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Do pathways of water movement and leaf anatomical dimensions allow development of gradients in H218O between veins and the sites of evaporation within leaves

Barbour, Margaret; Farquhar, Graham

Description

The oxygen isotope enrichment of bulk leaf water (ΔL) is often observed to be poorly predicted by the Craig-Gordon-type models developed for evaporative enrichment from a body of water (Δe). The discrepancy between ΔL and Δe may be explained by gradie

CollectionsANU Research Publications
Date published: 2003
Type: Journal article
URI: http://hdl.handle.net/1885/74347
Source: Plant Cell and Environment
DOI: 10.1046/j.0016-8025.2003.01132.x

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