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

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

项目摘要

项目成果

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中文摘要
翻译
河流网络的结构影响着地球表面的海拔、水和生命的空间分布。有趣的是,这种结构随着时间的推移而变化,因为水的运动将河流流域分开。分水岭迁移过程发生在当地的山坡尺度上,但其驱动力源于大规模的构造和气候变化。此外,分水岭迁移的局部过程会影响地球表面更广泛的地貌、水文和生态功能。 拟议的研究探讨了这些多尺度过程发生的机制。更具体地说,当地的地形,水文和岩性条件如何导致级联反馈,最终对地球系统产生大规模的影响。这个两国项目分别比较和对比了以色列和美国的干旱和潮湿研究地点,从而加强了两国之间的研究合作。该研究团队还将为宾夕法尼亚州和科罗拉多州的学校(包括代表性不足的人口出勤率高的学校)的K6-8学生开发和领导一个增强的科学教育计划。分水岭在控制景观的形式和塑造水文和地貌功能方面发挥着关键作用。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。与此同时,分水岭的流动性导致排水网络的重组,这显着影响大规模的地形,均衡和地层模式。目前,当地的山坡和河流制度与流域规模的排水重组和大规模的地形和均衡变化的相互作用的过程和反馈仍然普遍未被探索。为了解决这些知识的差距,本研究的重点是并列的地形陡崖和反向通道(重组的终端成员),其中划分迁移的初始条件相对较好的限制。在这种背景下,反向河道的地形和沉积物记录了分水岭迁移的历史。这些渠道保存的证据,当地的岩性和水文条件如何作为一个临界点,驱动系统进入级联响应,导致排水重组,地形变化和潜在的均衡调整。为了探索这些过程的一般性,研究人员将分别在不同的岩性和构造背景下,比较和对比以色列和美国干旱和潮湿场地的新兴景观动态。他们将使用实地测绘和地形分析,结合景观演变模型和地质年代学分析,以限制控制参数和与分水岭迁移、水流逆转和悬崖演变的不同过程相关的速率。该奖项反映了NSF的法定使命,并被认为值得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来支持。
英文摘要
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.
期刊论文(1)
专著(0)
科研奖励(0)
会议论文
Erosion and weathering in carbonate regions reveal climatic and tectonic drivers of carbonate landscape evolution
碳酸盐地区的侵蚀和风化揭示了碳酸盐景观演化的气候和构造驱动因素
DOI: 10.5194/esurf-11-247-2023
发表时间: 2023
期刊: Earth Surface Dynamics
影响因子: 3.4
作者: [Ott, Richard, Gallen, Sean F., Helman, David]
通讯作者: Helman, David
Collaborative Research: Testing Critical Zone Controls on Mountain-Scale Relief in a Tropical Climate
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国内基金
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