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- W2888891914 abstract "Abstract Investigation of δ 18 O of leaf water may improve our understanding of the evapotranspiration partitioning and material exchange between the inside and outside of leaves. In this study, δ 18 O of bulk leaf water ( δ L,b ) was estimated by both isotopic–steady–state (ISS) and non–steady–state (NSS) assumptions considering the Péclet effect. Specifically, we carefully modified kinetic fractionation coefficients ( α k ). The results showed that the Péclet effect is required to predict δ L,b . On the diel time scale, both NSS assumption + Péclet effect (NSS + P) and ISS assumption + Péclet effect (ISS + P) using modified α k ( α k–modified ) for δ L,b showed a good agreement with observed δ L,b ( p > 0.05). When using previously proposed α k , however, both NSS + P and ISS + P were not reliable estimators of δ L,b ( p < 0.05). On a longer time scale (days), estimates of daily mean δ L,b from ISS + P outperformed the estimates from NSS + P when using the same α k values. Also, the employment of α k–modified improved model performance in predicting daily mean δ L,b compared to the use of previously proposed α k . Clearly, special care must be taken concerning α k when using isotopic models to estimate δ L,b . Highlight For hourly and daily mean data sets, the employment of modified kinetic fractionation coefficients significantly improved model performance for δ 18 O of bulk leaf water." @default.
- W2888891914 created "2018-09-07" @default.
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- W2888891914 date "2018-08-29" @default.
- W2888891914 modified "2023-09-23" @default.
- W2888891914 title "Multiple isotopic models using various kinetic fractionation coefficients to estimateδ18O of leaf water" @default.
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- W2888891914 doi "https://doi.org/10.1101/403410" @default.
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