利用三维嵌套纽马克法计算地震诱发的斜坡永久位移

IF 2 3区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Qiang Li, Yan-Yang Tong, Jin-Nan Wang, Hui Xu
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引用次数: 0

摘要

纽马克法是评估地震荷载作用下斜坡永久位移的经典方法。本研究旨在极限分析运动学定理的框架内提出一种三维嵌套纽马克方法(3D-NNM)。经典的三维旋转破坏机制被离散化为一系列嵌套的旋转楔块,每个楔块都受到通过功速率平衡确定的相应屈服加速度的作用,每个楔块在地震激励下超过屈服加速度时都会产生相对位移。通过对从坡脚到坡顶的相对位移进行积分,进一步得到总的永久位移曲线。结果表明,所提出的三维-NNM 可以有效地评估地震作用下斜坡的永久位移剖面,而且所提出的三维-NNM 比 Leshchinsky 的二维嵌套 Newmark 方法提高了 30.7%;所得到的斜坡中间高处的总水平位移随嵌套块数的增加而减小,但随斜坡宽高比的增加而增大。此外,传统的单滑动块 Newmark 方法往往会高估地震震动下边坡的永久位移。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seismically-induced permanent displacements of slopes using 3D Nested Newmark method
The Newmark method is a classic method for evaluating the permanent displacements of a slope under seismic loads. This study aims at proposing a three-dimensional nested Newmark method (3D-NNM) in the framework of the kinematic theorem of limit analysis. The classical three-dimensional rotational failure mechanism is discretized into a series of nested rotating wedges, each of which is subjected to a corresponding yield acceleration determined by employing the work rate balance, and each of which produces relative displacements under seismic excitations when it exceeds the yield acceleration. The total permanent displacement profile is further obtained by integration of the relative displacements from the slope toe to the slope crest. The obtained results show that the proposed 3D-NNM can effectively evaluate the permanent displacement profile of slopes under earthquakes, and the proposed 3D-NNM improves the Leshchinsky’s 2D nested Newmark method by 30.7%; the obtained total horizontal displacement at the slope middle height reduces with the number of nested blocks, but increases with the increasing of the slope-width-to-height ratios. Besides, the traditional Newmark method with a single sliding block tends to overestimate the permanent displacements of slope under seismic shakings.
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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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