Abstract
Purpose
The differences in particle composition and consistency limits result in the challenge in comparing the freezing points of different types of loess. The clay activity that well links the clay content and the plasticity index suggests a response to the above challenge. The purpose of this study is to evaluate the relationship between freezing point and clay activity of loess in different areas of Loess Plateau of China.
Materials and methods
The test loess was sampled from eight typical areas of the Loess Plateau of China, which could be classified as the lean clay (CL). The clay activity of loess was obtained based on the plasticity index and the clay fraction (< 5 μm). The freezing point and soil freezing characteristic curve (SFCC) of loess were measured by the 5TM transducer from METER Group, while the soil water characteristic curves (SWCC) were determined by the filter-paper method.
Results
When the clay activity is below 0.948, the freezing point increases with higher clay activity; otherwise it rises slightly, which is in contrast to the change of matric suction. A proportional function was approximated between freezing point and matric suction. The SFCC decays more sharply at greater initial water content, compared to that at higher clay activity. The free water content increases slightly with higher clay activity while the weakly bound water content declines, resulting in an insignificant change in the freezable water content. Based on the normalization of SFCC, an exponential model incorporating the effect of clay activity was established and verified. The clay activity of loess decays as the calcium chloride content increases, which shows a good linear relationship with freezing point.
Conclusions
The freezing point of loess shows high relevance to the clay activity. The clay activity–based freezing point predictive model well considers the differences in clay content and consistency limits of loess in different regions.
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Acknowledgements
The authors would like to acknowledge Dr. Peng An and Dr. Hua Liu for the provision of additional data on the physical and chemical indexes of loess.
Funding
This research was financially supported by the National Natural Science Foundation of China (Grant Nos. 41972279 and 51778528), the Basic Research Program of Natural Science of Shaanxi Province (No. 2019JLM-56), and the Key Research and Development project of Shaanxi Province (No. 2022SF-197).
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Wang, S., Ye, W., Wang, Y. et al. Evaluation of the relationship between freezing point and clay activity of loess. J Soils Sediments 22, 2262–2280 (2022). https://doi.org/10.1007/s11368-022-03235-7
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DOI: https://doi.org/10.1007/s11368-022-03235-7