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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 Vapour Pressure Deficit ： ウィキペディア英語版 Vapour Pressure Deficit Vapour Pressure Deficit, or ''VPD'', is the difference (deficit) between the amount of moisture in the air and how much moisture the air can hold when it is saturated. Once air becomes saturated water will condense out to form clouds, dew or films of water over leaves. It is this last instance that makes VPD important for greenhouse regulation. If a film of water forms on a plant leaf it becomes far more susceptible to rot. On the other hand, as the VPD increases the plant needs to draw more water from its roots. In the case of cuttings, the plant may dry out and die. For this reason the ideal range for VPD in a greenhouse is from 0.45 kPa to 1.25 kPa, ideally sitting at around 0.85 kPa. As a general rule, most plants grow well at VPDs of between 0.8 to 0.95 kPa 〔(Autogrow Systems Ltd. web site, humidity page, accessed October 13, 2006 )〕 In ecology, it is the difference between the actual water vapour pressure and the saturation water vapour pressure at a particular temperature. Unlike relative humidity, vapour pressure deficit has a simple nearly straight-line relationship to the rate of evapotranspiration and other measures of evaporation. == Computing VPD for plants in a greenhouse == To compute the VPD〔(Ohio State University Extension Fact Sheet, Greenhouse Condensation Control, accessed October 13, 2006 )〕 we need the ambient (greenhouse) air temperature, the relative humidity and if possible, the canopy air temperature. We must then compute the saturation pressure. Saturation pressure can be looked up in a psychrometric chart or derived from the Arrhenius equation, a way to compute it directly from temperature is $vp\_\; =\; e^$ where: $vp\_$ is the saturation vapor pressure in kPa $A\; =\; -1.88\; \backslash times\; 10^4$ $B\; =\; -13.1$ $C\; =\; -1.5\; \backslash times\; 10^$ $D\; =\; 8\; \backslash times\; 10^$ $E\; =\; -1.69\; \backslash times\; 10^$ $F\; =\; 6.456$ $T\; =$Temperature of the air in Kelvin To convert between Kelvin and Celsius: $T(K)\; =\; T(C)\; +\; 273.15$ We compute this pressure for both the ambient and canopy temperatures. We then can compute the actual partial pressure of the water vapour in the air by multiplying by the relative humidity (): $vp\_\; =\; vp\_$ *relative humidity/100 and finally VPD using $vp\_\; -\; vp\_$ or $vp$canopy sat$-\; vp\_$ when the canopy temperature is known. 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「Vapour Pressure Deficit」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.