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Weathering of Oil Spills Under Arctic Conditions: Field Experiments with Different Ice Conditions Followed by In-Situ Burning

机译:北极条件下的漏油风化:野外实验,具有不同的冰条件,然后是原位燃烧

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The knowledge regarding weathering processes in Arctic oil spills and especially with the presence of ice is limited. Experimental studies have been performed in laboratories, but only to a limited degree in the field. This presentation summarized and compared results from field experiments performed in Norway in 1989, 1993 and 2003–2006. Two full-scale field measurements from experimental oil releases in Norway are initially used to compare the behavior of oil spilled in open water and in an Arctic broken ice scenario. Similar oil types and amounts (25–30 m3) were used in an experimental oil release in open water at Haltenbanken (65° N) in 1989 and in dynamic broken ice at Svalbard (75° N) in 1993. Results from small-scale field experiments performed later (2003–2006) on Svalbard are also discussed and compared to the earlier field data. Several weathering properties for the oil spill in broken ice are strongly influenced by the low temperature, reduced oil spreading and reduced wave action caused by the high ice coverage. Reduced water uptake, viscosity, evaporation and pour point extend the operational time window for several contingency methods compared to oil spills in open waters. This could open up for dispersant treatment and in-situ burning even after an extended period of weathering for an oil spill in broken ice. In the period of 2003–2006, SINTEF and the University Centre in Svalbard (UNIS), and later also co-workers from US (DF Dickins and Boise State University) have performed field weathering studies with oil entrapped in and under ice followed with in-situ burning. This presentation will present recent results from these field experiments regarding oil weathering under different ice conditions (slush ice, 30% and 90% ice coverage) and the consequences for the ignitability and in-situ burning of the weathered oil. This research has been funded by Norwegian and US authorities (the Norwegian Research council and US Mineral Management Services) and several oil and industry companies (Statoil, Norsk Hydro, Shell, Alaska Clean Seas, ExxonMobile, ConnocoPhillips and Store Norske Spitsbergen kullkompani).
机译:关于北极油泄漏的风化过程的知识,特别是冰的存在是有限的。实验研究已经在实验室进行,但仅在该领域的有限程度上进行。本介绍总结了1989年,1993年和2003 - 2006年在挪威进行的现场实验的结果。挪威实验油释放的两个全规模场测量最初用于比较溢出在开放水中的油的行为和北极破碎的冰场。在1989年,在哈尔滕库纳伦(65°N)的开放水中的实验油释放中使用了类似的油类型和量(25-30平方米),并在1993年在Svalbard(75°N)的动态破冰中。来自小规模的结果还讨论了在斯瓦尔巴特稍后(2003-2006)上进行的现场实验,并与早期的现场数据进行了讨论。破碎冰中的漏油泄漏的几种风化性能受到高温,减少的高冰覆盖引起的低温,降低的油蔓延和减少波动的影响。与开阔水域中的漏油相比,降低水吸收,粘度,蒸发和倾点扩展了几种应急方法的操作时间窗。即使在破碎的冰中的漏油泄漏的昂清风气之后,这也可以开辟分散剂处理和原位燃烧。在2003 - 2006年期间,辛特夫和斯瓦尔巴德(UNIS)的大学中心,后来也有来自美国(DF DICKINS和BOISE州立大学)的同事,已经进行了现场风化的研究,用夹在冰上陷入困境-situ燃烧。该介绍将在不同冰条件下的这些现场实验(浸泡冰,30%和90%的冰盖)下的这些现场实验的最新结果以及对风化油的可燃性和原位燃烧的后果。该研究得到了挪威和美国当局(挪威研究理事会和美国矿产管理服务)和几家石油和工业公司(Statoil,Norsk Hydro,Shell,阿拉斯加干净的海洋,埃克森省,Connocophillips和Store Norske Spitsbergen Kullkompani)资助。

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