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Determining soil water characteristic curve of lime treated loess using multiscale structure fractal characteristic
Soil–Water characteristic Curve (SWCC) is meant to describe the mechanical behavior of unsaturated soil. The present paper focuses on the internal multi-scale microstructure of Xining untreated loess and lime-treated loess with the use of scanning electron microscopy (SEM) and image processing techn...
Autores principales: | , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2020
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7725807/ https://www.ncbi.nlm.nih.gov/pubmed/33299015 http://dx.doi.org/10.1038/s41598-020-78489-7 |
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author | Li, Xiaojun Hu, Chenzhi Li, Fengyan Gao, Hongling |
author_facet | Li, Xiaojun Hu, Chenzhi Li, Fengyan Gao, Hongling |
author_sort | Li, Xiaojun |
collection | PubMed |
description | Soil–Water characteristic Curve (SWCC) is meant to describe the mechanical behavior of unsaturated soil. The present paper focuses on the internal multi-scale microstructure of Xining untreated loess and lime-treated loess with the use of scanning electron microscopy (SEM) and image processing technique. A new SWCC model was presented based on the fractal dimension of pore size distribution. The SWCC of untreated loess was calculated from fractal dimension and fitted well with curve tested from Fredlund SWCC device. The SWCC of lime-treated loess was then calculated. Two curves of Xining untreated loess and lime-treated loess have been compared and reasons for the difference have also been discussed. The results indicate that the content of large pores in lime-treated loess decreased and the content of micro-pore increased. The bracket pores were changed into cement pores. The pore fractal dimension D of Xining untreated loess is 1.39 and the pore fractal dimension D of Xining lime-treated loess is 1.53. Air-entry value of untreated loess is 12.16 kPa, while lime-treated Loess—35.15 kPa. In transition region, matric suction of lime-treated loess was in the range of 35.15 kPa ~ 4000 kPa, while matric suction of untreated loess—12.16 kPa ~ 2600 kPa. The range of the transition region in lime-treated loess is larger than that in the loess, while in the range of saturation region, the reverse applies. Under the condition of the same matrix suction, the saturation of lime-treated loess is greater than that of untreated loess. In the residual region, the difference of SWCC of soil samples is small. |
format | Online Article Text |
id | pubmed-7725807 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2020 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-77258072020-12-14 Determining soil water characteristic curve of lime treated loess using multiscale structure fractal characteristic Li, Xiaojun Hu, Chenzhi Li, Fengyan Gao, Hongling Sci Rep Article Soil–Water characteristic Curve (SWCC) is meant to describe the mechanical behavior of unsaturated soil. The present paper focuses on the internal multi-scale microstructure of Xining untreated loess and lime-treated loess with the use of scanning electron microscopy (SEM) and image processing technique. A new SWCC model was presented based on the fractal dimension of pore size distribution. The SWCC of untreated loess was calculated from fractal dimension and fitted well with curve tested from Fredlund SWCC device. The SWCC of lime-treated loess was then calculated. Two curves of Xining untreated loess and lime-treated loess have been compared and reasons for the difference have also been discussed. The results indicate that the content of large pores in lime-treated loess decreased and the content of micro-pore increased. The bracket pores were changed into cement pores. The pore fractal dimension D of Xining untreated loess is 1.39 and the pore fractal dimension D of Xining lime-treated loess is 1.53. Air-entry value of untreated loess is 12.16 kPa, while lime-treated Loess—35.15 kPa. In transition region, matric suction of lime-treated loess was in the range of 35.15 kPa ~ 4000 kPa, while matric suction of untreated loess—12.16 kPa ~ 2600 kPa. The range of the transition region in lime-treated loess is larger than that in the loess, while in the range of saturation region, the reverse applies. Under the condition of the same matrix suction, the saturation of lime-treated loess is greater than that of untreated loess. In the residual region, the difference of SWCC of soil samples is small. Nature Publishing Group UK 2020-12-09 /pmc/articles/PMC7725807/ /pubmed/33299015 http://dx.doi.org/10.1038/s41598-020-78489-7 Text en © The Author(s) 2020 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/. |
spellingShingle | Article Li, Xiaojun Hu, Chenzhi Li, Fengyan Gao, Hongling Determining soil water characteristic curve of lime treated loess using multiscale structure fractal characteristic |
title | Determining soil water characteristic curve of lime treated loess using multiscale structure fractal characteristic |
title_full | Determining soil water characteristic curve of lime treated loess using multiscale structure fractal characteristic |
title_fullStr | Determining soil water characteristic curve of lime treated loess using multiscale structure fractal characteristic |
title_full_unstemmed | Determining soil water characteristic curve of lime treated loess using multiscale structure fractal characteristic |
title_short | Determining soil water characteristic curve of lime treated loess using multiscale structure fractal characteristic |
title_sort | determining soil water characteristic curve of lime treated loess using multiscale structure fractal characteristic |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7725807/ https://www.ncbi.nlm.nih.gov/pubmed/33299015 http://dx.doi.org/10.1038/s41598-020-78489-7 |
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