@article{oai:setsunan.repo.nii.ac.jp:00000992,
 author = {廣瀬, 剛 and 伊藤, 譲 and HIROSE, Go and ITO, Yuzuru},
 issue = {1},
 journal = {摂南大学 融合科学研究所論文集, Bulletin of the Transdisciplinary Science Research Institute, Setsunan University},
 month = {Oct},
 note = {The purpose of this study is to evaluate the influence of freezing direction on the permeability of freeze-thawed soils. In this study, the permeability of both ice lens (IL) and IL orthogonal directions in the freeze-thawed soil were experimentally investigated. As a result, the permeability of IL direction was greater than IL orthogonal direction. Especially, the permeability of open-system freeze-thawed soils increased remarkably and it received not only the overburden pressure but also the influenced of both condition of pre-consolidation pressure and the number of freeze-thaw cycles. The permeability of closed-system freeze-thawed soils was lower than that of open-system. It was concluded that the permeability of freeze-thawed soil of IL direction is greater because of the remarkably greater void ratio in the colder temperature side of freezing.},
 pages = {40--50},
 title = {飽和細粒土の凍結融解によるアイスレンズ方向の透水係数変化 ―融解後の間隙比分布の影響―},
 volume = {2},
 year = {2016}
}