scholarly journals Dynamic response of herbaceous vegetation to gap opening in a Central European beech stand

Silva Fennica ◽  
2012 ◽  
Vol 46 (1) ◽  
Author(s):  
Kristóf Kelemen ◽  
Barbara Mihók ◽  
László Gálhidy ◽  
Tibor Standovár
Forests ◽  
2021 ◽  
Vol 12 (11) ◽  
pp. 1563
Author(s):  
Silvio Bagnato ◽  
Pasquale A. Marziliano ◽  
Maria Sidari ◽  
Carmelo Mallamaci ◽  
Federica Romeo ◽  
...  

The present study was focused on how cardinal directions inside gaps of different sizes (small, 200 m2; medium, 400 m2; and large, 600 m2) can affect soil characteristics and tree regeneration. Additionally, the effects of gap size on the growth dynamics of trees outside the gaps were evaluated. The study was carried out in a European beech stand located in Aspromonte National Park (Southern Apennines, Calabria, Italy). Microclimatic variables, physical, chemical, and biochemical soil properties, natural regeneration density, and growth trees outside the gaps density of natural regeneration were assessed. This study provided evidence for an important effect of cardinal points on micro-environmental parameter variability, nutrient cycle, physic-chemical soil properties, water availability, and biological processes such as trees growth and regeneration. The European beech natural regeneration was most abundant in the south part of the gaps. Thus, we can state that cardinal points affect the trees natural regeneration in a species-specific manner. The new microclimatic conditions due to the gap opening had positive effects on the tree growth located along the gap edge, especially in the trees sampled on the edges of the medium gaps. On the contrary, the trees located in the forest recorded a productivity coherent with the period prior the gap opening. In medium-sized gaps, the combination and interaction of microclimatic and soil parameters (humification and mineralization process and microbial activity) created the best conditions for beech natural regeneration and favored an increase in the productivity of the trees at the edge of the gaps.


2016 ◽  
Vol 403 (1-2) ◽  
pp. 343-360 ◽  
Author(s):  
Martin T. Schwarz ◽  
Sebastian Bischoff ◽  
Stefan Blaser ◽  
Steffen Boch ◽  
Fabrice Grassein ◽  
...  

2012 ◽  
Vol 60 (4) ◽  
pp. 319-332 ◽  
Author(s):  
Matus Hribik ◽  
Tomas Vida ◽  
Jaroslav Skvarenina ◽  
Jana Skvareninova ◽  
Lubomir Ivan

The paper evaluates the results of a 6-year-monitoring of the eco-hydrological influence of Norway spruce (Picea abies (L.) Karst.) and European beech (Fagus silvatica L.) forest stands on the hydro-physical properties of snow cover. The experiment was carried out in the artificially regenerated 20-25-year-old forest stands approaching the pole timber stage in the middle mountain region of the Polana Mts. - Biosphere reserve situated at about 600 m a.s.l. during the period of maximum snow supply in winters of years 2004 - -2009. Forest canopy plays a decisive role at both the snow cover duration and spring snow melting and runoff generation. A spruce stand is the poorest of snow at the beginning of winter. High interception of spruce canopy hampers the throughfall of snow to soil. During the same period, the soil surface of a beech stand accumulates greater amount of snow. However, a spruce stand accumulates snow by creating snow heaps during the periods of maximum snow cumulation and stand´s microclimate slows down snow melting. These processes are in detail discussed in the paper. The forest stands of the whole biosphere reserve slow down to a significant extent both the snow cover melting and the spring runoff of the whole watershed.


Plant Ecology ◽  
2020 ◽  
Vol 221 (10) ◽  
pp. 1005-1016
Author(s):  
Romana Prausová ◽  
Jan Doležal ◽  
Marcel Rejmánek

2012 ◽  
Vol 5 (5) ◽  
pp. 509-520 ◽  
Author(s):  
Tristan Cordier ◽  
Cécile Robin ◽  
Xavier Capdevielle ◽  
Marie-Laure Desprez-Loustau ◽  
Corinne Vacher

2005 ◽  
Vol 35 (11) ◽  
pp. 2756-2764 ◽  
Author(s):  
Werner Borken ◽  
Fritz Beese

Soil respiration was measured in adjacent pure and mixed stands of European beech (Fagus sylvatica L.) and Norway spruce (Picea abies (L.) Karst.) at Solling, Germany. Forest type had a significant effect on soil respiration, which was highest in the pure beech stand and lowest in the pure spruce stand. Both throughfall and soil temperature increased with the proportion of beech. Additionally, microbial respiration and biomass in the organic (O) horizons increased sequentially from the pure spruce to the pure beech stand, suggesting that abiotic and biotic factors enhanced the decomposition of litter under beech. Because the spruce litter decomposition rate was low, carbon (C) stocks of the O horizons increased with the proportion of spruce, from 1.6 to 5.1 kg C·m–2. The removal of the O horizons decreased soil respiration by 31%–45%, indicating a large contribution of the mineral soil and roots to total soil respiration. Turnover times of organic C in the O horizons ranged between 5.5 years in the pure beech stand and 20.6 years in the pure spruce stand. Our results suggest that tree species conversion may alter the turnover of soil organic matter, and thus the sequestration of organic C in the O horizons.


Plant Ecology ◽  
2006 ◽  
Vol 191 (1) ◽  
pp. 47-65 ◽  
Author(s):  
Goddert von Oheimb ◽  
Agnes Friedel ◽  
Annette Bertsch ◽  
Werner Härdtle

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