Wenting Nie , Zhihua Zhang , Li Li , Shulan Tan , YuHui Guo , Gigen Liu , Jinquan Huang , Jianming Li , Xiaoxia Tong
{"title":"The effects of overall slope on soil surface roughness estimation","authors":"Wenting Nie , Zhihua Zhang , Li Li , Shulan Tan , YuHui Guo , Gigen Liu , Jinquan Huang , Jianming Li , Xiaoxia Tong","doi":"10.1016/j.still.2025.106618","DOIUrl":null,"url":null,"abstract":"<div><div>Soil surface roughness (<em>SSR</em>) is essential for understanding and modeling soil erosion processes, while whether the overall slope of the investigated terrain surface must be corrected before <em>SSR</em> estimation is still unknown. This study aims to investigate the effects of overall slope on <em>SSR</em> and associated temporal change estimates by using the high-resolution digital elevation models (DEMs) from the rainfall simulation experiments of Nearing et al. (2017) wherein medium-term rainfalls (ca. 10–20 years) were simulated on a 2 m by 6.1 m stony plot under three slope treatments (5 %, 12 %, and 20 %). Square moving windows with different sizes (<span><math><msub><mrow><mi>W</mi></mrow><mrow><mi>Z</mi></mrow></msub></math></span>) covering the topographic DEMs were used to estimate <em>SSR</em> for each slope treatment before and after each rainfall simulation under the slope-detrending (DT) and no-detrending (NDT) scenarios. Results showed that: (1) The estimated <em>SSR</em> linearly increased with <span><math><msub><mrow><mi>W</mi></mrow><mrow><mi>Z</mi></mrow></msub></math></span> under the NDT scenario while it increased rapidly for small <span><math><msub><mrow><mi>W</mi></mrow><mrow><mi>Z</mi></mrow></msub></math></span> and tended toward asymptotes for large <span><math><msub><mrow><mi>W</mi></mrow><mrow><mi>Z</mi></mrow></msub></math></span> under the DT scenario. (2) With increasing window size, the standard deviations of <em>SSR</em> increased under the NDT scenario but decreased under the DT scenario. (3) Without correcting the overall slope effects, <em>SSR</em> was overestimated while the temporal change of <em>SSR</em> was significantly underestimated reaching up to −175 % as compared to the DT scenario, and the underestimation was positively correlated with slope gradient, the true <em>SSR</em> temporal change, and window size. We mathematically illustrated that the estimated <em>SSR</em> under the NDT scenario in fact consisted of oriented roughness that was resultant from the systematic elevation variation rather than soil surface random roughness alone, and the overall slope effects must be corrected before <em>SSR</em> estimation for effectively tracking <em>SSR</em> temporal changes. The results provide guidance about the level of accuracy one might expect in evaluating <em>SSR</em> and associated temporal changes at hillslopes with different overall slopes.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"252 ","pages":"Article 106618"},"PeriodicalIF":6.1000,"publicationDate":"2025-04-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Soil & Tillage Research","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0167198725001722","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
引用次数: 0
Abstract
Soil surface roughness (SSR) is essential for understanding and modeling soil erosion processes, while whether the overall slope of the investigated terrain surface must be corrected before SSR estimation is still unknown. This study aims to investigate the effects of overall slope on SSR and associated temporal change estimates by using the high-resolution digital elevation models (DEMs) from the rainfall simulation experiments of Nearing et al. (2017) wherein medium-term rainfalls (ca. 10–20 years) were simulated on a 2 m by 6.1 m stony plot under three slope treatments (5 %, 12 %, and 20 %). Square moving windows with different sizes () covering the topographic DEMs were used to estimate SSR for each slope treatment before and after each rainfall simulation under the slope-detrending (DT) and no-detrending (NDT) scenarios. Results showed that: (1) The estimated SSR linearly increased with under the NDT scenario while it increased rapidly for small and tended toward asymptotes for large under the DT scenario. (2) With increasing window size, the standard deviations of SSR increased under the NDT scenario but decreased under the DT scenario. (3) Without correcting the overall slope effects, SSR was overestimated while the temporal change of SSR was significantly underestimated reaching up to −175 % as compared to the DT scenario, and the underestimation was positively correlated with slope gradient, the true SSR temporal change, and window size. We mathematically illustrated that the estimated SSR under the NDT scenario in fact consisted of oriented roughness that was resultant from the systematic elevation variation rather than soil surface random roughness alone, and the overall slope effects must be corrected before SSR estimation for effectively tracking SSR temporal changes. The results provide guidance about the level of accuracy one might expect in evaluating SSR and associated temporal changes at hillslopes with different overall slopes.
期刊介绍:
Soil & Tillage Research examines the physical, chemical and biological changes in the soil caused by tillage and field traffic. Manuscripts will be considered on aspects of soil science, physics, technology, mechanization and applied engineering for a sustainable balance among productivity, environmental quality and profitability. The following are examples of suitable topics within the scope of the journal of Soil and Tillage Research:
The agricultural and biosystems engineering associated with tillage (including no-tillage, reduced-tillage and direct drilling), irrigation and drainage, crops and crop rotations, fertilization, rehabilitation of mine spoils and processes used to modify soils. Soil change effects on establishment and yield of crops, growth of plants and roots, structure and erosion of soil, cycling of carbon and nutrients, greenhouse gas emissions, leaching, runoff and other processes that affect environmental quality. Characterization or modeling of tillage and field traffic responses, soil, climate, or topographic effects, soil deformation processes, tillage tools, traction devices, energy requirements, economics, surface and subsurface water quality effects, tillage effects on weed, pest and disease control, and their interactions.