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The effect of the extreme summer drought and heatwave 2018 in Central Europe on wood properties of oaks at four sandy valley river sites (Quercus robur L.) and one south-exposed schist slope (Qu. petraea (Matt.) Liebl.) in the middle Rhine and lower Main valley were studied and compared to well-watered trees from a riparian stand. While properties of the 2018 tree rings mostly resembled those of the previous (wet) year, significant decreases in Δ13C, wood density and ring width occurred in 2019 at most drought-prone sites. In the sandy sites, ring widths correlated with previous-year precipitation from June to August over a 20-year period. In organs formed in 2018, in general, decreasing Δ13C values were obtained in the order leaves, twigs, wood and acorns, with the values from acorns often resembling those from 2019-year rings. The observed changes indicated an increased intrinsic water use efficiency and lack of starch reserve formation during the unprecedented hot and dry summer 2018. Qu. petraea revealed quite different values from Qu. robur (lower Δ13C, wider and denser year rings), but qualitatively showed the same reaction to the drought in 2018, except for an enhanced formation of tyloses in recent-year tree rings.
Young trees of deciduous Quercus robur and Q. petraea and evergreen Q. ilex were grown together in a competition lysimeter experiment to assess i) – whether the observed growth differences between evergreen Q. ilex and the deciduous Q. robur and Q. petraea on sandy soil in the field and ii) – whether the different natural distribution of Q. robur and Q. petraea could be attributed to physiological differences between the species under experimental drought stress (DS). Half of the plants were subjected to long-term DS in two consecutive years and monitored for physiological and growth parameters. In the first year, water withholding for more than three months did not lead to significant drought stress, probably because of a sufficient residual water volume in the lysimeter for the relatively small plants. However, in the second year, 2018, which was warmer, the bigger plants now competed for the residual water and clear drought stress symptoms developed for more than two months in all trees in the DS lysimeter basin. Growth was only moderately (and mostly not significantly) affected by the DS in the second year, except for a smaller total leaf area in DS Q. ilex as compared to DS Q. robur and Q. petraea and smaller root collar diameter in DS Q. ilex compared to DS Q. robur. Under DS, the deciduous species revealed significant decreases in ΔVIP, indicating a negative effect on electron transport through PS I. Pn, PIabs and water relations parameters (ΨPD and LWC) all decreased to various extents under DS in all three species, leading to clear separation of the deciduous from the evergreen species by PCA. However, PCA did not separate the two deciduous species from each other. It is concluded that longer root growth in the two deciduous species as compared to Q. ilex ameliorates DS effects in Q. robur and Q. petraea and may be the key to understand the better performance of deciduous oaks on sandy soil in the field.
Tree water relations of mature oaks in southwest Germany under extreme drought stress in summer 2018
(2021)
Mature oak stands of different tree height at four sandy valley river sites (Quercus robur) and one south-exposed schist slope (Qu. petraea) in the middle Rhine and lower Main valley were studied from early summer 2017 (normal wet year) until the end of 2018 (extremely hot and dry year). Tree water relations (ΨPD, RWC, sap flow rates) were monitored together with soil water relations, LAI and leaf chl content. In two sandy sites with presumed continuous capillary water access from the groundwater aquifer, sap flow rates of the large trees (30 m) and estimated canopy conductance decreased to about 50% of the maximum value in the course of summer 2018, but recovered in autumn. At two other sites, with smaller trees (14–24 m) and presumed interrupted capillary water access during mid-summer 2018, sap flow rates and canopy conductance broke down completely and trees shed a large proportion of leaves in summer. In one of these sites, ΨPD decreased (reversibly) to -4 MPa, one of the lowest values reported in the literature for central Europe, and tree damage resulted not only in extreme leaf shedding, but also in susceptibility to uprooting (in 2 out of 5 measured trees) by thunderstorm gusts in autumn 2018. At the schist slope site, where oaks reached the lowest height and stand density of all sites, sap flow rates remained similar to the values found at the presumed capillary-water supplied sandy sites, indicating access to rock fissure water even at the peak of the drought period. Our findings corroborate the prediction from vegetation modelling that several Qu. robur stands in the Rhine-Main valleys will be prone to severe forest dieback in the forthcoming decades.