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DTSTAMP:20260429T122011
DTSTART;TZID=America/Detroit:20260507T100000
DTEND;TZID=America/Detroit:20260507T160000
SUMMARY:Other:Michigan Robotics Hackathon
DESCRIPTION:Join us for the 2026 Inspired4Robotics Hackathon\, happening on May 7th and 8th! We’re celebrating the opening of the Robot Garage\, a library of free-to-use robots and robotics components\, by holding this hackathon!\n\nStarting at 10am on Thursday\, May 7th\, your goal is to build a prototype to pitch an idea for a product\, demonstration\, or even a research direction! Along with all the resources and components in the Robot Garage\, we will provide technical support\, access to a makerspace\, and mentorship to help you get started. The top three teams win cash prizes to fund their future work. And all teams have the opportunity to apply for mini-grants to continue their work using the space\, and fund their project. A panel of judges will select the group of winners based on a final presentation. Participants get bonus points if their project can double as a demonstration of a concept in STEM\, and be adapted by the department for future outreach and educational events! We’re looking for inspired explorations that showcase the interdisciplinary nature of robotics.
UID:148002-21902711@events.umich.edu
URL:https://events.umich.edu/event/148002
CLASS:PUBLIC
STATUS:CONFIRMED
CATEGORIES:Engineering,Graduate Students,Hackathon,Robotics
LOCATION:Ford Robotics Building - FRB 4150
CONTACT:
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DTSTAMP:20260505T103416
DTSTART;TZID=America/Detroit:20260507T100000
DTEND;TZID=America/Detroit:20260507T110000
SUMMARY:Lecture / Discussion:Peng Zhai Dissertation Defense
DESCRIPTION:The seismic cycle\, also known as sequences of earthquakes and aseismic slip (SEAS)\, is characterized by periodic accumulation and release of tectonic stress. This multi-timescale process encompasses both rapid coseismic rupture\, which unfolds over seconds\, and prolonged interseismic deformation lasting up to thousands of years. Physics-based numerical models of the seismic cycle aim to capture SEAS within a unified framework and to enhance our understanding of earthquake generation. In this dissertation\, I employ fully dynamic seismic cycle models\, including dynamic inertial effects\, to investigate earthquake nucleation and the coupled evolution of fault slip and inelastic fault zone deformation governed by damage rheology.\n\nChapter 2 focuses on exploring the influence of the characteristic weakening distance (DRS) in rate-and-state friction (RSF) on earthquake nucleation. The findings indicate that a larger value of a/b (>0.75)\, rather than the traditionally assumed 0.5\, is needed to produce expanding crack nucleation for a relatively small DRS. This suggests that fixed-length nucleation may be more common on both natural and laboratory faults\, and therefore earthquake nucleation style is strongly governed by both a/b and DRS.\n\nChapter 3 aims to develop a novel seismic cycle model integrating RSF and damage rheology to capture the coevolution of fault slip and fault zone deformation. Simulations reveal coseismic velocity drops consistent with seismological observations and a persistent shallow slip deficit (SSD). Off-fault damage is predominantly generated during earthquakes\, concentrating at shallow depths in a flower-like structure\, characterized by a distributed damage area surrounding a localized\, highly damaged inner core. Utilizing an experimentally based logarithmic healing law\, the model shows that coseismic reductions in off-fault rigidity only partially heal\, leading to a cumulative\, permanent rigidity loss over multiple seismic cycles. Consequently\, the fault zone width and rigidity eventually stabilize\, reaching a mature state with a large cumulative fault slip.\n\nIn Chapter 4\, I apply this earthquake coevolution model to examine the role of weak fault zone deformation on the generation of multiscale seismicity. The results demonstrate that relatively weak fault zones (i.e.\, when surrounding rocks have a low internal friction coefficient) facilitate the production of both large and small earthquakes\, reproducing key earthquake scaling relations observed in nature\, such as power-law magnitude-frequency distribution\, magnitude-invariant static stress drop\, and non-linear fracture energy scaling in a unified framework. These findings highlight the fundamental role of the coevolution of earthquakes and fault zone inelastic deformation in controlling earthquake behaviors.\n\nIn conclusion\, these findings highlight the significant role that fault friction and fault zone deformation play in governing earthquake nucleation\, slip behavior\, and earthquake scaling relations. Particularly\, by capturing the coevolution of fault slip and fault zone deformation over multiple seismic cycles\, Chapters 3 and 4 underscore the fundamental importance of fault zone inelastic deformation in shaping earthquake dynamics beyond fault friction and rock elasticity. The spontaneously generated inelastic deformation dissipates elastic strain energy and acts as natural rupture barriers to modulate earthquake size. The coevolution of fault slip and fault zone inelastic deformation provides an efficient way to generate fault stress heterogeneity and a wide spectrum of earthquake size over multiple seismic cycles. These insights offer new directions for interpreting natural fault systems and assessing seismic hazards.
UID:148094-21902941@events.umich.edu
URL:https://events.umich.edu/event/148094
CLASS:PUBLIC
STATUS:CONFIRMED
CATEGORIES:Dissertation,Earth And Environmental Sciences
LOCATION:1100 North University Building - 2540
CONTACT:
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