Collaborative Research: Meshed GNSS-Acoustic Array Design for Lower-Cost Dense Observation Fields

合作研究：用于低成本密集观测场的网状 GNSS 声学阵列设计

• 批准号: 2321297
• 负责人: Andrew Newman
• 金额: $ 49.01万
• 依托单位: Georgia Tech Research Corporation
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2024
• 资助国家: 美国
• 起止时间: 2024-01-01 至 2026-12-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2321297&HistoricalAwards=false
• 关键词: Collaborative; Research; Meshed; GNSS; Acoustic

Precise observations of seafloor deformation is important for assessing ongoing geologic processes and the hazards they pose, including the largest earthquakes, tsunamis, submarine volcanism, hydrocarbon changes, and submarine landslides. Making observations of the centimeter-scale deformation that occurs over a year or longer using a combination of sea surface and seafloor instrumentation is currently expensive, particularly when using a large research vessel as a part of the measurement design. In this project, the team will use a rather new but previously tested autonomous, green-powered vessel that replaces the ship-based measurement design, reducing measurement costs by more than an order of magnitude over prior methods. To further reduce instrumentation costs and enable more broad use, the project will test new design geometries that have the potential to significantly increase capabilities where dense observations are needed. During this project, a postdoctoral scholar will be trained as a next-generation scientist and educator. The data collected will be contributed to a community data archive, and methods will be incorporated into community software for research. Following the project, the instrumentation will become a part of an existing NSF-funded instrument pool, doubling the capabilities for deep-water observations from 3000 to 6000 meters. The surface vessel for these operations, a commercially available Wave Glider, will be outfitted with antennas for positioning itself using Global Navigational Satellite Systems (GNSS). The vessel will interrogate a mesh-network of seafloor transponders during the summers of 2024 and 2025 using a lower frequency acoustic signal than currently available with the US instrument pool to allow for the extended ranging needed for deeper water operation. The 10-transponder array will be deployed between 4 and 6 km depth along a segment of the Aleutian trench in 2024, combining ship-activities with an existing community geodetic experiment, that can only extend to 3 km depth. The dense mesh-network design with the shared use of transponders could potentially allow for a ten-fold increase in instrumental efficiency, depending on geometry, over existing methods existing methods that require three transponders per observation point. Lastly, the experiment will additionally evaluate the potentially increased errors associated with necessarily high-gradient seafloor environments that are common in subduction zones. Such steep measurements could be similarly applied to passive continental slopes that have the potential for destructive submarine landslides. While the design experiment tests methodology, the location was chosen because little is known about the behavior of faults in the region, where a large earthquake in 1946 created an outsized tsunami. Detailed information about ongoing fault behavior in the region can illuminate the currently unknown mechanical coupling in the region that builds for future earthquakes.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.

对海底变形的精确观测对于评估正在进行的地质过程及其造成的危害非常重要，包括最大的地震、海啸、海底火山活动、碳氢化合物变化和海底滑坡。 目前，使用海面和海底仪器对一年或更长时间内发生的厘米级变形进行观测的费用很高，特别是在使用大型研究船作为测量设计的一部分时。 在这个项目中，该团队将使用一个相当新的，但以前测试过的自主，绿色动力船舶，取代基于船舶的测量设计，降低测量成本超过一个数量级比以前的方法。 为了进一步降低仪器成本并实现更广泛的使用，该项目将测试新的设计几何形状，这些几何形状有可能显着提高需要密集观测的能力。在该项目中，一名博士后学者将被培养为下一代科学家和教育家。 收集到的数据将被贡献给社区数据档案，方法将被纳入社区软件进行研究。 该项目完成后，这些仪器将成为现有NSF资助的仪器池的一部分，使3000米至6000米的深水观测能力翻一番。用于这些行动的水面船只是一种商用波浪滑翔机，将配备天线，利用全球导航卫星系统进行定位。 该船将在2024年和2025年夏季使用比美国仪器池目前可用的频率更低的声学信号来询问海底应答器的网状网络，以允许更深水域操作所需的扩展范围。2024年，将在阿留申海沟的一段沿着4至6公里深处部署10个转发器阵列，将船舶活动与现有的社区大地测量实验相结合，该实验只能延伸到3公里深处。与每个观测点需要三个转发器的现有方法相比，共享转发器的密集网状网络设计可能使仪器效率提高十倍，这取决于几何形状。 最后，实验还将评估与俯冲带常见的高梯度海底环境相关的潜在增加的误差。 这种陡峭的测量可以同样适用于有可能造成破坏性海底山崩的被动大陆斜坡。虽然设计实验测试方法，但选择这个地点是因为对该地区断层的行为知之甚少，1946年的一次大地震造成了特大海啸。有关该地区正在进行的断层行为的详细信息可以阐明该地区目前未知的机械耦合，为未来的地震奠定基础。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进行评估，被认为值得支持。