In view of the prevailing preferences for health and recreation revealed by previous studies as the main expected benefits of forest visits, the research presented herein focuses on whether such expectations would translate into a significant increase in the number of forest visits (NFV) following pandemic outbreaks. In this context, a Slovak nationwide survey on forests was conducted, with the main objective of casting light on possible changes in NFV as a coping mechanism or behavioral response to the discomfort and severe restrictions stemming from coronavirus disease 2019 (COVID-19) and the related measures. The survey was administered on a statistically representative sample after the pandemic’s first wave ebbed and restrictions were eased in the summer months of 2020. Collected data were assessed using ANOVA, the results of which supported the importance of forests as places providing opportunities for restoration of mental and physical resources. Forest accessibility as represented by forest coverage and settlement size emerged as a paramount factor affecting NFV rates both before and during the COVID-19 pandemic. The pandemic and its accompanying measures affected the relationships between NFV and average per capita income, type of employment, and most importantly age, highlighting possible vulnerabilities and disadvantages in certain population segments.

Deadwood moisture affects multiple functions of downed logs in forest ecosystems. They include provision of habitats for xylobionts, additional water stores and organic carbon stocks. In contrast to Northern American forests, little is known about moisture variability in downed logs of important tree species within the Temperate Zone of Europe. Therefore, our study aimed at elucidating this variability according to species, site and decay class (DC). Measurements were taken by TDR during two vegetation periods in eight Carpathian natural forests representing distinct site conditions, ranging from xerothermophilous to subalpine. Downed logs of Quercus spp., Abies alba Mill., Fagus sylvatica L., and Picea abies L., belonging to various DCs, were selected and instrumented with TDR probes. Species and DC‐specific TDR calibration showed the importance of intrinsic wood porosity. The course of deadwood moisture consisted of drying during the early decay stage, except for A. alba and F. sylvatica, and an intense water reabsorption at later decay stages. Average moisture for all species and sites displayed seasonal trends, reflecting the occurrence of precipitation clusters and dry periods, as well as short‐term fluctuations. Cross‐spectral analysis revealed that both sapwood and heartwood participated in wetting and drying processes, but only after reaching an advanced stage of decay. New findings can be applied in interpreting, modelling and predicting deadwood water stores, habitat properties and respiration. Copyright © 2011 John Wiley & Sons, Ltd.

Little is known on soil organic carbon (SOC) stocks in karst areas worldwide, although many of them have seen long-term application of agroforestry systems with a potential for carbon sequestration. Therefore, our study aimed to assess landscape-level SOC concentration and stock in the Silica Plateau, a part of the Slovak Karst Biosphere Reserve located in the Western Carpathians (Slovakia) with a centuries-long agroforestry record. The most represented local soil units are Chromi-Rendzic Leptosols and Chromic Cambisols with clayey loam texture, C/N ratio 9-12, and pH H 2 O 6.6-6.2 in their organo-mineral surface horizons. Mull surface humus form prevails under mixed forest stands dominated by hornbeam (Carpinus betulus L.), oak (Quercus petraea L.), and beech (Fagus sylvatica L.). A total of 2,700 soil samples were collected from 150 soil pits. Both SOC concentrations and stocks were determined for the 0-60 cm mineral soil layer. Soil stoniness was accounted for by means of electrical resistivity tomography. According to the analysis of covariance, cropland SOC concentration (0.026 g g -1 ) is significantly lower compared to forestland (0.040 g g -1 ) and pastureland (0.041 g g -1 ) (P \ 0.01). During the period of 130 years after forest clearing, cropland SOC stock has been reduced at an exponential decay rate of ca 0.002 year -1 , while the SOC stock in pastureland has increased following land use change from cropland by approximately 30% during the same period of time. Irrespective of land use history, overall SOC stock is high reaching on average 207.4 Mg ha -1 , out of which 66% are stored within 0-30 cm and 34% within 30-60 cm soil layers.

There is a need for societal transformation towards bioeconomy, which promotes the replacement of non-renewable natural resources with renewable ones. Slovakia has considerable potential for bioeconomy development, yet this potential remains untapped. This article evaluates the public perception regarding the individual properties of renewable and non-renewable materials and their relation to the potential for bioeconomy development in Slovakia. It is found that Slovak consumers prefer natural renewable materials, regardless of other influencing factors, and realise the need for transformation towards a more sustainable economy.

Silvicultural opera ons increasingly aim to achieve desired water-related ecological services of forests and forest soils. Therefore, the eff ects of forest stand density, site, and soil depth on the water fl ow types were studied by conduc ng dye tracer experiments in two montane beech (Fagus sylva ca L.) forests located in the Western Carpathian Volcanic Range, Central Slovakia. Prevalent fl ow types were iden fi ed under usual weather condions. Brilliant Blue FCF dye tracer was periodically applied in powder form on 1-m 2 plots in forest stands with natural and reduced stand densi es, as well as in clear-cuts. When cumula ve precipita on reached approximately 100 mm, soil pits were excavated. The dye pa erns on the exposed profi les were photographed, and dye coverage, rela ve dye concentra on, and stain widths were determined at various soil depths using image analysis. These pa erns were used to discriminate two fl ow types. Con nuous ver cal dye plumes were interpreted as an indicator of surface-controlled fl ow type, which includes heterogeneous infi ltra on and macropore fl ow. The matrix-controlled fl ow type includes both homogeneous and heterogeneous matrix fl ow, as well as fi ngering. The log-linear analysis revealed that forest stand density and soil depth were signifi cantly related to the soil water fl ow type. Preferen al fl ow resulted from heterogeneous infi ltra on and fi ngering in the clear-cuts, from heterogeneous infi ltra on in the natural stands, and from macropore fl ow in the shelterwood stands. Dis nct humus forms and skeleton frac on played a crucial role for various fl ow pa erns observed in these beech stands.Abbrevia ons: LLA, log-linear analysis; MCF, matrix-controlled fl ow; SCF, surface-controlled fl ow. While matrix fl ow enhances various interactions between water and solutes withfi ne earth, preferential fl ow substantially reduces the contact time and area between the liquid and solid phases. Th us, both fl ow types have the potential to either promote or compromise various ecosystem services provided by forests, such as buff ering the alkaline dust imission load in soils (Pichler et al., 2006), waste water purifi cation (Kermen and