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Direct quantification of leaf transpiration isotopic composition

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dc.contributor.authorWang, Lixin
dc.contributor.authorGood, Stephen P
dc.contributor.authorCaylor, Kelly K
dc.contributor.authorCernusak, Lucas
dc.date.accessioned2015-12-10T22:23:43Z
dc.date.issued2012
dc.date.updated2016-02-24T11:27:39Z
dc.description.abstractThe stable isotopic composition of plant transpired water (δT) is a powerful tracer used to characterize plant processes in the fields of ecology, plant physiology and hydrology. However, δT is rarely directly measured due to the general difficulty in t
dc.identifier.issn0168-1923
dc.identifier.urihttp://hdl.handle.net/1885/52931
dc.publisherElsevier
dc.sourceAgricultural and Forest Meteorology
dc.subjectKeywords: dew point; hydrogen isotope; irradiance; isotopic composition; leaf; mass balance; oxygen isotope; physiology; precision; stable isotope; timescale; tracer; transpiration; water vapor; Kenya Dew point generator; Hydrogen; Isotope; Kenya; Mass balance; Oxygen
dc.titleDirect quantification of leaf transpiration isotopic composition
dc.typeJournal article
local.bibliographicCitation.lastpage135
local.bibliographicCitation.startpage127
local.contributor.affiliationWang, Lixin, Princeton University
local.contributor.affiliationGood, Stephen P, Princeton University
local.contributor.affiliationCaylor, Kelly K , Princeton University
local.contributor.affiliationCernusak, Lucas, College of Medicine, Biology and Environment, ANU
local.contributor.authoruidCernusak, Lucas, u4001780
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor060705 - Plant Physiology
local.identifier.absseo970106 - Expanding Knowledge in the Biological Sciences
local.identifier.ariespublicationu4956746xPUB259
local.identifier.citationvolume154-155
local.identifier.doi10.1016/j.agrformet.2011.10.018
local.identifier.scopusID2-s2.0-84858111993
local.identifier.thomsonID000312449200004
local.type.statusPublished Version

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