Efficient exploitation of hot dry
rock resources can alleviate
global energy supply pressure. However, the “low-porosity,
low-permeability” occurrence characteristics of hot dry rock
severely restrict the exploitation efficiency. To achieve efficient
exploitation of hot dry rock resources, artificial fracturing and
permeability-enhancing measures must be taken to transform the reservoir
and improve the heat-exchange efficiency. Liquid nitrogen cyclic cold
shock is an effective fracturing method for geothermal reservoirs.
The huge temperature difference between liquid nitrogen and hot rock
can cause uneven contraction between mineral particles, inducing fracture
networks. It is crucial to study the damage characteristics of hot
dry rock under liquid nitrogen cyclic cold shock. Therefore, this
paper carries out liquid nitrogen cold shock experiments on high-temperature
granite. Granite samples heated to different temperatures (200, 300,
400, 500, and 600 °C) were subjected to cyclic cold shocks (five
times) using liquid nitrogen. NMR testing and ultrasonic testing were
performed on the treated samples to study the damage characteristics
of hot dry rock. The results show that with the increase of heating
temperature and the number of cold shocks, the porosity of the cores
increases continuously. After five cold shocks, the porosity of the
cores heated at 200–600 °C increases by 1.108, 1.154,
1.158, 3.080, and 6.896%, respectively. The wave velocity decreases
continuously, and the time delay and distortion of the waveforms become
more obvious. The frequency distribution gradually shifts toward lower
frequencies, the wavelet packet energy distribution transfers to lower-frequency
sub-bands, the total energy of the Hilbert energy spectrum decreases
continuously, the duration of high instantaneous energy becomes shorter,
and the frequency distribution interval shifts toward lower frequencies.
The quality factor Q decreases with increasing heating
temperature and the number of liquid nitrogen cold shocks and has
a good linear relationship with the core porosity.