论文标题
Vuggy媒体的毛细管上升
Capillary rise in vuggy media
论文作者
论文摘要
碳酸盐是高度异质的地层,孔径分布和孔隙空间拓扑的变化很大,从而导致复杂的多相流动行为。在这里,我们研究了液体中流体的自发吸收行为。直径为1.0毫米的玻璃珠,具有溶解的夹杂物,被烧结,形成多种构型的异质性vuggy核心,具有矩阵孔隙率,VUG尺寸,VUG空间位置和VUG数量的变化。核心制造过程是可重复的,并允许以受控方式研究VUG纹理特性的影响。 毛细血管上升实验是在这些代理碳酸盐核心中进行的,并与均匀的非和胃核作为参考进行了比较。进行连续的光学成像以跟踪芯中空气水界面的位置。为了了解在存在VUG的情况下毛细血管高度的变化,在一组连接和断开的管子中进行了流体量的两相数值模拟。最后,进行了X射线层析成像扫描,以识别一些核心中空气水接口的形状。 结果可以概括如下:与非野合多孔介质相比,断开的VUG导致毛细管上升更高。 VUG充当毛细管屏障,将流体流动到相邻连接的通道,最终导致总体毛细管上升较高。 这项工作的结果表明,水相的自发入侵半径(例如断裂液和危险废物)受到孔隙孔隙率的影响,但不受其分布的影响。
Carbonates are highly heterogeneous formations with large variations in pore size distribution and pore space topology, which results in complex multiphase flow behavior. Here we investigate the spontaneous imbibition behavior of fluids in vuggy carbonates. Glass beads of 1.0 mm diameter, with dissolvable inclusions, are sintered to form multiple configurations of heterogeneous vuggy core with variations in matrix porosity, vug size, vug spatial location, and number of vugs. The core fabrication process is repeatable and allows the impact of vug textural properties to be investigated in a controlled manner. Capillary rise experiments are conducted in these proxy vuggy carbonate core and compared with the homogeneous non-vuggy core as reference. Continuous optical imaging is performed to track the position of the air-water interface in the cores. To understand the change in capillary height in the presence of a vug, a volume-of-fluid two-phase numerical simulation is performed in a parallel set of connected and disconnected tubes. Finally x-ray tomography scans are performed to identify the shape of the air-water interface in a select few cores. The results can be summarized as follows: disconnected vugs result in higher capillary rise compared to non-vuggy porous media. The vugs act as capillary barriers, diverting fluid flow to the adjacent connected channels, which ultimately results in a higher overall capillary rise. The results of this work highlight that radius of spontaneous invasion of aqueous phases, such as fracture fluid and hazardous wastes, are affected by vug porosity but not their distribution.