In the practice of the deep engineering, it is expected to improve
engineering efficiency by introducing the microwave energy. Therefore,
based on 1050 m deep sandstone, the heating characteristics of sandstone and
its constituent minerals in the microwave field are comprehensively explored
through experiments and nu?merical simulations. In the paper, the
asynchronism of the temperature rise in different areas of the sandstone
depends on the local characteristics of dielectric loss and maximum heat
storage capacity. With increase of the temperature, the evaporation of the
water leads to the decrease of the dielectric properties, the increase in
the constant-pressure heat capacity and the increase in the heat dissipation
coefficient, which suppresses the temperature growth trend. The temperature
rise of the amplitude of the material is lower than that expected from the
microwave power. The maximum temperature of dolomite, feldspar and quartz
under the power of 2000 W is 1.86, 1.71, and 1.63 times that of the power of
1000 W, respectively. It is necessary to select the reasonable microwave
power to maximize the engineering efficiency. The results are expected to
provide the theoretical and technical supports for the electromagnetic heat
generation in deep engineering.