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Water regime and osmotic adjustment under warming conditions on wheat in the Yaqui Valley, Mexico

dc.contributor.authorArgentel Martínez, Leandris
dc.contributor.authorGaratuza Payán, Jaime
dc.contributor.authorYepez González, Enrico Arturo
dc.contributor.authorArredondo Moreno, José Tulio
dc.contributor.authorde los Santos Villalobos, Sergio
dc.date.accessioned2020-03-12T23:37:12Z
dc.date.available2020-03-12T23:37:12Z
dc.date.issued2019
dc.identifier.citationArgentel-Martínez L, Garatuza-Payan J, Yepez EA, Arredondo T, de los Santos-Villalobos S. 2019. Water regime and osmotic adjustment under warming conditions on wheat in the Yaqui Valley, Mexico. PeerJ 7:e7029 https://doi.org/10.7717/peerj.7029
dc.identifier.urihttp://hdl.handle.net/11627/5322
dc.description.abstract"An experiment was carried out to evaluate the effect of increased temperature on roots and leaf water and osmotic potential, osmotic adjustment (OA) and transpiration on Triticum durum L. (CIRNO C2008 variety) during growth (seedling growth), tillering and heading phenophases. Wheat was sown under field conditions at the Experimental Technology Transfer Center (CETT-910), as a representative wheat crop area from the Yaqui Valley, Sonora Mexico. Thermal radiators were placed at 1.20 m from the crop canopy. Treatments included warmed plots (2 °C) and ambient canopy temperature with five replicates. Temperature treatment was controlled using a (proportional, integrative, derivative) feedback control system on plots covering a circular area of r = 1.5 m. Results indicated a significant decrease in the osmotic potential of roots and leaves for the warmed plots. Water potential, under warming treatment, also experienced a significant reduction and a potential gradient was observed in both, roots and leaves, while the phenophases were delayed. Such results demonstrate that, under warmer conditions, plants increase water absorption for cooling. Hence, transpiration experienced a significant increase under warming in all phenophases that was related to the low root and leaf water potential. CIRNO C2008 also experienced OA in all phenophases with glycine betaine as the osmolyte with major contribution."
dc.publisherPeerJ, Inc
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectWater potential
dc.subjectOsmotic potential
dc.subjectTranspiration
dc.subjectClimate change
dc.subjectOsmolytes
dc.subject.classificationCIENCIAS TECNOLÓGICAS
dc.titleWater regime and osmotic adjustment under warming conditions on wheat in the Yaqui Valley, Mexico
dc.typearticle
dc.identifier.doihttps://doi.org/10.7717/peerj.7029
dc.rights.accessAcceso Abierto


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Attribution-NonCommercial-NoDerivatives 4.0 Internacional
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 Internacional