岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2014年
5期
1329-1333,1339
,共6页
吕玺琳%赖海波%黄茂松
呂璽琳%賴海波%黃茂鬆
려새림%뢰해파%황무송
饱和土%城市固体废弃物%材料状态%静态液化%二阶功
飽和土%城市固體廢棄物%材料狀態%靜態液化%二階功
포화토%성시고체폐기물%재료상태%정태액화%이계공
saturated soil%municipal solid waste%material state%static liquefaction%second order work
通过在屈服准则和剪胀性方程中引入材料状态参数,建立了一个与材料状态相关的本构模型,用于模拟不同初始孔隙比和围压下土体的应力-应变关系。基于二阶功理论,建立了饱和土体静态液化失稳理论判别准则。通过预测一系列饱和松砂三轴不排水试验结果,验证了所建立的本构模型及判别预测准则的合理性。分析结果表明,静态液化发生于土体硬化阶段,静态液化触发伴随着剪应力达到峰值,其后剪应力降低且孔隙水压力持续增长。进一步地,模拟了充分降解的城市固体废弃物在不排水条件下的应力-应变特性,并预测到了潜在失稳线及静态液化触发点。
通過在屈服準則和剪脹性方程中引入材料狀態參數,建立瞭一箇與材料狀態相關的本構模型,用于模擬不同初始孔隙比和圍壓下土體的應力-應變關繫。基于二階功理論,建立瞭飽和土體靜態液化失穩理論判彆準則。通過預測一繫列飽和鬆砂三軸不排水試驗結果,驗證瞭所建立的本構模型及判彆預測準則的閤理性。分析結果錶明,靜態液化髮生于土體硬化階段,靜態液化觸髮伴隨著剪應力達到峰值,其後剪應力降低且孔隙水壓力持續增長。進一步地,模擬瞭充分降解的城市固體廢棄物在不排水條件下的應力-應變特性,併預測到瞭潛在失穩線及靜態液化觸髮點。
통과재굴복준칙화전창성방정중인입재료상태삼수,건립료일개여재료상태상관적본구모형,용우모의불동초시공극비화위압하토체적응력-응변관계。기우이계공이론,건립료포화토체정태액화실은이론판별준칙。통과예측일계렬포화송사삼축불배수시험결과,험증료소건립적본구모형급판별예측준칙적합이성。분석결과표명,정태액화발생우토체경화계단,정태액화촉발반수착전응력체도봉치,기후전응력강저차공극수압력지속증장。진일보지,모의료충분강해적성시고체폐기물재불배수조건하적응력-응변특성,병예측도료잠재실은선급정태액화촉발점。
By using state-dependent yield function and dilatancy function, a state-dependent non-associated elasto-plasticity hardening model is proposed to simulate the undrained behaviors of saturated soils with different initial densities and confining pressures. According to the second-order work theory, the criteria for potential instability and static liquefaction of saturated soils are proposed. The proposed model and criteria were employed to predict a series of undrained triaxial tests on loose sands. The results showed that the static liquefaction occurs at the hardening stage before the plastic limit, the onset of static liquefaction accompanies with the peak of shear stress; and then the pore water pressure increases and the shear stress decreases with further loading. The stress-strain relationship of the municipal solid waste under undrained condition was also analyzed;the potential instability line was obtained and the onset of static liquefaction was predicted.