Statistical Analysis of Fractures from the Hydraulic Fracture Test Site 1

2021 ◽  
Author(s):  
Frank Male ◽  
Bethany Rysak ◽  
Robin Dommisse
Keyword(s):  
Statistical Analysis ◽  
Hydraulic Fracture ◽  
Test Site ◽  
Fracture Test

An Integrated View of Hydraulic Induced Fracture Geometry in Hydraulic Fracture Test Site 2

2021 ◽  
Author(s):  
Gustavo A. Ugueto ◽  
Magdalena Wojtaszek ◽  
Paul T. Huckabee ◽  
Alexei A. Savitski ◽  
Artur Guzik ◽  
...  
Keyword(s):  
Hydraulic Fracture ◽  
Test Site ◽  
Fracture Test ◽  
Fracture Geometry

Gas Research Institute Hydraulic Fracture Test Site

1992 ◽  
Author(s):  
B.M. Robinson ◽  
F.E. Syfan ◽  
S.A. Holditch
Keyword(s):  
Hydraulic Fracture ◽  
Test Site ◽  
Fracture Test ◽  
Research Institute

scholarly journals Stratigraphically Controlled Stress Variations at the Hydraulic Fracture Test Site-1 in the Midland Basin, TX

Energies ◽  
2021 ◽  
Vol 14 (24) ◽  
pp. 8328
Author(s):  
Arjun Kohli ◽  
Mark Zoback
Keyword(s):  
Hydraulic Fracturing ◽  
Hydraulic Fracture ◽  
Active Faults ◽  
Horizontal Wells ◽  
Test Site ◽  
Stress Profile ◽  
Fracture Test ◽  
Orientation Data ◽  
Stress Measurements ◽  
Fracture Growth

We investigated the relationship between stratigraphy, stress, and microseismicity at the Hydraulic Fracture Test Site-1. The site comprises two sets of horizontal wells in the Wolfcamp shale and a deviated well drilled after hydraulic fracturing. Regional stresses indicate normal/strike-slip faulting with E-W compression. Stress measurements in vertical and horizontal wells show that the minimum principal stress varies with depth. Strata with high clay and organic content show high values of the least compressive stress, consistent with the theory of viscous stress relaxation. By integrating data from core, logs, and the hydraulic fracturing stages, we constructed a stress profile for the Wolfcamp sequence, which predicts how much pressure is required for hydraulic fracture growth. We applied the results to fracture orientation data from image logs to determine the population of pre-existing faults that are expected to slip during stimulation. We also determined microseismic focal plane mechanisms and found slip on steeply dipping planes striking NW, consistent with the orientations of potentially active faults predicted by the stress model. This case study represents a general approach for integrating stress measurements and rock properties to predict hydraulic fracture growth and the characteristics of injection-induced microseismicity.

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