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溢油 19 年后残留原油的可生物降解性。

Biodegradability of lingering crude oil 19 years after the Exxon Valdez oil spill.

机构信息

US Environmental Protection Agency, Cincinnati, Ohio 45268, USA.

出版信息

Environ Sci Technol. 2010 Oct 1;44(19):7613-21. doi: 10.1021/es101042h.

Abstract

In 2001 and 2003, geospatial surveys of lingering oil were conducted in Prince William Sound (PWS) resulting in a prediction of significant acreage being contaminated with substantial subsurface oil from the 1989 Exxon Valdez oil spill (EVOS). In 2007, other researchers developed a mass weathering index (MWI) based on the degree of weathering of PAHs normalized to conserved biomarkers: if the degree of weathering of oil is 70% or more, further attempts at bioremediation would be unjustified. The objective of our study was to measure the biodegradability of the 19-year lingering oil in laboratory microcosms. Samples of beach substrate were collected from representative sites in PWS contaminated with oil residues of varying weathering states according to the MWI model. Enough sacrificial microcosms were set up to accommodate two treatments for each site (natural attenuation and biostimulation). Results indicated that lingering oil is biodegradable. Nutrient addition stimulated biodegradation compared to natural attenuation in all treatments regardless of the degree of weathering. The most weathered oil according to the MWI was the most biodegradable. Substantial biodegradation occurred in the natural attenuation microcosms due to the high sediment Total Kjeldahl Nitrogen (TKN), which served as a nitrogen source for biodegradation. Most of the observed biodegradation was due to the presence of dissolved oxygen. Nitrogen was a limiting factor but oxygen was the predominant one.

摘要

2001 年和 2003 年,在威廉王子湾(PWS)进行了 lingering oil 的地理空间调查,预测有大片土地受到了 1989 年埃克森瓦尔迪兹号溢油事件(EVOS)的大量地下石油污染。2007 年,其他研究人员根据多环芳烃风化程度归一化为保守生物标志物,开发了一个质量风化指数(MWI):如果石油风化程度达到 70%或更高,进一步的生物修复尝试将是不合理的。我们的研究目的是在实验室微环境中测量 19 年 lingering oil 的生物降解性。根据 MWI 模型,从 PWS 受不同风化状态油残留污染的代表性地点采集海滩基质样本。为每个地点(自然衰减和生物刺激)设置了足够的牺牲性微环境,以容纳两种处理。结果表明,残留油是可生物降解的。与自然衰减相比,营养物质的添加刺激了所有处理中的生物降解,无论风化程度如何。根据 MWI,最风化的油是最可生物降解的。由于沉积物总凯氏氮(TKN)较高,自然衰减微环境中发生了大量生物降解,TKN 是生物降解的氮源。大部分观察到的生物降解归因于溶解氧的存在。氮是限制因素,但氧是主要因素。

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