Analysis of an Extensive Towed Streamer Dataset Collected on the New England Continental Shelf

对新英格兰大陆架收集的大量拖缆数据集的分析

• 批准号: 1953325
• 负责人: Alan Chave
• 金额: $ 18.21万
• 依托单位: Woods Hole Oceanographic Institution
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2020
• 资助国家: 美国
• 起止时间: 2020-05-01 至 2021-04-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1953325&HistoricalAwards=false
• 关键词: Analysis; Extensive; Towed; Streamer; Dataset

Groundwater on continental shelves is a new frontier in water sciences. A modeling study suggests that over a thousand cubic kilometers of fresh water could be trapped offshore New England, and hundreds of thousands of cubic kilometers exist within passive continental margins globally. For reference, the City of New York consumes roughly a cubic kilometer per year. Under recent NSF support, a towed electromagnetic (CSEM) system was designed, constructed, and tested that is aimed at surveying offshore groundwater. This technique builds on experience in the petroleum industry using a similar technology. CSEM is preferentially sensitive to resistive bodies, which include fresh water. During the course of an 8-day test cruise in August 2019, more than 700 km of data were collected over a region extending from the east end of Martha’s Vineyard to offshore Long Island and from coastal waters to the edge of the continental shelf. This proposal seeks to analyze, model, and interpret this exciting data set. Specifically, the inference that the entire New England shelf is underlain by freshwater is a hypothesis that can be partially tested. The result will contribute to national health and welfare, and has societal relevance given the increasing scarcity of fresh water. The towed streamer CSEM system is composed of a 1-km long receive streamer towed at half of the water depth, and a 250-m long transmit dipole towed near the surface. The transmit streamer is powered by a 250-A source producing a bespoke waveform between 0.1-10 Hz. Data are available in real time via optical fibers in the streamer cable. Data are collected in “shots”, each 60 s, of transmitted waveforms and 10 s with the transmitter off to measure noise levels. The work to be carried out under this proposal includes: 1) merging the navigation and streamer attitude data to produce a model for receiver location as a function of time, 2) computing the frequency response of each shot, removing the source response in the process, 3) devising a robust method for culling out the shots that are noisy to produce a final data set, 4) merging the navigation and shot data to produce a final data set containing location, depth, amplitude and phase, and 5) inverting the data to produce 2D resistivity maps along the various lines where data were collected.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.

大陆架地下水是水科学研究的新前沿。一项模拟研究表明，超过1000立方公里的淡水可能被困在新英格兰近海，全球有数十万立方公里的淡水存在于被动大陆边缘。作为参考，纽约市每年消耗大约1立方公里。在美国国家科学基金会最近的支持下，拖曳电磁（CSEM）系统的设计，建造和测试，旨在调查近海地下水。这种技术建立在石油工业使用类似技术的经验基础上。CSEM优先对包括淡水的电阻体敏感。在2019年8月为期8天的测试巡航过程中，从玛莎葡萄园岛的伦敦东区到长岛近海以及从沿海沃茨到大陆架边缘的区域收集了700多公里的数据。该提案旨在分析，建模和解释这一令人兴奋的数据集。具体来说，整个新英格兰大陆架都被淡水覆盖的推论是一个可以部分验证的假设。其结果将有助于国民健康和福利，并具有社会意义，因为淡水日益稀缺。拖曳式拖缆CSEM系统由一根1 km长的接收拖缆和一根250 m长的发射偶极子组成，接收拖缆在水深的一半处拖曳，发射偶极子在水面附近拖曳。发射拖缆由250 A电源供电，产生0.1-10 Hz之间的定制波形。数据可通过拖缆中的光纤进行真实的实时传输。数据是以“发射”的方式收集的，每60 s发射波形和10 s发射器关闭以测量噪声水平。根据这一建议开展的工作包括：1）合并导航和拖缆姿态数据以产生作为时间的函数的接收器位置的模型，2）计算每个炮点的频率响应，在该过程中去除源响应，3）设计用于剔除有噪声的炮点以产生最终数据集的鲁棒方法，4）合并导航和激发数据以产生包含位置、深度、幅度和相位的最终数据集，和5）反演数据，沿采集数据的各条线路沿着生成二维电阻率图。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准。