Evaluation of the Effects of Climate Change on Water Infiltration on Thickened Tailings in the Atacama Region

A. Arriagada, J. Riquelme, Tiaren García-Pérez
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Abstract

Chile is a country with high vulnerability associated with Climate Change, given among other factors, due to the need for development and growing social and environmental conflicts. This motivates the implementation of adaptation, transformation and mitigation measures at all aspects, to deal with climatological phenomena, which despite its future uncertainty, its development is a proven fact by robust and bulky scientific evidence. Motivated by the call from COP25 and the IPCC to assess adaptation and mitigation of effects and consequences of Climate Change, SRK Chile proposed to analyze the response of infrastructure associated with mining in northern Chile, considering General Circulation Models (GCM) downscaled for Atacama region at different elevations, based on the models considered by Chilean Water Directorate (DGA) in its Update of the National Water Balance of Chile (NWBC). This study considers Representative Concentration Pathways RCP 8.5 (most pessimistic scenario) as scenarios to evaluate, same as DGA – NWBC. To observe the effects of these scenarios we applied the GCM as boundary conditions in 1D numerical infiltration models using the software Hydrus. In the simulations water fluxes in a column of thickened tailing above natural soil is analyzed for different precipitation regimes from GCMs. Standard values according to our experience for the hydraulic and geometry properties of the materials forming the columns are used. The results of this study shed light upon the future precipitation’s scenarios affect the available water in the infrastructures at different elevations, providing a quantitative comparison of the infiltration fluxes within the tailing for the GCMs in the Atacama region.
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气候变化对阿塔卡马地区浓密尾砂入渗影响的评价
Chile是一个高度易受气候变化影响的国家,除其他因素外,由于发展的需要和日益增长的社会和环境冲突。这促使在各个方面实施适应、转变和缓解措施,以应对气候现象,尽管气候现象未来存在不确定性,但其发展已被有力和大量的科学证据证明是事实。在COP25和IPCC关于评估适应和减缓气候变化影响和后果的呼吁的推动下,SRK智利提出,在智利水务局(DGA)在其《智利国家水平衡更新》(NWBC)中考虑到阿塔卡马地区不同海拔高度的一般环流模式(GCM)的基础上,分析智利北部与采矿相关的基础设施的响应。本研究与DGA - NWBC一样,以代表性浓度路径RCP 8.5(最悲观情景)作为评估情景。为了观察这些情景的影响,我们利用Hydrus软件将GCM作为一维数值入渗模型的边界条件。在模拟中,分析了不同降水条件下自然土壤上浓密尾砂柱的水通量。根据我们的经验,对形成柱的材料的水力和几何特性使用标准值。本研究结果揭示了未来降水情景对不同海拔基础设施中有效水量的影响,为阿塔卡马地区gcm在尾砂中的入渗通量提供了定量比较。
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