2D model of groundwater flow and total dissolved HCH transport through the Gállego alluvial aquifer downstream the Sardas landfill (Huesca, Spain)

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC
Brais Sobral , Javier Samper , Luis Montenegro , Alba Mon , Joaquín Guadaño , Jorge Gómez , Javier San Román , Felipe Delgado , Jesús Fernández
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引用次数: 0

Abstract

The organic pollutants disposed at the Sardas landfill in Sabiñánigo (Huesca, northeastern Spain) by the INQUINOSA lindane factory have reached the Gállego alluvial aquifer and could affect the Sabiñánigo reservoir. The daily oscillations of the reservoir water level produce a tidal effect on the piezometric heads of the aquifer. These oscillations are transmitted in a damped way with a time lag, thus attesting that the silting sediments of the reservoir and the natural silts of the Gállego alluvial are interposed between the reservoir water and the layer of sands and gravels. A 2D finite element groundwater flow and total dissolved hexachlorocyclohexane (HCH) transport model through the Gállego alluvial aquifer is presented here. The flow model was constructed to: (1) Quantify the tidal effect, produced by the daily fluctuations of the reservoir water level on the aquifer; (2) Estimate the hydrodynamic parameters of the layer of sands and gravels; and 3) Estimate the vertical hydraulic conductivity of the silting sediments and silts; and (4) Quantify aquifer/reservoir interactions. The flow model reproduces the dynamics of the tidal effect and attests that groundwater velocity and flow direction changes daily in response to the oscillations of the reservoir level. Model results reproduce the measured well hydrographs and the Darcy velocity derived from tracer tests and confirm the validity of the conceptual model. The transport model of total dissolved HCH simulates the time evolution of the contaminant plume. The computed concentrations of total dissolved HCH and the contaminant mass outflux are very sensitive to changes in the source terms and the distribution coefficient, Kd of HCH. The best fit to the measured HCH plumes in September 2010 and December 2020 is obtained with a Kd ranging from 1 to 3 L/kg. The computed flux of dissolved HCH leaving the Sardas site in 2020 towards the Sabiñánigo reservoir ranges from 0.6 kg/year for Kd = 3 L/kg to 3.1 kg/year for Kd = 1 L/kg. The findings of this study will be most useful for planning and designing remedial and containment actions at the Sardas site and other similar lindane-affected sites.

Abstract Image

通过 SARDAS 垃圾填埋场下游 GÁLLEGO 冲积含水层的地下水流和总溶解六氯环己烷迁移的二维模型(西班牙 HUESCA)
INQUINOSA 林丹工厂在 Sabiñánigo(西班牙韦斯卡省东北部)的 Sardas 垃圾填埋场排放的有机污染物已进入 Gállego 冲积含水层,并可能对 Sabiñánigo 水库造成影响。水库水位的日常波动对含水层的压水头产生潮汐效应。这些振荡以阻尼的方式传递,具有时间滞后性,从而证明水库的淤积沉积物和 Gállego 冲积层的天然淤泥介于水库水和砂砾石层之间。本文介绍了通过 Gállego 冲积含水层的二维有限元地下水流和总溶解六氯环己烷(HCH)迁移模型。建立流动模型的目的是(1) 量化水库水位每日波动对含水层产生的潮汐效应;(2) 估算砂砾石层的水动力参数;(3) 估算淤积沉积物和淤泥的垂直导水性;(4) 量化含水层与水库之间的相互作用。水流模型再现了潮汐效应的动态,并证明地下水的流速和流向每天都随着水库水位的波动而变化。模型结果再现了测井水文图和示踪试验得出的达西速度,证实了概念模型的有效性。总溶解六氯环己烷的迁移模型模拟了污染物羽流的时间演变。计算得出的总溶解六氯环己烷浓度和污染物质量流出量对六氯环己烷源项和分布系数 Kd 的变化非常敏感。2010 年 9 月和 2020 年 12 月测量的六氯环己烷羽流在 Kd 为 1 到 3 升/千克时拟合效果最佳。计算得出的 2020 年溶解的六氯环己烷从萨尔达斯地点流向萨比纳尼戈水库的流量范围为:Kd = 3 升/千克时为 0.6 千克/年,Kd = 1 升/千克时为 3.1 千克/年。这项研究的结果将对规划和设计萨达斯遗址和其他类似的受林丹影响遗址的补救和遏制行动非常有用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
7.20
自引率
4.30%
发文量
567
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