Reconstructing relative humidity from plant delta 18O and delta D as deuterium deviations from the global meteoric water line

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F14%3A43887411" target="_blank" >RIV/60076658:12310/14:43887411 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Reconstructing relative humidity from plant delta 18O and delta D as deuterium deviations from the global meteoric water line

Popis výsledku v původním jazyce

Cellulose delta O-18 and delta D can provide insights on climates and hydrological cycling in the distant past and how these factors differ spatially. However, most studies of plant cellulose have used only one isotope, most commonly delta O-18, resulting in difficulties partitioning variation in delta O-18 of precipitation vs. evaporative conditions that affect leaf water isotopic enrichment. Moreover, observations of pronounced diurnal differences from conventional steady-state model predictions of leaf water isotopic fractionation have cast some doubt on single isotope modeling approaches for separating precipitation and evaporation drivers of cellulose delta O-18 or delta D. We explore a dual isotope approach akin to the concept of deuterium-excess(d), to establish deuterium deviations from the global meteoric water line in leaf water (Delta d(l)) as driven by relative humidity (RH). To demonstrate this concept, we survey studies of leaf water delta O-18 and delta D in hardwood vs

Název v anglickém jazyce

Reconstructing relative humidity from plant delta 18O and delta D as deuterium deviations from the global meteoric water line

Popis výsledku anglicky

Cellulose delta O-18 and delta D can provide insights on climates and hydrological cycling in the distant past and how these factors differ spatially. However, most studies of plant cellulose have used only one isotope, most commonly delta O-18, resulting in difficulties partitioning variation in delta O-18 of precipitation vs. evaporative conditions that affect leaf water isotopic enrichment. Moreover, observations of pronounced diurnal differences from conventional steady-state model predictions of leaf water isotopic fractionation have cast some doubt on single isotope modeling approaches for separating precipitation and evaporation drivers of cellulose delta O-18 or delta D. We explore a dual isotope approach akin to the concept of deuterium-excess(d), to establish deuterium deviations from the global meteoric water line in leaf water (Delta d(l)) as driven by relative humidity (RH). To demonstrate this concept, we survey studies of leaf water delta O-18 and delta D in hardwood vs

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

CE - Biochemie

OECD FORD obor

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Projekt

<a href="/cs/project/GAP501%2F12%2F1261" target="_blank" >GAP501/12/1261: Oxid uhličitý jako signál při výměně plynů a vývoji listu</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

ECOLOGICAL APPLICATIONS

ISSN

1051-0761

e-ISSN

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Svazek periodika

24

Číslo periodika v rámci svazku

5

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

16

Strana od-do

960-975

Kód UT WoS článku

000338109700006

EID výsledku v databázi Scopus

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