The soil–water characteristic curve, which illustrates the relationship between water content and matric suction, is crucial for both unsaturated soil theory and engineering applications. Since water content significantly affects unsaturated soil strength, experimentally examine the distribution of water within the soil matrix. First, three types of soil are prepared for nuclear magnetic resonance and pressure plate tests, conducted over a range of matric suctions from 0 to 1400 kPa. Then, the pressure plate testreveals that matric suction expels free water first, leaving bound water, which remains until reaching critical suction point. NMR test is also performed to analyze the dynamics of pore water distribution during drying process. As matric suction increases, the peak of signal amplitude decreases, shifting leftward, reflecting water drainage from larger to smaller pores. In addition, two drainage stages are identified, considering distinct ranges of matric suction. Large pores drain more quickly, while smaller pores retain water for a longer period, challenging simpler models of pore drainage. The dynamic distribution of pore water reveals the evolution of water expulsion from the soil over time. This sheds light on water distribution and drainage behavior, emphasizing the need for advanced models that account for pore connectivity and water retention mechanisms.
Read full abstract