Numerical simulation study on rock breakage by low temperature jet impact

A 3-D model with specific parameters was established, utilizing the conjugate heat transfer method to calculate heat exchange between the rock and fluid, and the smoothed particle hydrodynamics-finite element method approach to simulate rock fragmentation. Upon contact, the liquid nitrogen jet induced significant heat exchange, with the 25 MPa jet showing larger contact area and higher efficiency. Notably, the impact center of the 400?C rock exhibited a slight temperature rise due to energy release. Liquid nitrogen reduced the rock?s tensile, compressive strengths, and elastic modulus. High temperature rocks (400?C) had a 15.8% higher eroded volume fraction than those at 200?C. Increasing jet pressure from 20-25 MPa resulted in a 32.0% erosion increase. Additionally, a decrease in elastic modulus for 200?C granite led to a 19.9% increase in erosion.

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Publication Details

Journal
Thermal Science
Published
2025-01-01
DOI
https://doi.org/10.2298/tsci2502503w
Primary Topic
Rock Mechanics and Modeling
Type
article
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article

Numerical simulation study on rock breakage by low temperature jet impact

Chengzheng Cai, Hu Wang, Yong Hu, Bo Wang et al.
Thermal Science
Rock Mechanics and Modeling
article

Numerical simulation study on rock breakage by low temperature jet impact

Chengzheng Cai, Hu Wang, Yong Hu, Bo Wang, Yi Lyv
article en

Abstract

A 3-D model with specific parameters was established, utilizing the conjugate heat transfer method to calculate heat exchange between the rock and fluid, and the smoothed particle hydrodynamics-finite element method approach to simulate rock fragmentation. Upon contact, the liquid nitrogen jet induced significant heat exchange, with the 25 MPa jet showing larger contact area and higher efficiency. Notably, the impact center of the 400?C rock exhibited a slight temperature rise due to energy release. Liquid nitrogen reduced the rock?s tensile, compressive strengths, and elastic modulus. High temperature rocks (400?C) had a 15.8% higher eroded volume fraction than those at 200?C. Increasing jet pressure from 20-25 MPa resulted in a 32.0% erosion increase. Additionally, a decrease in elastic modulus for 200?C granite led to a 19.9% increase in erosion.

Thermal ScienceVol. 29(2 Part B)
China University of Mining and Technology (CN)
Openalex Percentile: Top 87%
Rock Mechanics and Modeling
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