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Influence of topography on the asymmetry of rill cross-sections in the Yuanmou dry-hot valley
Rill erosion is one of the most common types of erosion, and the development conditions of the asymmetric characteristics of rill cross-sections are still relatively poorly understood. To explore the relationship between rill topography and rill cross-sectional asymmetry, we used the microtopographi...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2022
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9385726/ https://www.ncbi.nlm.nih.gov/pubmed/35978084 http://dx.doi.org/10.1038/s41598-022-18198-5 |
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author | Gu, Xingli Luo, Jun Zhang, Bin Wang, Lei Wu, Qiangjianzhong |
author_facet | Gu, Xingli Luo, Jun Zhang, Bin Wang, Lei Wu, Qiangjianzhong |
author_sort | Gu, Xingli |
collection | PubMed |
description | Rill erosion is one of the most common types of erosion, and the development conditions of the asymmetric characteristics of rill cross-sections are still relatively poorly understood. To explore the relationship between rill topography and rill cross-sectional asymmetry, we used the microtopographic profiler method to measure 712 groups of rill cross-sections in the Yuanmou dry-hot valley area. The results of correlation analysis and principal component analysis to investigate the topographical conditions of rill development show that: (1) asymmetry is the main feature in rill cross-sections; 53% of rill cross-sections are right-biased and 47% are left-biased. (2) There is an extremely significant positive correlation between the slope difference and the rill cross-section asymmetry ratio (p < 0.01); the asymmetry ratio increases as the slope difference on both sides (B) increases, and the directionality of the asymmetry ratio is affected by B. The difference between the catchment areas on both sides has a significant linear correlation with the asymmetry ratio of the width (r = 0.07, p < 0.05). (3) Seven topographic factors were divided into two types of principal components: the first represents the rill slope surface shape and the rill shape, and the second represents the difference between the two sides of the rill. |
format | Online Article Text |
id | pubmed-9385726 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-93857262022-08-19 Influence of topography on the asymmetry of rill cross-sections in the Yuanmou dry-hot valley Gu, Xingli Luo, Jun Zhang, Bin Wang, Lei Wu, Qiangjianzhong Sci Rep Article Rill erosion is one of the most common types of erosion, and the development conditions of the asymmetric characteristics of rill cross-sections are still relatively poorly understood. To explore the relationship between rill topography and rill cross-sectional asymmetry, we used the microtopographic profiler method to measure 712 groups of rill cross-sections in the Yuanmou dry-hot valley area. The results of correlation analysis and principal component analysis to investigate the topographical conditions of rill development show that: (1) asymmetry is the main feature in rill cross-sections; 53% of rill cross-sections are right-biased and 47% are left-biased. (2) There is an extremely significant positive correlation between the slope difference and the rill cross-section asymmetry ratio (p < 0.01); the asymmetry ratio increases as the slope difference on both sides (B) increases, and the directionality of the asymmetry ratio is affected by B. The difference between the catchment areas on both sides has a significant linear correlation with the asymmetry ratio of the width (r = 0.07, p < 0.05). (3) Seven topographic factors were divided into two types of principal components: the first represents the rill slope surface shape and the rill shape, and the second represents the difference between the two sides of the rill. Nature Publishing Group UK 2022-08-17 /pmc/articles/PMC9385726/ /pubmed/35978084 http://dx.doi.org/10.1038/s41598-022-18198-5 Text en © The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/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/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Article Gu, Xingli Luo, Jun Zhang, Bin Wang, Lei Wu, Qiangjianzhong Influence of topography on the asymmetry of rill cross-sections in the Yuanmou dry-hot valley |
title | Influence of topography on the asymmetry of rill cross-sections in the Yuanmou dry-hot valley |
title_full | Influence of topography on the asymmetry of rill cross-sections in the Yuanmou dry-hot valley |
title_fullStr | Influence of topography on the asymmetry of rill cross-sections in the Yuanmou dry-hot valley |
title_full_unstemmed | Influence of topography on the asymmetry of rill cross-sections in the Yuanmou dry-hot valley |
title_short | Influence of topography on the asymmetry of rill cross-sections in the Yuanmou dry-hot valley |
title_sort | influence of topography on the asymmetry of rill cross-sections in the yuanmou dry-hot valley |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9385726/ https://www.ncbi.nlm.nih.gov/pubmed/35978084 http://dx.doi.org/10.1038/s41598-022-18198-5 |
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