Javascript must be enabled to continue!
Research on characterization of the deterioration of sandstone physical and mechanical properties under mining and water action
View through CrossRef
Abstract
Mining geological disasters occur frequently in Guizhou, with mine mining and rainfall-induced avalanche geological disasters mainly, the investigation concluded that the hard rock of the overlying slide body is mostly sandstone, which can be seen, sandstone has a greater impact on mine mining avalanche geological disasters, and it is crucial to study the physical and mechanical properties of sandstone under the action of mine mining(hereinafter referred to as the action of mining) and water action. The paper takes the sandstone before and after the action of mining and water as the research object, analyzes the deterioration characteristics of sandstone hydrophysical and mechanical properties under the action of mining and water, and researches the microstructure of sandstone.The main research results are as follows: (1) the water absorption rate of sandstone increased by 0.056% under the action of mining, the water absorption rate of sandstone increased with a good exponential relationship under the action of dry and wet cycles, the swelling rate of sandstone increased by 0.3% under the action of mining, and the index of disintegration resistance decreased by 0.3% in 5 cycles; (2) the damage rate of uniaxial compressive strength of sandstone after being subjected to mining was 6.367%, and the total degradation rate increased with the increase of the number of dry and wet cycles. The total deterioration rate increases with the number of wet and dry cycles, the stage deterioration rate and the average stage deterioration rate first decrease and then increase, and the degree of fragmentation gradually increases; (3) The average pore porosity of the quarried sandstone gradually increased at 0, 1, 5, and 10 of the dry and wet cycles, and the sandstone's ability to adsorb water increased,which establishes the microstructural evolution of "mining cracking → water adsorption → water-rock action" model was established. The sandstone undergoes the action of mining and water cycle, the internal structure is weakened faster, and the physical and mechanical properties are deteriorated.
Springer Science and Business Media LLC
Title: Research on characterization of the deterioration of sandstone physical and mechanical properties under mining and water action
Description:
Abstract
Mining geological disasters occur frequently in Guizhou, with mine mining and rainfall-induced avalanche geological disasters mainly, the investigation concluded that the hard rock of the overlying slide body is mostly sandstone, which can be seen, sandstone has a greater impact on mine mining avalanche geological disasters, and it is crucial to study the physical and mechanical properties of sandstone under the action of mine mining(hereinafter referred to as the action of mining) and water action.
The paper takes the sandstone before and after the action of mining and water as the research object, analyzes the deterioration characteristics of sandstone hydrophysical and mechanical properties under the action of mining and water, and researches the microstructure of sandstone.
The main research results are as follows: (1) the water absorption rate of sandstone increased by 0.
056% under the action of mining, the water absorption rate of sandstone increased with a good exponential relationship under the action of dry and wet cycles, the swelling rate of sandstone increased by 0.
3% under the action of mining, and the index of disintegration resistance decreased by 0.
3% in 5 cycles; (2) the damage rate of uniaxial compressive strength of sandstone after being subjected to mining was 6.
367%, and the total degradation rate increased with the increase of the number of dry and wet cycles.
The total deterioration rate increases with the number of wet and dry cycles, the stage deterioration rate and the average stage deterioration rate first decrease and then increase, and the degree of fragmentation gradually increases; (3) The average pore porosity of the quarried sandstone gradually increased at 0, 1, 5, and 10 of the dry and wet cycles, and the sandstone's ability to adsorb water increased,which establishes the microstructural evolution of "mining cracking → water adsorption → water-rock action" model was established.
The sandstone undergoes the action of mining and water cycle, the internal structure is weakened faster, and the physical and mechanical properties are deteriorated.
Related Results
Evaluating the Science to Inform the Physical Activity Guidelines for Americans Midcourse Report
Evaluating the Science to Inform the Physical Activity Guidelines for Americans Midcourse Report
Abstract
The Physical Activity Guidelines for Americans (Guidelines) advises older adults to be as active as possible. Yet, despite the well documented benefits of physical a...
Use of Formation Water and Associated Gases and their Simultaneous Utilization for Obtaining Microelement Concentrates Fresh Water and Drinking Water
Use of Formation Water and Associated Gases and their Simultaneous Utilization for Obtaining Microelement Concentrates Fresh Water and Drinking Water
Abstract Purpose: The invention relates to the oil industry, inorganic chemistry, in particular, to the methods of complex processing of formation water, using flare gas of oil and...
Acidizing Sandstone Formations Using a Sandstone Acid System For High Temperatures
Acidizing Sandstone Formations Using a Sandstone Acid System For High Temperatures
Abstract
Regular mud acid mixtures have been extensively used to stimulate sandstone formations; however, the use of this acid in a deep well has some major drawback...
The Influence of Bioturbation on Sandstone Brittleness: A Comparative Analysis of Massive Sandstone versus Bioturbated Sandstone (Ordovician Qasim Formation-Saudi Arabia)
The Influence of Bioturbation on Sandstone Brittleness: A Comparative Analysis of Massive Sandstone versus Bioturbated Sandstone (Ordovician Qasim Formation-Saudi Arabia)
Bioturbation is the reorganization of sediment particles by living organisms, mainly infauna, as they move through and over sediment, feed, and construct dwellings. The biosediment...
Study on Brittleness Characteristics and Fracturing Crack Propagation Law of Deep Thin-Layer Tight Sandstone in Longdong, Changqing
Study on Brittleness Characteristics and Fracturing Crack Propagation Law of Deep Thin-Layer Tight Sandstone in Longdong, Changqing
Tight-sandstone oil and gas resources are the key areas of unconventional oil and gas resources exploration and development. Because tight-sandstone reservoirs usually have the cha...
STUDY OF HYDROTHERMAL CYCLING ON DETERIORATION AND DAMAGE MECHANISM OF SANDSTONE
STUDY OF HYDROTHERMAL CYCLING ON DETERIORATION AND DAMAGE MECHANISM OF SANDSTONE
Since water and high temperature are significant variables that control the strength of deep rock formations, it is vital for deep geological engineering to explore the mechanical ...
Experiments on Water-Gas Flow Characteristics under Reservoir Condition in a Sandstone Gas Reservoir
Experiments on Water-Gas Flow Characteristics under Reservoir Condition in a Sandstone Gas Reservoir
For gas reservoirs that contain water, investigating characteristics of water–gas seepage is crucial to the formulation of gas field development plans and predicting the production...
Optimisation of potash mining technology for cell and pillar mining method
Optimisation of potash mining technology for cell and pillar mining method
The diverse demand for inorganic fertilizers has predetermined the intensification of potash mining, which is a raw material for their production. In this regard, it has become nec...

