Testing plant use of mobile vs immobile soil water sources using stable isotope experiments

© 2017 The Authors. New Phytologist © 2017 New Phytologist Trust.

Bibliographische Detailangaben
Veröffentlicht in:The New phytologist. - 1990. - 215(2017), 2 vom: 15. Juli, Seite 582-594
1. Verfasser: Vargas, Ana I (VerfasserIn)
Weitere Verfasser: Schaffer, Bruce, Yuhong, Li, Sternberg, Leonel da Silveira Lobo
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2017
Zugriff auf das übergeordnete Werk:The New phytologist
Schlagworte:Journal Article bound water isotope fractionation mobile water plant water uptake stable isotopes two water worlds Oxygen Isotopes Soil Water mehr... 059QF0KO0R Deuterium AR09D82C7G
LEADER 01000caa a22002652 4500
001 NLM272378402
003 DE-627
005 20250221174127.0
007 cr uuu---uuuuu
008 231224s2017 xx |||||o 00| ||eng c
024 7 |a 10.1111/nph.14616  |2 doi 
028 5 2 |a pubmed25n0907.xml 
035 |a (DE-627)NLM272378402 
035 |a (NLM)28556977 
040 |a DE-627  |b ger  |c DE-627  |e rakwb 
041 |a eng 
100 1 |a Vargas, Ana I  |e verfasserin  |4 aut 
245 1 0 |a Testing plant use of mobile vs immobile soil water sources using stable isotope experiments 
264 1 |c 2017 
336 |a Text  |b txt  |2 rdacontent 
337 |a ƒaComputermedien  |b c  |2 rdamedia 
338 |a ƒa Online-Ressource  |b cr  |2 rdacarrier 
500 |a Date Completed 11.04.2018 
500 |a Date Revised 30.09.2020 
500 |a published: Print-Electronic 
500 |a Citation Status MEDLINE 
520 |a © 2017 The Authors. New Phytologist © 2017 New Phytologist Trust. 
520 |a We tested for isotope exchange between bound (immobile) and mobile soil water, and whether there is isotope fractionation during plant water uptake. These are critical assumptions to the formulation of the 'two water worlds' hypothesis based on isotope profiles of soil water. In two different soil types, soil-bound water in two sets of 19-l pots, each with a 2-yr-old avocado plant (Persea americana), were identically labeled with tap water. After which, one set received isotopically enriched water whereas the other set received tap water as the mobile phase water. After a dry down period, we analyzed plant stem water as a proxy for soil-bound water as well as total soil water by cryogenic distillation. Seventy-five to 95% of the bound water isotopically exchanged with the mobile water phase. In addition, plants discriminated against 18 O and 2 H during water uptake, and this discrimination is a function of the soil water loss and soil type. The present experiment shows that the assumptions for the 'two water worlds' hypothesis are not supported. We propose a novel explanation for the discrepancy between isotope ratios of the soil water profile and other water compartments in the hydrological cycle 
650 4 |a Journal Article 
650 4 |a bound water 
650 4 |a isotope fractionation 
650 4 |a mobile water 
650 4 |a plant water uptake 
650 4 |a stable isotopes 
650 4 |a two water worlds 
650 7 |a Oxygen Isotopes  |2 NLM 
650 7 |a Soil  |2 NLM 
650 7 |a Water  |2 NLM 
650 7 |a 059QF0KO0R  |2 NLM 
650 7 |a Deuterium  |2 NLM 
650 7 |a AR09D82C7G  |2 NLM 
700 1 |a Schaffer, Bruce  |e verfasserin  |4 aut 
700 1 |a Yuhong, Li  |e verfasserin  |4 aut 
700 1 |a Sternberg, Leonel da Silveira Lobo  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t The New phytologist  |d 1990  |g 215(2017), 2 vom: 15. Juli, Seite 582-594  |w (DE-627)NLM09818248X  |x 1469-8137  |7 nnns 
773 1 8 |g volume:215  |g year:2017  |g number:2  |g day:15  |g month:07  |g pages:582-594 
856 4 0 |u http://dx.doi.org/10.1111/nph.14616  |3 Volltext 
912 |a GBV_USEFLAG_A 
912 |a SYSFLAG_A 
912 |a GBV_NLM 
912 |a GBV_ILN_350 
951 |a AR 
952 |d 215  |j 2017  |e 2  |b 15  |c 07  |h 582-594