In northwestern China, loess is extremely important and covers 630,000 km 2, primarily in the Shanxi, Shaanxi, Gansu, and Ningxia regions. Loess deposits cover 10% of the world’s continents, including Asia, Africa, central and southern Europe, the American Midwest, and northern France. This does not alter the authors’ adherence to all the Plos ONE policies on sharing data and materials. There are no patents, products in development or marketed products to declare. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.Ĭompeting interests: Xiang-fei Lü is employed by CCCC First Highway Consultants Co., LTD. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.ĭata Availability: All relevant data are within the paper and its Supporting information files.įunding: This study was supported by The China Postdoctoral Science Foundation in the form of grants awarded to XL (2019T120873, 2018M631117), by the Postdoctoral Research Project in Shaanxi Province in the form of a grant awarded to XL (2018BSHGZZHQYXMZZ26), by The Key Program of the National Natural Science Foundation of China in the form of a grant awarded to WN (41931285), by the key research and development program of Shaanxi Province in the form of a grant awarded to WN (2019ZDLSF05-07), and by CCCC First Highway Consultants Co., LTD in the form of a salary to XL. Received: MaAccepted: JPublished: June 28, 2021Ĭopyright: © 2021 Yuan et al. PLoS ONE 16(6):Įditor: Jianguo Wang, China University of Mining and Technology, CHINA Therefore, the change in permeability characteristics of compacted loess is determined by aggregate size, loess surface morphology, and the total pore volume occupied by macropores.Ĭitation: Yuan K-z, Ni W-k, Lü X-f, Wang X-j (2021) Permeability characteristics and structural evolution of compacted loess under different dry densities and wetting-drying cycles. Variations in aggregate size and connection relationships made it easier to form overhead structures between aggregates, and the increased of macropore volume will form more water channels. The proportion of macropores in the total pore volume shows the most drastic change. The pore volume of the compacted loess after three wetting-drying cycles increased by 8.56%, 8.61%, and 6.15%, respectively. Meanwhile, the change in micropores was relatively small. NMR analyses revealed that with increasing dry density, the volume of macropores in the compacted loess rapidly decreased, the volume of mesopores and small pores increased. Therefore, the size of 10–50 μm aggregates represented the transition zone of compacted loess. And the interesting finding was that the area occupied by 10–50 μm aggregates remained basically unchanged with the number of wetting-drying cycles increasing. It showed that the size of compacted loess aggregates for different dry densities were concentrated from 10–100 μm, occupying 65.0%, 58.19%, and 51.64% of the total aggregates area respectively. The size of compacted loess aggregates was quantitatively analyzed by Image-Pro Plus (IPP) software. Meanwhile, the evolution of the microstructure was investigated by Scanning Electron Microscope (SEM) and Nuclear Magnetic Resonance (NMR) to explain the change of its permeability characteristics. However, the wetting-drying cycle presented the opposite result. This study explored the permeability characteristics of compacted loess under different dry densities and wetting-drying cycles, and found that as the dry density increases, the compacted loess surface became denser, the saturation permeability coefficient and saturation infiltration rate decreased. Permeability characteristics of compacted loess is always an important topic in soil mechanics and geotechnical engineering.
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