Ephemeral gully evolution and morphological changes in the erosion-tillage-erosion cycle on steep loess slopes

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Wenqian Liang , Ximeng Xu , Fenli Zheng , Chao Qin
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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.
黄土陡坡侵蚀-耕作-侵蚀循环中沟壑的短暂演化与形态变化
短期沟分布在世界各地的农田中,在土壤流失和土地退化中起着重要作用。然而,EG河道的完整旋回演化过程,包括形成、耕作湮没和随后降雨下的改造,仍未得到充分研究。因此,本研究旨在利用地面激光扫描仪(Terrestrial Laser Scanner)获取的0.01 m分辨率数字高程模型(dem),研究黄土陡坡面侵蚀-耕作-侵蚀循环的EG演化和形态变化。共提取了3个EG的107个断面,得到了EG的6个形态指标,包括W (EG通道宽度)、D (EG通道深度)、A (EG通道截面积)、α (EG侧水区边界到EG通道边界的夹角)、β (EG通道边界到底部的夹角)和W/D (EG通道宽深比)。结果表明,2014年雨季后至2015年雨季后,W、D和A分别增加了8% ~ 25%、20% ~ 40%和35% ~ 69%,而α、β和W/D变化较小。上坡流域面积较大的EG演化更为明显,D、A和α随上坡流域面积的增加呈线性增加,分别为0.05 m ~ 0.49 m、67 cm2 ~ 2062 cm2和10°~ 26°。引入了一种结合上坡和侧向水流贡献的新断面形态指标α·tan(β),该指标与上坡流域面积与局部坡度平方的乘积呈一致的线性关系,为预测EG断面形态提供了工具。该研究揭示了土壤侵蚀演化过程,阐明了耕作方式在土壤侵蚀演化过程中的作用,可为建立沟壑区侵蚀预测模型提供科学依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
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.
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