{"title":"Ephemeral gully evolution and morphological changes in the erosion-tillage-erosion cycle on steep loess slopes","authors":"Wenqian Liang , Ximeng Xu , Fenli Zheng , Chao Qin","doi":"10.1016/j.catena.2025.109257","DOIUrl":null,"url":null,"abstract":"<div><div>Ephemeral gullies (EGs) are distributed on the farmlands across the world and play a significant role in soil loss and land degradation. However, the complete cyclic evolution process of EG channels, including formation, obliteration by tillage, and reformation under subsequent rainfall, remains underexplored. Thus, this study aims to investigate the EG evolution and morphological changes in the erosion-tillage-erosion cycle on a steep loess slope by using 0.01 m resolution digital elevation models (DEMs) obtained from Terrestrial Laser Scanner. A total of 107 cross-sections across three EGs were extracted, and six morphological indices, including <em>W</em> (EG channel width), <em>D</em> (EG channel depth), <em>A</em> (EG channel cross-sectional area), <em>α</em> (the angle from the EG lateral drainage area border to the EG channel border), <em>β</em> (the angle from the EG channel border to the bottom), and <em>W/D</em> (EG channel width-depth ratio), were obtained. The results revealed that, from the post-rainy season in 2014 to the post-rainy season in 2015, <em>W</em>, <em>D</em>, and <em>A</em> increased by 8%–25%, 20%–40%, and 35%–69%, respectively, while <em>α</em>, <em>β</em>, and <em>W</em>/<em>D</em> exhibited minor changes. EG with larger upslope drainage areas experienced more pronounced evolution, with <em>D</em>, <em>A</em>, and <em>α</em> increasing linearly with upslope drainage area across the three EGs, ranging from 0.05 m to 0.49 m, 67 cm<sup>2</sup> to 2062 cm<sup>2</sup>, and 10° to 26°, respectively. A new cross-section morphological index incorporating upslope and lateral flow contributions, <em>α</em>·tan(<em>β</em>), was introduced, which showed a consistent linear relationship with the product of the upslope drainage area and the square of local slope gradient in EGs, offering a tool for predicting EG cross-sectional morphology. This study provided insights into EG evolution and illustrated the role of tillage practices in EG evolution processes, which can provide a scientific basis for the construction of gully erosion prediction models.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"258 ","pages":"Article 109257"},"PeriodicalIF":5.4000,"publicationDate":"2025-06-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0341816225005594","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
Ephemeral gullies (EGs) are distributed on the farmlands across the world and play a significant role in soil loss and land degradation. However, the complete cyclic evolution process of EG channels, including formation, obliteration by tillage, and reformation under subsequent rainfall, remains underexplored. Thus, this study aims to investigate the EG evolution and morphological changes in the erosion-tillage-erosion cycle on a steep loess slope by using 0.01 m resolution digital elevation models (DEMs) obtained from Terrestrial Laser Scanner. A total of 107 cross-sections across three EGs were extracted, and six morphological indices, including W (EG channel width), D (EG channel depth), A (EG channel cross-sectional area), α (the angle from the EG lateral drainage area border to the EG channel border), β (the angle from the EG channel border to the bottom), and W/D (EG channel width-depth ratio), were obtained. The results revealed that, from the post-rainy season in 2014 to the post-rainy season in 2015, W, D, and A increased by 8%–25%, 20%–40%, and 35%–69%, respectively, while α, β, and W/D exhibited minor changes. EG with larger upslope drainage areas experienced more pronounced evolution, with D, A, and α increasing linearly with upslope drainage area across the three EGs, ranging from 0.05 m to 0.49 m, 67 cm2 to 2062 cm2, and 10° to 26°, respectively. A new cross-section morphological index incorporating upslope and lateral flow contributions, α·tan(β), was introduced, which showed a consistent linear relationship with the product of the upslope drainage area and the square of local slope gradient in EGs, offering a tool for predicting EG cross-sectional morphology. This study provided insights into EG evolution and illustrated the role of tillage practices in EG evolution processes, which can provide a scientific basis for the construction of gully erosion prediction models.
期刊介绍:
Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment.
Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.