Mechanical properties and crystal textures of Greenland deep ice cores グリーンランド氷床コアの力学的性質と結晶組織
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Bibliographic Information
- Title
-
Mechanical properties and crystal textures of Greenland deep ice cores
- Other Title
-
グリーンランド氷床コアの力学的性質と結晶組織
- Author
-
宮本, 淳
- Author(Another name)
-
ミヤモト, アツシ
- University
-
北海道大学
- Types of degree
-
博士 (地球環境科学)
- Grant ID
-
甲第4940号
- Degree year
-
1999-09-30
Note and Description
博士論文
資料形態 : テキストデータ プレーンテキスト
コレクション : 国立国会図書館デジタルコレクション > デジタル化資料 > 博士論文
学位論文本体及び論文要旨 : 1-124コマ
参考論文は、国立国会図書館内でのみ閲覧できます。
Table of Contents
- CONTENTS
- Abstract
- 1.Introduction
- 1.1.The earth environment and climate change
- 1.2.Ice core studies
- 2.Plastic flow of ice
- 2.1.Mechanical properties of ice single crystal
- 2.2.Mechanical properties of polycrystalline ice
- 3.Greenland ice sheet
- 3.1.Greenland ice core project(GRIP)
- 3.2.The GRIP ice core
- 4.Experiments
- 4.1.Electric conductivity measurements
- 4.2.Grain size measurements
- 4.3.C-axis orientation measurements and statistics for analysis of directional data
- 4.4.Stratigraphic studies
- 4.5.Mechanical tests of ice core
- 5.Results
- 5.1.Electric conductivity measurements
- 5.2.Grain size
- 5.3.C-axis orientation distribution
- 5.4.Stratigraphic studies
- 5.5.Mechanical tests of ice core
- 6.Discussion
- 6.1.Flow enhancement factor
- 6.2.Schmid factor
- 6.3.Effect of various factor on mechanical properties of ice cores
- 6.4.The development of c-axis orientation and flow behavior in the Greenland ice sheet
- 7.Application to ice sheet flow
- 7.1.Horizontal flow velocity
- 7.2.Instability of dome position
- 7.3.Flow behavior of ice with cloudy band structure
- 7.4.Mechanical properties of the Dome F ice core from the dome summit of Antarctica
- 8.Conclusions
- Acknowledgments
- References
- AN ATTEMPT AT DEFORMATION TESTS OF DEEP ICE CORE SAMPLES CONTAINING CLOUDY BANDS
- Ice sheet flow conditions deduced from mechanical tests of ice core
- PRELIMINARY DISCUSSION OF PHYSICAL PROPERTIES OF THE DOME FUJI SHALLOW ICE CORE IN 1993, ANTARCTICA
- Anisotropic behavior of GRIP ices and flow in Central Greenland