Marine CSEM study of the southern Hikurangi Margin: A first step towards estimating the global gas hydrate carbon budget
希库朗吉边缘南部的海洋 CSEM 研究:估算全球天然气水合物碳预算的第一步
基本信息
- 批准号:1916553
- 负责人:
- 金额:$ 73.49万
- 依托单位:
- 依托单位国家:美国
- 项目类别:Continuing Grant
- 财政年份:2019
- 资助国家:美国
- 起止时间:2019-08-01 至 2021-07-31
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
Gas hydrate is a solid ice-like mixture of water and gas, usually methane, that forms in seafloor sediments when pressure is high enough and temperature is cold enough. Such conditions are found in water depths greater than about 500 m, and gas hydrate is found on continental slopes world-wide wherever there is methane produced from the decay of organic matter or leaking from hydrocarbon systems. Vast amounts of carbon have accumulated this way, but estimates of the total quantity vary by several orders of magnitude, mainly because of limitations in using seismic methods to assess hydrate concentration, especially at lower concentrations. This gap in knowledge is a problem, because hydrate can have a big impact on human activity and well-being. Changes in sea level or temperature can cause hydrate to decompose, possibly contributing to seafloor landslides that can trigger tsunamis. Loss of sediment stability from hydrate decomposition can damage man-made seafloor infrastructure. Methane leaking from the seafloor is used as energy by some biological systems, but if too much escapes it can add to acidification and impact the health of the oceans. This project will begin to plug the gaps in knowledge about offshore hydrate by using a novel non-seismic geophysical method to image hydrate under hundreds of square kilometers of seafloor off the southern margin of New Zealand's North Island, where abundant seismic data have been collected and hydrate is inferred to exist in both low and high concentrations over broad regions. The project supports the training of an early career scientist.The electrical resistivity of methane hydrate is four orders of magnitude greater than seafloor sediment, and sediment resistivity varies smoothly and monotonically with hydrate saturation. We have developed a deep-towed controlled source electromagnetic (CSEM) system to image seafloor resistivity and have validated its use for quantifying seafloor hydrate concentrations off California, Japan, and the Gulf of Mexico. Typically CSEM studies target known methane seeps and hydrate deposits, but in this project data will be collected on a basin-scale to capture the broad distribution, using the Hikurangi subduction zone as a model to develop an understanding of the global hydrate inventory by extrapolation to subduction zones worldwide. By combining existing seismic data with the new CSEM data, through a collaboration with colleagues in New Zealand, the processes that concentrate hydrate will be examined, how much hydrate sits at the upper edge of the stability field (and thus vulnerable to dissociation) will be assessed, the relationships between free gas and gas hydrate (both resistive but easily distinguished in seismic data) will be studied, and the background levels of hydrate and the total hydrate inventory of the Pegasus Basin will be estimated.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
天然气水合物是一种固体冰状的水和气体(通常是甲烷)的混合物,当压力足够高,温度足够低时,它会在海底沉积物中形成。 在水深超过500米的地方都有这种情况,在世界各地的大陆坡上,只要有有机物腐烂产生的甲烷或碳氢化合物系统的泄漏,都有天然气水合物。 大量的碳以这种方式积累起来,但对总量的估计相差几个数量级,主要是因为使用地震方法评估水合物浓度的局限性,特别是在较低浓度时。 这种知识差距是一个问题,因为水合物可能对人类活动和福祉产生重大影响。海平面或温度的变化可能会导致水合物分解,可能会导致海底山体滑坡,从而引发海啸。水合物分解造成的沉积物稳定性丧失会破坏人造海底基础设施。 从海底泄漏的甲烷被一些生物系统用作能源,但如果泄漏太多,它可能会增加酸化并影响海洋的健康。该项目将开始填补关于海上水合物的知识空白,方法是使用一种新的非地震地球物理方法,对新西兰北岛南部边缘数百平方公里海底下的水合物进行成像,在那里收集了丰富的地震数据,并推断水合物在广泛的区域内以低浓度和高浓度存在。甲烷水合物的电阻率比海底沉积物大四个数量级,沉积物电阻率随水合物饱和度的变化平稳而单调。 我们已经开发了一种深拖可控源电磁(CSEM)系统,以成像海底电阻率,并验证了其用于量化加州,日本和墨西哥湾海底水合物浓度。 通常,CSEM研究针对已知的甲烷渗漏和水合物矿床,但在本项目中,将在盆地规模上收集数据,以获取广泛的分布,使用Hikurangi俯冲带作为模型,通过外推到全球俯冲带来了解全球水合物库存。 通过与新西兰同事的合作,将现有地震数据与新的CSEM数据相结合,将检查浓缩水合物的过程,(因此容易分解)将被评估,游离气体和天然气水合物之间的关系(两者都是电阻性的,但在地震数据中容易区分)将被研究,和水合物的背景水平和飞马座盆地的总水合物库存将估计。这一奖项反映了NSF的法定使命,并已被视为通过使用基金会的知识价值和更广泛的影响审查标准进行评估,
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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Steven Constable其他文献
Conduction by mantle hydrogen
地幔氢传导
- DOI:
10.1038/362704a0 - 发表时间:
1993-04-22 - 期刊:
- 影响因子:48.500
- 作者:
Steven Constable - 通讯作者:
Steven Constable
Steven Constable的其他文献
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{{ truncateString('Steven Constable', 18)}}的其他基金
Collaborative Research: NSFGEO-NERC: Magnetotelluric imaging and geodynamical/geochemical investigations of plume-ridge interaction in the Galapagos
合作研究:NSFGEO-NERC:加拉帕戈斯群岛羽流-山脊相互作用的大地电磁成像和地球动力学/地球化学研究
- 批准号:
2334542 - 财政年份:2024
- 资助金额:
$ 73.49万 - 项目类别:
Continuing Grant
Collaborative Research: Magnetotelluric Investigation of the Salton Trough
合作研究:索尔顿海槽的大地电磁调查
- 批准号:
2243695 - 财政年份:2023
- 资助金额:
$ 73.49万 - 项目类别:
Continuing Grant
Collaborative research: A better understanding of seismic hazard in Tehuantepec, Mexico, using amphibious MT studies
合作研究:利用两栖 MT 研究更好地了解墨西哥特万特佩克的地震灾害
- 批准号:
2105776 - 财政年份:2021
- 资助金额:
$ 73.49万 - 项目类别:
Standard Grant
NSFGEO-NERC: Quantifying evolution of magmatism and serpentinisation during the onset of seafloor spreading
NSFGEO-NERC:量化海底扩张开始期间岩浆作用和蛇纹石化的演化
- 批准号:
2026866 - 财政年份:2020
- 资助金额:
$ 73.49万 - 项目类别:
Standard Grant
The Mendocino Fracture Zone: A natural laboratory to study aging of the lithosphere and asthenosphere
门多西诺断裂带:研究岩石圈和软流圈老化的天然实验室
- 批准号:
1736590 - 财政年份:2017
- 资助金额:
$ 73.49万 - 项目类别:
Continuing Grant
Central Atlantic Lithosphere-Asthenosphere Boundary Study
中大西洋岩石圈-软流圈边界研究
- 批准号:
1536400 - 财政年份:2015
- 资助金额:
$ 73.49万 - 项目类别:
Continuing Grant
A mineral-physics based model of mantle electrical conductivity
基于矿物物理学的地幔电导率模型
- 批准号:
1112861 - 财政年份:2011
- 资助金额:
$ 73.49万 - 项目类别:
Continuing Grant
Collaborative Research: SERPENT: Serpentinite, Extension and Regional Porosity Experiment across the Nicaraguan Trench
合作研究:SERPENT:尼加拉瓜海沟的蛇纹岩、延伸和区域孔隙度实验
- 批准号:
0841114 - 财政年份:2009
- 资助金额:
$ 73.49万 - 项目类别:
Standard Grant
Constraining the Magmatic Budget of the EPR at 9-N Using Broadband Marine MT
使用宽带海洋 MT 将 EPR 的岩浆预算限制在 9-N
- 批准号:
0241597 - 财政年份:2003
- 资助金额:
$ 73.49万 - 项目类别:
Standard Grant
Collaborative Research: Global Conductivity by Spatiotemporal Analysis
合作研究:时空分析的全球电导率
- 批准号:
0087391 - 财政年份:2001
- 资助金额:
$ 73.49万 - 项目类别:
Continuing Grant
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- 批准号:42274104
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- 资助金额:23.0 万元
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基于共轭梯度再加权优化的时间域海洋CSEM 1D各向异性反演研究
- 批准号:41406020
- 批准年份:2014
- 资助金额:25.0 万元
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相似海外基金
MRI: Development of a Towed Streamer Controlled Source Electromagnetic (CSEM) System for Groundwater Mapping on the Continental Shelf
MRI:开发用于大陆架地下水测绘的拖缆控制源电磁 (CSEM) 系统
- 批准号:
1726798 - 财政年份:2017
- 资助金额:
$ 73.49万 - 项目类别:
Standard Grant
Market study to assess the market acceptability of CSEM and to quantify the Economic and environmental benefits
市场研究,评估 CSEM 的市场可接受性并量化经济和环境效益
- 批准号:
NE/P008933/1 - 财政年份:2016
- 资助金额:
$ 73.49万 - 项目类别:
Research Grant
Transformation of CSEM data for determination of resistivities by seismic data processing methods.
通过地震数据处理方法转换 CSEM 数据以测定电阻率。
- 批准号:
NE/L008432/1 - 财政年份:2013
- 资助金额:
$ 73.49万 - 项目类别:
Research Grant
Forwaed Modeling and Inversion of Controlled Source Electromagnetic (CSEM) data
可控源电磁 (CSEM) 数据的前沿建模和反演
- 批准号:
319220-2006 - 财政年份:2006
- 资助金额:
$ 73.49万 - 项目类别:
Postgraduate Scholarships - Master's
Forwaed Modeling and Inversion of Controlled Source Electromagnetic (CSEM) data
可控源电磁 (CSEM) 数据的前沿建模和反演
- 批准号:
319220-2005 - 财政年份:2005
- 资助金额:
$ 73.49万 - 项目类别:
Alexander Graham Bell Canada Graduate Scholarships - Master's
CSEM Scholarships at the University of Colorado at Colorado Springs
科罗拉多大学科罗拉多斯普林斯分校 CSEM 奖学金
- 批准号:
0422524 - 财政年份:2004
- 资助金额:
$ 73.49万 - 项目类别:
Standard Grant
Recruitment and Retention of CSEM Students in the Underrepresented Groups
代表性不足群体中 CSEM 学生的招募和保留
- 批准号:
0220695 - 财政年份:2002
- 资助金额:
$ 73.49万 - 项目类别:
Standard Grant
Computer Science, Engineering, and Mathematics (CSEM) Scholarships for the 21st Century
21 世纪计算机科学、工程和数学 (CSEM) 奖学金
- 批准号:
0220547 - 财政年份:2002
- 资助金额:
$ 73.49万 - 项目类别:
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Department of CSEM Enhancment Program at JSU
JSU CSEM 强化项目部
- 批准号:
0122929 - 财政年份:2001
- 资助金额:
$ 73.49万 - 项目类别:
Standard Grant














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