{"title":"灌丛根径等级对蚌钢崩落墙土体抗剪强度的影响","authors":"Fang Shuai, Wei Wu, Ying Meng, Yiyang Zhou, Yuyang Chen, Yue Zhang, Jinshi Lin, Yanhe Huang, Fangshi Jiang","doi":"10.1002/esp.70128","DOIUrl":null,"url":null,"abstract":"<p>A Benggang is a typical soil erosion landform in the red-soil region of southern China. Its collapsing-wall stability is closely related to the soil shear performance, which can be mechanically reinforced by plant roots. Shrub-root reinforcement mechanisms and model optimization have not been studied systematically. This study considers <i>Melastoma candidum</i>, a dominant shrub species in southern Benggang areas. Using remolded soil direct shear tests, the effects of different moisture content levels and root diameter classes on the shear characteristics of root–soil composites are explored. A shear strength equation for root-soil composites, based on the Wu–Waldron model (WWM), was established, incorporating soil moisture content and root diameter (Equations (12) and (13)). The key findings are as follows: (1) Roots significantly enhance soil shear strength and cohesion. At 15% moisture content, 1.50–3.00-mm roots provide optimal shear strength improvement; at 25% moisture content, 0.00–1.50-mm roots perform best, but achieve maximum cohesion enhancement under both moisture conditions. (2) Increased moisture content significantly reduces root–soil composite shear strength and cohesion. (3) Root diameter variation minimally affects the soil internal friction angle, which decreases with increasing moisture content. (4) The WWM overestimated the measured shear strength by ≥5.60 times. Incorporating the moisture content and root diameter, the WWM correction coefficient was 0.02–0.18, and the newly established shear strength prediction equations based on the Mohr-Coulomb criterion and the WWM model demonstrated significantly improved accuracy (<i>R</i><sup><i>2</i></sup>, Nash–Sutcliffe efficiency [<i>NSE</i>] ≥ 0.92). These findings elucidate shrub-root regulatory mechanisms on collapsing-wall stability and provide theoretical support for vegetation allocation strategies and soil-reinforcement model optimization in red-soil erosion areas.</p>","PeriodicalId":11408,"journal":{"name":"Earth Surface Processes and Landforms","volume":"50 9","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2025-07-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Effect of shrub root diameter classes on shear strength of soil in Benggang collapsing walls\",\"authors\":\"Fang Shuai, Wei Wu, Ying Meng, Yiyang Zhou, Yuyang Chen, Yue Zhang, Jinshi Lin, Yanhe Huang, Fangshi Jiang\",\"doi\":\"10.1002/esp.70128\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>A Benggang is a typical soil erosion landform in the red-soil region of southern China. Its collapsing-wall stability is closely related to the soil shear performance, which can be mechanically reinforced by plant roots. Shrub-root reinforcement mechanisms and model optimization have not been studied systematically. This study considers <i>Melastoma candidum</i>, a dominant shrub species in southern Benggang areas. Using remolded soil direct shear tests, the effects of different moisture content levels and root diameter classes on the shear characteristics of root–soil composites are explored. A shear strength equation for root-soil composites, based on the Wu–Waldron model (WWM), was established, incorporating soil moisture content and root diameter (Equations (12) and (13)). The key findings are as follows: (1) Roots significantly enhance soil shear strength and cohesion. At 15% moisture content, 1.50–3.00-mm roots provide optimal shear strength improvement; at 25% moisture content, 0.00–1.50-mm roots perform best, but achieve maximum cohesion enhancement under both moisture conditions. (2) Increased moisture content significantly reduces root–soil composite shear strength and cohesion. (3) Root diameter variation minimally affects the soil internal friction angle, which decreases with increasing moisture content. (4) The WWM overestimated the measured shear strength by ≥5.60 times. Incorporating the moisture content and root diameter, the WWM correction coefficient was 0.02–0.18, and the newly established shear strength prediction equations based on the Mohr-Coulomb criterion and the WWM model demonstrated significantly improved accuracy (<i>R</i><sup><i>2</i></sup>, Nash–Sutcliffe efficiency [<i>NSE</i>] ≥ 0.92). These findings elucidate shrub-root regulatory mechanisms on collapsing-wall stability and provide theoretical support for vegetation allocation strategies and soil-reinforcement model optimization in red-soil erosion areas.</p>\",\"PeriodicalId\":11408,\"journal\":{\"name\":\"Earth Surface Processes and Landforms\",\"volume\":\"50 9\",\"pages\":\"\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2025-07-09\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Earth Surface Processes and Landforms\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1002/esp.70128\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth Surface Processes and Landforms","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/esp.70128","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
Effect of shrub root diameter classes on shear strength of soil in Benggang collapsing walls
A Benggang is a typical soil erosion landform in the red-soil region of southern China. Its collapsing-wall stability is closely related to the soil shear performance, which can be mechanically reinforced by plant roots. Shrub-root reinforcement mechanisms and model optimization have not been studied systematically. This study considers Melastoma candidum, a dominant shrub species in southern Benggang areas. Using remolded soil direct shear tests, the effects of different moisture content levels and root diameter classes on the shear characteristics of root–soil composites are explored. A shear strength equation for root-soil composites, based on the Wu–Waldron model (WWM), was established, incorporating soil moisture content and root diameter (Equations (12) and (13)). The key findings are as follows: (1) Roots significantly enhance soil shear strength and cohesion. At 15% moisture content, 1.50–3.00-mm roots provide optimal shear strength improvement; at 25% moisture content, 0.00–1.50-mm roots perform best, but achieve maximum cohesion enhancement under both moisture conditions. (2) Increased moisture content significantly reduces root–soil composite shear strength and cohesion. (3) Root diameter variation minimally affects the soil internal friction angle, which decreases with increasing moisture content. (4) The WWM overestimated the measured shear strength by ≥5.60 times. Incorporating the moisture content and root diameter, the WWM correction coefficient was 0.02–0.18, and the newly established shear strength prediction equations based on the Mohr-Coulomb criterion and the WWM model demonstrated significantly improved accuracy (R2, Nash–Sutcliffe efficiency [NSE] ≥ 0.92). These findings elucidate shrub-root regulatory mechanisms on collapsing-wall stability and provide theoretical support for vegetation allocation strategies and soil-reinforcement model optimization in red-soil erosion areas.
期刊介绍:
Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with:
the interactions between surface processes and landforms and landscapes;
that lead to physical, chemical and biological changes; and which in turn create;
current landscapes and the geological record of past landscapes.
Its focus is core to both physical geographical and geological communities, and also the wider geosciences