Department of Civil and Environmental Engineering, University of California-Davis, One Shields Avenue, Davis, California 95616, USA.
J Contam Hydrol. 2011 Nov 1;126(3-4):235-47. doi: 10.1016/j.jconhyd.2011.08.006. Epub 2011 Aug 27.
A methyl tert-butyl ether (MTBE) / tert-butyl alcohol (TBA) plume originating from a gasoline spill in late 1994 at Vandenberg Air Force Base (VAFB) persisted for over 15 years within 200 feet of the original spill source. The plume persisted until 2010 despite excavation of the tanks and piping within months after the spill and excavations of additional contaminated sediments from the source area in 2007 and 2008. The probable history of MTBE concentrations along the plume centerline at its source was estimated using a wide variety of available information, including published details about the original spill, excavations and monitoring by VAFB consultants, and our own research data. Two-dimensional reactive transport simulations of MTBE along the plume centerline were conducted for a 20-year period following the spill. These analyses suggest that MTBE diffused from the thin anaerobic aquifer into the adjacent anaerobic silts and transformed to TBA in both aquifer and silt layers. The model reproduces the observation that after 2004 TBA was the dominant solute, diffusing back out of the silts into the aquifer and sustaining plume concentrations much longer than would have been the case in the absence of such diffusive exchange. Simulations also suggest that aerobic degradation of MTBE or TBA at the water table in the overlying silt layer significantly affected concentrations of MTBE and TBA by limiting the chemical mass available for back diffusion to the aquifer.
一个甲基叔丁基醚 (MTBE)/叔丁醇 (TBA) 羽流源于 1994 年底在范登堡空军基地 (VAFB) 的汽油泄漏,在最初泄漏源的 200 英尺范围内持续了超过 15 年。尽管在泄漏后数月内挖掘了储罐和管道,并在 2007 年和 2008 年从源区挖掘了更多受污染的沉积物,但羽流仍持续到 2010 年。使用各种可用信息,包括关于原始泄漏、VAFB 顾问进行的挖掘和监测以及我们自己的研究数据,估计了羽流中心线沿线 MTBE 浓度的可能历史。对泄漏后 20 年沿羽流中心线进行了 MTBE 的二维反应传输模拟。这些分析表明,MTBE 从稀薄的厌氧含水层扩散到相邻的厌氧淤泥中,并在含水层和淤泥层中转化为 TBA。该模型再现了这样一个观察结果,即在 2004 年后,TBA 是主要的溶质,从淤泥中扩散回含水层,并维持羽流浓度的时间远远长于没有这种扩散交换的情况。模拟还表明,上覆淤泥层中地下水位处 MTBE 或 TBA 的好氧降解通过限制可用于回扩散到含水层的化学物质质量,显著影响 MTBE 和 TBA 的浓度。