钻探废水污染的北极浅海沉积物中痕量金属的持久性

Elaine Snyder-Conn, David Densmore, Cathryn Moitoret, Jerald Stroebele
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引用次数: 10

摘要

海上石油勘探活动通常需要将钻井泥浆和地层岩屑排放到邻近水域或这些水域上方的冰上。尽管这些泥浆在中高能量的海洋环境中扩散有很好的记录,但在浅层、低能量的北极环境中,钻井泥浆的命运却很少受到关注。这项研究的重点是阿拉斯加波弗特海Stefansson海湾附近的三个钻井废水处理场。所有站点均位于浅水(小于5米)、低能海洋环境中。对钻井废水中常见的六种金属(铝、砷、钡、铬、铅和锌)的沉积物浓度进行了检测。从沿100米样带的重复抓取样本中获得的金属浓度与在四个浅水近海岛屿控制点采集的金属浓度以及其他研究的数据进行了比较。结果表明,在所有三个排放点的某些站点中,钡、铬、铅和锌持续存在,并且在排放后2-4年采样时,三个站点中有一个站点的铝浓度升高。当金属浓度升高时,通常在排放点附近最高,在风诱导的岸上运输方向继续,并且通常随着距离排放点的距离而减少。然而,分布显示出一些斑块性,表明冰载泥浆在当地融化,或水流或冰刨作用对沉积物进行了改造。需要进一步的工作来评估钻井废水的生物影响。然而,这些物质的缓慢扩散表明,有必要对波弗特海浅层低能量区域的钻井废水持久性问题进行更密切的评估。
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Persistence of trace metals in shallow arctic marine sediments contaminated by drilling effluents

Offshore oil exploration activity usually requires the discharge of drilling muds and formation cuttings into adjacent waters or on ice above these waters. Although dispersal of these muds is well documented in marine environments of moderate to high energy, the fate of drilling muds in shallow, low-energy Arctic environments has received little attention. This study focused on three drilling effluent disposal sites around Stefansson Sound in the Alaskan Beaufort Sea. All sites were in shallow (less than 5 m), low-energy marine environments. Sediment concentrations of six metals often present in drilling effluents (aluminum, arsenic, barium, chromium, lead and zinc) were examined. Metal concentrations obtained from replicate grab samples along 100 m transects were compared with those taken at four shallow-water offshore island control sites, and with data from other studies.

The results indicate persistence of barium, chromium, lead and zinc at certain stations at all three discharge sites, and elevated concentrations of aluminum at one of the three sites when sampled 2–4 years after the discharges. Metal concentrations, when elevated, were typically highest near the discharge points, continued in the direction of wind-induced longshore transport, and generally diminished with distance from the discharge site. However, distributions displayed some patchiness indicative of in place melting of ice-rafted muds or reworking of sediments by currents or icegouging.

Further work will be needed to evaluate the biological impacts of drilling effluents. However, the slow dispersal of these materials suggests there is a need for closer evaluation of drilling effluent persistence problems at shallow, lowenergy locations in the Beaufort Sea.

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