracture Zone and recent rift zone (Skjálfandi and Öxarfjöreður bays), Iceland. Marine Chemistry, 101(3-4): 153-165 Hunt J M. 1996. Petroleum Geochemistry and Geology. New York: Freeman and Co, 743 Ishiwatari R, Fukushima K. 1979. Generation of unsaturated and aromatic hydrocarbons by thermal alteration of young kerogen. Geochim Cosmochim Acta, 43(8): 1343-1349 Konn C, Charlou J L, Donval J P, et al. 2009. Hydrocarbons and oxidized organic compounds in hydrothermal fluids from Rainbow and Lost City ultramafic-hosted vents. Chemical Geology, 258(3-4): 299-314 Konn C, Testemale D, Querellou J, et al. 2011. New insight into the contributions of thermogenic processes and biogenic sources to the generation of organic compounds in hydrothermal fluids. Geobiology, 9(1): 79-93 Kvenvolden K A, Rapp J B, Hostettler F D, et al. 1986. Petroleum associated with polymetallic sulfide in sediment from Gorda Ridge. Science, 234(4781): 1231-1234 Li Jiwei, Peng Xiaotong, Zhou Huaiyang, et al. 2012. Characteristics and source of polycyclic aromatic hydrocarbons in the surface hydrothermal sediments from two hydrothermal fields of the Central Indian and Mid-Atlantic Ridges. Geochemical Journal, 46(1): 31-43 Li Jiwei, Zhou Huaiyang, Peng Xiaotong, et al. 2011. Abundance and distribution of fatty acids within the walls of an active deep-sea sulfide chimney. Journal of Sea Research, 65(3): 333-339 Michaelis W, Jenisch A, Richnow H H. 1990. Hydrothermal petroleum generation in Red Sea sediments from the Kebrit and Shaban Deeps. In: Simoneit B R T, ed. Organic Matter Alteration in Hydrothermal Systems-Petroleum Generation, Migration and Biogeochemistry. Appl Geochem, 5(1-2): 103-114 Morgunova I P, Ivanov V N, Litvinenko I V, et al. 2012. Geochemistry of organic matter in bottom sediments of the Ashadze hydrothermal field. Oceanology, 52(3): 345-353 Plummer P. 1994. Seismic anomalies suggest giant oil fields may lie off Seychelles. Oil Gas J, 92(35): 93-97 Rushdi A I, Simoneit B R T. 2002a. Hydrothermal alteration of organic matter in sediments of the Northeastern Pacific Ocean: Part 1. Middle Valley, Juan de Fuca Ridge. Applied Geochemistry, 17: 1401-1428 Rushdi A I, Simoneit B R T. 2002b. Hydrothermal alteration of organic matter in sediments of the Northeastern Pacific Ocean: Part 2. Escanaba Trough, Gorda Ridge. Applied Geochemistry, 17: 1467-1494 Schoell M. 1983. Genetic characterization of natural gases. AAPG Bull, 67(12): 2225-2238 Shao Zongze, Cui Zhisong, Dong Chunming, et al. 2010. Analysis of a PAH-degrading bacterial population in subsurface sediments on the Mid-Atlantic Ridge. Deep-Sea Research Part I, 57(5): 724-730 Simoneit B R T. 1977. Organic matter in eolian dusts over the Atlantic Ocean. Marine Chemistry, 5: 443-464 Simoneit B R T, Fetzer J C. 1996. High molecular weight polycyclic aromatic hydrocarbons in hydrothermal petroleums from the Gulf of California and Northeast Pacific Ocean. Org Geochem, 24: 1065-1077 Simoneit B R T, Grimalt J O, Hayes J M, et al. 1987. Low temperature hydrothermal maturation of organic matter in sediments from the Atlantis II Deep, Red Sea. Geochim Cosmochim Acta, 51(4): 879-894 Simoneit B R T, Lein A Y, Peresypkin V I, et al. 2004. Composition and origin of hydrothermal petroleum and associated lipids in the sulfide deposits of the Rainbow Field (Mid-Atlantic Ridge at 36°N). Geochimica et Cosmochimica Acta, 68(10): 2275-2294 Tissot B P, Welte D H. 1984. Petroleum Formation and Occurrence, 2nd ed. New York: Springer, 699 Towler B F. 1993. Statistical, economic analyses given for surface exploration projects. Oil Gas J, 91(19): 69-72 Venkatesan M I, Ruth E, Rao P S, et al. 2003. Hydrothermal petroleum in the sediments of the Andaman Backarc Basin, Indian Ocean. Applied Geochemistry, 18(6): 845-861 Yamanaka T, Sakata S. 2004. Abundance and distribution of fatty acids in hydrothermal vent sediments of the western Pacific Ocean. Organic Geochemistry, 35(5): 573-582
点击查看大图
计量
- 文章访问数: 1350
- HTML全文浏览量: 38
- PDF下载量: 1577
- 被引次数: 0