生物炭-植被协同防护膨胀土边坡的抗裂防渗特性研究OA
Cracking resistance and anti-seepage performance of expansive soil slopes under biochar-vegetation synergistic protection
为提升干湿循环作用下膨胀土边坡表层的抗裂防渗性能,充分发挥植被护坡的生态效益,本文提出一种生物炭-植被协同防护新方法.通过开展室外膨胀土边坡干湿循环试验,实时监测边坡体积含水率、植被生长参数和裂隙形态特征指标,探明生物炭-植被协同作用对膨胀土边坡裂隙演化以及雨水入渗行为的影响规律.研究结果表明:生物炭-植被协同防护可显著增强膨胀土边坡的抗裂性能;在干湿循环过程中,素膨胀土边坡(S1)和植被防护膨胀土边坡(S2)的坡面易产生大量裂隙,相邻主次裂隙快速交叉相连,形成复杂的裂隙网络,而生物炭-植被协同防护膨胀土边坡(S3)的坡面裂隙发育相对缓慢,与S1和S2的坡面裂隙相比,其裂缝率最高分别减小了51.92%和40.89%;生物炭-植被主要通过减弱膨胀土的胀缩性、降低干燥引发的张拉应力以及提高土体抗拉强度来协同抑制膨胀土边坡的裂隙发育,显著提升膨胀土边坡的防渗性能;在裂隙优先流作用下,S1和S2的坡体内部均形成暂态饱和区并使基质吸力大幅降低,而S3的坡体内部体积含水率和基质吸力无明显变化.研究结果可为膨胀土边坡表层的生态防护设计提供参考.
To enhance the cracking resistance and anti-seepage performance of expansive soil slope surfaces in wetting-drying cycles while maximizing the ecological benefits of vegetation,a novel synergistic protection method combining biochar and vegetation was proposed.Outdoor wetting-drying cycle tests were conducted on expansive soil slopes,with real-time monitoring of volumetric water content,vegetation growth parameters and crack morphological indicators.The influence of the biochar-vegetation synergistic effect on crack evolution and rainwater infiltration behavior were elucidated.The results indicate that the synergistic protection significantly strengthens the cracking resistance of expansive soil slopes.During wetting-drying cycles,extensive cracks develop on surfaces of bare expansive soil slope(S1)and the vegetation-only protected slope(S2),where adjacent primary and secondary cracks rapidly intersects to form complex networks.In contrast,crack development on biochar-vegetation protected slope(S3)is relatively slow,with the peak crack ratio reduced by 51.92%and 40.89%compared to S1 and S2,respectively.The synergistic mechanism primarily involves mitigating the swell-shrink potential,reducing the dehydration-induced tensile stress field,and enhancing the tensile strength of the soil.Consequently,the anti-seepage performance of the slope is significantly improved due to crack suppression.Under the influence of preferential flow through cracks,transient saturated zones are formed within S1 and S2,leading to a sharp decline in matric suction.Conversely,the volumetric water content and matric suction within S3 remain relatively stable.These findings provide a theoretical basis and practical reference for the ecological protection design of expansive soil slope surfaces.
欧阳淼;兰素恋;谢云鹏;张红日;覃永晖;李珍玉;林宇亮
湖南文理学院 土木建筑工程学院,湖南 常德,415000广西交通职业技术学院,广西 南宁,530001山东大学 齐鲁交通学院,山东 济南,250100广西交科集团有限公司,广西 南宁,530007||上海交通大学土木工程系,上海,200240||广西大学 土木建筑工程学院,广西 南宁,530004湖南文理学院 土木建筑工程学院,湖南 常德,415000中南林业科技大学 土木工程学院,湖南 长沙,410004中南大学 土木工程学院,湖南 长沙,410083
交通工程
防灾减灾膨胀土生物炭协同防护裂隙演化优先流
disaster prevention and mitigationexpansive soilbiocharsynergistic protectioncrack evolutionpreferential flow
《中南大学学报(自然科学版)》 2026 (5)
2281-2291,11
国家自然科学基金资助项目(42330701,42477143)广西重大人才项目(2024)广西重点研发计划项目(桂科AB23075184)博士科研启动项目(25BSQD68)崇左市特殊土与工程防灾减灾重点实验室2025年度开放课题项目(TST202503)(Projects(42330701,42477143)supported by the National Natural Science Foundation of ChinaProject(2024)supported by the Major Talent Project of Guangxi Zhuang Autonomous RegionProject(Guike AB23075184)supported by the Key Research and Development Program of Guangxi Zhuang AutonomousProject(25BSQD68)supported by the Doctoral Scientific Research Startup FoundationProject(TST202503)supported by the 2025 Open Project of Chongzuo Key Laboratory of Special Soil and Engineering Disaster Prevention and Mitigation)
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