CLC number: TU433
On-line Access: 2024-08-27
Received: 2023-10-17
Revision Accepted: 2024-05-08
Crosschecked: 2019-12-11
Cited: 0
Clicked: 6139
Citations: Bibtex RefMan EndNote GB/T7714
Chuan-xun Li, Jin-yang Xiao, Wen-bing Wu, Guo-xiong Mei, Peng-peng Ni, Chin-jian Leo. Analysis of 1D large strain consolidation of structured marine soft clays[J]. Journal of Zhejiang University Science A,in press.Frontiers of Information Technology & Electronic Engineering,in press.https://doi.org/10.1631/jzus.A1900268 @article{title="Analysis of 1D large strain consolidation of structured marine soft clays", %0 Journal Article TY - JOUR
Abstract: 1. This paper presents a new method for estimating large strain consolidation of structured soft clays. Overall, the paper is well written and easy to follow. 2. This manuscript treats with one dimensional large strain consolidation problem on the marine soft clay composed of structured soils. Analytical procedure is proposed for structured soils to estimate the settlements. The manuscript is overall well written and large strain and structured soils are new point.
海相沉积结构性软土一维大应变固结分析创新点:1. 建立考虑天然沉积软土结构性影响的一维大应变固结模型,且该模型能考虑结构屈服压力随初始有效应力的变化; 2. 分析天然结构性软土大、小应变固结性状的差异,为实际工程中的软土固结计算提供理论依据. 方法:1. 总结结构性软土对压缩和渗透特性的影响及结构屈服压力与初始有效应力间的关系; 2. 通过理论推导,构建考虑结构性影响的软体一维大应变固结模型(公式(15)和(16)); 3. 通过对模型进行数值求解,分析软土结构性对大应变固结性 状的影响,以及考虑结构性影响的大、小应变固结性状的差异. 结论:1. 大应变假定下结构性软土中超静孔压的消散速率要比小应变假定下快,且这种差异随着土层应变增大而增大; 当应变值超过15%时必须采用大应变假定. 2. 如果土层的初始有效应力计算方法相同,则大、小应变不同假定下土层的最终沉降值是相同的. 3. 相同几何假定下,初始有效应力计算方法对超静孔压消散速率几乎无影响,但对沉降变形影响明显. 4. 大、小应变假定下固结性状间的差异随结构屈服压力的增大而减小. 关键词组: Darkslateblue:Affiliate; Royal Blue:Author; Turquoise:Article
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