توصيفگر ها :
شكستگي سنگي زبر , تك شكستگي , شكستگي متقاطع , جريان سيال , روش حجم محدود , مدلسازي فيزيكي و عددي
چكيده انگليسي :
Fluid flow in rock fractures, as one of the most important hydrogeological phenomena, plays a determining role in subsurface engineering applications, including geothermal energy systems, groundwater resource management, carbon storage, in-situ mining, and prediction of induced earthquakes. Mining and tectonic activities alter stress equilibrium and fracture geometry, directly impacting hydraulic behavior, flow distribution, and preferential fluid pathways. The geometric complexity of natural fractures—including surface roughness, variable apertures, contact points, and multiple intersections—imposes serious limitations on simplified models such as the cubic law and Darcyʹs law. This study aims to achieve a deeper understanding of fluid flow dynamics in rough and intersecting rock fractures by employing a comprehensive combination of physical, numerical, and machine learning approaches. In this study, a novel method for producing artificial fracture physical samples was first developed, based on the integration of 3D printing technology, photogrammetry, and concrete casting. This method enables the production of repeatable samples with precise control over geometric parameters. evaluation of the quality of produced samples using the Joint Roughness Coefficient index and advanced statistical parameters demonstrated a suitable match between artificial and real samples. Numerical modeling was performed based on the precise solution of the Navier-Stokes equations using a developed code. Comprehensive validation of numerical models with laboratory data for geometries with varying degrees of roughness showed high agreement. The design of laboratory equipment ensured boundary conditions identical to those in numerical simulations. Extensive parametric studies on single fractures revealed that increasing the fracture scale reduces the effect of roughness on outlet flow rate. The transition of the flow regime from linear Darcy to nonlinear Forchheimer was identified using the critical Reynolds number, which is highly dependent on roughness, dimensions, and fracture aperture. Results indicated that the equivalent hydraulic aperture is always less than the physical aperture, and relative permeability decreases with increasing Reynolds number. For the first time, a new sigmoidal relationship was developed to describe relative permeability as a function of Reynolds number, which accurately combines linear and nonlinear behaviors. Using design of experiments and machine learning algorithms, high-accuracy predictive models for flow rate and hydraulic aperture were developed. Analysis of intersecting fractures showed that geometric parameters such as intersection angle, intersection location, fracture length, and surface roughness have significant effects on flow distribution and permeability. Larger intersection angles led to reduced mixing and permeability, while increasing fracture length facilitated flow. Studies on multiple intersecting fractures, by comparing regular, irregular, and scaffold geometries, demonstrated that increasing network complexity has a significant impact on velocity patterns, fluctuations, and vorticity. In regular geometries, increasing the number of fractures led to reduced fluctuations and greater flow stability, whereas in irregular geometries, geometric complexities remained dominant. The results of this research, by providing new empirical relationships, machine learning models, and better understanding of physical mechanisms, offer practical tools for the design and optimization of engineering systems related to fractured rock environments.