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Magnetic resonance imaging of nonaqueous phase liquid during soil vapor extraction in heterogeneous porous media

机译:非均相多孔介质中土壤水汽萃取过程中非水相液体的磁共振成像

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Soil vapor extraction (SVE) is commonly used to remediate nonaqueous phase liquids (NAPLs) from the vadose zone. This paper aims to determine the effect of grain size heterogeneity on the removal of NAPL in porous media during SVE. Magnetic resonance imaging (MRI) was used to observe and quantify the amount and location of NAPL in flow-through columns filled with silica gel grains. MRI is unique because it is nondestructive, allowing three-dimensional images to be taken of the phases as a function of space and time. Columns were packed with silica gel in three ways: coarse grains (250-550 μm) only, fine grains (32-63 μm) only, and a core of fine grains surrounded by a shell of coarse grains. Columns saturated with water were drained under a constant suction head, contaminated with decane, and then drained to different decane saturations. Each column was then continuously purged with water-saturated nitrogen gas and images were taken intermittently. Results showed that at residual saturation, a sharp volatilization front moved through the columns filled with either coarse-grain or fine-grain silica gel. In the heterogeneous columns, the volatilization front in the core lagged just behind the shell because gas flow was greater through the shell and decane in the core diffused outward to the shell. When decane saturation in the core was above residual saturation, decane volatilization occurred near the inlet, the relative decane saturation throughout the core dropped uniformly, and decane in the core flowed in the liquid phase to the shell to replenish volatilized decane. These results indicate that NAPL trapped in low-permeability zones can flow to replenish areas where NAPL is lost due to SVE. However, when residual NAPL saturation is reached, NAPL flow no longer occurs and diffusion limits removal from low-permeability zones.
机译:土壤蒸气提取(SVE)通常用于补救渗流带中的非水相液体(NAPL)。本文旨在确定粒度异质性对SVE过程中多孔介质中NAPL去除的影响。磁共振成像(MRI)用于观察和定量NAPL在充满硅胶颗粒的流通柱中的数量和位置。 MRI的独特之处在于它是无损的,因此可以根据空间和时间获取相位的三维图像。色谱柱以三种方式用硅胶填充:仅粗颗粒(250-550μm),仅细颗粒(32-63μm)和由粗颗粒壳包围的细颗粒核。用水饱和的色谱柱在恒定的吸头下排出,被癸烷污染,然后排出至不同的癸烷饱和度。然后用饱和水的氮气连续吹扫每个柱,并间歇地拍摄图像。结果表明,在残留饱和度下,急剧的挥发前沿穿过填充有粗粒硅胶或细粒硅胶的色谱柱。在非均相塔中,核中的挥发前沿滞后于壳的后面,因为气体通过壳的流量更大,并且核中的癸烷向外扩散至壳。当岩心中的癸烷饱和度高于残留饱和度时,入口附近会发生癸烷挥发,整个岩心中的相对癸烷饱和度会均匀下降,并且岩心中的癸烷会以液相形式流到壳层,以补充挥发的癸烷。这些结果表明,困在低渗透区内的NAPL可以流向补充由于SVE而导致NAPL损失的区域。但是,当达到残留的NAPL饱和度时,NAPL流量将不再发生,并且扩散会限制从低渗透率区域的去除。

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