Variation in the electrical properties of gabbro after microwave heating

IF 1.7 4区 工程技术 Q3 MECHANICS
Zhenlong Ge, Yuhua Guan, Chao Lyu
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Abstract

Microwave assistance has the potential to reduce the energy input required for mechanical rock breaking. This study systematically investigated the changes in electrical properties (specifically resistivity, capacitance, and impedance) of gabbro after microwave heating during the graded loading process, as well as its internal fracture mechanism. The findings indicate that the variations in resistivity, impedance, and capacitance of gabbro can be divided into three stages during the graded loading process: the compaction stage, elastic-steady cracking stage, and nonlinear crack propagation stage. When the strain level exceeds 70%, the resistivity and impedance start to increase, and the capacitance begins to decrease. The study also identifies a significant positive correlation between microwave power and the rate of temperature increase on the rock surface. A critical power threshold of approximately 2 kW is observed, below which achieving rapid temperature rise becomes challenging, but beyond which the temperature escalates swiftly with the energy input. Once the temperature exceeds 350 °C, rupturing mineral inclusions generate numerous microcracks, causing resistivity and impedance to exponentially increase. Furthermore, microwave heating induces a temperature differential exceeding 200 °C between the internal and external regions of the rock. Under the same radiation energy, high-power short-duration radiation is more likely to generate thermally induced cracks within the rock. The rapid expansion and heating of absorbent minerals, as well as the rupture of inclusions, further intensify the propagation of microcracks, greatly reducing the mechanical properties of the rock. This study will provide theoretical guidance for microwave-assisted mechanical rock excavation.

Abstract Image

微波加热后辉长岩电特性的变化
微波辅助有可能减少机械破岩所需的能量输入。本研究系统地研究了辉长岩在分级加载过程中经过微波加热后的电特性(特别是电阻率、电容和阻抗)变化及其内部断裂机制。研究结果表明,辉长岩在分级加载过程中的电阻率、阻抗和电容变化可分为三个阶段:压实阶段、弹性-稳定开裂阶段和非线性裂纹扩展阶段。当应变水平超过 70% 时,电阻率和阻抗开始增大,电容开始减小。研究还发现,微波功率与岩石表面温度上升率之间存在显著的正相关关系。观察到一个临界功率阈值约为 2 千瓦,低于这个阈值,实现快速升温就变得很困难,但超过这个阈值,温度就会随着输入能量的增加而迅速升高。一旦温度超过 350 °C,破裂的矿物包裹体会产生大量微裂缝,导致电阻率和阻抗成倍增加。此外,微波加热会导致岩石内部和外部区域的温差超过 200 °C。在辐射能量相同的情况下,高功率短时辐射更有可能在岩石内部产生热诱导裂缝。吸收性矿物的快速膨胀和加热以及包裹体的破裂会进一步加剧微裂缝的扩展,从而大大降低岩石的机械性能。这项研究将为微波辅助机械开凿岩石提供理论指导。
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来源期刊
Heat and Mass Transfer
Heat and Mass Transfer 工程技术-力学
CiteScore
4.80
自引率
4.50%
发文量
148
审稿时长
8.0 months
期刊介绍: This journal serves the circulation of new developments in the field of basic research of heat and mass transfer phenomena, as well as related material properties and their measurements. Thereby applications to engineering problems are promoted. The journal is the traditional "Wärme- und Stoffübertragung" which was changed to "Heat and Mass Transfer" back in 1995.
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