Pore Structure Evolution and Failure Mechanism of Limestone in the Taiyuan Formation of the Ordos Basin under High Temperature.

The comprehensive analysis shows that within the temperature range of 25–1200 °C, the average pore throat radius increases, and the displacement pressure shows a decreasing trend, indicating that the difficulty of mercury entering the pores decreases, the mercury removal efficiency gradually increases, and the connectivity of limestone becomes better. 3.1.3.

also in 47,180 other papers

Variation of Pore Throat Volume with Temperature It can be seen from Figure 4 that with the increase of pressure, the cumulative mercury input of chert samples at different temperatures shows an increasing trend.

also in 63,971 other papers