首页|冻融循环条件下含根系土的力学特性

冻融循环条件下含根系土的力学特性

扫码查看
植物根系对土体有力学加筋作用,可以有效提高土体的强度,防止浅层滑坡和地表侵蚀,因而广泛应用于边坡防护。然而在中西部的季节冻土区,植被边坡的土体反复冻结融化,在植物根系力学加筋和冻融损伤的双重作用下,其力学性质也会发生变化,对边坡稳定性产生不确定因素。因此,为探究冻融和根系分布对土体的复合影响,采用贡嘎山海螺沟流域土壤及花楸根系进行三轴固结不排水试验,研究了冻融循环作用下,含根系土体的强度变化。考虑不同冻融循环次数(0、1、5次)和根系分布方式(竖向均匀分布:三层各一根;水平均匀分布:中间一层三根),绘制应力应变曲线和孔压应变曲线,对比分析两种试样的应力应变特性,并通过抗剪强度包线获得总应力抗剪强度指标和有效应力抗剪强度指标。结果表明:(1)随冻融循环次数的增加,三层各一根试样和中间三根试样的峰值强度均逐渐降低,黏聚力和内摩擦力也逐渐减小,在低围压(25 kPa)条件下冻融循环作用对含根系土强度减弱作用较为明显,但在高围压条件下,植物根系对土的强度的增强作用仍不可忽视;(2)即使发生了冻融循环,根系仍在一定程度上提高了土体的强度,其增强效果受到分布方式的影响,三层各一根的排列方式增强作用最显著;(3)在相同围压、相同冻融循环次数条件下,根系沿竖向分布的试样峰值强度和黏聚力均较高,此外,相较于不含根的素土,根系分布方式主要影响土的黏聚力,对内摩擦角的影响不明显。研究成果可为寒区植被护坡的工程实践提供理论依据。
Mechanical properties of root-bearing soils under freeze-thaw cycles
Plants are the engineers of the nature,they can effectively improve the strength of the soil and can en-hance the stability of shallow soil slopes and minimizing surface erosion.for their mechanical reinforcement to soil.Therefore,they are widely used in slope protection.However,in the seasonal frozen soil regions of the central and western areas,the repeated freeze-thaw cycles of vegetation slopes lead to changes in soil mechanics under the dual effects of plant root reinforcement and freeze-thaw damage,introducing uncertainties in slope sta-bility.Therefore,to explore the combined impact of freeze-thaw cycles and root distribution on soil,triaxial consolidation undrained(CU)tests were conducted under confining pressure from 25 kPa to 400 kPa,consider-ing different freeze-thaw cycles(0,1,5 cycles)and root distribution(vertical uniform distribution:one root in each of the three layers;horizontal uniform distribution:three roots in the middle layer).The materials were prepared with sands and sorbus pohuashanensis roots from Hailuogou in Minya Konka.To investigated the strength variations of root-containing soil under freeze-thaw cycles,stress-strain curves and pore pressure-strain curves were plotted respectively.Then the analysis of the stress-strain characteristics of the samples under differ-ent conditions was performed,and the total stress strength parameters and effective stress strength parameters were obtained from the shear strength envelopes.The results revealed that:(1)with the increase of freeze-thaw cycles,the peak strength of both the one-root-per-layer and three-roots-in-the-middle-layer samples gradually de-creased,along with reduced cohesion and internal friction.Under low confining pressure(25 kPa),the weaken-ing effect of freeze-thaw cycles on root-containing soil strength was more pronounced.However,under high confining pressure,the strengthening effect of plant roots on soil strength remained significant.(2)Under differ-ent freeze-thaw cycles,roots can still enhance the soil's strength to a certain extent,and the arrangement of one root in each of the three layers showed the most significant enhancement effect.The roots contact with soil,which leads to irregular occlusions and"self-locking",which has a positive effect on the enhancement of shear strength.(3)Under the same freeze-thaw cycle and confining pressure,samples with vertically distributed roots exhibited higher strength and cohesion,because the contact area was larger of roots placed in three layers along the height of the sample than the other distribution of samples.The distribution pattern of roots mainly influ-enced the soil's cohesion,with minimal impact on the internal friction angle.These findings can provide a theo-retical basis for ecological slope protection in cold regions.

freeze-thaw cyclesroot-bearing soiltriaxial testsshear strength

唐诗佳、刘恩龙、杨柳新

展开 >

四川大学 水利水电学院 水力学与山区河流开发保护国家重点实验室,四川 成都 610065

中国科学院西北生态环境资源研究院 冻土工程国家重点实验室,甘肃 兰州 730000

冻融循环 含根系土 三轴试验 抗剪强度

国家自然科学基金重大项目

41790431

2024

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCD
影响因子:2.546
ISSN:1000-0240
年,卷(期):2024.46(1)
  • 19