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首页> 外文期刊>Geophysical Research Letters >Water flow and slip on NAPL-wetted surfaces of a parallel-walled fracture
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Water flow and slip on NAPL-wetted surfaces of a parallel-walled fracture

机译:平行壁裂缝在NAPL润湿的表面上的水流和滑动

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摘要

The effects of various wetting conditions and aperture sizes on water flow and slip in a parallel-walled fracture were investigated. Water flow experiments showed that a larger slip occurred as the surface became more hydrophobic. For a creosote-wetted surface of the fracture with an aperture of 508 mm, the increase in the water flow rate due to the slip was as much as 10.0% compared to that in a water-wetted surface. Similarly to a water-wetted surface, no slip took place at a gasoline-wetted surface, which was weakly hydrophobic. The slip lengths, a notional distance from the wall to a point inside the wall where fluid velocity extrapolates to zero, for light oil- and creosote-wetted surfaces were constant over a range of flow velocities in the laminar flow regime. The study indicates that no slip boundary condition-based equations are not adequate for quantifying water flow through NAPL-wetted fractures.
机译:研究了不同润湿条件和孔径大小对平行壁裂缝中水流和滑动的影响。水流实验表明,随着表面变得更疏水,发生了更大的滑移。对于开孔为508 mm的裂缝的经creosote润湿的表面,与在水润湿的表面中相比,由于滑移引起的水流速增加了10.0%。与水润湿的表面相似,在汽油润湿的疏水性较弱的表面上也没有发生打滑。滑移长度,即从壁到壁内流体速度外推至零的点的名义距离,对于轻油和杂酚油润湿的表面,在层流状态下的一定流速范围内是恒定的。研究表明,没有基于滑动边界条件的方程式不足以量化流经NAPL润湿裂缝的水流。

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