👉 The Paso Fluid, often referred to as the Paso de Fluxo or Flow Passage, is a concept in fluid dynamics that describes a specific type of flow pattern in porous media, such as soil or rock, where fluid movement is significantly influenced by the geometry and connectivity of the pore spaces. In this model, fluid flow occurs preferentially through interconnected pathways rather than randomly, leading to higher permeability in these preferred channels. This results in a more efficient and directed flow compared to isotropic flow, where fluid movement is uniform in all directions. The Paso Fluid concept is crucial for understanding and predicting fluid transport in natural systems like groundwater flow, oil recovery, and environmental processes.
