翻訳と辞書 Words near each other ・ Void (law) ・ Void (Vanna album) ・ VOID (Video Overview in Deceleration) ・ Void coefficient ・ Void contract ・ Void Cube ・ Void deck ・ Void Dweller ・ Void galaxy ・ Void Indigo ・ Void Linux ・ Void marriage ・ Void Moon ・ Void of Silence ・ Void pantograph ・ Void ratio ・ Void safety ・ Void Server ・ Void Terra Firma ・ Void Trilogy ・ Void type ・ Void-Vacon ・ Voidable ・ Voidable contract ・ Voidable floating charge ・ Voidable marriage ・ Voidable marriages (Australia) ・ Voided biaxial slab ・ Voiding cystourethrogram ・ Voidokilia beach Dictionary Lists mini英和辞書 mini和英辞書 Webster 1913 Latin-English FOLDOC Wikipedia English ウィキペディア

翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Void ratio ： ウィキペディア英語版 Void ratio Void ratio, in materials science, is related to porosity and defined as the ratio: :$e\; =\; \backslash frac\; =\; \backslash frac\; =\; \backslash frac$ and :$\backslash phi\; =\; \backslash frac\; =\; \backslash frac\; =\; \backslash frac$ where $e$ is void ratio, $\backslash phi$ is porosity, ''V''V is the volume of void-space (such as fluids), ''V''S is the volume of solids, and ''V''T is the total or bulk volume. This figure is relevant in composites, in mining (particular with regard to the properties of tailings), and in soil science. In geotechnical engineering, it is considered as one of the state variables of soils and represented by the symbol ''e''.〔Lambe, T. William & Robert V. Whitman. ''Soil Mechanics''. Wiley, 1991; p. 29. ISBN 978-0-471-51192-2〕〔Santamarina, J. Carlos, Katherine A. Klein, & Moheb A. Fam. ''Soils and Waves: Particulate Materials Behavior, Characterization and Process Monitoring''. Wiley, 2001; pp. 35-36 & 51-53. ISBN 978-0-471-49058-6〕 Note that in geotechnical engineering, the symbol $\backslash phi$ usually represents the angle of shearing resistance, a shear strength (soil) parameter. Because of this, the equation is usually written: :$e\; =\; \backslash frac\; =\; \backslash frac\; =\; \backslash frac$ and :$n\; =\; \backslash frac\; =\; \backslash frac\; =\; \backslash frac$ where $e$ is void ratio, $n$ is porosity, ''V''V is the volume of void-space (air and water), ''V''S is the volume of solids, and ''V''T is the total or bulk volume.〔Craig, R. F. ''Craig's Soil Mechanics.'' London: Spon, 2004, p.18. ISBN 0-203-49410-5.〕 ==Engineering applications== * Volume change tendency control. If void ratio is high (loose soils) voids in a soil skeleton tend to minimize under loading - adjacent particles contract. The opposite situation, i.e. when void ratio is relatively small (dense soils), indicates that the volume of the soil is vulnerable to increase under loading - particles dilate. * Fluid conductivity control (ability of water movement through the soil). Loose soils show high conductivity, while dense soils are not so permeable. * Particles movement. In a loose soil particles can move quite easily, whereas in a dense one finer particles cannot pass through the voids, which leads to clogging. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Void ratio」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.