首页> 外文学位 >Gas Transport Through Layered Snow and Firn
【24h】

Gas Transport Through Layered Snow and Firn

机译:气体通过层状积雪和碎屑的运输

获取原文
获取原文并翻译 | 示例

摘要

Regional climate and weather conditions dictate the microstructural properties of falling snow and influence metamorphosis of the snowpack following deposition. For both the polar and seasonal snow cover, differences in the depositional events and post-depositional processes lead to snow that is both porous and highly layered. It is within this connected, interstitial porous space of snow's layers that atmospheric gases are able to move in response to various agents. Part of this thesis focuses on quantifying the role of seasonal snow as a conduit for carbon dioxide respired during the wintertime. Through in-situ studies of seasonal snow, this work provides the first measurements of effective gas diffusivity of seasonal snow as a function of crystal type and density. Results of this work provide improved guidance for gas diffusivity estimates of seasonal snow to be used in surface-atmosphere gas flux models. Another part of this thesis examines the unexpected effect that permeable layers of firn (old polar snow) have on pressure gradients developed when using air driven, rotating drills in the polar regions. Results from this project indicate drilling in areas where regions of highly permeable firn layers are present could be problematic. Results show pressure differential within the borehole is highly sensitive to the permeability of the surrounding firn, particularly near the drill head.;In the final section I discuss preliminary investigations that compare measurements of diffusivity of multilayered firn cores and the diffusivity measured on cut subsections of the cores. Initial results show a decrease in diffusivity as a result of cutting that was not seen on samples from a subsection of firn cores from previous studies. Further work will be pursued to determine the correct lab technique to avoid this problem. The research presented in this thesis will improve the understanding of gas transport through polar and seasonal snow for both scientific and engineering endeavors.
机译:区域气候和天气条件决定了降雪的微观结构特性,并影响沉积后积雪的变质。对于极地和季节性积雪,沉积事件和沉积后过程的差异都会导致积雪既多孔又高度分层。正是在雪层的这个连通的间隙多孔空间内,大气气体才能响应各种媒介而移动。本文的一部分重点是定量分析季节性降雪作为冬季呼吸的二氧化碳的管道的作用。通过对季节性雪的原位研究,这项工作首次测量了季节性雪的有效气体扩散率随晶体类型和密度的变化。这项工作的结果为在地面-大气气体通量模型中使用的季节性降雪的气体扩散率估算提供了改进的指导。本论文的另一部分研究了在极地地区使用气动旋转钻头时,杉木(老极地雪)的可渗透层对压力梯度产生的意外影响。该项目的结果表明,在存在高渗透性烧结层区域的地区进行钻探可能会出现问题。结果表明,井眼内的压差对周围钻头的渗透率高度敏感,特别是在钻头附近。;在最后一节中,我讨论了初步研究,该研究比较了多层钻头岩心的扩散率测量值和在钻探切面的测量结果核心。初步结果显示,由于切割,扩散率降低了,这是先前研究的火烧芯子部分的样品所未见的。将会进行进一步的工作来确定正确的实验室技术来避免此问题。本文的研究将为科学和工程方面的工作加深对通过极地雪和季节性雪进行气体传输的理解。

著录项

  • 作者

    Whelsky, Amber N.;

  • 作者单位

    Dartmouth College.;

  • 授予单位 Dartmouth College.;
  • 学科 Environmental engineering.
  • 学位 Ph.D.
  • 年度 2017
  • 页码 120 p.
  • 总页数 120
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号