Characterization of unfrozen water in highly organic turfy soil during freeze–thaw by nuclear magnetic resonance

• Published in: Engineering geology 2023-01, Vol.312, p.106937, Article 106937
• Main Authors: He, Yuanyuan, Xu, Yan, Lv, Yan, Nie, Lei, Kong, Fansheng, Yang, Shengtao, Wang, Hong, Li, Tingting
• Format: Article
• Language: English
• Subjects: Freeze–thaw process; NMR; Soil properties; Turfy soil; Unfrozen water
• ISSN: 0013-7952; 1872-6917
• DOI: 10.1016/j.enggeo.2022.106937

The unfrozen water content (ωu) is an important parameter affecting the hydrothermal-mechanical characteristics of soil and is of important significance with regard to engineering construction and environmental effects in cold regions. In this study, a widely-distributed special humus soil called turfy soil, with poor engineering geological properties, from seasonally frozen regions of northeastern China was investigated. Soil fundamental properties were determined, and ωu under various temperatures during a freeze–thaw process was measured by the nuclear magnetic resonance (NMR) method. Based on NMR theory and transverse relaxation time (T2) distribution curves, two thresholds were determined to divide the types of pore water in soil. Soil freezing characteristic curves (SFCC) of the total and pore water were drawn, and changes in the internal microstructure and pore characteristics of the soil during the freeze–thaw process were analyzed. The results showed that a drastic phase change within the soil occurs during −2 °C to −4 °C, and the freezing process can be divided into three stages. The formation of small pores and the connection of large pores make the soil looser after freeze–thaw. The division of pore water and variation in ωu show that freezing starts from large pores, while thawing starts from small pores. The capillary water content significantly decreases after freeze–thaw, and the bulk water content tends to increase. At freezing Stage I, ωu is closely related to the initial properties of the soil, whereas ωu at −3 °C almost determines the value of ωu during subsequent freeze–thaw. Finally, a ωu-power function for turfy soil was proposed, and good fitting results were obtained for both freezing and thawing soil. This work can serve as the basis of studies on soil with high organic matter content as well as soil unfrozen water content during freeze–thaw cycles in cold regions. •Two T2 cutoffs were determined to identify the pore water types of turfy soil.•Capillary water within turfy soil decreased significantly after freeze–thaw.•Pores formed and larger pores connected due to frost heaving after freeze–thaw.•ωu after drastic phase change affected ωu during the freeze–thaw process.•ωu parameterization considering of turfy soil properties showed good effects.