层间土的动剪切刚度衰减特性试验研究:以长江冲积平原为例

IF 2 3区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Frontiers in Earth Science Pub Date : 2024-08-29 DOI:10.3389/feart.2024.1421253
Haizhi Liu, Zhilei Huo, Danxi Chen, Ruirong Zhou, Qi Wu
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引用次数: 0

摘要

为探讨河相(相对于河口)洪积平原层间土的动剪模量特征,对南京长江洪积平原未扰动层间土进行了应变控制循环三轴试验,研究了初始有效约束压力(σʹm)、固结比(kc)和固结度(U)对最大动剪模量Gmax和动剪模量比G/Gmax的影响。结果表明,对于这种土壤,G 随应变振幅的增大而减小,在给定的应变振幅下,G 随 σʹm、kc 和 U 的增大而增大。最后,提出了一种改进的马丁-达维登科夫模型,用于预测不同σʹm、kc 和 U 条件下河漫滩层间土的 G/Gmax 值。
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Experimental study of dynamic shear stiffness decay characteristics of interbedded soil: a case study in Yangtze River floodplain
To explore the characteristics of the dynamic shear modulus of river-phase (as opposed to estuarine) floodplain interbedded soil, undisturbed interbedded soil from the floodplain of the Yangtze River in Nanjing was subjected to strain-controlled cyclic triaxial tests to investigate how the initial effective confining pressure (σʹm), consolidation ratio (kc), and degree of consolidation (U) influence the maximum dynamic shear modulus Gmax and the dynamic shear modulus ratio G/Gmax. The results show that for this soil, G decreases with increasing strain amplitude, and for a given strain amplitude, G increases with increasing σʹm, kc, and U. Compared with soil from the Yangtze estuary, kc has a greater effect on Gmax of the floodplain interbedded soil. Finally, a modified Martin-Davidenkov model is proposed for predicting G/Gmax of river-phase floodplain interbedded soil under different σʹm, kc, and U.
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来源期刊
Frontiers in Earth Science
Frontiers in Earth Science Earth and Planetary Sciences-General Earth and Planetary Sciences
CiteScore
3.50
自引率
10.30%
发文量
2076
审稿时长
12 weeks
期刊介绍: Frontiers in Earth Science is an open-access journal that aims to bring together and publish on a single platform the best research dedicated to our planet. This platform hosts the rapidly growing and continuously expanding domains in Earth Science, involving the lithosphere (including the geosciences spectrum), the hydrosphere (including marine geosciences and hydrology, complementing the existing Frontiers journal on Marine Science) and the atmosphere (including meteorology and climatology). As such, Frontiers in Earth Science focuses on the countless processes operating within and among the major spheres constituting our planet. In turn, the understanding of these processes provides the theoretical background to better use the available resources and to face the major environmental challenges (including earthquakes, tsunamis, eruptions, floods, landslides, climate changes, extreme meteorological events): this is where interdependent processes meet, requiring a holistic view to better live on and with our planet. The journal welcomes outstanding contributions in any domain of Earth Science. The open-access model developed by Frontiers offers a fast, efficient, timely and dynamic alternative to traditional publication formats. The journal has 20 specialty sections at the first tier, each acting as an independent journal with a full editorial board. The traditional peer-review process is adapted to guarantee fairness and efficiency using a thorough paperless process, with real-time author-reviewer-editor interactions, collaborative reviewer mandates to maximize quality, and reviewer disclosure after article acceptance. While maintaining a rigorous peer-review, this system allows for a process whereby accepted articles are published online on average 90 days after submission. General Commentary articles as well as Book Reviews in Frontiers in Earth Science are only accepted upon invitation.
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