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Monomethylmercury concentrations on the eastern Texas-Louisiana shelf during the formation, peak, and disappearance of hypoxia

机译:在低氧的形成,峰值和消失过程中,东德克萨斯-路易斯安那架子上的单甲基汞浓度

摘要

A study of monomethylmercury (MMHg) concentrations in the water and sediment ofthe hypoxic zone in the northeastern Gulf of Mexico was conducted on several cruisesbetween April 2004 and May 2005. Surface water MMHg concentrations were low andconstant throughout the sampling period. Bottom water concentrations displayed aseasonal trend: maximum MMHg concentrations were in June/July 2004, decreased to aminimum in October 2004, and in May 2005 concentrations had begun to increase.MMHg concentrations and MMHg as a percent of THg in surface sediment (0-2 cm)also followed this trend. Bottom water dissolved oxygen and temperature displayedinverse relationships with bottom water MMHg concentrations. This correlation betweendissolved oxygen and MMHg is typical for low-oxygen waters, but the relationshipbetween temperature and MMHg is relatively unique. A possible explanation is thatwarmer summer temperatures inhibited bacterial methylation. Stratification intensity(quantified as N2) was strongly correlated with bottom water MMHg concentrations,indicating either increased methylation at the pycnocline or that the pycnocline inhibitedvertical mixing, thus limiting MMHg to the bottom water. Benthic flux estimationsindicate that sediment release of MMHg could be a significant source of MMHg tobottom water. The presence of an oxygenated layer in the surface sediment could haveplayed a role in inhibiting MMHg flux during oxic conditions; a decrease in thethickness of this layer under hypoxic conditions likely allowed MMHg to diffuse into thebottom water. Dissolved oxygen seemed to play an important role in controllingsediment MMHg concentrations with highest methylation rates in sediment underhypoxic water. Overall, sites closest to the Mississippi River mouth displayed the highest MMHg concentrations. Further research will need to be done in this area to fullycharacterize the relationship between biogeochemical parameters and MMHgconcentrations.
机译:在2004年4月至2005年5月的几次航行中,对墨西哥东北海湾缺氧区的水和沉积物中的单甲基汞(MMHg)浓度进行了研究。在整个采样期间,地表水MMHg浓度较低且恒定。底部水浓度呈季节变化趋势:MMHg最高浓度在2004年6月/ 7月,在2004年10月降至最低,2005年5月浓度开始增加.MMHg浓度和MMHg占表层沉积物中THg的百分比(0-2厘米)也遵循了这一趋势。底水中溶解氧和温度与底水中MMHg浓度呈反比关系。对于低氧水,溶解氧与MMHg之间的这种关系是典型的,但温度与MMHg之间的关系相对独特。一个可能的解释是夏天的高温抑制了细菌的甲基化。分层强度(量化为N2)与底水MMHg浓度密切相关,表明在比浓可可林甲基化增加或比浓可可林抑制了垂直混合,从而将MMHg限制在底水中。底栖通量估算表明,MMHg的沉积物释放可能是MMHg向底水的重要来源。在有氧条件下,表面沉积物中氧化层的存在可能起到了抑制MMHg通量的作用。在低氧条件下该层厚度的降低可能使MMHg扩散到底部水中。溶解氧似乎在控制沉积物在低氧水中的甲基化率最高的MMHg浓度中起着重要作用。总体而言,最靠近密西西比河河口的站点显示出最高的MMHg浓度。为了充分表征生物地球化学参数与MMHg浓度之间的关系,将需要在这一领域进行进一步的研究。

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    Keach Sara Elizabeth;

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  • 年度 2007
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