Collaborative Research: Antarctic Airborne ElectroMagnetics (ANTAEM) - Revealing Subsurface Water in Coastal Antarctica
合作研究:南极机载电磁学 (ANTAEM) - 揭示南极洲沿海的地下水
基本信息
- 批准号:1644187
- 负责人:
- 金额:$ 50.96万
- 依托单位:
- 依托单位国家:美国
- 项目类别:Standard Grant
- 财政年份:2017
- 资助国家:美国
- 起止时间:2017-09-01 至 2024-08-31
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
In Antarctica, millions of years of freezing have led to the development of hundreds of meters of thick permafrost (i.e., frozen ground). Recent research demonstrated that this slow freezing has trapped and concentrated water into local and regional briny aquifers, many times more salty than seawater. Because salt depresses the freezing point of water, these saline brines are able to persist as liquid water at temperatures well below the normal freezing point of freshwater. Such unusual groundwater systems may support microbial life, supply nutrients to coastal ocean and ice-covered lakes, and influence motion of glaciers. These briny aquifers also represent potential terrestrial analogs for deep life habitats on other planets, such as Mars, and provide a testing ground for the search for extraterrestrial water. Whereas much effort has been invested in understanding the physics, chemistry, and biology of surface and near-surface waters in cold polar regions, it has been comparably difficult to investigate deep subsurface aquifers in such settings. Airborne ElectroMagnetics (AEM) subsurface imaging provides an efficient way for mapping salty groundwater. An international collaboration with the University of Aarhus in Denmark will enable knowledge and skill transfer in AEM techniques that will enhance US polar research capabilities and provide US undergraduates and graduate students with unique training experiences. This project will survey over 1000 km2 of ocean and land near McMurdo Station in Antarctica, and will reveal if cold polar deserts hide a subsurface pool of liquid water. This will have significant implications for understanding cold polar glaciers, ice-covered lakes, frozen ground, and polar microbiology as well as for predictions of their response to future change. Improvements in permafrost mapping techniques and understanding of permafrost and of underlying groundwaters will benefit human use of high polar regions in the Antarctic and the Arctic.The project will provide the first integrative system-scale overview of subsurface water distribution and hydrological connectivity in a partly ice-free coastal region of Antarctica, the McMurdo Dry Valleys. Liquid water is relatively scarce in this environment but plays an outsized role by influencing, and integrating, biological, biogeochemical, glaciological, and geological processes. Whereas surface hydrology and its role in ecosystem processes has been thoroughly studied over the last several decades, it has been difficult to map out and characterize subsurface water reservoirs and to understand their interactions with regional lakes, glaciers, and coastal waters. The proposed project builds on the "proof-of-concept" use of AEM technology in 2011. Improvements in sensor and data processing capabilities will result in about double the depth of penetration of the subsurface during the new data collection when compared to the 2011 proof-of-concept survey, which reached depths of 300-400m. The first field season will focus on collecting deep soundings with a ground-based system in key locations where: (i) independent constraints on subsurface structure exist from past drilling projects, and (ii) the 2011 resistivity dataset indicates the need for deeper penetration and high signal-to-noise ratios achievable only with a ground-based system. The regional airborne survey will take place during the second field season and will yield subsurface electrical resistivity data from across several valleys of different sizes and different ice cover fractions.
在南极洲,数百万年的冰冻导致了数百米厚的永久冻土层的形成(即,冻结的土地)。最近的研究表明,这种缓慢的冻结已经将水捕获并浓缩到当地和区域的盐水含水层中,其盐度比海水高出许多倍。由于盐降低了水的冰点,这些盐水能够在远低于淡水正常冰点的温度下作为液态水存在。这种不寻常的地下水系统可能支持微生物的生命,为沿海海洋和冰雪覆盖的湖泊提供营养,并影响冰川的运动。这些咸水层也代表了其他行星(如火星)上深层生命栖息地的潜在陆地类似物,并为寻找外星水提供了试验场。尽管人们在了解寒冷极地地区地表和近地表沃茨的物理、化学和生物学方面投入了大量努力,但在这种环境下调查深层地下含水层却非常困难。航空电磁(AEM)地下成像提供了一种有效的方法来测绘咸水。与丹麦奥胡斯大学的国际合作将实现AEM技术的知识和技能转移,这将提高美国极地研究能力,并为美国本科生和研究生提供独特的培训经验。该项目将调查南极洲麦默多站附近超过1000平方公里的海洋和陆地,并将揭示寒冷的极地沙漠是否隐藏着液态水的地下水池。这将对了解寒冷的极地冰川、冰封的湖泊、冻土和极地微生物学以及预测它们对未来变化的反应产生重大影响。永久冻土测绘技术的改进以及对永久冻土和地下水的了解将有利于人类利用南极和北极的高极地区,该项目将首次提供南极洲部分无冰沿海地区(麦克默多干谷)地下水分布和水文连通性的综合系统规模概览。在这种环境中,液态水相对稀缺,但通过影响和整合生物,地球化学,冰川学和地质过程发挥着巨大的作用。尽管地表水文学及其在生态系统过程中的作用在过去几十年中得到了深入的研究,但很难绘制地下水库的地图并确定其特征,也很难了解它们与区域湖泊、冰川和沿海沃茨的相互作用。拟议的项目建立在2011年使用AEM技术的“概念验证”的基础上。与2011年的概念验证调查相比,传感器和数据处理能力的改进将使新数据收集期间的地下穿透深度增加一倍,该调查达到300- 400米的深度。第一个勘探季节将侧重于在以下关键地点使用地基系统收集测深数据:(i)过去钻探项目对地下结构存在独立的限制,(ii)2011年电阻率数据集表明需要更深的穿透和只有地基系统才能实现的高信噪比。区域航空勘测将在第二个实地季节进行,并将从不同大小和不同冰盖分数的几个山谷中获得地下电阻率数据。
项目成果
期刊论文数量(8)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Mapping geothermal heat flux using permafrost thickness constrained by airborne electromagnetic surveys on the western coast of Ross Island, Antarctica
- DOI:10.1080/08123985.2019.1651618
- 发表时间:2020-01
- 期刊:
- 影响因子:0.9
- 作者:N. Foley;S. Tulaczyk;E. Auken;D. Grombacher;J. Mikucki;N. Foged;K. Myers;H. Dugan;P. Doran;R. Virginia
- 通讯作者:N. Foley;S. Tulaczyk;E. Auken;D. Grombacher;J. Mikucki;N. Foged;K. Myers;H. Dugan;P. Doran;R. Virginia
Brief communication: The hidden labyrinth: deep groundwater in Wright Valley, Antarctica
简讯:隐藏的迷宫:南极洲莱特谷的深层地下水
- DOI:10.5194/tc-16-4977-2022
- 发表时间:2022
- 期刊:
- 影响因子:0
- 作者:Dugan, Hilary A.;Doran, Peter T.;Grombacher, Denys;Auken, Esben;Bording, Thue;Foged, Nikolaj;Foley, Neil;Mikucki, Jill;Virginia, Ross A.;Tulaczyk, Slawek
- 通讯作者:Tulaczyk, Slawek
The role of electrical conductivity in radar wave reflection from glacier beds
电导率在冰川床雷达波反射中的作用
- DOI:10.5194/tc-14-4495-2020
- 发表时间:2020
- 期刊:
- 影响因子:0
- 作者:Tulaczyk, Slawek M.;Foley, Neil T.
- 通讯作者:Foley, Neil T.
Thermal legacy of a large paleolake in Taylor Valley, East Antarctica, as evidenced by an airborne electromagnetic survey
机载电磁调查证明,东南极洲泰勒谷一个大型古湖的热遗产
- DOI:10.5194/tc-15-3577-2021
- 发表时间:2021
- 期刊:
- 影响因子:0
- 作者:Myers, Krista F.;Doran, Peter T.;Tulaczyk, Slawek M.;Foley, Neil T.;Bording, Thue S.;Auken, Esben;Dugan, Hilary A.;Mikucki, Jill A.;Foged, Nikolaj;Grombacher, Denys
- 通讯作者:Grombacher, Denys
Evidence for Pathways of Concentrated Submarine Groundwater Discharge in East Antarctica from Helicopter-Borne Electrical Resistivity Measurements
- DOI:10.3390/hydrology6020054
- 发表时间:2019-06-01
- 期刊:
- 影响因子:3.2
- 作者:Foley, Neil;Tulaczyk, Slawek M.;Virginia, Ross
- 通讯作者:Virginia, Ross
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Slawek Tulaczyk其他文献
Ice-sheet mass balance and climate change
冰盖质量平衡与气候变化
- DOI:
10.1038/nature12238 - 发表时间:
2013-06-05 - 期刊:
- 影响因子:48.500
- 作者:
Edward Hanna;Francisco J. Navarro;Frank Pattyn;Catia M. Domingues;Xavier Fettweis;Erik R. Ivins;Robert J. Nicholls;Catherine Ritz;Ben Smith;Slawek Tulaczyk;Pippa L. Whitehouse;H. Jay Zwally - 通讯作者:
H. Jay Zwally
Uranium-series isotopes as tracers of physical and chemical weathering in glacial sediments from Taylor Valley, Antarctica
- DOI:
10.1016/j.chemgeo.2024.122463 - 发表时间:
2025-01-05 - 期刊:
- 影响因子:
- 作者:
Graham Harper Edwards;Gavin G. Piccione;Terrence Blackburn;Slawek Tulaczyk - 通讯作者:
Slawek Tulaczyk
Slawek Tulaczyk的其他文献
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{{ truncateString('Slawek Tulaczyk', 18)}}的其他基金
Ross Ice Shelf Geothermal Flux (RISGF) - Direct Borehole Measurements as Part of the New Zealand Ross Ice Shelf Programme
罗斯冰架地热通量 (RISGF) - 直接钻孔测量是新西兰罗斯冰架计划的一部分
- 批准号:
1745124 - 财政年份:2019
- 资助金额:
$ 50.96万 - 项目类别:
Standard Grant
NSF-NERC: Thwaites Interdisciplinary Margin Evolution (TIME): The Role of Shear Margin Dynamics in the Future Evolution of the Thwaites Drainage Basin
NSF-NERC:思韦茨跨学科边缘演化(TIME):剪切边缘动力学在思韦茨流域未来演化中的作用
- 批准号:
1739027 - 财政年份:2018
- 资助金额:
$ 50.96万 - 项目类别:
Continuing Grant
Collaborative Research: EAGER: Processing, Interpretation and Dissemination of the Proof-of-Concept Transient Electromagnetic Survey of the McMurdo Dry Valleys Region
合作研究:EAGER:麦克默多干谷地区概念验证瞬态电磁调查的处理、解释和传播
- 批准号:
1344349 - 财政年份:2013
- 资助金额:
$ 50.96万 - 项目类别:
Standard Grant
Collaborative Research: Developing New Science and Technology for Subglacial Studies of the Whillans Ice Plain and West Antarctic Ice Sheet
合作研究:为威兰斯冰原和西南极冰盖的冰下研究开发新科学技术
- 批准号:
1346251 - 财政年份:2013
- 资助金额:
$ 50.96万 - 项目类别:
Standard Grant
Collaborative Research: MIDGE: Minimally Invasive Direct Glacial Exploration of Biogeochemistry, Hydrology and Glaciology of Blood Falls, McMurdo Dry Valleys
合作研究:MIDGE:麦克默多干谷血瀑布生物地球化学、水文学和冰川学的微创直接冰川探索
- 批准号:
1144192 - 财政年份:2012
- 资助金额:
$ 50.96万 - 项目类别:
Standard Grant
Collaborative Research: Integrative Study of Marine Ice Sheet Stability & Subglacial Life Habitats in W Antarctica - Lake & Ice Stream Subglacial Access Research Drilling (
合作研究:海洋冰盖稳定性综合研究
- 批准号:
0839142 - 财政年份:2009
- 资助金额:
$ 50.96万 - 项目类别:
Standard Grant
Collaborative Research: Integrative Study of Marine Ice Sheet Stability and Subglacial Life Habitats - Robotic Access to Grounding-zones for Exploration and Science (RAGES)
合作研究:海洋冰盖稳定性和冰下生命栖息地的综合研究 - 机器人进入勘探和科学接地区(RAGES)
- 批准号:
0838947 - 财政年份:2009
- 资助金额:
$ 50.96万 - 项目类别:
Standard Grant
COLLABORATIVE RESEARCH: Elevation Change Anomalies in West Antarctica and Dynamics of Subglacial Water Transport Beneath Ice Streams and their Tributaries
合作研究:南极洲西部的海拔变化异常以及冰流及其支流下方冰下水输送的动态
- 批准号:
0636970 - 财政年份:2007
- 资助金额:
$ 50.96万 - 项目类别:
Continuing Grant
Collaborative Research: IPY, The Next Generation: A Community Ice Sheet Model for Scientists and Educators With Demonstration Experiments in Amundsen Sea Embayment Region
合作研究:IPY,下一代:为科学家和教育工作者在阿蒙森海湾地区进行示范实验的社区冰盖模型
- 批准号:
0632346 - 财政年份:2007
- 资助金额:
$ 50.96万 - 项目类别:
Standard Grant
Was the Deepest Lake in North America a Subglacial Lake?
北美最深的湖泊是冰下湖吗?
- 批准号:
0612385 - 财政年份:2006
- 资助金额:
$ 50.96万 - 项目类别:
Standard Grant
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