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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Relative humidity ： ウィキペディア英語版 Relative humidity Relative humidity (abbreviated RH) is the ratio of the partial pressure of water vapor to the equilibrium vapor pressure of water at the same temperature. Relative humidity depends on temperature and the pressure of the system of interest. == Definition == The relative humidity $\backslash left(\backslash phi\backslash right)$ of an air-water mixture is defined as the ratio of the partial pressure of water vapor $\backslash left(\backslash right)$ in the mixture to the equilibrium vapor pressure of water $\backslash left(\_w\}\backslash right)$ at a given temperature:〔Perry, R.H. and Green, D.W, ''Perry's Chemical Engineers' Handbook'' (7th Edition), McGraw-Hill, ISBN 0-07-049841-5 , Eqn 12-7〕 ::$\backslash phi\; =\; \backslash over\; \_w\}\}$ Relative humidity is normally expressed as a percentage; a higher percentage means that the air-water mixture is more humid. 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「Relative humidity」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.