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王义江, 郁东旭, 孙立鹏, 朱启银, 王建州. 激光照射岩石热裂特性与裂隙分布研究[J]. 岩土工程学报. DOI: 10.11779/CJGE20230396
引用本文: 王义江, 郁东旭, 孙立鹏, 朱启银, 王建州. 激光照射岩石热裂特性与裂隙分布研究[J]. 岩土工程学报. DOI: 10.11779/CJGE20230396
Thermal-breaking characteristics and crack distribution of rock irradiated by laser beam[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20230396
Citation: Thermal-breaking characteristics and crack distribution of rock irradiated by laser beam[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20230396

激光照射岩石热裂特性与裂隙分布研究

Thermal-breaking characteristics and crack distribution of rock irradiated by laser beam

  • 摘要: 激光辅助破岩是一种非接触式破岩技术,破岩效果主要受激光功率、照射时间和离焦距离等照射参数影响。选择石灰岩、砂岩和花岗岩三类岩石,开展了不同照射参数的破岩实验,分析了温度、射孔参数、比能、热裂效能、裂隙分布、矿物组分和微观结构等变化规律。结果表明,激光照射下三类岩石表面温度均超过2000 ℃、温度梯度最高可达1500 ℃/mm,相同位置处花岗岩表面温度和温度梯度最高、砂岩次之、石灰岩最低;三类岩石射孔直径、射孔深度和射孔速率均与照射参数密切相关,砂岩、石灰岩和花岗岩最大射孔速率分别为3.18 mm/s、2.68 mm/s和0.8 mm/s。相同照射参数下,比能和热裂效能变化规律相同,但比能较热裂效能高1-2个数量级,三类岩石比能排序为:花岗岩>石灰岩>砂岩。照射后岩样均存在数条主裂隙,沿径向延伸至试样边缘,石灰岩和花岗岩次生裂隙发育,砂岩未发现明显次生裂隙。照射后岩石矿物衍射强度和微观结构发生显著改变。

     

    Abstract: Laser-assisted rock breaking is a non-contacted technology used to break rock, and its effectiveness is mainly dependent on the laser power, irradiation time, and defocusing distance. Rock-breaking experiments with different irradiation parameters were conducted on three types of rocks, including limestone, sandstone and granite. The temperature field, perforation parameters, specific energy, thermal fracturing efficiency, crack distribution, mineral constituent and microstructures were investigated. The results demonstrated that the surface temperature of the three types of rocks irradiated by laser beam increased significantly and exceeded 2000 ℃, and the maximum temperature gradient could reach up to about 1500 ℃/mm. At the same radius, the granite sample exhibited the highest surface temperature and temperature gradient, followed by sandstone, and the limestone had the lowest values. The perforation diameter, depth and speed of the three types of rocks were closely related to the corresponding irradiation parameters, and the maximum perforation speeds of sandstone, limestone and granite were 3.18 mm/s, 2.68 mm/s and 0.8 mm/s, respectively. The variation of specific energy with the irradiation parameters was similar to that of thermal fracturing efficiency when the same irradiation parameters were applied. However, the value of specific energy was about 1-2 orders of magnitude greater than that of thermal fracturing efficiency. The ranking of specific energy for the three types of rocks was granite > sandstone > limestone. These rock samples displayed several prominent cracks that extended radially to the edge of the samples. Secondary cracks were extensively developed in limestone and granite specimens, while no significant secondary cracks were detected in sandstone. The irradiated rock samples exhibited obvious changes in both diffraction intensity and microstructures compared with the corresponding original specimens.

     

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