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Reaction of different rock types to low-power (3.2 kW) microwave irradiation in a multimode cavity

机译:不同岩石类型对多模腔的低功率(3.2 kW)微波辐射的反应

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摘要

This study deals with low-power (3.2 kW) microwave irradiation of a range of rocks and provide an indication of the suitability of certain rock types for this treatment method for rock fragmentation and mineral comminution. The influence of microwave irradiation was assessed physically by measuring rock properties and observing cracking phenomena and chemically by analysing the mineralogical and chemical composition before and after microwave irradiation. The results show that the reaction to microwave irradiation strongly depends on the mineralogy or the water content of the rock. Rocks with low content of microwave absorbers (like granite and sandstone) heat slowly and do not show strong physical changes, whereas rocks with better microwave absorption (basalt, mafic volcanites) heat quickly leading to significant physical changes. It is apparent that the presence of water either in the porous volume of the rock or in the mineralogical structure (e.g. clay minerals) adds to the destructive work with the help of the generated steam pressure.
机译:本研究涉及一系列岩石的低功率(3.2 kW)微波辐射,并为该处理方法提供了某些岩石类型的适用性的指示。通过测量岩石性能和观察微波辐射前后分析矿物学和化学成分,通过测量岩石性能和化学方式来物理评估微波辐射的影响。结果表明,对微波辐射的反应强烈取决于岩石的矿物学或岩石的含水量。微波吸收剂含量低(如花岗岩和砂岩)的岩石慢慢热,并没有显示出强烈的物理变化,而具有更好的微波吸收(玄武岩,MAFIC Volcanites)的岩石迅速导致显着的物理变化。显然,在岩石的多孔体积或矿物学结构中存在水的存在(例如粘土矿物质)在产生的蒸汽压力的帮助下增加了破坏性的工作。

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