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Dušan Gömöry, Elena Foffová, Jaroslav Kmeť, Roman Longauer and Ivana Romšáková

Norway Spruce (Picea abies [L.] Karst.) Provenance Variation in Autumn Cold Hardiness: Adaptation or Acclimation?

We tested autumn frost hardiness in three Norway spruce (Picea abies [L.] Karst.) provenances originating from different altitudes at two trial plots in Slovakia (Vel'ký Lom at 450 m a.s.l., Mútne-Zákamenné at 1,250 m a.s.l.) in a spinoff experiment of the IUFRO 1964/68 Inventory Provenance Experiment with Norway spruce. Two approaches were used to assess hardiness: the electrolyte-leakage method based on artificial freezing, and measurements of chlorophyll a fluorescence parameters. The frost injury index at -20°C differed between provenances, with a significant provenance-by-plot interaction. In material from the lower-altitude Vel'ký Lom trial plot, the high-elevation TANAP provenance exhibited much lower frost injury than the middle-elevation Habovka and low-elevation Beňuš provenances. In material from the high-altitude Mútne-Zákamenné trial plot, all three tested provenances showed approximately the same degree of frost injury. At -80°C no differences between provenances were observed, and the trees growing at the high-elevation site exhibited lower average frost injury than the trees at Vel'ký Lom. Most parameters of the kinetics of chlorophyll a fluorescence followed the same trends as frost injury, and differed significantly between plots. We suggest that the observed differences resulted from acclimation of trees to the conditions of the trial plots rather than from adaptation through natural selection.

Open access

Tibor Priwitzer, Daniel Kurjak, Jaroslav Kmeť, Zuzana Sitková and Adriana Leštianska

Abstract

Physiological response of European beech under soil and atmospheric drought conditions was investigated in this study. A group of six beech trees was irrigated during the growing season 2012, while the second group of non-irrigated (control) beech trees was treated under natural soil drought. During the experiment, we observed more than 45-day long period when no precipitation fell on the soil surface. The relationship of PN (CO2 assimilation rate) to gS (stomatal conductance) was very tight in both groups, which indicates that stomatal opening was the main factor limiting PN. The statistically significant differences in gS between the groups of trees were revealed only on the last measuring day. The significant differences in PN were confirmed on the days when the differences in soil water potential (ΨS) appeared. On these measurement days, the PN values of irrigated individuals were approximately 1.9 or 3.3 times greater than the values of non-irrigated individuals. At the level of primary photosynthetic processes (chlorophyll fluorescence parameters) we did not observe lower values of the control individuals in comparison with the irrigated trees in any of the evaluated parameters. Long-term soil water deficit caused strong decrease of leaf water potential (ΨL) in the control trees, but ΨL values of the irrigated trees were also rather low due to diurnal dynamics in higher parts of crown. Close relationship between ΨL and gS was confirmed for the control (non-irrigated) trees, but could not be confirmed for the irrigated trees. We revealed significant influence of VPD (vapour pressure deficit of the air) on gS only in the control group. On the days when ΨS decreased, the stomata of the non-irrigated trees were closed in spite of the low VPD values. Almost complete stomatal closure in both groups of trees was caused by the increase of VPD to 1.2 kPa.