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Estimating the change of porosity in the saturated zone during air sparging

机译:估算空气喷射过程中饱和区的孔隙度变化

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Air sparging is a remedial method for groundwater. The remedial region is similar to the air flow region in the saturated zone. If soil particles are transported during air sparging, the porosity distributions in the saturated zone change, which may alter the flow path of the air. To understand better the particle movement, this study performed a sandbox test to estimate the soil porosity change during air sparging. A clear fracture was formed and the phenomenon of particle movement was observed when the air injection was started. The moved sand filled the porous around the fracture and the reparked sand filled the fracture, reducing the porosity around the fracture. The results obtained from the photographs of the sandbox, the current measurements and the direct sand sample measurements were close to each other and are credible. Therefore, air injection during air sparging causes sand particle movement of sand, altering the characteristic of the sand matrix and the air distribution.
机译:空气喷射是对地下水的一种补救方法。补救区域类似于饱和区域中的气流区域。如果在空气喷射过程中运输了土壤颗粒,则饱和区中的孔隙度分布会发生变化,这可能会改变空气的流动路径。为了更好地了解颗粒的运动,本研究进行了沙箱测试,以估算鼓入空气期间土壤孔隙率的变化。开始注入空气后,形成了清晰的裂缝并观察到了颗粒运动的现象。移动的沙子填充了裂缝周围的孔隙,而重新沉积的沙子填充了裂缝,从而降低了裂缝周围的孔隙率。从沙盒的照片,电流测量值和直接砂样测量值获得的结果彼此接近且可信。因此,在空气喷射过程中注入空气会引起沙子的沙粒运动,从而改变沙基质的特性和空气分布。

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