Evolution of Friction and Permeability in a Propped Fracture under Shear

We explore the evolution of friction and permeability of a propped fracture under shear. We examine the effects of normal stress, proppant thickness, proppant size, and fracture wall texture on the frictional and transport response of proppant packs confined between planar fracture surfaces. The pro...

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Main Authors: Fengshou Zhang, Yi Fang, Derek Elsworth, Chaoyi Wang, Xiaofeng Yang
Format: Article
Language:English
Published: Wiley 2017-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2017/2063747
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author Fengshou Zhang
Yi Fang
Derek Elsworth
Chaoyi Wang
Xiaofeng Yang
author_facet Fengshou Zhang
Yi Fang
Derek Elsworth
Chaoyi Wang
Xiaofeng Yang
author_sort Fengshou Zhang
collection DOAJ
description We explore the evolution of friction and permeability of a propped fracture under shear. We examine the effects of normal stress, proppant thickness, proppant size, and fracture wall texture on the frictional and transport response of proppant packs confined between planar fracture surfaces. The proppant-absent and proppant-filled fractures show different frictional strength. For fractures with proppants, the frictional response is mainly controlled by the normal stress and proppant thickness. The depth of shearing-concurrent striations on fracture surfaces suggests that the magnitude of proppant embedment is controlled by the applied normal stress. Under high normal stress, the reduced friction implies that shear slip is more likely to occur on propped fractures in deeper reservoirs. The increase in the number of proppant layers, from monolayer to triple layers, significantly increases the friction of the propped fracture due to the interlocking of the particles and jamming. Permeability of the propped fracture is mainly controlled by the magnitude of the normal stress, the proppant thickness, and the proppant grain size. Permeability of the propped fracture decreases during shearing due to proppant particle crushing and related clogging. Proppants are prone to crushing if the shear loading evolves concurrently with the normal loading.
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publishDate 2017-01-01
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series Geofluids
spelling doaj-art-807cea823bc14630bbf5ac1c80825f0f2025-02-03T05:57:43ZengWileyGeofluids1468-81151468-81232017-01-01201710.1155/2017/20637472063747Evolution of Friction and Permeability in a Propped Fracture under ShearFengshou Zhang0Yi Fang1Derek Elsworth2Chaoyi Wang3Xiaofeng Yang4Key Laboratory of Geotechnical & Underground Engineering of Ministry of Education, Tongji University, Shanghai 200092, ChinaDepartment of Energy and Mineral Engineering, EMS Energy Institute and G3 Center, The Pennsylvania State University, University Park, PA 16802, USADepartment of Energy and Mineral Engineering, EMS Energy Institute and G3 Center, The Pennsylvania State University, University Park, PA 16802, USADepartment of Energy and Mineral Engineering, EMS Energy Institute and G3 Center, The Pennsylvania State University, University Park, PA 16802, USASchool of Mechanics and Civil Engineering, China University of Mining and Technology (Beijing), Beijing 10083, ChinaWe explore the evolution of friction and permeability of a propped fracture under shear. We examine the effects of normal stress, proppant thickness, proppant size, and fracture wall texture on the frictional and transport response of proppant packs confined between planar fracture surfaces. The proppant-absent and proppant-filled fractures show different frictional strength. For fractures with proppants, the frictional response is mainly controlled by the normal stress and proppant thickness. The depth of shearing-concurrent striations on fracture surfaces suggests that the magnitude of proppant embedment is controlled by the applied normal stress. Under high normal stress, the reduced friction implies that shear slip is more likely to occur on propped fractures in deeper reservoirs. The increase in the number of proppant layers, from monolayer to triple layers, significantly increases the friction of the propped fracture due to the interlocking of the particles and jamming. Permeability of the propped fracture is mainly controlled by the magnitude of the normal stress, the proppant thickness, and the proppant grain size. Permeability of the propped fracture decreases during shearing due to proppant particle crushing and related clogging. Proppants are prone to crushing if the shear loading evolves concurrently with the normal loading.http://dx.doi.org/10.1155/2017/2063747
spellingShingle Fengshou Zhang
Yi Fang
Derek Elsworth
Chaoyi Wang
Xiaofeng Yang
Evolution of Friction and Permeability in a Propped Fracture under Shear
Geofluids
title Evolution of Friction and Permeability in a Propped Fracture under Shear
title_full Evolution of Friction and Permeability in a Propped Fracture under Shear
title_fullStr Evolution of Friction and Permeability in a Propped Fracture under Shear
title_full_unstemmed Evolution of Friction and Permeability in a Propped Fracture under Shear
title_short Evolution of Friction and Permeability in a Propped Fracture under Shear
title_sort evolution of friction and permeability in a propped fracture under shear
url http://dx.doi.org/10.1155/2017/2063747
work_keys_str_mv AT fengshouzhang evolutionoffrictionandpermeabilityinaproppedfractureundershear
AT yifang evolutionoffrictionandpermeabilityinaproppedfractureundershear
AT derekelsworth evolutionoffrictionandpermeabilityinaproppedfractureundershear
AT chaoyiwang evolutionoffrictionandpermeabilityinaproppedfractureundershear
AT xiaofengyang evolutionoffrictionandpermeabilityinaproppedfractureundershear