Middle East Technical University, Department of Environmental Engineering, Dumlupınar Bulvarı No: 1, 06800 Ankara, Turkey.
J Contam Hydrol. 2013 Jul;150:77-92. doi: 10.1016/j.jconhyd.2013.02.010. Epub 2013 Mar 5.
The August 1999 earthquake in Turkey damaged three acrylonitrile (AN) storage tanks at a plant producing synthetic fiber by polymerization. A numerical modeling study was carried out to analyze the groundwater flow and contaminant (AN) transport at the spill site. This study presents the application of a numerical groundwater model to determine the hydrogeological parameters of the site, where such data were not available during the field surveys prior to the simulation studies. The two- and three-dimensional transient flow and transport models were first calibrated using the first 266days of observed head and concentration data and then verified using the remaining 540-day observed data set. Off-site migration of the contaminant plume was kept under control within the site boundaries owing to the favorable geology of the site, the characteristics of the local groundwater flow regime and the pumping operations. As expected, the applied pump-and-treat system was effective at high-permeability zones, but not fully effective at low-permeability zones. The results of long-term simulations for unconfined aquifer showed that the size of the plume in the high permeability zone shrank significantly due to the dilution by natural recharge. However, in the low permeability zone, it was not significantly affected. The study showed that accurate and sufficient data regarding the source characteristics, concentration and groundwater level measurements, groundwater pumping rates and their durations at each of the extraction points involved in the pump-and-treat system along with the hydrogeological site characterization are the key parameters for successful flow and transport model calibrations.
1999 年 8 月,土耳其发生地震,导致一家生产合成纤维的工厂的三个丙烯腈(AN)储存罐受损。为了分析泄漏点的地下水流动和污染物(AN)迁移情况,进行了数值建模研究。本研究介绍了数值地下水模型在确定现场水文地质参数中的应用,在进行模拟研究之前的实地调查中,这些数据无法获得。首先,使用前 266 天的水头和浓度观测数据对二维和三维瞬态流动和传输模型进行了校准,然后使用剩余的 540 天观测数据集进行了验证。由于场地地质条件有利、局部地下水流动特征和抽水作业,污染物羽流的场外迁移被控制在场地边界内。不出所料,所采用的抽吸处理系统在高渗透带是有效的,但在低渗透带效果并不完全理想。无压含水层的长期模拟结果表明,由于天然补给的稀释作用,高渗透带羽流的规模显著缩小。然而,在低渗透带,它并没有受到显著影响。研究表明,成功的流动和传输模型校准的关键参数包括与抽吸处理系统相关的每个抽提点的源特征、浓度和地下水位测量、地下水抽提率及其持续时间的准确而充分的数据,以及水文地质场地特征描述。