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• W254920360 abstract "The analysis of leaf water isotopes can provide insight into the movement of water in the plant-atmosphere system at a number of levels. During transpiration the isotopic composition of leaf water (the O/O ratio, or δOlw) becomes enriched, as light water molecules tend to evaporate more rapidly. The extent of isotopic enrichment at the evaporation site depends mainly on leaf temperate and air humidity, and the impact of this localized enrichment on bulk leaf water depends on the interplay between the advection of initially unenriched source water in the transpiration stream and the back-diffusion of enriched water through the mesophyll and vein compartments. Hence the spatial distribution of δOlw will depend on factors affecting the relative strength of the advection and diffusion processes, such as resistances, gradients, flow paths and distances. Analysis of the isotopic composition of leaf water can therefore be used to develop and test models of water movement through leaves. Furthermore, the transpiration flux from these enriched leaf water pools contributes to variations in isotopic composition of ecosystem water vapour, and combining isotopic measurements with appropriate models are necessary for interpreting fluctuations in atmospheric signals and partitioning biosphere-atmosphere evapotranspiration exchange into soil and plant water flux contributions." @default.
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• W254920360 date "2009-04-01" @default.
• W254920360 modified "2023-10-16" @default.
• W254920360 title "The contribution of diffusion processes and leaf temperature variations to the spatial distribution of leaf water isotopes." @default.
• W254920360 hasPublicationYear "2009" @default.
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