Three-dimensional numerical modeling of soil-roots system based on X-ray computed tomography: Hydraulic effects study

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC
Ji-Peng Wang , Jun-Feng Sha , Shangqi Ge , Xu-Guang Gao , Abdelali Dadda
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Abstract

Vegetation roots enhance soil stability by influencing saturation and pore structure, playing a pivotal role in stabilizing slopes, reducing erosion, and enhancing soil structure. However, current research on the hydraulic effects of roots on soil remains relatively limited. The micro-mechanisms of vegetation's impact on soil and the macro-level connections are not yet fully understood, which poses a challenge to the modeling of root-soil system. This study develops a three-dimensional (3D) finite element model of root-soil composites based on root computed tomography (CT) images and experimental results. Four different groups are modeled, including the rootless group, and those with Festuca arundinacea (FA) roots at various growth stages. The simulation results show that the saturation in the shallow layers significantly decreases in root-soil composite groups, and the rhizosphere water content is lower than that away from the roots, resulting in a net water flux toward the roots. The influence range of roots on suction is gradually amplified with increasing root growth process and root water uptake time. Higher levels of root development result in a stronger overall water uptake effect, leading to a more pronounced decrease in saturation. Closer proximity to the surface roots results in a more rapid increase in soil suction. Compared with one-dimensional root water uptake models, this model considers the effects of spatial heterogeneity of root structures on soil, which provides a comprehensive modeling basis for studying the effect of root system on soil.
基于 X 射线计算机断层扫描的土壤-根系三维数值建模:水力效应研究
植被根系通过影响饱和度和孔隙结构来增强土壤稳定性,在稳定斜坡、减少侵蚀和增强土壤结构方面发挥着举足轻重的作用。然而,目前关于根系对土壤的水力影响的研究仍然相对有限。植被对土壤影响的微观机制和宏观层面的联系尚未被完全理解,这给根系-土壤系统建模带来了挑战。本研究基于根部计算机断层扫描(CT)图像和实验结果,建立了根-土复合材料的三维(3D)有限元模型。模拟了四组不同的根-土复合材料,包括无根组和有不同生长阶段的根的根。模拟结果表明,在根-土复合组中,浅层的饱和度明显降低,根圈含水量低于远离根部的含水量,导致净水流向根部。根系对吸力的影响范围随着根系生长过程和根系吸水时间的增加而逐渐扩大。根系发育程度越高,整体吸水效果越强,导致饱和度下降越明显。更靠近表层的根系会使土壤吸力增加得更快。与一维根系吸水模型相比,该模型考虑了根系结构的空间异质性对土壤的影响,为研究根系对土壤的影响提供了全面的建模基础。
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
CiteScore
7.20
自引率
4.30%
发文量
567
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