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An Assessment of Mercury Loading in Core Sediments of Sunderban Mangrove Wetland, India (A Preliminary Report)

机译:印度桑德班红树林湿地核心沉积物中汞含量的评估(初步报告)

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This is a preliminary report on total mercury (THg) in core sediments (<63 μm particle size) of Sunderban mangrove wetland, northeastern part of the Bay of Bengal, India. Cold vapor atomic absorption spectrometry (CVAAS) was used for THg determination. The concentration varies from 9.8 to 535.1 ppb (ngg−1). Results revealed variations over premonsoon and postmonsoon month at different core depth, as well as in studied three sampling stations, located at the site of three rivers: Hugli River (S1), Matla River (S2) and Bidyadhari River (S3). Elevated concentration of THg in subsurface layer (4–8 cm) of the core at S2 is attributed to remobilization of mercury from deeper sediment (32–36 cm). Positive correlation is present between total Hg and clay content. Based on index of geoaccumulation (Igeo) and Effects-Range Low (ER-L) value (150 ppb) it is considered that the sediments are till now unpolluted. As a consequence, there is less chance of ecotoxicological risk to organisms living in studied sediments. Two statistical methods were applied to determine THg anomalies. Box plot method showed one extreme and three outliers in S1 at postmonsoon season. Two extremes were found at S2 at 4–8 and at 32–36 cm in premonsoon period. In S3 there was no anomaly by box plot method. MAD method was more sensitive than box plot method and THg anomaly was detected at 12–16 cm in S3 during postmonsoon season. The data reported are useful baselines for THg in Sunderban mangrove wetland, India and would be of help in future sediment quality studies.
机译:这是关于印度孟加拉湾东北部的桑德班红树林湿地核心沉积物(粒径<63μm)中总汞(T Hg )的初步报告。采用冷蒸气原子吸收光谱法(CVAAS)测定T Hg 。浓度范围从9.8到535.1 ppb(ngg -1 )。结果揭示了季风和季风后月份在不同核心深度的变化,以及位于三个河流站点(休利河(S 1 ),马特拉河(S 2 )和Bidyadhari河(S 3 )。在S 2 的岩心地下层(4–8 cm)中T Hg 的浓度升高归因于汞从较深沉积物(32–36 cm)中的迁移。总汞和粘土含量之间存在正相关关系。根据地质累积指数(I geo )和效应范围低(ER-L)值(150 ppb),目前认为沉积物尚未受到污染。结果,对生活在研究沉积物中的生物产生生态毒理学风险的可能性较小。采用两种统计方法确定T Hg 异常。箱形图法显示季风季节S 1 的一个极端和三个异常值。在季风期的S 2 在4-8和32-36 cm处发现了两个极端。 S 3 中的盒图法没有异常。季风季节,MAD方法比箱线图方法更敏感,在S 3 的12–16 cm处检测到T Hg 异常。所报告的数据是印度桑德班红树林湿地中T Hg 的有用基准,将有助于将来的沉积物质量研究。

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