


No 1 (2025)
RESEARCH
Aftermath of Fires for Mesophytic Forests’ Soils in Western Caucasus
Abstract
Every year, vast areas of forests burn down during fires all over the world. The literature contains contradictory data on the effects of fires on individual components of ecosystems, in particular on soils. This necessitates the study of the aftermath of fires in different climatic and soil conditions. The aim of this work is studying the consequences of a ground fire on the properties of phaeozems of the Khamyshinsky district forestry unit of the Adygea Republic 4 years after the impact. The chemical (CEC, hydrolytic acidity, pH, organic carbon and active carbon content) and biological (activity of catalase, dehydrogenases, invertase, urease, phosphatase) properties of post-pyrogenic soils on one fully and two partially burnt areas have been studied. The ground fire did not cause significant changes in the composition of the forest stand for burnt areas No. 2 (1159 m above sea level) and No. 3 (1359 m above sea level), while the burnt area No. 1 (651 m above sea level) was characterised by completely charred trees, abundant growth of pontic rhododendron, and poorly developed herbaceous vegetation. A 51% decrease in catalase activity compared to the control was found in the three areas. The activity of dehydrogenases and urease in post-pyrogenic soils exceeded the control values by an average of 62%. The activity of invertase and phosphatase varied depending on the study area. In general, there was a tendency toward an increase in the activity of these enzymes. At the same time, a high spatial variation in the activity of soil dehydrogenases and invertase was found for burnt-out area No. 1. There also was an increase in hydrolytic acidity by an average of 43% compared to the control values. The CEC, the content of organic and active carbon differs to a lesser extent from the control values 4 years after the fire. The acidity index (pH) of the area devoid of grassy vegetation reaches 5.8, with control having pH of 4. Notably, higher values of the CEC correspond to higher pH values. Factor analysis showed that changes in the enzymatic activity of post-pyrogenic phaeozem are associated with the peculiarities of the soils’ chemical properties. The activity of hydrolases (urease, phosphatase) is closely related to the content of organic carbon, and the activity of other enzymes – to the CEC, hydrolytic acidity and pH. The content of active carbon changes insignificantly and does not affect the enzymatic activity.



Scots Pine Trees’ Sap Wood Density in Trans-Volga Forests of the Mari El Republic
Abstract
The relevance of the study is due to the need to improve the accuracy of assessing the quality of the Russia’s forests resource potential and the efficiency of its use. That can only be done via an in-depth study of the tree coenopopulations’ structure regarding their economically valuable traits, one of which is the basic density of wood. The purpose of the study is to assess the patterns of individual and group variability in the basic sapwood density of Scots pine trees in forest stands of different ages, origins, density and growing conditions located in the Mari El Republic, which will allow to select and subsequently reproduce the most economically promising individuals. The studies were conducted on 13 sample plots in pure, even-aged forest stands. To estimate the value of the basic density of sapwood, which was carried out by stereometric and hydrostatic methods, we used 50 mm long cores, manually extracted with a Pressler borer from 1072 trees at a height of 1.3 m from the base of the trunk. Standard methods of mathematical statistics were used in processing the empirical material. Results. It was found that the value of the estimated parameter varies in trees from 291 to 660 kg m–3, overlapping with the limits established by domestic researchers. It is virtually independent of growing conditions, density and origin of tree stands, rank position of individuals in coenopopulations, width of the annual wood growth and the proportion of the late summer layer in it, and is mainly linked to the age of the trees (R2 = 0.9). It has been proven that the ecological requirements for environmental conditions are different for trees with different wood density, which is reflected in the nature of their radial annual growth dynamics. A scale has been developed for assessing the economic value of trees in coenopopulations of different ages based on the density of their sapwood. Natural selection of trees based on wood density in coenopopulations that reaches its maximum at the age of 100–110 years does not occur, and thus targeted selection based on this parameter will not subsequently affect the productivity of plantations.



STRUCTURE OF LINDEN COENOSES ON THE NORTH-EASTERN BORDER OF THE BROADLEAVED-CONIFEROUS FORESTS AREA IN THE KIROV REGION
Abstract
On the territory of 8 planning quarters of the state natural reserve “Bushkovsky forest”, located on the north-eastern border of hemiboreal broadleaved-coniferous forests, a structural description of four groups of plantations was performed: linden with spruce and birch, spruce-birch-linden, elm-linden and birch-linden stands. The multi-species composition was made up of small-leaved linden, spruce, pine, fir, elm, Norway maple, ash, birch, aspen and grey alder. Linden was found to have a high ontogenesis polyvariance under conditions of low insolation and high humidity of the environment. The following life forms were described: single-trunk, coppice-forming, clump-forming, multi-trunk trees and facultative trailing shrub. The categories of tree vitality were defined and indices of forest stand condition were established. The average index value was found to be 0.9: individuals were described as “healthy”, although with values close to the lower limit. Most of the stands were two-storey with promising specimens of broadleaved species, such as maple and elm, gradually entering the first storey. Natural regrowth was assessed in different communities. The most resource-intensive in terms of development was the elm and maple undergrowth. The vitality index of the elm undergrowth never went lower than 91%; all individuals were sustainable and evenly distributed. In 71% of the coenoses, the undergrowth of this category had medium density values. Maple undergrowth was sustainable and healthy, with a vitality index surpassing 87%. It was evenly distributed in 62% of stands, 67% of coenoses had average density of its regrowth. Regarding spruce, the undergrowth was found to be weakened in 86% of cases, the minimal vitality index was 33%. Only in 10% of all stands has this species reached medium undergrowth density. The linden undergrowth was determined to be the most unreliable in terms of development: 71% of individuals had questionable vitality, while 29% were wilting. Only in 10% of the coenoses, linden trees grow in quantities slightly exceeding two thousand per hectare; in other cases, it was defined as scarce, numbering up to one and a half thousand. The data obtained can be used to analyse the dynamics of coenoses development and their transformations monitoring near the borders of their natural distribution area.



Disruptions of the autumnal aging of larch needles in the Krasnoyarsk city and its surroundings
Abstract
A disruption of the needle fall in Siberian larch was recorded during the autumn of 2016 in the Krasnoyarsk city, the Krasnoyarsk Pillars National Park, and, according to media reports, in other Siberian cities. To determine the causes of this phenomenon, the chlorophyll a content and the quantum yield of photosystem II (PS II) were assessed in Siberian larch trees of the Krasnoyarsk city under natural growing conditions (Mansky District, Krasnoyarsk Territory) during the autumn of 2016 and compared with the data obtained in the autumn of 2017. Data on air temperature and precipitation for September and October in Krasnoyarsk city, the Mansky District, and the Krasnoyarsk Pillars National Park over the entire course of observations were also analysed. Based on the analysis of the weather data, it can be assumed that the main cause of the needle fall disruptions were the abnormally warm average and average minimum air temperatures in September 2016 and the abnormally cold average and average minimum temperatures that followed them in October 2016.



ANALYSING THE TRANSFORMATION OF FOREST LITTER’S ORGANIC MATTER ON DIFFERENT STAGES OF SECONDARY SUCCESSION OF A MIDDLE TAIGA FOREST USING THE FOURIER-TRANSFORM INFRARED SPECTROMETRY
Abstract
Organic matter decomposition is a key process in the carbon cycle that controls the rate of carbon dioxide emission, carbon accumulation in the soil, and the availability of mineral elements for plants. Changes in the forest stand’s composition during secondary succession result in changes in the quality of litter, which affects the rate and depth of its transformation. We analysed how the chemical structure of the L-horizons of litter changes from October to August at different stages of secondary succession in typical forest ecosystems of Western Siberia’s middle taiga using IR spectrometry and elemental analysis. It turned out that the structure of organic matter in the L-horizons was transformed to the largest degree at intermediate stages of succession (in an aspen forest with a dark coniferous second storey), while at previous (monodominant aspen forests) and subsequent successional stages (mixed and dark coniferous forests), changes were less pronounced. These changes include a decrease in the proportion of relatively easily decomposable components (cellulose and carbohydrates) and accumulation of aromatic compounds and polyesters that are more recalcitrant to decomposition. Aspen forest with the dark coniferous second storey and dark coniferous forest turned out to be the objects with the highest difference in terms of changes in the litter’s elemental composition: the ratio of total carbon to nitrogen over the period from October to August increased the least in the former and the most in the latter. This combination of IR spectrometry and elemental analysis results can be explained by differences in the efficiencies of depolymerisation of nitrogen-containing compounds in litter. In general, the obtained results show that litter transformation during decomposition does not always depend only on its initial quality, even in closely located ecosystems where physical conditions are virtually identical. The functioning of the microbial community may be the cause of these differences in transformation at different stages of succession.



Ensuring sustainable water supply of forest plantations on intrazonal gleyic kastanozems of the northern Caspian Sea region
Abstract
Groundwater level, mineralisation and gradients were studied under different types of soils occupied by virgin field and forest vegetation to substantiate the possibility of creating sustainable forest stands. Summarised were the results of studying the characteristics of water cycle on saline haplic kastanozems and sodic solonetz soils, as well as on desalinated gleyic kastanozems. Vertical multidirectional moisture exchange with the underlying sandy horizon along local meso-depressions of the relief (depressions with meadow-chestnut soils) was demonstrated: descending during infiltration of thaw water and ascending as a result of an updraft by massive forest plantations. Explored has been the possibility of creating hydrologically neutral sustainable small groves and narrow shelter belts in the depressions, their water supply ensured by infiltrating thaw water, which has been historically irretrievably lost to groundwater outflow through the underlying sandy horizon.



Structure of the middle taiga Vaccinium spruce forest forty years after intensive selective logging in the fish spawning protection zone of Lake Onega
Abstract
The condition and structure of the stand formed over 40 years after high-intensity, even, gradual logging in the fish spawning protection zone of Lake Onega were studied. In the test plots laid out in 1982 before logging in a relatively uneven-aged mixed spruce forest of the vaccinium type of forest of III–IV quality class with a wood stock of about 220 m3 ha–1, the proportion of spruce was 40%, and the density of medium and large spruce undergrowth was about 1 thousand trees ha–1. As a result of logging, the reserve decreased by 50–70%, and the proportion of spruce in it was 60–65%. By 2023, stepped-closed mixed stands with a predominance of spruce and a total reserve of 250-300 m3 ha–1 were formed on the logging site. Half of the available stock is concentrated in the lower part of the canopy, under which there are more than 3 thousand trees ha-1 of spruce undergrowth. The spatial variability of density, stock, species composition of the stand and natural regeneration in the context of ensuring the sustainability of the stand is studied. Data on the dynamics of increment, large woody debris, age structure of the stand and undergrowth are analysed. The role of the technological network in the formation of heterogeneity of the stock, increment, species composition and undergrowth was clarified. The species composition and projective cover of the living ground cover as an indicator and factor of the dynamics of the stand are studied. Statistical relationships between the structural elements of the phytocoenosis are revealed, contributing to the understanding of its development and stability. The correspondence of the stand formed after felling to the main criteria for identifying biologically valuable forests is shown. Based on the results of the analysis of the obtained data and literary sources, a conclusion was made about the prospects of continuing selective management in the interests of further growth and sustainability of the spruce forest and the performance of its protective functions.



FOREST STANDS’ AND PEAT DEPOSITS STRUCTURE IN EUTROPHIC BOGS OF THE ZAPADNODVINSKY DISTRICT IN TVER REGION
Abstract
A comparative assessment of the silvicultural characteristics of tree stands, peat deposits and the dynamics of the virgin lowland eutrophic black alder bogs development has not been previously carried out, which determined the choice of the purpose of this study. In the forests of the Zapadnodvinsk district of the Tver region. Lowland rain-groundwater black alder bogs were selected for analysis, one of which has variable circulating water supply, while the other was stagnant. Studied within the framework of the study were the age, dynamic, and renewal characteristics, the condition of trees and forest stands, indicators of tree mortality, and the infestation of forest stands with wood-decaying fungi. A comparative assessment of the peats characteristics was carried out regarding the pH of the salt extract, the ash content, the bulk mass (density) and the carbon content in soil horizons. Eutrophic black alder swamps have a large presence of Norway spruce in different proportions and an insignificant presence of downy birch. When edaphic conditions change, this feature determines the possibility of changing the alder formation to the spruce one. Using the exponential approximation, high values of the relationship between the presence of spruce in age generations of age series were shown for the biogeocenosis with circulating water – R2 = 0.696. Under eutrophic growth conditions, downy birch can reach an age of 150 years. The soils of black alder forests are considered lowland peats, are high in ash content and composed of thick woody peats up to 2–4 m with a high degree of decomposition throughout the deposit (40–55%). The carbon content in peats with a fairly high ash content is different: 34–46 and 46–51% respectively in black alder forests with stagnant and flowing water. A comparative assessment of two black alder eutrophic bogs shows that Norway spruce occupies a subordinate position in relation to black alder. Under conditions of flow-through moisture, the productivity of black alder is 1-2 quality classes higher than that of European spruce. In more stagnant moisture conditions, Norway spruce actively replaces black alder both in the tree layer and in the undergrowth. In terms of the structure of age series, successional dynamics and tree mortality, indigenous eutrophic black alder bogs of different ages maintain the balance of biomass as climax stable forest communities.



The Content of Heavy Metals and Sulfur in Forest Ecosystemsin the Pechenganikel Smelter’s Zone of Impact Due to the Reductionof Atmospheric Emissions
Abstract
The relevance of the study is determined by the need to study the state of forest ecosystems in conditions of changing anthropogenic pressure and the practical significance of improving the monitoring system for sustainable forest management. The dynamics of the intake of pollutants with atmospheric precipitation, their accumulation in the soil and tree layer (using the example of an edificator species – Pinus sylvestris L.)with prolonged anthropogenic impact on forest ecosystems, as well as during the period of a sharp reduction in atmospheric emissions in the impact zone of the Pechenganikel smelter (Nickel village, Murmansk region). The studies were carried out in the period from 1991 to 2021 on the test areas of permanent monitoring plots located in pine forests at various distances from the source of atmospheric emissions (7, 14, 44 km). Between 1991 and 2020, the annual volume of industrial emissions of SO2, Ni and Cu into the atmosphere decreased. In December 2020, the release of pollutants into the atmosphere practically stopped due to the Pechenganikel metallurgical smelter being shut down. First of all, a sharp reduction in the emissions of pollutants into the atmosphere led to a change in the composition of snow and rainwater, the concentrations of pollutants (Ni, Cu, Co, Pb и Cd) in them approached regional background values. However, the concentrations of heavy metals and sulfur in the soil are still significantly higher than in typical forest ecosystems of the Murmansk region, due to the long period required for soil regeneration and self-purification.



Changes in physiological and biochemical parameters in the kidneys of Siberian larch during the change of phenological phases in the middle taiga of the Komi Republic
Abstract
The paper includes the results of physiological and biochemical studies of L. sibirica vegetative buds in the taiga zone of the Komi Republic (Russia). The change in the phenological state of L. sibirica during the dormancy period and the transition to vegetative period is accompanied by a significant alteration of metabolism. In the autumn-winter period, the buds of L. sibirica synthesise a large amount of cryoprotective compounds such as soluble sugars, soluble protein and free amino acids. During this period, the buds also contain a considerable quantity of unsaturated fatty acids (about 60% of the sum of all fatty acids), mainly linoleic and oleic fatty acids. The beginning of the sap flow period is marked by a gradual increase in content of sugars and soluble proteins which reach tmaximum values towards the end of April. The fatty acid composition of the buds changed significantly. The content of the unsaturated FAs decreased significantly and the one of the saturated FAs increased, indicating the activation of a fatty acid synthase, the final product of which is palmitic acid. The water content and the share of freezing water in buds decreases to 45% and 16%, respectively, in December. The low water content and the presence of a significant fraction of non-freezing water allows us to be certain about the development of quite sufficient cryo-resistance in larch bud tissues against low negative temperatures in the autumn-winter period. The biochemical changes in the buds adapting to low temperatures are primarily aimed at changing the state of water whereby its phase transitions become relatively safe.



Litter Production and Decomposition in Dry Forestsof East Nusa Tenggara, Indonesia
Abstract
This 12-month long study explores the litterfall production and decomposition at four different sites in tropical dry forests of East Nusa Tenggara, Indonesia. The total litterfall, leaf litter and branch litter production values were found to be significantly different (p < 0.05) at all sites. The production of total litterfall, leaf litter, and branch litter was greater in Binafun (2778.125 g∙m–2∙year–1 and 2453.125 g∙m–2∙yr–1) and Bonmuti (300.437 g∙m–2∙yr–1). The annual mean litterfall decomposition rate followed the order of Binafun < Letkole < Bonmuti < Oelbanu (p < 0.05), which positively correlated with the monthly mean precipitation, mean humidity, and mean temperature. The turnover rate calculation indicated that the forest floor was replaced every year with a turnover time of 1.083 years.


