System and Methods for Controlled Fracturing in Formations
First Claim
1. A method of generating fractures in geologic formation, the method comprising:
- providing a plurality of boreholes in the formation;
placing a plurality of electrodes in the boreholes with one electrode per borehole, with the plurality of electrodes defining a fracture pattern for the geologic formation;
applying a sufficient amount of energy to the electrodes to generate a least a conductive channel between a pair of electrodes, wherein the conductivity in the channel between the pair of electrodes is defined has a ratio of final to initial channel conductivity of 10;
1 to 50,000;
1; and
applying electrical impulses to the electrodes, the electrical impulses having a voltage output ranging from 100-2000 kV, an energy output of 10-1000 kJ, wherein the pulses have a rise time ranging from 0.05-500 microseconds and a half-value time of 50-5000 microseconds;
wherein the application of the electrical pulses generates multiple fractures within and about the conductive channel by disintegration of minerals and pyrolysis of organic materials in the formation.
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Abstract
Controlled fracturing in geologic formations is carried out in a method employing a combination of alternating and impulsive current waveforms, applied in succession to achieve extensive fracturing and disintegration of rock materials for liquid and gas recovery. In a pre-conditioning step, high voltage discharges and optionally with highly ionizable gas injections are applied to a system of borehole electrodes, causing the formation to fracture with disintegration in multiple directions but confined between the locations of electrode pairs of opposite polarity. After pre-conditioning, intense current waveform of pulse energy is then applied to the system of borehole electrodes to create waves of ionization or shock waves with bubbles of heated gas that propagate inside and outside the high conductivity channels, resulting in rock disintegration with attendant large scale multiple fracturing.
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Citations
36 Claims
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1. A method of generating fractures in geologic formation, the method comprising:
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providing a plurality of boreholes in the formation; placing a plurality of electrodes in the boreholes with one electrode per borehole, with the plurality of electrodes defining a fracture pattern for the geologic formation; applying a sufficient amount of energy to the electrodes to generate a least a conductive channel between a pair of electrodes, wherein the conductivity in the channel between the pair of electrodes is defined has a ratio of final to initial channel conductivity of 10;
1 to 50,000;
1; andapplying electrical impulses to the electrodes, the electrical impulses having a voltage output ranging from 100-2000 kV, an energy output of 10-1000 kJ, wherein the pulses have a rise time ranging from 0.05-500 microseconds and a half-value time of 50-5000 microseconds; wherein the application of the electrical pulses generates multiple fractures within and about the conductive channel by disintegration of minerals and pyrolysis of organic materials in the formation. - View Dependent Claims (2, 3, 4, 5, 6, 7, 8, 9, 10, 15, 16, 17, 18, 19, 20, 21, 22, 23, 24, 25, 26, 27, 28, 30, 31, 32, 33, 34, 35, 36)
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- 11. The method of claim 11, wherein the voltage waveform has a frequency spectrum coinciding with a Cole-Cole plots for complex dielectric constant and Smith Chart plots for complex impedance.
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29. A method of generating fractures in a formation containing connate water, the method comprising:
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providing a plurality of boreholes in the formation; placing a plurality of electrodes in the boreholes with one electrode per borehole, with the plurality of electrodes defining a fracture pattern for the geologic formation; applying a sufficient amount of energy to the electrodes to heat the connate water in the formation to any of subcritical condition or supercritical condition; and applying electrical impulses having a voltage output ranging from 100-2000 kV, an energy output of 10-1000 kJ, wherein the pulses have a rise time ranging from 0.05-500 microseconds and a half-value time of 50-5000 microseconds; wherein the application of the electrical pulses generates allow plasma shock waves in the water creating multiple fractures in the formation.
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Specification