Discovering the Underlying Mechanism of Snow Crystal Growth and Bringing Modern Laboratory Learning to the Classroom

发现雪晶生长的潜在机制并将现代实验室学习带入课堂

• 批准号: 9703123
• 负责人: Benjamin Herman
• 金额: $ 38.92万
• 依托单位: University of Arizona
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 1997
• 资助国家: 美国
• 起止时间: 1997-09-15 至 1999-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9703123&HistoricalAwards=false
• 关键词: Discovering; Underlying; Mechanism; Snow; Crystal

Nelson/Abstract 9703123 The goals of this project are: 1) to discover the physical causes of snow crystal shape by the measurement of key surface parameters used in crystal growth models, and 2) to improve instruction in physical meteorology by introducing experiments into a required undergraduate/graduate lecture course. A new method of controlled ice crystal growth that was successfully developed to measure critical supersaturations for vapor growth on both basal and prism faces of ice above -16 degrees Celsius. The improvements are need to extend the range of conditions measured, but will also increase control over the crystal environment. This method can be used for related fundamental and applied studies in cloud physics with little or no modification. Five to six research quality experiments will be added to our existing physical meteorology course for seniors and first-year graduate students. Each student would perform approximately 3 experiments per semester. Experiments would be 2 hours long or more and treated like a homework assignment. The experiments will be chosen to complement the lectures and faculty research projects and therefore can be used for additional undergraduate research with the appropriate professor when the equipment is available. For example; a simplified version of our ice crystal growth apparatus could be used both for a laboratory exercise to illustrate crystal growth and the different snow crystal shapes, and for an undergraduate research project to measure the effect of electric fields on the critical supersaturations for vapor growth of ice.

Nelson/摘要9703123这个项目的目标是：1)通过测量晶体生长模型中使用的关键表面参数来发现雪晶形状的物理原因，2)通过在必修的本科生/研究生讲座课程中引入实验来改进物理气象学的教学。成功开发了一种新的受控冰晶生长方法，用于测量零下16摄氏度以上冰的基面和棱柱面上水蒸气生长的临界过饱和度。这些改进需要扩大测量条件的范围，但也将增加对晶体环境的控制。该方法只需稍加修改即可用于云物理的相关基础和应用研究。我们现有的物理气象学课程将为大四学生和一年级研究生增加五到六个研究质量实验。每个学生每学期大约要做3次实验。实验将长达2小时或更长，并被视为家庭作业。这些实验将被选择来补充讲课和教师研究项目，因此当设备可用时，可以与适当的教授一起用于额外的本科生研究。例如，我们的冰晶生长装置的简化版本既可用于说明晶体生长和不同雪晶形状的实验室练习，也可用于本科生研究项目，以测量电场对冰蒸汽生长的临界过饱和度的影响。