摘要
冻结饱水黄土的拉伸试验表明,拉伸破坏均属脆性破坏类型,拉断面上矿物颗粒剪移错粒,裂隙发育。拉伸的应力-应变过程,视荷载作用的快慢大致可分为粘弹-塑性、粘-弹性和脆性破坏三类,它们可用统一的方程形式加以描述。此外,对饱水冻结黄土的峰值应力、破坏应变和破坏时间等特性进行了分析.对抗拉、抗压强度作分析比较后指出,它们的比值为0.44-0.63,与负温和加载速率的关系不大。
Tensile tests on the frozen saturated loess show that their failure is brittle. Shear and displacement of the mineral grain occur and mini-fissures grow on the cross section of the crack. The stress-strain processes of the tensile are classified into three types depending on the load rates i.e.viscoelastic-plastic, viscoelastic and brittle deformation. They may be described by an unitized expression. The features of stress-strain, peak stress, strain and time to failure of frozen saturated loess are also discussed in this paper. The ratio of tensile strength to compressive strength is 0.44-0.63 independently of the temperature and load rate.
出处
《冰川冻土》
CSCD
北大核心
1995年第4期315-321,共7页
Journal of Glaciology and Geocryology