期刊
FUNCTIONAL ECOLOGY
卷 34, 期 3, 页码 561-574出版社
WILEY
DOI: 10.1111/1365-2435.13508
关键词
diffuse-porous temperate trees; drought; hydraulic redistribution driving factors; hydraulic redistribution quantity; ring-porous temperate trees; split-root experiment; stable water isotope labelling (H-2; deuterium); temperate conifer trees
类别
资金
- Europamobel Umweltstiftung
- Hartig Stiftung
- German Federal Environmental Foundation
Hydraulic redistribution (HR) of soil water through plant roots is widely described; however its extent, especially in temperate trees, remains unclear. Here, we quantified HR of five temperate tree species. We hypothesized that both, HR within a plant and into the soil increase with higher water-potential gradients, larger root conduit diameters and root-xylem hydraulic conductivities as HR driving factors. Saplings of conifer (Picea abies, Pseudotsuga menziesii), diffuse-porous (Acer pseudoplatanus) and ring-porous species (Castanea sativa, Quercus robur) were planted in split-root systems, where one plant had its roots split between two pots with different water-potential gradients (0.23-4.20 MPa). We quantified HR via deuterium labelling. Species redistributed 0.39 +/- 0.14 ml of water overnight (0.08 +/- 0.01 ml/g root mass). Higher pre-dawn water-potential gradients, hydraulic conductivities and larger conduits significantly increased HR quantity. Hydraulic conductivity was the most important driving factor on HR amounts, within the plants (0.03 +/- 0.01 ml/g) and into the soil (0.06 +/- 0.01 ml/g). Additional factors as soil-root contact should be considered, especially when calculating water transfer into the soil. Nevertheless, trees maintaining high-xylem hydraulic conductivity showed higher HR amounts, potentially making them valuable 'silvicultural tools' to improve plant water status. A free Plain Language Summary can be found within the Supporting Information of this article.
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