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Full waveform modeling and inversion of seismic attenuation and application to characterizing near-surface fractures at Susquehanna Shale Hills Critical Zone Observatory

Full waveform modeling and inversion of seismic attenuation and application to characterizing near-surface fractures at Susquehanna Shale Hills Critical Zone Observatory
地震衰减的全波形建模和反演以及用于表征萨斯奎哈纳页岩山关键区域观测站近地表裂缝的应用
批准号:
1919650
负责人:
Tieyuan Zhu
金额:
$12.5万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2019
资助国家:
美国
项目状态:
已结题
起止时间:
2019-12-01 至 2022-06-30

项目摘要

项目成果

Tieyuan Zhu的其他基金

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中文摘要
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英文摘要
Seismologists often use seismic waves to study the Earth's interior. This is because seismic wave properties are very sensitive to the physical and chemical state of the Earth, from the shallow to the deep Earth. This project explores one such property, seismic attenuation, which is considered to be a direct indicator for temperature of the Earth with depth, as well as the presence of fluids. Because of its multi-purpose use, a map of this property in Earth structure can improve our understanding of how the Earth's interior works. The main goal of this project is to develop a method to image seismic attenuation using seismic waves. Broader impacts include the mentoring of a postdoctoral researcher at Penn State University and the development of new methods for the scientific community to use.Measurements of seismic wave attenuation potentially provide valuable source of information about the physical and chemical state of the Earth's interior. Seismic full waveform inversion (FWI) as a promising measurement tool for inverting Q still has several key issues to be investigated: 1) whether or not the existing fractional anelastic wave equation, that separates amplitude absorption and phase dispersion, can facilitate the development of FWI; 2) explicit Q embedded in fractional anelastic wave equations will simplify the computations of gradient; 3) how cross-talks between velocity and Q in FWI could be alleviated. To address these issues, this project will conduct three main tasks. First, starting from the newly developed fractional anelastic wave equation that parameterize an explicit Q, a Q-FWI method will be developed using adjoint-state approaches. Second, a suitable inversion strategy for multi-parameters (velocity and Q) will be sought. Third, the Q-FWI will be validated using synthetic near-surface geological models.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
期刊论文(4)
专著(0)
科研奖励(0)
会议论文
DOI: 10.1093/gji/ggaa549
发表时间: 2020-12
期刊: Geophysical Journal International
影响因子: 2.8
作者: [G. Xing;T. Zhu]
通讯作者: G. Xing;T. Zhu
DOI: 10.1029/2019jb017985
发表时间: 2019-11
期刊: Journal of Geophysical Research: Solid Earth
影响因子: --
作者: [G. Xing;T. Zhu]
通讯作者: G. Xing;T. Zhu
DOI: 10.1029/2021jb023321
发表时间: 2022-02
期刊: Journal of Geophysical Research: Solid Earth
影响因子: --
作者: [Xuejian Liu;T. Zhu;J. Hayes]
通讯作者: Xuejian Liu;T. Zhu;J. Hayes
Decoupled Fréchet kernels based on a fractional viscoacoustic wave equation
基于分数粘声波方程的解耦 Fréchet 核
DOI: 10.1190/geo2021-0248.1
发表时间: 2022
期刊: GEOPHYSICS
影响因子: 3.3
作者: [Xing, Guangchi, Zhu, Tieyuan]
通讯作者: Zhu, Tieyuan
CIVIC-FA Track A: Leveraging existing fiber-optic cables to identify and manage urban environmental hazards
CIVIC-PG Track A: Leveraging Existing Fiber-Optic Cables to Identify and Manage Urban Environmental Hazards
国内基金
海外基金
用卫星测高数据研究内陆水域的水位变化及其与环境的相关性
  • 批准号:
    40304001
  • 项目类别:
    青年科学基金项目
  • 资助金额:
    25.0万元
  • 批准年份:
    2003
  • 负责人:
    姜卫平
  • 依托单位: