Archeomagnetism of Southern Africa: Implications for Longevity of the South Atlantic Anomaly

南部非洲的考古地磁学:对南大西洋异常长期存在的影响

基本信息

  • 批准号:
    1448227
  • 负责人:
  • 金额:
    $ 31万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Standard Grant
  • 财政年份:
    2015
  • 资助国家:
    美国
  • 起止时间:
    2015-03-01 至 2019-02-28
  • 项目状态:
    已结题

项目摘要

A broad low intensity area in Earth's recent magnetic field spans the southern Atlantic Ocean, Africa and South America. This is commonly called the South Atlantic Anomaly (SAA). The SAA allows a relatively close approach of Earth's radiation belts, affecting spacecraft operations. The low magnetic intensity decreases the efficiency of magnetic shielding in the region, which can influence atmospheric ozone. Many believe the SAA is linked to the dramatic decay of the dipole geomagnetic field intensity during the last 160 years, and the growth of an area of reversed magnetic field on Earth's core beneath South Africa. Some have even speculated Earth is heading toward a geomagnetic field reversal. But understanding these phenomena within the context of longer-term geomagnetic history has been limited by a lack of Southern Hemisphere archeomagnetic data (that is, data from archeological objects that were fired to high temperature and subsequently preserved a record of Earth's magnetic field as they cooled). Our research and education program is aimed at understanding the history of the geomagnetic field in the SAA region as recorded in southern Africa. The main focus of the work is the collection and subsequent analysis of archeomagnetic data from Iron Age burnt structures, and tests of models addressing how the nature of the boundary between Earth's core and mantle may be giving rise to recent changes seen in the geomagnetic field.Archeomagnetic data from Iron Age sites of southern Africa (ca. 1000-1650 AD) show a sharp intensity drop at 1300 AD, at a rate comparable to modern field changes in the present-day South Atlantic Anomaly (SAA), but to lower values. The recurrence of low field values may reflect magnetic flux expulsion from the core promoted by the unusual core-mantle boundary composition and structure beneath southern Africa defined by seismology (specifically the African Large Low Velocity Seismic Province, or LLVSP). Because the African LLVSP is a longstanding structure, this region might be a steady site of flux expulsion, and perhaps the triggering site for geomagnetic reversals, on time scales of millions of years. If correct, this conceptual model is transformative because it suggests reversals do not initiate at random locations, but instead nucleate at core-mantle boundary sites that promote flux to leak upward. The model predicts modulation of the field on time scales of the lifetime of an eddy in the core flow, and will be tested by extending the archeomagnetic record of Iron Age southern Africa. The research program is integrated with undergraduate and graduate education and will be conducted with geologists and archeologists from South Africa, Botswana, and Zimbabwe. This project was co-funded by the GVF fund in the Office of International Science Engineering.
地球近代磁场中的一个广阔的低强度区域横跨南大西洋、非洲和南美洲。这通常被称为南大西洋异常(SAA)。SAA允许相对接近地球的辐射带,影响航天器的操作。低磁场强度降低了该区域的磁屏蔽效率,这可能会影响大气臭氧。许多人认为SAA与过去160年中偶极子地磁场强度的急剧衰减以及南非下方地球核心上反向磁场区域的增长有关。有些人甚至推测地球正在走向地磁场逆转。但是,由于缺乏南半球的古地磁数据(也就是说,来自考古对象的数据被烧到高温,随后在冷却时保存了地球磁场的记录),因此在较长期的地磁历史背景下理解这些现象受到了限制。我们的研究和教育计划旨在了解南部非洲记录的SAA地区地磁场的历史。工作的主要重点是收集和随后分析来自铁器时代燃烧结构的古地磁数据,并测试模型,说明地核和地幔之间的边界性质如何引起地磁场的近期变化。1000-1650 AD)在1300 AD显示了急剧的强度下降,与现代南大西洋异常(SAA)的现代场变化相当,但值较低。低场值的重现可能反映了由地震学(特别是非洲大低速地震省,或LLVSP)定义的南部非洲下不寻常的核-幔边界成分和结构促进的来自核的磁通量排出。由于非洲LLVSP是一个长期存在的结构,这个地区可能是一个稳定的网站的通量驱逐,也许是触发网站的地磁反转,在数百万年的时间尺度。 如果正确的话,这个概念模型是变革性的,因为它表明逆转不会在随机位置开始,而是在核幔边界处成核,促进通量向上泄漏。该模型预测调制的时间尺度上的涡流的核心流的生命周期的字段,并将通过延长铁器时代南部非洲的古地磁记录进行测试。该研究计划与本科和研究生教育相结合,将与来自南非,博茨瓦纳和津巴布韦的地质学家和考古学家进行。 该项目由国际科学工程办公室的GVF基金共同资助。

项目成果

期刊论文数量(1)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
New Archeomagnetic Directional Records From Iron Age Southern Africa (ca. 425-1550 CE) and Implications for the South Atlantic Anomaly
  • DOI:
    10.1002/2017gl076007
  • 发表时间:
    2018-02-16
  • 期刊:
  • 影响因子:
    5.2
  • 作者:
    Hare, Vincent J.;Tarduno, John A.;Cottrell, Rory D.
  • 通讯作者:
    Cottrell, Rory D.
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John Tarduno其他文献

Past and future preservation of the terrestrial hydrosphere by Earth’s magnetic field
地球磁场过去和未来对陆地水圈的保护
  • DOI:
  • 发表时间:
    2020
  • 期刊:
  • 影响因子:
    0
  • 作者:
    John Tarduno;Eric Blackman and Hirokuni Oda
  • 通讯作者:
    Eric Blackman and Hirokuni Oda

John Tarduno的其他文献

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{{ truncateString('John Tarduno', 18)}}的其他基金

Collaborative Research: Archeomagnetism of southern Africa and dynamo modeling: Testing the hypothesis of South Atlantic Anomaly-Large Low Shear Velocity Province Agency
合作研究:南部非洲的考古地磁学和发电机建模:检验南大西洋异常-大低切变速度省机构的假设
  • 批准号:
    2201460
  • 财政年份:
    2022
  • 资助金额:
    $ 31万
  • 项目类别:
    Continuing Grant
The First Billion Years of the Geodynamo
地球发电机的第一个十亿年
  • 批准号:
    2051550
  • 财政年份:
    2021
  • 资助金额:
    $ 31万
  • 项目类别:
    Continuing Grant
Collaborative Research: Geomagnetic field strength and stability between 500 and 800 Ma: Constraining inner core growth
合作研究:500 至 800 Ma 之间的地磁场强度和稳定性:限制内核生长
  • 批准号:
    1828817
  • 财政年份:
    2019
  • 资助金额:
    $ 31万
  • 项目类别:
    Continuing Grant
The First Billion Years of the Geodynamo
地球发电机的第一个十亿年
  • 批准号:
    1656348
  • 财政年份:
    2017
  • 资助金额:
    $ 31万
  • 项目类别:
    Continuing Grant
The nature of the Ediacaran to early Cambrian geomagnetic field
埃迪卡拉纪至早寒武世地磁场的性质
  • 批准号:
    1520681
  • 财政年份:
    2015
  • 资助金额:
    $ 31万
  • 项目类别:
    Standard Grant
Neoarchean to Early Proterozoic evolution of Earth's core: Paleomagnetic tests using dikes and sills of the Zimbabwe craton
地核的新太古代到早元古代演化:利用津巴布韦克拉通的岩墙和岩台​​进行的古地磁测试
  • 批准号:
    1045651
  • 财政年份:
    2011
  • 资助金额:
    $ 31万
  • 项目类别:
    Continuing Grant
The ultra-warm Arctic ca. 90 million years ago
超温暖的北极大约。
  • 批准号:
    1107801
  • 财政年份:
    2011
  • 资助金额:
    $ 31万
  • 项目类别:
    Standard Grant
MRI: Development of a SERF Atomic Magnetometer for Paleomagnetic Applications
MRI:开发用于古地磁应用的 SERF 原子磁力计
  • 批准号:
    1039846
  • 财政年份:
    2010
  • 资助金额:
    $ 31万
  • 项目类别:
    Standard Grant
The First Billion Years of the Geodynamo
地球发电机的第一个十亿年
  • 批准号:
    1015269
  • 财政年份:
    2010
  • 资助金额:
    $ 31万
  • 项目类别:
    Continuing Grant
Iron Age (300-1800 AD) Geomagnetic Paleointensity of Southern Africa
铁器时代(公元 300-1800 年)南部非洲的地磁古强度
  • 批准号:
    0838185
  • 财政年份:
    2009
  • 资助金额:
    $ 31万
  • 项目类别:
    Continuing Grant

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