首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Source characterization using molecular distribution and stable carbon isotopic composition of n-alkanes in sediment cores from the tropical Mundaú-Manguaba estuarine-lagoon system, Brazil
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Source characterization using molecular distribution and stable carbon isotopic composition of n-alkanes in sediment cores from the tropical Mundaú-Manguaba estuarine-lagoon system, Brazil

机译:利用巴西Mundaú-Manguaba河口-泻湖系统沉积物核心中正构烷烃的分子分布和稳定碳同位素组成进行源表征

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摘要

The Mundaú-Manguaba estuarine-lagoon system (MMELS) constitutes one of the most representative ecosystems in the state of Alagoas, NE Brazil. Approximately 30% or 60,000ha of the lower surrounding drainage basin of the MMELS are covered by sugar cane and a total of 250,000 inhabitants contribute untreated effluent to the system. Short sediment cores from MMELS were collected in 2007 at three sites: Manguaba Lagoon (C03), Mundaú Lagoon (C07) and Mundaú River (C08) in order to characterize the delivery and deposition of n-alkanes over the past 40yr. The n-alkanes ranged from C_(15) to C_(35), with total aliphatic hydrocarbon (TAH) concentration in the range 27.8-139.5μgg~(-1). An unresolved complex mixture (UCM) was observed in all sediments. The terrigenous/aquatic ratio (TAR), carbon preference index (CPI) and average chain length (ACL) showed that the terrigenous input dominated. The (δ~(13)C) values of individual n-alkanes (C_(16)-C_(33)) varied between -22.6‰ and -34.2‰, suggesting a dominance of ~(12)C-enriched n-alkanes that originated from C_3 plants and lacustrine algae. The data reflect how anthropogenic input (via sewage, industrial pollution and agriculture) has influenced the organic content of the system through time.
机译:Mundaú-Manguaba河口-泻湖系统(MMELS)构成巴西东北部阿拉戈斯州最具代表性的生态系统之一。 MMELS下部周围流域的大约30%或60,000公顷被甘蔗覆盖,共有250,000居民向该系统排放未经处理的污水。 MMELS的短沉积岩心于2007年在三个地点收集:Manguaba泻湖(C03),Mundaú泻湖(C07)和Mundaú河(C08),以表征过去40年中正构烷烃的输送和沉积特征。正构烷烃的范围从C_(15)到C_(35),总脂肪烃(TAH)浓度在27.8-139.5μgg〜(-1)范围内。在所有沉积物中均观察到未解决的复杂混合物(UCM)。陆源/水比(TAR),碳偏好指数(CPI)和平均链长(ACL)表明,陆源输入占主导地位。各个正构烷烃(C_(16)-C_(33))的(δ〜(13)C)值在-22.6‰至-34.2‰之间变化,表明〜(12)C富集的正构烷烃占主导地位。起源于C_3植物和湖藻。数据反映了人为输入(通过污水,工业污染和农业)如何随时间影响系统的有机成分。

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