NSF-BSF: Collaborative research: The Processes and feedbacks that induce multi-scale interactions between local divide migration, drainage reversal and escarpment evolution

NSF-BSF：合作研究：引起局部鸿沟迁移、排水逆转和悬崖演化之间多尺度相互作用的过程和反馈

基本信息

批准号：
1945970
负责人：
Sean Gallen
金额：
$ 5.54万
依托单位：
Colorado State University
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：
2020-01-15 至 2023-12-31
项目状态：
已结题

来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=1945970&HistoricalAwards=false
关键词：
NSF BSF Collaborative research Processes

项目摘要

The structure of river networks impacts the spatial distribution of elevation, water, and life across Earth’s surface. Interestingly, this structure changes through time by movement of the water divides that separate river basins. The divide migration process occurs at the local hillslope scale but the driving forces for it are rooted in large scale tectonic and climatic changes. Furthermore, local processes of divide migration influence the broader geomorphic, hydrologic, and ecologic functionality of the Earth’s surface. The proposed research explores the mechanisms through which these multi-scale processes occur. More specifically, how local topographic, hydrologic, and lithologic conditions lead to a cascade of feedbacks that can ultimately have a large scale impact on the Earth system. This binational project compares and contrasts arid and humid research sites in Israel and the USA, respectively, and will thus strengthen research collaboration between the two countries. The research team will also develop and lead an enhanced science education program for K6-8 students in schools in Pennsylvania and Colorado, including schools with high attendance of underrepresented populations.Water divides play a critical role in controlling the form of landscapes and shaping hydrologic and geomorphic functionality. The mobility of water divides is inherently related to the local hillslope and fluvial processes that control the adjacent relief. At the same time, divide mobility leads to reorganization of the drainage network, which significantly influence large-scale topographic, isostatic, and stratigraphic patterns. At present, the processes and feedbacks by which local hillslope and fluvial regimes interact with basin-scale drainage reorganization and with large scale topographic and isostatic changes remain generally unexplored. To address these knowledge gaps, this research focuses on the juxtaposition of topographic escarpments and reversed channels (an end-member of reorganization), where the initial conditions for divide migration are relatively well constrained. In this setting, the topology and sediments of the reversed channels record the history of divide migration. These channels preserve evidence for how local lithologic and hydrologic conditions act as a tipping point that drives the system into a cascading response that results in drainage reorganization, topographic changes and potentially isostatic adjustments. To explore the generality of these processes, the investigators will compare and contrast the emerging landscape dynamics in both arid and humid field sites in Israel and the USA, respectively, across different lithologic and tectonic settings. They will use field mapping and topographic analyses, in conjunction with landscape evolution models and geochronological analyses to constrain the controlling parameters and the rates associated with different processes of divide migration, flow reversals, and the evolution of escarpments.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.

河流网络的结构暗示性地影响着地球表面的海拔、水和生命的空间分布，这种结构通过分隔河流流域的水分流的运动而变化。分水岭迁移过程发生在局部山丘尺度上。其驱动力植根于大规模的构造和气候变化。此外，分水岭迁移的局部过程影响地球表面更广泛的地貌、水文和生态功能。本研究探讨了这些多尺度过程的机制。更具体地说，当地的地形、水文和岩性条件如何导致一系列反馈，最终对地球系统产生大规模影响。这个两国项目对以色列和美国的干旱和潮湿研究地点进行了比较和对比。研究团队还将分别为宾夕法尼亚州和科罗拉多州学校的 K6-8 学生制定和领导一项强化科学教育计划，其中包括少数群体出勤率较高的学校。在控制景观形态和塑造水文和地貌功能方面发挥着关键作用。水分水岭的流动性与控制邻近地形的当地山坡和河流过程有着内在的联系。同时，分水岭的流动性导致了水体的重组。排水网络，对大尺度地形、均衡和地层格局产生显着影响。目前，局部山坡和河流状况与盆地尺度排水重组以及大尺度地形和均衡相互作用的过程和反馈。为了解决这些知识差距，本研究重点关注地形悬崖和反向通道（重组的最终成员）的并置，其中分水岭迁移的初始条件相对较好地受到限制。反向河道的沉积物记录了分水岭迁移的历史，这些河道保留了当地岩性和水文条件如何作为临界点驱动系统进入级联反应从而导致排水重组的证据，为了探索这些过程的普遍性，研究人员将分别在不同的岩性和构造环境中比较和对比以色列和美国干旱和潮湿地区的新兴景观动态。实地测绘和地形分析，结合景观演化模型和地质年代学分析，反映了限制与分水岭迁移、水流逆转和悬崖演化的不同过程相关的控制参数和速率。该奖项是美国国家科学基金会的法定奖项使命，并通过使用基金会的智力价值和更广泛的影响审查标准进行评估，被认为值得支持。