雨滴溅落与集中流相互作用对不同坡度土壤剥离能力的影响

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Chenfeng Wang , Fuchun Li , Jian Wang , Xiaoming Zhang , Xiaoping Wang , Yunqi Wang , Shoujun Zhu
{"title":"雨滴溅落与集中流相互作用对不同坡度土壤剥离能力的影响","authors":"Chenfeng Wang ,&nbsp;Fuchun Li ,&nbsp;Jian Wang ,&nbsp;Xiaoming Zhang ,&nbsp;Xiaoping Wang ,&nbsp;Yunqi Wang ,&nbsp;Shoujun Zhu","doi":"10.1016/j.catena.2025.109252","DOIUrl":null,"url":null,"abstract":"<div><div>The interaction between raindrop splash and concentrated flow affecting soil detachment capacity (<em>D<sub>c</sub></em>) on gentle-to-steep slopes has rarely been studied. Three series of experiments (upstream inflow, raindrop splash, and upstream inflow with rainfall) were conducted on clay loam soil across different slope gradients. Results indicated that <em>D<sub>c</sub></em> was in the 0.0043 to 0.0058 kg m<sup>−2</sup> s<sup>−1</sup> range under raindrop splash conditions and in the 0.011 to 4.81 kg m<sup>−2</sup> s<sup>−1</sup> range under upstream inflow conditions. Compared with raindrop splash, concentrated flow scouring more significantly affected <em>D<sub>c</sub></em>. The presence of raindrop splash increased <em>D<sub>c</sub></em> by 6.45 %–85.64 % under lower unit width inflow discharge conditions and predominantly on gentler slopes under a limited number of experimental conditions. This result was attributed to the dominant effect of the additional flow discharge from rainfall-induced runoff, increasing the flow energy. Conversely, under most experimental conditions with higher inflow discharges and steeper slopes, raindrop splash reduced <em>D<sub>c</sub></em> by 10.44 %–81.91 %, which was attributed to the intensified turbulent motion and flow resistance, decreasing the flow energy. The relationships between <em>D<sub>c</sub></em> and slope gradient varied for gentle and steep slopes. A critical <em>D<sub>c</sub></em> threshold of 10°–12° slope gradients distinguished between gentle and steep slopes across all experimental treatments. The contribution of raindrop-impacted concentrated flow to <em>D<sub>c</sub></em> increased rapidly at lower flow discharges and on gentler slopes. Still, it increased more slowly at higher flow discharges and on steeper slopes. The contribution of raindrop-impacted concentrated flow to <em>D<sub>c</sub></em> ranged from 49.84 % to 99.78 %. The <em>D<sub>c</sub></em> reduction rates for this interaction effect ranged from –33.36 % to 82.02 %. This study revealed the interaction between raindrops and concentrated flow on <em>D<sub>c</sub></em> and established a slope threshold for <em>D<sub>c</sub></em>. These findings elucidate the mechanisms underlying soil detachment driven by raindrop-impacted concentrated flow and facilitate the development of process-based soil erosion models.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"258 ","pages":"Article 109252"},"PeriodicalIF":5.4000,"publicationDate":"2025-06-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Understanding the interaction between raindrop splash and concentrated flow on soil detachment capacity across different slope gradients\",\"authors\":\"Chenfeng Wang ,&nbsp;Fuchun Li ,&nbsp;Jian Wang ,&nbsp;Xiaoming Zhang ,&nbsp;Xiaoping Wang ,&nbsp;Yunqi Wang ,&nbsp;Shoujun Zhu\",\"doi\":\"10.1016/j.catena.2025.109252\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The interaction between raindrop splash and concentrated flow affecting soil detachment capacity (<em>D<sub>c</sub></em>) on gentle-to-steep slopes has rarely been studied. Three series of experiments (upstream inflow, raindrop splash, and upstream inflow with rainfall) were conducted on clay loam soil across different slope gradients. Results indicated that <em>D<sub>c</sub></em> was in the 0.0043 to 0.0058 kg m<sup>−2</sup> s<sup>−1</sup> range under raindrop splash conditions and in the 0.011 to 4.81 kg m<sup>−2</sup> s<sup>−1</sup> range under upstream inflow conditions. Compared with raindrop splash, concentrated flow scouring more significantly affected <em>D<sub>c</sub></em>. The presence of raindrop splash increased <em>D<sub>c</sub></em> by 6.45 %–85.64 % under lower unit width inflow discharge conditions and predominantly on gentler slopes under a limited number of experimental conditions. This result was attributed to the dominant effect of the additional flow discharge from rainfall-induced runoff, increasing the flow energy. Conversely, under most experimental conditions with higher inflow discharges and steeper slopes, raindrop splash reduced <em>D<sub>c</sub></em> by 10.44 %–81.91 %, which was attributed to the intensified turbulent motion and flow resistance, decreasing the flow energy. The relationships between <em>D<sub>c</sub></em> and slope gradient varied for gentle and steep slopes. A critical <em>D<sub>c</sub></em> threshold of 10°–12° slope gradients distinguished between gentle and steep slopes across all experimental treatments. The contribution of raindrop-impacted concentrated flow to <em>D<sub>c</sub></em> increased rapidly at lower flow discharges and on gentler slopes. Still, it increased more slowly at higher flow discharges and on steeper slopes. The contribution of raindrop-impacted concentrated flow to <em>D<sub>c</sub></em> ranged from 49.84 % to 99.78 %. The <em>D<sub>c</sub></em> reduction rates for this interaction effect ranged from –33.36 % to 82.02 %. This study revealed the interaction between raindrops and concentrated flow on <em>D<sub>c</sub></em> and established a slope threshold for <em>D<sub>c</sub></em>. These findings elucidate the mechanisms underlying soil detachment driven by raindrop-impacted concentrated flow and facilitate the development of process-based soil erosion models.</div></div>\",\"PeriodicalId\":9801,\"journal\":{\"name\":\"Catena\",\"volume\":\"258 \",\"pages\":\"Article 109252\"},\"PeriodicalIF\":5.4000,\"publicationDate\":\"2025-06-25\",\"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/S0341816225005545\",\"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}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0341816225005545","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

摘要

在缓陡坡上,雨滴溅落与集中流相互作用对土壤脱离能力的影响研究较少。在不同坡度的粘壤土上进行了上游入流、雨滴溅射和上游降雨入流3个系列试验。结果表明,雨滴溅射条件下Dc在0.0043 ~ 0.0058 kg m−2 s−1范围内,上游入流条件下Dc在0.011 ~ 4.81 kg m−2 s−1范围内。与雨滴溅射相比,集中流冲刷对直流的影响更为显著。在较低单位宽度入流条件下,雨滴溅射的存在使直流增加了6.45% ~ 85.64%,在有限的试验条件下,主要是在较平缓的斜坡上。这一结果的主要原因是降雨径流的附加流量增加了径流能量。相反,在大多数较大流入流量和较陡坡度的实验条件下,雨滴飞溅使Dc降低了10.44% ~ 81.91%,这是由于湍流运动和流动阻力加剧,流动能降低所致。缓坡和陡坡的Dc与坡度的关系有所不同。在所有试验处理中,10°-12°坡度的临界Dc阈值区分了平缓和陡峭的斜坡。在低流量和缓坡条件下,雨滴影响的集中流对直流电的贡献迅速增加。尽管如此,在高流量和陡坡上,它增加得更慢。雨滴冲击集中流对直流的贡献在49.84% ~ 99.78%之间。这种相互作用的直流降低率从- 33.36%到82.02%不等。本研究揭示了直流上雨滴与集中流的相互作用,建立了直流的斜率阈值。这些发现阐明了雨滴影响的集中流驱动土壤剥离的机制,促进了基于过程的土壤侵蚀模型的发展。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Understanding the interaction between raindrop splash and concentrated flow on soil detachment capacity across different slope gradients
The interaction between raindrop splash and concentrated flow affecting soil detachment capacity (Dc) on gentle-to-steep slopes has rarely been studied. Three series of experiments (upstream inflow, raindrop splash, and upstream inflow with rainfall) were conducted on clay loam soil across different slope gradients. Results indicated that Dc was in the 0.0043 to 0.0058 kg m−2 s−1 range under raindrop splash conditions and in the 0.011 to 4.81 kg m−2 s−1 range under upstream inflow conditions. Compared with raindrop splash, concentrated flow scouring more significantly affected Dc. The presence of raindrop splash increased Dc by 6.45 %–85.64 % under lower unit width inflow discharge conditions and predominantly on gentler slopes under a limited number of experimental conditions. This result was attributed to the dominant effect of the additional flow discharge from rainfall-induced runoff, increasing the flow energy. Conversely, under most experimental conditions with higher inflow discharges and steeper slopes, raindrop splash reduced Dc by 10.44 %–81.91 %, which was attributed to the intensified turbulent motion and flow resistance, decreasing the flow energy. The relationships between Dc and slope gradient varied for gentle and steep slopes. A critical Dc threshold of 10°–12° slope gradients distinguished between gentle and steep slopes across all experimental treatments. The contribution of raindrop-impacted concentrated flow to Dc increased rapidly at lower flow discharges and on gentler slopes. Still, it increased more slowly at higher flow discharges and on steeper slopes. The contribution of raindrop-impacted concentrated flow to Dc ranged from 49.84 % to 99.78 %. The Dc reduction rates for this interaction effect ranged from –33.36 % to 82.02 %. This study revealed the interaction between raindrops and concentrated flow on Dc and established a slope threshold for Dc. These findings elucidate the mechanisms underlying soil detachment driven by raindrop-impacted concentrated flow and facilitate the development of process-based soil erosion models.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
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.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信