干湿循环条件下黏性土龟裂特征.pdfVIP

This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: /copyright Authors personal copy Geoderma 166 (2011) 111–118 Contents lists available at ScienceDirect Geoderma j ournal homepage: www. /locate /geoderma Desiccation and cracking behaviour of clay layer from slurry state under wetting–drying cycles Chao-Sheng Tang a,⁎, Yu-Jun Cui b, Bin Shi a, Anh-Minh Tang b, Chun Liu a a School of Earth Sciences and Engineering, Nanjing University, 22 Hankou Road, Nanjing 210093, China b Ecole des Ponts ParisTech, UR Navier/CERMES, 6 et 8, avenue Blaise Pascal, Cité Descartes, Champs-sur-Marne, 77455 Marne-la-Vallée CEDEX 2, France a r t i c l e i n f o a b s t r a c t Article history: Laboratory tests were conducted to investigate the effect of wetting–drying (W–D) cycles on the initiation Received 2 November 2010