Soil surface roughness impacts erosion behavior through selective regulation of flow properties in rainfall-seepage scenarios

IF 6.1 1区农林科学 Q1 SOIL SCIENCE Soil & Tillage Research Pub Date : 2024-11-05 DOI:10.1016/j.still.2024.106350

Nana Wang , Zicheng Zheng , Tingxuan Li , Shuqin He , Xizhou Zhang , Yongdong Wang , Haiying Yu , Huagang Huang , Daihua Ye

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Abstract

Soil surface roughness (SSR) impacts runoff dynamics of surface-subsurface and the magnitude of soil erosion, limited attention has been paid to how SSR governs runoff hydrodynamics to affect erosion behavior and the effectiveness of erosion reduction under rainfall-seepage scenarios on low-permeability purple soil slopes. Herein the seepage rates of 2, 4, and 8 L min⁻¹ were sequentially simulated under a rainfall intensity of 1.0 mm min⁻¹ among different microrelief treatments (CT: conventional tillage; AD: artificial digging; RT: ridge tillage) on purple soil slopes with gradients of 5°, 10°, and 15°. These simulations aimed to investigate the mechanisms underlying the erosion reduction benefits associated with flow properties due to microrelief. The results showed that increased SSR altered erosion kinetic energy under rainfall-seepage conditions. The benefits of rough slopes to control erosion decreased as rainfall-seepage intensity and slope gradient increased. During rainfall-seepage events, the variation in runoff behavior was regulated positively by the effect of SSR on unit stream power. However, the increasing net output power of runoff due to flow turbulence altered sediment output, thereby affecting sediment control benefits. Overall, the impact of rainfall-seepage intensity on surface roughness became more significant with increasing slope gradient. Our findings suggest the capable of integrating for interrelated microrelief and runoff processes in factors analysis of driving soil erosion at rainfall-seepage hydrologic states to elucidate erosion effect.

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土壤表面粗糙度通过选择性调节降雨-渗流情景中的流动特性影响侵蚀行为

土壤表面粗糙度（SSR）影响表层-次表层径流动力学和土壤侵蚀程度，但人们对 SSR 如何调节径流流体力学以影响侵蚀行为以及在低渗透性紫色土斜坡上降雨-渗流情况下减少侵蚀效果的关注还很有限。本文模拟了在梯度为 5°、10° 和 15°的紫色土壤斜坡上，在降雨强度为 1.0 mm min-¹ 的情况下，不同微灌处理（CT：常规耕作；AD：人工挖掘；RT：脊耕）的渗流率依次为 2、4 和 8 L min-¹。这些模拟旨在研究微疏松带来的与流动特性相关的侵蚀减少效益的内在机制。结果表明，在降雨-渗流条件下，SSR 的增加改变了侵蚀动能。随着降雨-渗流强度和坡度的增加，糙面斜坡对控制侵蚀的益处也在减少。在降雨-渗流事件中，径流行为的变化受 SSR 对单位水流功率影响的正向调节。然而，由于水流湍动导致径流净输出功率增加，从而改变了沉积物的输出量，从而影响了沉积物控制效益。总体而言，降雨-渗流强度对地表粗糙度的影响随着坡度的增加而变得更加显著。我们的研究结果表明，在对降雨-渗流水文状态下的土壤侵蚀驱动因素进行分析时，可以综合考虑相互关联的微解脱过程和径流过程，以阐明侵蚀效应。

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来源期刊

Soil & Tillage Research 农林科学-土壤科学

CiteScore

13.00

自引率

6.20%

发文量

266

审稿时长

5 months

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.