書誌事項
- タイトル別名
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- A model of layered ice-formation in unconfined water-saturated spherical glass particles.
- ガラス フンリュウタイ チュウ ノ ソウジョウヒョウ セイセイ モデル
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抄録
When fine particles bearing water was frozen unidirectionally, segregated ice layers reject particles. The segregated ice layers stratify in the direction of heat flow and affect particles and water near the advancing interface. This paper presents a model to simulate the ice segregation in water-saturated, air-free, solute-free, unconfined micro glass spheres. The model has three aspects: exclusion of particles dependent on the velocity of ice growing; ice growth dependent on the supercooling at the interface; and discontinuous change in particle density and critical freezing velocity near the ice-water interface. This model can be applied to the ice segregation in soils and other water-soaked media.
収録刊行物
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- 雪氷
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雪氷 61 (3), 207-214, 1999
公益社団法人 日本雪氷学会
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詳細情報 詳細情報について
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- CRID
- 1390282681436769280
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- NII論文ID
- 10002384375
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- NII書誌ID
- AN00131221
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- ISSN
- 18836267
- 03731006
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- NDL書誌ID
- 4739868
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可