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回溯建模以定位沿印度西海岸沉积的焦油球的起源。

Backtrack modeling to locate the origin of tar balls depositing along the west coast of India.

机构信息

CSIR-National Institute of Oceanography, Dona Paula, Goa 403004, India.

e-geos/ASI-Telespazio, via Tiburtina 965, 00156 Roma, Italy.

出版信息

Sci Total Environ. 2016 Nov 1;569-570:31-39. doi: 10.1016/j.scitotenv.2016.06.101. Epub 2016 Jun 18.

DOI:10.1016/j.scitotenv.2016.06.101
PMID:27328397
Abstract

Tar ball (TB) deposition along the West Coast of India (WCI) is a common phenomenon during the southwest monsoon season, particularly along the coast of Goa and Gujarat, and it is a major concern to the stake holders. Our earlier studies showed that the source oil for the TBs deposited on the Goa coast in August 2010 is the tanker wash, and the source for subsequent TBs deposited on the Gujarat coast during July 2012 and June 2013 and Goa coast in May 2013 is from Bombay High (BH) oil fields. In the present study, the TBs that were deposited during May 2013 and May 2014 on the Goa coast were backtracked through a trajectory model, primarily to simulate their pathways and identify the reason for the occurrence of TBs only in May, and eventually to identify the origin and the source. The backtracking results re-confirmed that the TBs deposited in 2010 were originated from the tanker routes and that of both 2013 and 2014 TBs from the BH oil fields. The climatology of wind and surface circulation showed that the TBs deposited on the Goa coast during May/June only are from the oil fields and those during August from the tanker route. The results of backtracking simulations showed that the residence time of the oil residues/TBs is approximately 22days for August 2010 TBs, ≈30days for May 2013 TBs and 65days for May 2014 TBs. The residence time (in water) of TBs that deposit (on the coast) in the month of May could be as much as 7months, and could be around one month if deposit in August, primarily because of winds and hydrodynamic conditions of the Arabian Sea.

摘要

在印度西海岸(WCI),西南季风季节经常出现焦油球(TB)沉积现象,尤其是在果阿和古吉拉特邦的海岸线上,这是利益相关者关注的主要问题。我们之前的研究表明,2010 年 8 月沉积在果阿海岸的 TB 的源油是油轮冲洗水,而随后在 2012 年 7 月和 2013 年 6 月沉积在古吉拉特邦海岸以及 2013 年 5 月沉积在果阿海岸的 TB 的源油来自孟买高地(BH)油田。在本研究中,通过轨迹模型回溯了 2013 年 5 月和 2014 年 5 月沉积在果阿海岸的 TB,主要是为了模拟它们的路径,确定仅在 5 月出现 TB 的原因,并最终确定它们的起源和来源。回溯结果再次证实,2010 年沉积的 TB 来自油轮航线,2013 年和 2014 年的 TB 都来自 BH 油田。风和表面环流的气候学表明,5 月/6 月仅沉积在果阿海岸的 TB 来自油田,而 8 月的 TB 来自油轮航线。回溯模拟结果表明,2010 年 8 月 TB 的油残留物/TB 的停留时间约为 22 天,2013 年 5 月 TB 的停留时间约为 30 天,2014 年 5 月 TB 的停留时间约为 65 天。5 月沉积(在海岸上)的 TB 在水中的停留时间可能长达 7 个月,如果在 8 月沉积,停留时间可能约为 1 个月,这主要是由于阿拉伯海的风和水动力条件。

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