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Moisture stress : ウィキペディア英語版 | Moisture stress Moisture stress occurs when the water in a plant's cells is reduced to less than normal levels. This can occur because of a lack of water in the plant's root zone, higher rates of transpiration than the rate of moisture uptake by the roots, for example, because of an inability to absorb water due to a high salt content in the soil water or loss of roots due to transplantation. Moisture stress is more strongly related to water potential than it is to water content.〔 〕〔 〕〔 〕 ==See also==
*Nonlimiting water range *Permanent wilting point *Soil plant atmosphere continuum
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「Moisture stress」の詳細全文を読む
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