CAREER Development in Geomodeling: Seeing and Creating Connections in Earth Science

地理建模的职业发展:观察并建立地球科学中的联系

基本信息

  • 批准号:
    0448871
  • 负责人:
  • 金额:
    --
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Continuing grant
  • 财政年份:
    2005
  • 资助国家:
    美国
  • 起止时间:
    2005-02-01 至 2011-09-30
  • 项目状态:
    已结题

项目摘要

Modeling of coupled continental tectonics, mantle dynamics, and surfaceprocesses will be undertaken to explore surface deformation and deepermantle flow during continental collision. Surface erosion will beincorporated into the models to explore the interaction between tectonicsand atmospheric processes. Model predictions will be compared to data fromcollisional settings to provide a better understanding of continentalcollision. The links between continental growth and the Earth's thermalevolution will also be explored. A combination of theory, numericalsimulations, and lab experiments will be used to provide insight intocoupled planetary cooling and continental growth. Geochemical data willprovide constraints on continental growth. The methodologies developed tomodel the interaction between conducting continents and the convectingmantle will also be used to address hydrothermal convection belowinsulating cap rock and the cooling history of magma chambers within hostrock. The PI's modeling across earth science sub-fields will provide unitybetween his teaching and research. Lecture demonstrations, i.e., modelsdesigned for education, can convey general foundational ideas that studentsthen link to approach a range of earth science problems. This will allowstudents in introductory classes to see that scientific ideas are not isolatedbits of information. The broader impact is that a portion of the studentpopulation that will not go into science will have a clearer view of whatscience is. Demonstrations will also be used in a reverse mode. A workshopwill be developed where advanced students will build demonstrations and simpleexperiments of their own design to convey key ideas from their primary earthscience field. In presenting their work to each other they will see how manykey concepts do not care about artificial sub-field boundaries. They willsee connections and be better prepared to make new ones. The space will alsohouse a scientific visualization studio where students will work on effectivevisual communication of scientific ideas. The workspace/studio will beavailable to K-12 educator colleagues in the Houston area.
将进行耦合大陆构造、地幔动力学和地表过程的建模,以探索大陆碰撞期间的地表变形和更深的地幔流动。地表侵蚀将被纳入模型中,以探索构造与大气过程之间的相互作用。模型预测将与碰撞环境中的数据进行比较,以更好地了解大陆碰撞。还将探讨大陆生长与地球热演化之间的联系。理论、数值模拟和实验室实验的结合将用于深入了解行星冷却和大陆生长的耦合。地球化学数据将为大陆的增长提供限制。为模拟传导大陆与对流地幔之间的相互作用而开发的方法也将用于解决绝缘盖岩下方的热液对流以及主岩内岩浆室的冷却历史。 PI 跨地球科学子领域的建模将提供他的教学和研究之间的统一。讲座演示,即为教育而设计的模型,可以传达一般的基本思想,然后学生将这些基本思想联系起来解决一系列地球科学问题。这将使入门课程的学生看到科学思想并不是孤立的信息。更广泛的影响是,一部分不会进入科学领域的学生将对科学有更清晰的认识。演示也将采用反向模式。将举办一个研讨会,高级学生将进行自己设计的演示和简单实验,以传达他们主要地球科学领域的关键思想。在向彼此展示他们的工作时,他们会看到有多少关键概念不关心人为的子领域边界。他们将看到联系并为建立新的联系做好更好的准备。该空间还将设有一个科学可视化工作室,学生将在那里进行科学思想的有效视觉传达。该工作空间/工作室将向休斯顿地区的 K-12 教育工作者同事开放。

项目成果

期刊论文数量(0)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)

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Adrian Lenardic其他文献

Plug flow in the Earth's asthenosphere
  • DOI:
    10.1016/j.epsl.2018.05.030
  • 发表时间:
    2018-08-15
  • 期刊:
  • 影响因子:
  • 作者:
    Alana G. Semple;Adrian Lenardic
  • 通讯作者:
    Adrian Lenardic
A supercontinental boost
超级大陆助推
  • DOI:
    10.1038/ngeo2862
  • 发表时间:
    2016-12-12
  • 期刊:
  • 影响因子:
    16.100
  • 作者:
    Adrian Lenardic
  • 通讯作者:
    Adrian Lenardic

Adrian Lenardic的其他文献

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{{ truncateString('Adrian Lenardic', 18)}}的其他基金

Collaborative Research: The Asthenosphere and Mantle Dynamics
合作研究:软流圈和地幔动力学
  • 批准号:
    1522012
  • 财政年份:
    2016
  • 资助金额:
    --
  • 项目类别:
    Standard Grant
Collaborative Research: The Asthenosphere and Mantle Dynamics
合作研究:软流圈和地幔动力学
  • 批准号:
    0944156
  • 财政年份:
    2010
  • 资助金额:
    --
  • 项目类别:
    Continuing Grant
The Thermo-Chemical State and Thermo-Tectonic Evolution of Cratons and Deep Cratonic Lithosphere
克拉通及克拉通深部岩石圈的热化学状态与热构造演化
  • 批准号:
    0001029
  • 财政年份:
    2000
  • 资助金额:
    --
  • 项目类别:
    Standard Grant

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