Analysis of surface wave formation of icicles and its application to the formation of stalactites
Analysis of surface wave formation of icicles and its application to the formation of stalactites
批准号:
16540349
负责人:
OGAWA Naohisa
金额:
$1.28万
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (C)
财政年份:
2004
资助国家:
日本
项目状态:
已结题
起止时间:
2004 至 2006
中文摘要
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英文摘要
We have proposed a new model for the surface formation of icicle, we also proposed some mathematically related works, and some experiments and some field works are done.For the problem of icicle, it was found that we cannot express the experimental fact (formation of surface wave with specific wave length) when we take into account the surface tension of water. Further consideration is necessary to find some physical factors which explain the experimental results. On the other hand, the similar model made by Ueno says that every experimental result can be explained. However, first, his boundary condition for the temperature field can not be accepted physically. Second, his result which suggests the motion of wave going upward is asserted to be proved by the trace of bubbles inside of icicles. But we cannot find the explicit motion of waves on the surface of icicle by hundreds video filming and the picture of formation of many crystals inside of icicles. So we have concluded that there is no reason to connect the wave motion and the trace of bubbles inside of icicles. And it should be said that this problem is still an open one. We will further continue the research on this point.Next we have considered the related mathematical problems. One is about the surface tension. We considered its value from the statistical mechanics view point, and next tried the problem of measurement of one from the form of pendant drop. Further the morphology of snow grains from the view point of Gaussian curvature is discussed. This is really related to the surface energy. On the other hand, To study the relation between the thermal problem and surface formation, phase field model is studied to compare to the usual theories.The field works to take the data on ice-stalagmites, stalactites, stalagmites and rim stones are done in 6 caves in Hokkaido, Iwate prefecture and Okinawa islands. These data are used to construct the new morphological theories for these objects.
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Chaplygin gas and Brane
查普雷金气体和膜
DOI:
--
发表时间:
2007
期刊:
Geometry, Integrability and Quantization, Proceedings of International Conference in Varna, Bulgaria, Bulgarian Academy of Science Vol.8
影响因子:
--
作者:
[Y.Hattori, R.Rubinstein, A.Ishizawa, Naohisa Ogawa]
通讯作者:
Naohisa Ogawa
Using Gaussian Curvature for the 3D segmentation of snow grains from microtomographic data
使用高斯曲率对显微断层扫描数据中的雪粒进行 3D 分割
DOI:
--
发表时间:
2006
期刊:
Physics and Chemistry of Ice, Proceedings of the 11^<th> International Conference on the Physics and Chemistry of Ice, held at Bremerhaven, Germany, on 23-28 July 2006 RSC Publishing
影响因子:
--
作者:
[J.B.Brzoska, Frederic Flin, Naohisa Ogawa]
通讯作者:
Naohisa Ogawa
タンパク質溶液の表面張力II
蛋白质溶液的表面张力II
DOI:
--
发表时间:
2007
期刊:
北海道工業大学紀要 35号
影响因子:
--
作者:
[Y.Hattori, R.Rubinstein, A.Ishizawa, Naohisa Ogawa, 福原朗子]
通讯作者:
福原朗子
Sharp interface limit of Phase Field Model
相场模型的锐界面极限
DOI:
--
发表时间:
2007
期刊:
北海道工業大学紀要 35号
影响因子:
--
作者:
[Y.Hattori, R.Rubinstein, A.Ishizawa, Naohisa Ogawa, 福原朗子, Naohisa Ogawa]
通讯作者:
Naohisa Ogawa
Using Gaussian Curvature for the 3D segmentation of snow grains from microtomograohic data
使用高斯曲率对显微断层扫描数据中的雪粒进行 3D 分割
DOI:
--
发表时间:
2007
期刊:
Physics and Chemistry of Ice, Proceedings of the International Conference on the Physics and Chemistry of Ice Vol.11
影响因子:
--
作者:
[Y.Hattori, R.Rubinstein, A.Ishizawa, Naohisa Ogawa, 福原朗子, Naohisa Ogawa, J.B.Brzoska]
通讯作者:
J.B.Brzoska
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