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The effect of dissolved gas on rock desaturation in artificial openings in geological formations

机译:溶解气对地质形成中人造开口岩岩去饱和的影响

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The construction and operation of geological repositories require excavation and ventilation of galleries,with significant groundwater drainage.Desaturation of rock around galleries is unavoidable and may affect hydraulic properties and redox conditions.This study used numerical modeling to assess the influence of dissolved gas on the degree of saturation of rock surrounding excavated galleries,focusing on siliceous mudstone rock in the 140 m,250 m,and 350-m-deep galleries of the Horonobe Underground Research Laboratory,Japan.A previous in situ electrical resistivity survey indicated that the degree of saturation in the 250 m gallery was higher than that in the 140 m and 350 m galleries.In the Horonobe area,deep groundwater contains high concentrations of dissolved methane,and exsolution of this methane from pore water can affect desaturation.Simple numerical modeling,including simulation of multiphase flows,was undertaken for each gallery to confirm the effect of dissolved gas and rock permeability on desaturation.A sensitivity analysis was performed by varying dissolved gas contents and permeability.Results indicate that the dissolved gas content affects both the degree of saturation and its spatial extent,whereas rock permeability affects only the latter.Higher dissolved gas concentrations result in lower degrees of saturation with a greater spatial extent of desaturation,and higher permeability leads to greater extents of desaturation.It is therefore likely that gas content,rather than rock permeability,caused the observed variations in electrical resistivity.
机译:地质储存库的建设和运营需要挖掘和通风画廊,具有显着的地下水排放。围绕画廊的岩石的饱和度是不可避免的,可能影响液压性能和氧化还原条件。使用数值模拟来评估溶解气对程度的影响岩石周围挖掘画廊的饱和度,专注于硅石泥岩岩石在140米,250米和350-M-深的Horonobe地下研究实验室,日本。之前的原位电阻率调查表明饱和度在250米的画廊中高于140米和350米画廊。在Horonobe区域,深层地下水含有高浓度的溶解甲烷,并且该甲烷来自孔隙水的exolution可以影响去饱和。数值模拟,包括模拟对于每个画廊进行多相流动,以确认溶解气体和ROC的效果K渗透性在去饱和下。通过改变溶解的气体含量和渗透性进行敏感性分析。结果表明溶解气体含量影响饱和度及其空间程度,而岩石渗透性仅影响后者。高溶解气体浓度导致具有更高的饱和度,具有更大的去饱和空间程度,并且较高的渗透性导致去饱和的更大范围。因此,可能是气体含量,而不是岩石渗透性,导致观察到的电阻率变化。

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