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   hydraulic fracture propagation: analytical solutions versus lattice simulations  
   
نویسنده bakhshi e. ,rasouli v. ,ghorbani a. ,fatehi marji m.
منبع journal of mining and environment - 2019 - دوره : 10 - شماره : 2 - صفحه:451 -464
چکیده    In this work, we used a grainbased numerical model based on the concept of lattice. the modelling was done to simulate the lab experiments carried out on the mortar samples. also the analytical solutions corresponding to the viscositydominated regime were used to estimate the fracture length and width, and the results obtained were compared with the numerical simulations. as the analytical solutions are proposed for a pennyshaped fracture with no presence of any obstacle such as natural interfaces, in this work, we presented the results of lattice simulations for hydraulic fracturing in the cement sample, similar to the lab, but with no natural fractures, and compared the results obtained with analytical solutions. the results indicated that in the case of a continuous medium, the analytical solutions may present a reasonable estimation of the fracture geometry. also the viscositydominated leakoff model showed a better match between the analytical solutions and the numerical simulation results, confirmed by observing fluid loss into the sample in the lab postexperiment. in the case of assuming leakoff, the results indicated that the fracture width and length would reduce. however, it should be noted that in real cases, rock formations exhibit fractures and inhomogeneity at different scales so that the applications of the analytical solutions are limited.
کلیدواژه hydraulic fracturing propagation ,lattice ,numerical simulations ,analytical solutions
آدرس yazd university, department of mining and metallurgical engineering, iran, university of north dakota, department of petroleum engineering, usa, yazd university, department of mining and metallurgical engineering, iran, yazd university, department of mining and metallurgical engineering, iran
پست الکترونیکی mohammad.fatehi@gmail.com
 
     
   
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