【目的】实现黏性土壤离散元模型的接触参数与接触模型参数标定。【方法】基于土壤堆积角物理试验结果,采用考虑颗粒间黏结力的"Hertz-Mindlin with JKR"接触模型进行土壤堆积角仿真试验,借助GEMM(Generic EDEM material mode...【目的】实现黏性土壤离散元模型的接触参数与接触模型参数标定。【方法】基于土壤堆积角物理试验结果,采用考虑颗粒间黏结力的"Hertz-Mindlin with JKR"接触模型进行土壤堆积角仿真试验,借助GEMM(Generic EDEM material model database)数据库获得离散元模型关键参数(包括JKR表面能、恢复系数、静摩擦系数与动摩擦系数),进一步运用Box-Behnken试验方法进行堆积角仿真试验。【结果】通过对试验结果进行多元回归拟合分析获得了堆积角回归模型,回归模型的方差分析表明该模型极显著,试验因素对堆积角的影响为二次多项式,且存在复杂的一次与二次交互作用。以堆积角40.45°为目标对回归模型进行寻优,得到了优化解:JKR表面能7.91J·m-2;恢复系数0.66;静摩擦系数0.83;动摩擦系数0.25。以此优化解进行仿真试验获得的堆积角为39.73°。堆积角仿真试验与物理试验在堆积角度和形状上具有较高的相似性。【结论】可利用该优化参数对样品土壤进行进一步的黏性土壤与触土部件间的离散元仿真,从而揭示黏性土壤在触土部件作用下的运动规律。展开更多
为获取南方地区黏弹性壤土颗粒离散元接触模型的本征物理参数和接触力学参数,建立其用于离散元仿真的接触模型。以试验测定的堆积角为40.95°的壤土为研究对象,选取Hertz–Mindlin with JKR接触模型,通过实测试验获取壤土的本征物...为获取南方地区黏弹性壤土颗粒离散元接触模型的本征物理参数和接触力学参数,建立其用于离散元仿真的接触模型。以试验测定的堆积角为40.95°的壤土为研究对象,选取Hertz–Mindlin with JKR接触模型,通过实测试验获取壤土的本征物理参数值;借助GEMM数据库推荐的土壤接触力学参数初选范围,通过最陡爬坡试验得到接触力学参数值的最优值区间。利用Design–Expert软件对最优值区间的接触力学参数进行4因素3水平二次正交旋转组合试验,获取堆积角回归模型,以实测土壤堆积角40.95°为目标,对回归模型进行接触力学参数寻优,得到接触力学参数的最优组合为:JKR表面能13.05 J/m2,恢复系数0.5,动摩擦因数0.15,静摩擦因数1.06,该最优组合参数仿真堆积角均值为41.07°,与实测堆积角误差为0.3%。展开更多
A small problem about soil particle regularization and contacts but essential to geotechnical engineering was studied.The soils sourced from Guangzhou and Xiamen were sieved into five different particle scale ranges(d...A small problem about soil particle regularization and contacts but essential to geotechnical engineering was studied.The soils sourced from Guangzhou and Xiamen were sieved into five different particle scale ranges(d<0.075 mm,0.075 mm≤d<0.1 mm,0.1 mm≤d<0.2 mm,0.2 mm≤d<0.5 mm and 0.5 mm≤d<1.0 mm)to study the structures and particle contacts of granite residual soil.The X-ray micro computed tomography method was used to reconstruct the microstructure of granite residual soil.The particle was identified and regularized using principal component analysis(PCA).The particle contacts and geometrical characteristics in 3D space were analyzed and summarized using statistical analyses.The results demonstrate that the main types of contact among the particles are face-face,face-angle,face-edge,edge-edge,edge-angle and angle-angle contacts for particle sizes less than 0.2 mm.When the particle sizes are greater than 0.2 mm,the contacts are effectively summarized as face-face,face-angle,face-edge,edge-edge,edge-angle,angle-angle,sphere-sphere,sphere-face,sphere-edge and sphere-angle contacts.The differences in porosity among the original sample,reconstructed sample and regularized sample are closely related to the water-swelling and water-disintegrable characteristics of granite residual soil.展开更多
文摘【目的】实现黏性土壤离散元模型的接触参数与接触模型参数标定。【方法】基于土壤堆积角物理试验结果,采用考虑颗粒间黏结力的"Hertz-Mindlin with JKR"接触模型进行土壤堆积角仿真试验,借助GEMM(Generic EDEM material model database)数据库获得离散元模型关键参数(包括JKR表面能、恢复系数、静摩擦系数与动摩擦系数),进一步运用Box-Behnken试验方法进行堆积角仿真试验。【结果】通过对试验结果进行多元回归拟合分析获得了堆积角回归模型,回归模型的方差分析表明该模型极显著,试验因素对堆积角的影响为二次多项式,且存在复杂的一次与二次交互作用。以堆积角40.45°为目标对回归模型进行寻优,得到了优化解:JKR表面能7.91J·m-2;恢复系数0.66;静摩擦系数0.83;动摩擦系数0.25。以此优化解进行仿真试验获得的堆积角为39.73°。堆积角仿真试验与物理试验在堆积角度和形状上具有较高的相似性。【结论】可利用该优化参数对样品土壤进行进一步的黏性土壤与触土部件间的离散元仿真,从而揭示黏性土壤在触土部件作用下的运动规律。
文摘为获取南方地区黏弹性壤土颗粒离散元接触模型的本征物理参数和接触力学参数,建立其用于离散元仿真的接触模型。以试验测定的堆积角为40.95°的壤土为研究对象,选取Hertz–Mindlin with JKR接触模型,通过实测试验获取壤土的本征物理参数值;借助GEMM数据库推荐的土壤接触力学参数初选范围,通过最陡爬坡试验得到接触力学参数值的最优值区间。利用Design–Expert软件对最优值区间的接触力学参数进行4因素3水平二次正交旋转组合试验,获取堆积角回归模型,以实测土壤堆积角40.95°为目标,对回归模型进行接触力学参数寻优,得到接触力学参数的最优组合为:JKR表面能13.05 J/m2,恢复系数0.5,动摩擦因数0.15,静摩擦因数1.06,该最优组合参数仿真堆积角均值为41.07°,与实测堆积角误差为0.3%。
基金Projects(41572277,41877229) supported by the National Natural Science Foundation of ChinaProject(2015A030313118) supported by the Natural Science Foundation of Guangdong Province,ChinaProject(201607010023) supported by the Science and Technology Program of Guangzhou,China
文摘A small problem about soil particle regularization and contacts but essential to geotechnical engineering was studied.The soils sourced from Guangzhou and Xiamen were sieved into five different particle scale ranges(d<0.075 mm,0.075 mm≤d<0.1 mm,0.1 mm≤d<0.2 mm,0.2 mm≤d<0.5 mm and 0.5 mm≤d<1.0 mm)to study the structures and particle contacts of granite residual soil.The X-ray micro computed tomography method was used to reconstruct the microstructure of granite residual soil.The particle was identified and regularized using principal component analysis(PCA).The particle contacts and geometrical characteristics in 3D space were analyzed and summarized using statistical analyses.The results demonstrate that the main types of contact among the particles are face-face,face-angle,face-edge,edge-edge,edge-angle and angle-angle contacts for particle sizes less than 0.2 mm.When the particle sizes are greater than 0.2 mm,the contacts are effectively summarized as face-face,face-angle,face-edge,edge-edge,edge-angle,angle-angle,sphere-sphere,sphere-face,sphere-edge and sphere-angle contacts.The differences in porosity among the original sample,reconstructed sample and regularized sample are closely related to the water-swelling and water-disintegrable characteristics of granite residual soil.
