Method for controlling the trajectory of a hydraulic fracture in strata-containing natural fractures
a hydraulic fracture and strata-containing technology, applied in the direction of fluid removal, survey, borehole/well accessories, etc., can solve the problems of increasing the capital investment required for implementation of this method, the complexity of the criss-cross fracture network, and the inability of conventional tools intended for developing optimum hydraulic fracturing treatment strategies and based on planar distribution to produce the required effect when used, so as to achieve the effect of reducing the capital investment and improving efficiency and accuracy
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[0021]There are many factors that control the complexity of a hydraulic fracture geometry. In cases where the hydraulic fracture interacts with a bedding layer, a natural fracture, or a fractional fault (all of them being hereinafter referred to as the “interface”), the hydraulic fracture may expand right through the interface, may end at the interface, or may continue to propagate at a certain offset along the interface (FIG. 3).
[0022]The key parameters which control the selection of one of the possible fracture propagation paths listed above include, but are not limited to, the following: a fracturing fluid injection rate (Q); a fracturing fluid viscosity (μ); a remote stress difference (σ1-σ3); interface properties, such as a friction (σ), an adhesion (C), an angle of approach (β) of the hydraulic fracture to the interface, and a gap (d) between the nearest hydraulic fracture tip and the interface (FIG. 1).
[0023]FIG. 2 shows possible hydraulic fracture propagation paths in case w...
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