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Collaborative Research: Logistically Light Instrument Deployment for Estimation of Antarctic Basal Temperatures and Geothermal Heat Fluxes

Collaborative Research: Logistically Light Instrument Deployment for Estimation of Antarctic Basal Temperatures and Geothermal Heat Fluxes
合作研究:用于估算南极基础温度和地热热通量的后勤轻型仪器部署
批准号:
1543552
负责人:
John Selker
金额:
$1.0万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2016
资助国家:
美国
项目状态:
已结题
起止时间:
2016-06-01 至 2017-05-31

项目摘要

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中文摘要
翻译
非技术描述:对南极冰盖变量的新观测对于选择钻探地点以记录气候、了解冰动力如何影响海平面以及调查该大陆的地质历史至关重要。温度深度剖面对于估计南极洲的基础温度和地热通量具有特别重要的意义。除最近的钻探地点外,目前对南极地热通量知之甚少,是确定基本条件的最大未知数。然而,目前的物流成本极大地限制了钻探以获取温度分布。我们的长期目标是开发、测试和试运行一种新的方法,以比现有方法低得多的成本获取大气温度分布。为此,我们将进行实验室实验和数值模拟,以开发一种新的方法,使用融冰探头,而不是传统的钻探,将温度测量设备部署到一公里或更深的地方。为了使用熔化探头,我们必须防止探头上方融化的冰完全冻结,这样电缆才能在探头下降时不断地向下输送到探头。这一进展还将为回收熔融探头开辟道路,以防止对环境的影响和现场遗留设备的费用。我们的初步实验和建模将测试我们方法的有效性,并为进一步的现场测试做好准备。技术描述:我们将进行实验室和建模工作,(1)降低我们部署拉曼分布式温度传感(DTS)电缆的熔化探头的技术风险;(2)开始开发可回收的融冰探头。具体地说,我们将使用具有圆柱对称性的Stefan问题的数值模拟来指导电缆加热和防冻注射的详细设计,并将通过实验室测试的方式测试和修改候选设计。我们将测试乙醇填充的熔体孔的长期稳定性,以衡量它们是否适合用于温度测量的可回收熔体测头系统(安装后需要长达数月的热平衡)。在我们的实验室实验中,我们将通过使用DTS测量临界温度数据来获得拉曼DTS方法的经验,无论是在融化孔内还是在邻近的冰中。为了解决回收问题,我们将为我们的冰融化探测器的上端设计和测试一个新的融化头,并演示向上穿过部分重新冻结的融化孔。最后,我们将在同行评议的出版物上公布建模和实验结果,并将在西雅图科学技术博物馆的一次特别活动中向广大公众展示该项目。这项工作的结果将展示技术准备情况,以便在后续项目中尽早在更大的冰钻试验设施中进行测试(预期在该项目完成后不久在威斯康星大学进行),然后在实地进行测试。
英文摘要
Title: Logistically Light Instrument Deployment for Estimation of Antarctic Basal Temperatures and Geothermal Heat FluxesNon-Technical Description: New observations of Antarctic ice sheet variables are essential for drill-site selection for climate records, for understanding how ice dynamics affect sea level, and for investigating the geologic history of the continent. Temperature depth-profiles are of particular current interest for estimating basal temperature and geothermal heat flux in Antarctica. Antarctic geothermal heat flux is presently poorly known except at recent drilling sites, and is the largest unknown in determining basal conditions. However, current logistical costs greatly limit drilling to acquire temperature profiles. Our long-term goal is the development, testing and commissioning of a new means of acquiring englacial temperature profiles at much lower costs than existing methods. To that end, we will undertake laboratory experiments and numerical modeling to develop to a new way to use ice melt probes, rather than traditional drilling, to deploy temperature measurement equipment to depths of a kilometer and greater. To use melt probes for this purpose, we must keep the melted ice above such probes from freezing completely, so that cable can be fed continually down to the probe as it descends. This development will also open the way toward recovering melt probes, so as to prevent environmental impacts and expense of equipment left in the field. Our initial experiments and modeling will test the validity of our approach and make it ready for further testing in the field.Technical Description: We will undertake laboratory and modeling work (1) to reduce the technical risk in our approach to melt-probe deployment of Raman Distributed Temperature Sensing (DTS) cables; and (2) to begin development of a recoverable ice melt probe. Specifically, we will use numerical modeling of the Stefan problem with cylindrical symmetry to guide detailed designs for cable-heating and anti-freeze injection, and will test and revise candidate designs by means of laboratory testing. We will test the long-term stability of ethanol-filled melt holes, to gauge their suitability for recoverable melt probe systems for temperature measurement (where months-long thermal equilibration after installation will be required). We will gain experience with Raman DTS methods by employing DTS to measure critical temperature data in our laboratory experiments, both within the melt hole and in adjacent ice. To address recoverability, we will design and test a new melt head for the upper end of our ice melt probe, and demonstrate upward travel through a partially refrozen melt hole. Finally, we will publish both modeling and experimental results in peer-reviewed publications, and will present the project to a broad public audience in a special event at a Seattle museum of science and technology. The result of this work will be demonstrated technical readiness for testing in a subsequent project at larger ice-drilling test facilities at the earliest opportunity (prospectively, at the University of Wisconsin, following soon after completion of this project) and, following that, in the field.
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Collaborative Research: CFS (Track III): Centers for Transformative Environmental Monitoring Programs (CTEMPs)
  • 批准号:
    2243964
  • 项目类别:
    Continuing Grant
  • 资助金额:
    $125.83万
  • 财政年份:
    2023
  • 负责人:
    John Selker
  • 依托单位:
Conference: Cargese Graduate Summer School: Connecting Ecosystem processes to hydrogeophysical fundamentals
  • 批准号:
    2408146
  • 项目类别:
    Standard Grant
  • 资助金额:
    $5.0万
  • 财政年份:
    2023
  • 负责人:
    John Selker
  • 依托单位:
Collaborative Research: Community Facility Support: Centers for Transformative Environmental Monitoring Programs (CTEMPs)
  • 批准号:
    1832170
  • 项目类别:
    Continuing Grant
  • 资助金额:
    $124.99万
  • 财政年份:
    2019
  • 负责人:
    John Selker
  • 依托单位:
Collaborative Research: Toward Dense Observation of Geothermal Fluxes in Antarctica Via Logistically Light Instrument Deployment
  • 批准号:
    1744899
  • 项目类别:
    Standard Grant
  • 资助金额:
    $1.0万
  • 财政年份:
    2018
  • 负责人:
    John Selker
  • 依托单位:
国内基金
海外基金
Research on Quantum Field Theory without a Lagrangian Description
  • 批准号:
    24ZR1403900
  • 项目类别:
    省市级项目
  • 资助金额:
    --
  • 批准年份:
    2024
  • 负责人:
    SATOSHI NAWATA
  • 依托单位:
Cell Research
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