scholarly journals Long-term effects of stem girdling on needle structure in Scots pine

2018 ◽  
Vol 11 (4) ◽  
pp. 476-481
Author(s):  
R Gebauer ◽  
R Plichta ◽  
J Foit ◽  
V Cermák ◽  
J Urban
1996 ◽  
Vol 86 (1-3) ◽  
pp. 27-37 ◽  
Author(s):  
Göran Örlander ◽  
Gustaf Egnell ◽  
Arne Albrektson

2011 ◽  
Vol 41 (2) ◽  
pp. 279-288 ◽  
Author(s):  
Eva Ring ◽  
Staffan Jacobson ◽  
Lars Högbom

Adding nitrogen to coniferous forests on mineral soils will increase stem-wood growth in most boreal forests. The addition of nitrogen affects soils and waters as well. This investigation was conducted to evaluate the long-term effects of nitrogen fertilization at different intensities on soil chemistry in nitrogen-limited ecosystems. The study was performed at three experimental sites that were originally established around 1980 in Scots pine ( Pinus sylvestris L.) stands. Fertilization regimes with applications ranging from conceivable commercial rates to very intensive rates (3× 150 kg N·ha–1 up to 12× 150 kg N·ha–1) had been applied. Samples were collected from the FH horizon at all sites and 0–20 cm in the mineral soil at two sites and analyzed for pH and major nutrients. The carbon to nitrogen ratio in the FH horizon decreased with increasing total nitrogen application, while the concentrations and contents of nitrogen and exchangeable magnesium and phosphorus increased. The concentration and contents of exchangeable potassium decreased in both the FH horizon and the mineral soil. In general, larger effects on soil chemistry were observed with increasing fertilization intensity.


2020 ◽  
Vol 40 (10) ◽  
pp. 1366-1380
Author(s):  
Galina Timofeeva ◽  
Kerstin Treydte ◽  
Harald Bugmann ◽  
Yann Salmon ◽  
Andreas Rigling ◽  
...  

Abstract In many regions, drought is suspected to be a cause of Scots pine decline and mortality, but the underlying physiological mechanisms remain unclear. Because of their relationship to ecohydrological processes, δ18O values in tree rings are potentially useful for deciphering long-term physiological responses and tree adaptation to increasing drought. We therefore analyzed both needle- and stem-level isotope fractionations in mature trees exposed to varying water supply. In a first experiment, we investigated seasonal δ18O variations in soil and needle water of Scots pine in a dry inner Alpine valley in Switzerland, comparing drought-stressed trees with trees that were irrigated for more than 10 years. In a second experiment, we analyzed twentieth-century δ18O variations in tree rings of the same forest, including a group of trees that had recently died. We observed less 18O enrichment in needle water of drought-stressed compared with irrigated trees. We applied different isotope fractionation models to explain these results, including the Péclet and the two-pool correction, which considers the ratio of unenriched xylem water in the needles to total needle water. Based on anatomical measurements, we found this ratio to be unchanged in drought-stressed needles, although they were shorter. The observed lower 18O enrichment in needles of stressed trees was therefore likely caused by increased effective path length for water movement within the leaf lamina. In the tree-ring study, we observed lower δ18O values in tree rings of dead trees compared with survivors during several decades prior to their death. These lower values in declining trees are consistent with the lower needle water 18O enrichment observed for drought-stressed compared with irrigated trees, suggesting that this needle-level signal is reflected in the tree rings, although changes in rooting depth could also play a role. Our study demonstrates that long-term effects of drought are reflected in the tree-ring δ18O values, which helps to provide a better understanding of past tree physiological changes of Scots pine.


2020 ◽  
Vol 26 (10) ◽  
pp. 5796-5815 ◽  
Author(s):  
Jörg Prietzel ◽  
Wolfgang Falk ◽  
Birgit Reger ◽  
Enno Uhl ◽  
Hans Pretzsch ◽  
...  

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