Collaborative Research: He-CO2-N2 Isotopes and Dissolved Gases in Groundwaters of the Costa Rica Fore-arc Margin

合作研究：哥斯达黎加弧前缘地下水中的 He-CO2-N2 同位素和溶解气体

• 批准号: 1049748
• 负责人: David Hilton
• 金额: $ 24.46万
• 依托单位: University of California-San Diego Scripps Inst of Oceanography
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2011
• 资助国家: 美国
• 起止时间: 2011-08-01 至 2016-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1049748&HistoricalAwards=false
• 关键词: Collaborative; Research; He; CO2; N2

Fluid flow through subduction zones is a fundamental process on Earth. As oceanic plates get subducted into Earths interior, water and other volatiles (i.e. CO2, N2) are released from the subducting plate into the overlying mantle wedge. These fluids are the primary cause for the melting of the mantle and the production of water-rich magmas that cause explosive volcanic eruptions. In addition, volatiles are either efficiently recycled back to the atmosphere through subduction-related volcanoes (as is the case for N2) or are potentially carried into the deep mantle (as may be the case for CO2). The extent of volatile recycling in subduction zones, therefore, has significant bearing on the overall volatile composition of the mantle and the atmosphere. In this proposal, the research team will target localities within the Costa Rica subduction zone complex where gas-rich cold springs release volatiles to the atmosphere. In addition, several springs will be monitored continuously for gas composition in order to investigate temporal changes related to earthquake activity occurring in the region. The research plan of this project involves producing a volatile dataset - comprising the isotope systematics and abundance characteristics of He, CO2, N2, CH4, O2, and Ar together with major/trace element, stable isotope (D/H and 18O/16O) and carbon-14 signatures of aqueous fluids (groundwaters), with the aim of understanding details of volatile provenance, flux and temporal variability. These springs are located trench-ward of the volcanic front and therefore sample volatiles that are potentially released from the mantle lithosphere and/or crust of the subducting slab before it reaches a depth corresponding to the volcanic front. In this way, this work aims at investigating what proportions of the volatiles that are subducted actually reach the volcanic front. Additionally, as various volatile species are expected to have different release/retention characteristics on the down-going plate, we can gauge how volatiles fractionate from one another by sampling profiles parallel to the direction of plate convergence. Moreover, by taking advantage of well-mapped structural controls on the hydrogeology, we will also determine the influence of faulting on the loss of volatiles along three targeted sections of the Costa Rica fore-arc (Nicoya, Central Pacific Coast and Oso Peninsula). Finally, because the fore-arc region of Costa Rica is the location of numerous large earthquakes occurring on a large number of active faults, it is proposed to investigate the relationships between fault localities, the occurrence of cold springs, gas compositions, and earthquake activity through (a) a widespread sampling campaign targeting ~ 100 sampling locations at the three sections of the forearc, and (b) continuously monitoring the gas composition of several selected springs using specifically-developed instrumentation (Spartah device). In the case of a local earthquake, the team anticipates being able to capture such an event by continuous monitoring of gas chemistry and documenting any changes in the gas composition of the springs. This part of the project has the potential to better understand earthquake processes in this region. To further these aims and to provide research opportunities for local scientists, the PIs will contribute to the M.Sc. Hydrogeology program at the University of Costa Rica through lectures, practical sessions and field-based training modules covering various aspects of hydrogeology, hydrochemistry, volcanology and structural geology. Monitoring efforts at Poas volcano in Costa Rica will also continue to investigate the potential role of volatiles in signaling the onset of impending hazardous conditions at the volcano.

通过俯冲带的流体流动是地球上的一个基本过程。 随着大洋板块俯冲到地球内部，水和其他挥发性物质（即CO2，N2）从俯冲板块释放到上覆的地幔楔中。 这些流体是地幔熔化和产生富水岩浆的主要原因，这些岩浆导致火山爆发。 此外，挥发物要么通过与俯冲有关的火山有效地再循环回大气（如N2的情况），要么可能被带入地幔深处（如CO2的情况）。 因此，俯冲带中挥发性物质再循环的程度对地幔和大气的整体挥发性成分有着重要的影响。 在这项提议中，研究小组将目标对准哥斯达黎加俯冲带复合体内的地点，那里富含气体的冷泉将挥发物释放到大气中。 此外，还将持续监测几个泉水的气体成分，以调查与该地区发生的地震活动有关的时间变化。该项目的研究计划包括制作一个挥发性数据集-包括He、CO2、N2、CH 4、O2和Ar的同位素系统学和丰度特征，以及主要/微量元素、稳定同位素（D/H和18 O/16 O）和含水流体（地下水）的碳-14特征，目的是了解挥发性物质来源、通量和时间变异性的细节。 这些泉水位于火山锋面的海沟方向，因此在俯冲板片到达与火山锋面对应的深度之前，对可能从俯冲板片的地幔岩石圈和/或地壳释放的挥发物进行采样。通过这种方式，这项工作的目的是调查什么比例的挥发物是俯冲实际上达到火山前。此外，由于预计各种挥发性物质在下行板上具有不同的释放/保留特性，因此我们可以通过平行于板会聚方向的采样剖面来测量挥发性物质如何彼此分离。此外，通过利用绘制良好的水文地质结构控制，我们还将确定断层对哥斯达黎加弧前（尼科亚，中太平洋海岸和奥索半岛）的三个目标部分沿着挥发物损失的影响。最后，由于哥斯达黎加的弧前地区是发生在大量活动断层上的许多大地震的位置，因此建议通过以下方式调查断层位置、冷泉的出现、气体成分和地震活动之间的关系：（a）在弧前三个部分的大约100个采样点进行广泛的采样活动，和（B）使用专门开发的仪器（Spartah装置）连续监测几个选定弹簧的气体组成。在当地发生地震的情况下，该团队预计能够通过持续监测气体化学并记录泉水气体成分的任何变化来捕获此类事件。该项目的这一部分有可能更好地了解该地区的地震过程。为了进一步实现这些目标，并为当地科学家提供研究机会，PI将通过讲座，实践课程和实地培训模块，涵盖水文地质学，水文化学，火山学和结构地质学的各个方面，为哥斯达黎加大学的水文地质学硕士课程做出贡献。对哥斯达黎加波阿斯火山的监测工作也将继续调查挥发物在发出火山即将发生危险情况的信号方面的潜在作用。