A Laboratory Study of Texture Development During Grain Size Sensitive Creep of Ice, with Applications to the Flow of Glaciers and Ice Sheets

冰晶尺寸敏感蠕变过程中纹理发展的实验室研究及其在冰川和冰盖流动中的应用

• 批准号: 0230190
• 负责人: David Goldsby
• 金额: $ 13.74万
• 依托单位: Brown University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2003
• 资助国家: 美国
• 起止时间: 2003-01-01 至 2005-12-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0230190&HistoricalAwards=false
• 关键词: Laboratory; Study; Texture; Development; During

This award supports a project to conduct laboratory experiments to investigate textures formed in ice during superplastic flow. Superplastic flow has recently been discovered in the laboratory and can be considered a new flow mechanism for ice. A simple extrapolation of these new data for superplastic flow from laboratory to natural conditions suggests that glaciers and ice sheets flow via this mechanism. Furthermore, several grain-scale features in ice (e.g., crystal shape) produced during superplastic flow in the laboratory are remarkably similar to those observed in glaciers and ice sheets. Despite this exciting discovery, however, important questions remain before we can apply with full confidence these new flow data in mathematical models of glacier and ice sheet flow. The textures seen in laboratory studies will be compared with those observed in field studies of glaciers and ice sheets. These comparisons, coupled with comparisons of the new superplastic flow data from the laboratory with flow measurements from field studies, will provide a powerful method for further assessing the importance of superplastic flow in nature and thereby improve our understanding of glacier and ice sheet dynamics and global climate change. Experiments will be conducted by the PI and an undergraduate research assistant. Experimental results will be published in relevant refereed journals, presented at glaciology meetings and incorporated into coursework.

该奖项支持一个项目，进行实验室实验，以研究超塑性流动过程中冰中形成的纹理。 超塑性流动是近年来在实验室中发现的一种新的流动机制。 从实验室到自然条件下的超塑性流动的这些新数据的简单外推表明，冰川和冰盖通过这种机制流动。 此外，冰中的几个颗粒尺度特征（例如，晶体形状）在实验室中超塑性流动过程中产生的与在冰川和冰盖中观察到的非常相似。 然而，尽管有了这一令人兴奋的发现，在我们能够满怀信心地将这些新的流动数据应用于冰川和冰盖流动的数学模型之前，仍然存在一些重要的问题。 实验室研究中看到的纹理将与冰川和冰盖实地研究中观察到的纹理进行比较。 这些比较，再加上来自实验室的新的超塑性流动数据与来自实地研究的流动测量结果的比较，将为进一步评估超塑性流动在自然界中的重要性提供一种强有力的方法，从而提高我们对冰川和冰盖动力学以及全球气候变化的理解。实验将由PI和本科生研究助理进行。实验结果将发表在相关的期刊上，在冰川学会议上提出，并纳入课程。