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Shallow stratigraphy of the mid-atlantic bight: Constraints on siting of offshore wind projects.

机译:大西洋中部浅层地层:限制海上风电项目的选址。

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摘要

Fluctuations in sea level during the Quaternary have resulted in pronounced three-dimensional variation of surficial and subsurface marine sediments along the Mid-Atlantic. This region presents possible development opportunities for emerging domestic energy production, specifically renewable wind energy. Infrastructure for offshore wind energy development is highly dependent on the nature of the site conditions including the type and distribution of sediments. Water depth, bathymetry, and the geotechnical properties of sediments are some of the factors that affect the design and dimensions of wind turbine foundations.;In this thesis, geological and geophysical investigations of the shallow stratigraphy within Delaware's Wind Energy Area (WEA), including multibeam bathymetry, echosounder sub-bottom profiles, acoustic Doppler current profiler measurements, and grab samples have been used to interpret bottom erosion and deposition patterns. I have identified variable surface sediments, including surficial, large, well-rounded cobbles, subsurface paleochannels, and complex subsurface bedding. These observations suggest that fluvial and near-shore coastal processes have had lasting influences on sedimentation patterns throughout periods of transgression. The most recent sea level rise associated with the early Holocene epoch in-filled fluvial channels with sediments progressing from fine muds, to estuarine sands and marine sands. These interpretations are confirmed through correlation with geophysical survey results in surrounding offshore areas within the Mid-Atlantic Bight. Probable sediment types and their associated engineering soil properties have been inferred from these studies. The data collected here support the fluvial and near-shore influence on the distribution of sediments and correlate with well studied transgressive facies patterns. Our interpretation provides valuable constraints on the development of offshore wind projects within the Mid-Atlantic Bight, in general, and, in particular, the type, design and location of turbine foundations within Delaware's WEA.
机译:第四纪期间海平面的波动导致大西洋中部沿表层和地下海洋沉积物出现了明显的三维变化。该地区为新兴的国内能源生产(尤其是可再生风能)提供了可能的发展机会。海上风能开发的基础设施高度依赖于现场条件的性质,包括沉积物的类型和分布。水深,测深和沉积物的岩土工程特性是影响风力涡轮机基础设计和尺寸的一些因素。多束测深法,回声测井仪的下底剖面,声多普勒电流剖面仪测量和抓取样品已被用来解释底部侵蚀和沉积模式。我发现了各种表面沉积物,包括表面的,大的,圆润的鹅卵石,地下古河道和复杂的地下层理。这些观察结果表明,在整个海侵期间,河流和近岸沿海过程对沉积模式具有持久的影响。最近的海平面上升与全新世早期充满河床相关,沉积物从细泥浆发展到河口砂和海洋砂。这些解释是通过与大西洋中部海岸线附近海上地区的地球物理调查结果的相关性得到证实的。从这些研究中推断出可能的沉积物类型及其相关的工程土壤特性。这里收集的数据支持了河流和近岸对沉积物分布的影响,并与深入研究的海相相联系。通常,我们的解释为大西洋中部地区海上风电项目的开发提供了宝贵的约束条件,尤其是特拉华州WEA中涡轮机基础的类型,设计和位置。

著录项

  • 作者

    Metz, Trevor L.;

  • 作者单位

    University of Delaware.;

  • 授予单位 University of Delaware.;
  • 学科 Geology.
  • 学位 M.S.
  • 年度 2015
  • 页码 146 p.
  • 总页数 146
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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