矿冶工程
礦冶工程
광야공정
2014年
4期
1-5
,共5页
石熊%张家生%彭状%王嵩%宋良良
石熊%張傢生%彭狀%王嵩%宋良良
석웅%장가생%팽상%왕숭%송량량
加筋粗粒土%大型三轴试验%大型直剪试验
加觔粗粒土%大型三軸試驗%大型直剪試驗
가근조립토%대형삼축시험%대형직전시험
reinforced coarse-grained soil%large-scale triaxial test%large-scale direct shear test
采用大型三轴仪与大型直剪仪,对粗粒土、加筋土强度变形特性进行了实验研究。直剪试验结果表明:不同竖向荷载下粗粒土和加筋粗粒土剪切的剪应力-剪切位移关系类似,应力应变曲线均出现应变软化现象,但软化特性变化不大;加筋土法向位移-剪切位移变化曲线表现为法向应力越低,剪胀现象越明显;粗粒土加筋后的内聚力增加,但是内摩擦角却降低。三轴试验结果表明,不同围压条件下粗粒土和加筋土主应力差与轴向应变关系曲线表现为应变硬化型,围压越大,主应力差与轴向应变关系曲线越陡,应变硬化特性越明显,最大主应力差越大;围压越低,剪胀作用越明显,越容易由剪缩发展到剪胀,反之围压越高,则剪缩作用越明显;当轴向应变较小时,加筋效果不明显,随着轴向应变的逐渐增大,加筋效果逐渐发挥。加筋土的内聚力明显大于粗粒土,而内摩擦角基本上相等;利用三轴试验结果对邓肯-张模型的适用性进行了分析研究,表明邓肯-张模型能合理地确定粗粒土与加筋土的强度以及切线弹性模量,但难以描述和确定粗粒土的变形特性和切线泊松比,且不能反映粗粒土的剪胀性。
採用大型三軸儀與大型直剪儀,對粗粒土、加觔土彊度變形特性進行瞭實驗研究。直剪試驗結果錶明:不同豎嚮荷載下粗粒土和加觔粗粒土剪切的剪應力-剪切位移關繫類似,應力應變麯線均齣現應變軟化現象,但軟化特性變化不大;加觔土法嚮位移-剪切位移變化麯線錶現為法嚮應力越低,剪脹現象越明顯;粗粒土加觔後的內聚力增加,但是內摩抆角卻降低。三軸試驗結果錶明,不同圍壓條件下粗粒土和加觔土主應力差與軸嚮應變關繫麯線錶現為應變硬化型,圍壓越大,主應力差與軸嚮應變關繫麯線越陡,應變硬化特性越明顯,最大主應力差越大;圍壓越低,剪脹作用越明顯,越容易由剪縮髮展到剪脹,反之圍壓越高,則剪縮作用越明顯;噹軸嚮應變較小時,加觔效果不明顯,隨著軸嚮應變的逐漸增大,加觔效果逐漸髮揮。加觔土的內聚力明顯大于粗粒土,而內摩抆角基本上相等;利用三軸試驗結果對鄧肯-張模型的適用性進行瞭分析研究,錶明鄧肯-張模型能閤理地確定粗粒土與加觔土的彊度以及切線彈性模量,但難以描述和確定粗粒土的變形特性和切線泊鬆比,且不能反映粗粒土的剪脹性。
채용대형삼축의여대형직전의,대조립토、가근토강도변형특성진행료실험연구。직전시험결과표명:불동수향하재하조립토화가근조립토전절적전응력-전절위이관계유사,응력응변곡선균출현응변연화현상,단연화특성변화불대;가근토법향위이-전절위이변화곡선표현위법향응력월저,전창현상월명현;조립토가근후적내취력증가,단시내마찰각각강저。삼축시험결과표명,불동위압조건하조립토화가근토주응력차여축향응변관계곡선표현위응변경화형,위압월대,주응력차여축향응변관계곡선월두,응변경화특성월명현,최대주응력차월대;위압월저,전창작용월명현,월용역유전축발전도전창,반지위압월고,칙전축작용월명현;당축향응변교소시,가근효과불명현,수착축향응변적축점증대,가근효과축점발휘。가근토적내취력명현대우조립토,이내마찰각기본상상등;이용삼축시험결과대산긍-장모형적괄용성진행료분석연구,표명산긍-장모형능합리지학정조립토여가근토적강도이급절선탄성모량,단난이묘술화학정조립토적변형특성화절선박송비,차불능반영조립토적전창성。
An experimental research was conducted on strength-deformation characteristics of reinforced coarse-grained soil by employing a large-scale triaxial and direct shear apparatus. The large-scale direct shear test showed similar relations of shear stress to shear displacement for coarse-grained and reinforced coarse-grained soil under different vertical load, and strain softening appearing on both stress-strain curves without great change in softening characteristics. It can be seen from the curve of normal displacement to shear displacement for reinforced coarse-grained soil that shear dilatation turned to be more noticeable with lower normal strain, and coarse-grained soil got an enhanced cohesion, but a smaller internal friction angle after being reinforced. Then from the triaxial shearing test, a relation curve of deviator stress and axial strain of coarse-grained soil before and after being reinforced under the conditions of different confining pressure was obtained showing strain hardening characteristics. With an increase in the confining pressure, the relation of deviator stress and axial strain turned to be a steeper curve, with more significant strain hardening characteristics and greater difference in the maximum principle stress. While a decreased confining pressure brought about a more noticeable shear dilatation due to the shear contraction liable to become shear dilatation, and vice versa. Besides, the smaller axial strain resulted in an unobvious reinforcement effect, and only with the increasing of axial strain, the reinforcement effect turned to be noticeable. Compared with coarse-grained soils, the reinforced coarse-grained soil gets a larger cohesion, but almost similar internal friction angle. After analyzing applicability of Duncan-Chang material model with the tri-axial shearing test results, it is concluded that Duncan-Chang material model can reasonably determine the strength and tangent modulus of elasticity for coarse-grained and reinforced soil. However, it can′t be used to describe and define deformation characteristics and tangent Poisson′s ratio, neither reflect the shear dilatation of coarse-grained soil.