首页> 外文期刊>Engineering Geology >Reply to the discussion by Ling Xu on 'Weak tensile characteristicsof loess in China — An important reason for ground fissure' by PingSun, Jian-Bing Peng, Li-Wei Chen, Yue-Ping Yin and Shu-Ren Wu,[Engineering Geology 108 (2009) 153-159]
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Reply to the discussion by Ling Xu on 'Weak tensile characteristicsof loess in China — An important reason for ground fissure' by PingSun, Jian-Bing Peng, Li-Wei Chen, Yue-Ping Yin and Shu-Ren Wu,[Engineering Geology 108 (2009) 153-159]

机译:回复徐灵关于孙平,彭建兵,陈立伟,尹跃平和吴树人的“中国黄土的弱拉伸特性—地裂缝的重要原因”的讨论,[工程地质108 (2009)153-159]

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摘要

The authors would like to express their thanks and appreciation tothe discusser's interest in this paper and for the comments raised. Thediscusser's contribution stresses two main points: (a)the discusserthink that the information presented in this paper is not sufficient toobtain the conclusions on loess tensile strength, and it seems that sheis looking for more detailed discussion or description on the rangeof water content for loess samples in tensile strength test; (b)thediscusser deems that the loess still has the similar collapse character-istics with the increase in water content (decreasing suction), even inshearing. The following is a response to,the points raised by thediscusser and clarification for the readers.
机译:作者要对讨论者对本文的关注以及提出的评论表示感谢和赞赏。讨论者的贡献强调了两个主要问题:(a)讨论者认为本文中提供的信息不足以得出有关黄土抗张强度的结论,似乎她正在寻找有关黄土样品含水量范围的更详细的讨论或描述。在抗拉强度测试中; (b)讨论者认为,随着含水量的增加(吸力降低)甚至黄土的剪切,黄土仍具有类似的崩塌特征。以下是对讨论者提出的观点和对读者的澄清的回应。

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