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Pore characteristics and permeability changes of high-temperature limestone after rapid cooling by dry ice

By A Mystery Man Writer

Pore characteristics and permeability changes of high-temperature limestone  after rapid cooling by dry ice

PDF] Some engineering properties of limestone : Tunnel Stražina case study (Croatia)

Pore characteristics and permeability changes of high-temperature limestone  after rapid cooling by dry ice

PDF) Pore characteristics and permeability changes of high-temperature limestone after rapid cooling by dry ice

Pore characteristics and permeability changes of high-temperature limestone  after rapid cooling by dry ice

UPV of limestone with varying duration of individual pre-treatment

Pore characteristics and permeability changes of high-temperature limestone  after rapid cooling by dry ice

The relationship between the ratio of the original radon emission rate

Pore characteristics and permeability changes of high-temperature limestone  after rapid cooling by dry ice

UPV of limestone with combined process of pre-treatment at 600 °C for

Pore characteristics and permeability changes of high-temperature limestone  after rapid cooling by dry ice

UPV of limestone with combined process of pre-treatment at 600 °C for

Pore characteristics and permeability changes of high-temperature limestone  after rapid cooling by dry ice

Yuyang ZHAO, Master of Engineering, Xi'an University of Science and Technology, Xi'an, Department of Geology

Pore characteristics and permeability changes of high-temperature limestone  after rapid cooling by dry ice

Effects of liquid-nitrogen cooling on pore characteristics of high-temperature limestone based on NMR

Pore characteristics and permeability changes of high-temperature limestone  after rapid cooling by dry ice

Study on the effect of high-temperature dry–wet cycles on argillaceous sandstone

Pore characteristics and permeability changes of high-temperature limestone  after rapid cooling by dry ice

PDF) Pore characteristics and permeability changes of high-temperature limestone after rapid cooling by dry ice