Investigation on Creep Behavior and Permeability Evolution Characteristics of Sandstone under Different Pore Pressures

To investigate the influence of pore pressure (σw) on the creep behavior and permeability of red sandstone, triaxial creep test with permeability test under different pore pressures was conducted using MTS 815 testing system. The experimental results demonstrate that water has significant weakening...

Full description

Bibliographic Details
Main Author: Hongcai Shi
Format: Article
Language:English
Published: Hindawi-Wiley 2021-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2021/6693131
id doaj-50fe218f109d4238a1d0cdcf607213b1
record_format Article
spelling doaj-50fe218f109d4238a1d0cdcf607213b12021-04-26T00:03:51ZengHindawi-WileyGeofluids1468-81232021-01-01202110.1155/2021/6693131Investigation on Creep Behavior and Permeability Evolution Characteristics of Sandstone under Different Pore PressuresHongcai Shi0Department of Civil Architecture and EnvironmentTo investigate the influence of pore pressure (σw) on the creep behavior and permeability of red sandstone, triaxial creep test with permeability test under different pore pressures was conducted using MTS 815 testing system. The experimental results demonstrate that water has significant weakening effect on the long-term mechanical properties of sandstone, and the long-term strength of sandstone gradually decreases with increase in pore pressures. All permeability-time curves demonstrate a “decreasing-increasing” trend, but two different permeability evolution trends during the steady creep stage are observed, which are related to deviatoric stress. The permeability of both intact (k0) and fractured sandstone (kf) samples increases with the increase in pore pressure, which are in consistent with the failure mode analysis of fractured sandstone samples. However, while the relationship between k0 and σw is positive linear, it is a positive exponential function relationship between kf and σw.http://dx.doi.org/10.1155/2021/6693131
collection DOAJ
language English
format Article
sources DOAJ
author Hongcai Shi
spellingShingle Hongcai Shi
Investigation on Creep Behavior and Permeability Evolution Characteristics of Sandstone under Different Pore Pressures
Geofluids
author_facet Hongcai Shi
author_sort Hongcai Shi
title Investigation on Creep Behavior and Permeability Evolution Characteristics of Sandstone under Different Pore Pressures
title_short Investigation on Creep Behavior and Permeability Evolution Characteristics of Sandstone under Different Pore Pressures
title_full Investigation on Creep Behavior and Permeability Evolution Characteristics of Sandstone under Different Pore Pressures
title_fullStr Investigation on Creep Behavior and Permeability Evolution Characteristics of Sandstone under Different Pore Pressures
title_full_unstemmed Investigation on Creep Behavior and Permeability Evolution Characteristics of Sandstone under Different Pore Pressures
title_sort investigation on creep behavior and permeability evolution characteristics of sandstone under different pore pressures
publisher Hindawi-Wiley
series Geofluids
issn 1468-8123
publishDate 2021-01-01
description To investigate the influence of pore pressure (σw) on the creep behavior and permeability of red sandstone, triaxial creep test with permeability test under different pore pressures was conducted using MTS 815 testing system. The experimental results demonstrate that water has significant weakening effect on the long-term mechanical properties of sandstone, and the long-term strength of sandstone gradually decreases with increase in pore pressures. All permeability-time curves demonstrate a “decreasing-increasing” trend, but two different permeability evolution trends during the steady creep stage are observed, which are related to deviatoric stress. The permeability of both intact (k0) and fractured sandstone (kf) samples increases with the increase in pore pressure, which are in consistent with the failure mode analysis of fractured sandstone samples. However, while the relationship between k0 and σw is positive linear, it is a positive exponential function relationship between kf and σw.
url http://dx.doi.org/10.1155/2021/6693131
work_keys_str_mv AT hongcaishi investigationoncreepbehaviorandpermeabilityevolutioncharacteristicsofsandstoneunderdifferentporepressures
_version_ 1714657658368163840