Case Histories: Damage Preventions by Leakoff Control of Fracturing Fluids in Appalachian Gas Reservoirs

Author(s):  
Javad Paktinat ◽  
Curtis Williams ◽  
Joseph Allen Pinkhouse ◽  
Gary Allen Clark ◽  
Glenn S. Penny
1990 ◽  
Author(s):  
T.A. Juranek ◽  
M.T. Llewellyn ◽  
G.P. Drescher ◽  
H.C. Tan ◽  
J.M. McGowen

2003 ◽  
Author(s):  
Ruyan Sheng ◽  
Zhenquan Li ◽  
Hua Liu ◽  
Xiyong Xiang

2019 ◽  
Vol 62 ◽  
pp. 302-313 ◽  
Author(s):  
Bo Yang ◽  
Jinzhou Zhao ◽  
Jincheng Mao ◽  
Hongzhong Tan ◽  
Yang Zhang ◽  
...  

2005 ◽  
Author(s):  
Javad Paktinat ◽  
Joseph Allen Pinkhouse ◽  
William P. Stoner ◽  
Curtis Williams ◽  
Gregory Alden Carder ◽  
...  

2005 ◽  
Author(s):  
Jorge A. Arevalo Villagran ◽  
Teodulo Gutierrez Acosta ◽  
Nestor Martinez Romero

2006 ◽  
Author(s):  
R.S. Taylor ◽  
R.S. Lestz ◽  
L. Wilson ◽  
G.P. Funkhouser ◽  
H. Watkins ◽  
...  

Geophysics ◽  
2016 ◽  
Vol 81 (6) ◽  
pp. A13-A16 ◽  
Author(s):  
Nigel Rees ◽  
Simon Carter ◽  
Graham Heinson ◽  
Lars Krieger

The magnetotelluric (MT) method is introduced as a geophysical tool to monitor hydraulic fracturing of shale gas reservoirs and to help constrain how injected fluids propagate. The MT method measures the electrical resistivity of earth, which is altered by the injection of fracturing fluids. The degree to which these changes are measurable at the surface is determined by several factors, such as the conductivity and quantity of the fluid injected, the depth of the target interval, the existing pore fluid salinity, and a range of formation properties, such as porosity and permeability. From an MT monitoring survey of a shale gas hydraulic fracture in the Cooper Basin, South Australia, we have found temporal and spatial changes in MT responses above measurement error. Smooth inversions are used to compare the resistivity structure before and during hydraulic fracturing, with results showing increases in bulk conductivity of 20%–40% at a depth range coinciding with the horizontal fracture. Comparisons with microseismic data lead to the conclusion that these increases in bulk conductivity are caused by a combination of the injected fluid permeability and an increase in wider scale in situ fluid permeability.


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