V. Sivakumar, I. G. Doran
{"title":"Yielding characteristics of unsaturated compacted soils","authors":"V. Sivakumar, I. G. Doran","doi":"10.1002/(SICI)1099-1484(200005)5:4<291::AID-CFM95>3.0.CO;2-D","DOIUrl":null,"url":null,"abstract":"The elasto-plastic constitutive model for unsaturated soils postulates the existence of a loading collapse yield locus (LC) and a suction increase yield locus (SI) in the p:s stress plane. The characteristics of the LC yield locus have been reasonably well established in recent years but there is a much greater degree of uncertainty in relation to the SI yield locus. In the work reported in this paper a number of stress path tests in the p:s plane were conducted on samples of unsaturated compacted kaolin in a modified triaxial apparatus. Two series of tests were conducted on samples compacted to an identical initial condition so as to ensure a uniform soil structure prior to testing. Samples tested in Series 1 were taken through three stages: wetting at constant mean net stress, drying at constant mean net stress and a combination of isotropic compression and wetting. Samples tested in Series 2 were taken to pre-selected values of suction prior to isotropic compression. Data obtained from these tests indicate a possible form of single yield locus for unsaturated compacted soil. The data also indicate that the position of the yield locus, initially imposed by the compaction process will be influenced by the subsequent wetting process. Copyright © 2000 John Wiley & Sons, Ltd.","PeriodicalId":100899,"journal":{"name":"Mechanics of Cohesive-frictional Materials","volume":"31 1","pages":"291-303"},"PeriodicalIF":0.0000,"publicationDate":"2000-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"10","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mechanics of Cohesive-frictional Materials","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1002/(SICI)1099-1484(200005)5:4<291::AID-CFM95>3.0.CO;2-D","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 10
非饱和压实土的屈服特性
非饱和土弹塑性本构模型假定在p:s应力面上存在加载崩溃屈服轨迹(LC)和吸力增加屈服轨迹(SI)。近年来,LC产量轨迹的特征已经相当好地建立起来,但与SI产量轨迹相比,存在更大程度的不确定性。本文在改进的三轴装置上对非饱和压实高岭土试样进行了p:s平面应力路径试验。为保证试验前土体结构均匀,对初始压实条件相同的试样进行了两组试验。在系列1中测试的样品经过三个阶段:恒定平均净应力下的润湿,恒定平均净应力下的干燥以及各向同性压缩和润湿的组合。在系列2中测试的样品在各向同性压缩之前被带到预先选择的吸力值。从这些试验中获得的数据表明,非饱和压实土可能存在单一屈服轨迹。数据还表明,最初由压实过程施加的屈服轨迹位置将受到随后的润湿过程的影响。版权所有©2000约翰威利父子有限公司
本文章由计算机程序翻译,如有差异,请以英文原文为准。