Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings

Geostructures experience repetitive load cycles, which gradually affect their long-term performance. This thesis explores the long-term response of soils subjected to mechanical load-unload, heat-cool, freeze-thaw, and atmospheric pressure oscillations. The research methodology involves new instrume...

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Main Author: Cha, Wonjun
Other Authors: Santamarina, Carlos
Language:en
Published: 2021
Subjects:
Online Access:Cha, W. (2021). Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings. KAUST Research Repository. https://doi.org/10.25781/KAUST-07L5T
http://hdl.handle.net/10754/673777
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spelling ndltd-kaust.edu.sa-oai-repository.kaust.edu.sa-10754-6737772021-11-27T05:06:50Z Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings Cha, Wonjun Santamarina, Carlos Physical Science and Engineering (PSE) Division Jonsson, Sigurjon Burns, Susan E. Finkbeiner, Thomas McCabe, Matthew Renewable energy Sustainability Repetitive loading Shakedown / Ratcheting Terminal density Strain accumulation Geostructures experience repetitive load cycles, which gradually affect their long-term performance. This thesis explores the long-term response of soils subjected to mechanical load-unload, heat-cool, freeze-thaw, and atmospheric pressure oscillations. The research methodology involves new instrumented cells (oedometer, temperature-controlled triaxial chamber, and pressure-controlled drying chamber), various geophysical monitoring methods (X-ray micro-CT, NMR, S-wave, and EM-waves), and simulations using discrete element modeling. Results show that soils subjected to repetitive mechanical or environmental loading experience shear and volumetric strain accumulation and changes in saturation (during barometric pressure cycles). In all cases, soils evolve towards an asymptotic terminal void ratio; the change in void ratio is pronounced when the soil exhibits grain-displacive ice formation during freeze-thaw cycles. The initial stress obliquity defines the shear strain response, which may be either shakedown -at low stress obliquity-, or ceaseless shear strain accumulation in ratcheting mode when the maximum stress obliquity approaches failure conditions. Finally, we provide simple engineering guidelines to estimate the long-term behavior of soils subjected to repetitive mechanical or environmental loading. 2021-11-25T10:40:42Z 2021-11-25T10:40:42Z 2021-06 Dissertation Cha, W. (2021). Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings. KAUST Research Repository. https://doi.org/10.25781/KAUST-07L5T 10.25781/KAUST-07L5T http://hdl.handle.net/10754/673777 en 2022-11-25 At the time of archiving, the student author of this dissertation opted to temporarily restrict access to it. The full text of this dissertation will become available to the public after the expiration of the embargo on 2022-11-25.
collection NDLTD
language en
sources NDLTD
topic Renewable energy
Sustainability
Repetitive loading
Shakedown / Ratcheting
Terminal density
Strain accumulation
spellingShingle Renewable energy
Sustainability
Repetitive loading
Shakedown / Ratcheting
Terminal density
Strain accumulation
Cha, Wonjun
Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings
description Geostructures experience repetitive load cycles, which gradually affect their long-term performance. This thesis explores the long-term response of soils subjected to mechanical load-unload, heat-cool, freeze-thaw, and atmospheric pressure oscillations. The research methodology involves new instrumented cells (oedometer, temperature-controlled triaxial chamber, and pressure-controlled drying chamber), various geophysical monitoring methods (X-ray micro-CT, NMR, S-wave, and EM-waves), and simulations using discrete element modeling. Results show that soils subjected to repetitive mechanical or environmental loading experience shear and volumetric strain accumulation and changes in saturation (during barometric pressure cycles). In all cases, soils evolve towards an asymptotic terminal void ratio; the change in void ratio is pronounced when the soil exhibits grain-displacive ice formation during freeze-thaw cycles. The initial stress obliquity defines the shear strain response, which may be either shakedown -at low stress obliquity-, or ceaseless shear strain accumulation in ratcheting mode when the maximum stress obliquity approaches failure conditions. Finally, we provide simple engineering guidelines to estimate the long-term behavior of soils subjected to repetitive mechanical or environmental loading.
author2 Santamarina, Carlos
author_facet Santamarina, Carlos
Cha, Wonjun
author Cha, Wonjun
author_sort Cha, Wonjun
title Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings
title_short Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings
title_full Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings
title_fullStr Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings
title_full_unstemmed Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings
title_sort long-term sediment response under repetitive mechanical and environmental loadings
publishDate 2021
url Cha, W. (2021). Long-term Sediment Response Under Repetitive Mechanical and Environmental Loadings. KAUST Research Repository. https://doi.org/10.25781/KAUST-07L5T
http://hdl.handle.net/10754/673777
work_keys_str_mv AT chawonjun longtermsedimentresponseunderrepetitivemechanicalandenvironmentalloadings
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